Christian-Albrechts-University Kiel, P…

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Web Service, OGC Web Map Service 1.3.0
Keywords
WFS, WMS, GEOSERVER, hydrological modelling, infoMapAccessService, CLIMB, EU-FP7
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no conditions apply
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copyright
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No INSPIRE Extended Capabilities (including service language support) given. See INSPIRE Technical Guidance - View Services for more information.
Data provider

Christian-Albrechts-University Kiel, Physical Geography - Landscape Ecology and Geoinformation Science (unverified)

Contact information:

Michael Blaschek

Christian-Albrechts-University Kiel, Physical Geography - Landscape Ecology and Geoinformation Science

Mailing and physical address:
Ludewig-Meyn-Str.14, 24106 Kiel, Germany

Email: 

Phone: +49 431/880-3486

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No INSPIRE Extended Capabilities (including service metadata) given. See INSPIRE Technical Guidance - View Services for more information.

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This Web Map Server presents output created within the EU-FP7 project CLIMB - Climate Induced Changes on the Hydrology of Mediterranean Basins (Ludwig et al. 2010, www.climb-fp7.eu).

Available map layers (3088)

Azienda San Michele - CAU/LMU weather station (geonode:azienda_cauclimatetower_vgn)

Location of the CAU/LMU weather station at the Azienda San Michele in southern Sardinia, Italy. The CAU/LMU weather station has been installed during an extended field campaign in early October 2010. Its deconstruction took place in late March 2013.

Azienda San Michele - CAU soil profiles 2011 (geonode:azienda_causoilprofiles11_vgn)

Location of four soil profiles at the Azienda San Michele in southern Sardinia, Italy. Exact positions were chosen according to main soil units from Angelo Aru (1966). Field protocol corresponding to KA5 (german). Lab-analyzed in Kiel.

Azienda San Michele - CAU soil profiles 2013 (geonode:azienda_causoilprofiles13_vgn)

Location of four soil profiles at the Azienda San Michele in southern Sardinia, Italy. Exact positions were chosen according to main soil units from Angelo Aru (1966). Field protocol corresponding to KA5 (german). Lab-analyzed in Kiel.

Azienda San Michele - Land use map with field boundaries 2011 (geonode:azienda_landuse11_vgn)

This layer represents the land use and field boundaries at the Azienda San Michele in southern Sardinia, Italy. The landuse classification is in English and does not follow a particular standard. Measuring the field boundaries has been done using a Trimble Juno SB Handheld.

Azienda San Michele - Land use map with field boundaries 2013 (geonode:azienda_landuse13_vgn)

This layer represents the land use and field boundaries at the Azienda San Michele in southern Sardinia, Italy. The landuse classification is in English and does not follow a particular standard. Measuring the field boundaries has been done using a Trimble Juno SB Handheld.

Azienda San Michele - Soil bulk density (geonode:azienda_soilbulkdensity10_vgn)

Soil bulk density sampled at 19 locations in October 2010 using soil sample rings with an inner volume of 100 cm³. Three undisturbed soil samples (soil surface layer, 30cm) per point has been analyzed in the lab facilities of the Azienda San Michele, AGRIS, and were averaged afterwards.

CHT_CSM_BTH_M01_WAS_ERC_BDM_250_DLR (geonode:cht_csm_bth_m01_was_erc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M01_WAS_ERE_BDM_250_DLR (geonode:cht_csm_bth_m01_was_ere_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M01_WAS_ERM_BDM_250_DLR (geonode:cht_csm_bth_m01_was_erm_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M01_WAS_HRC_BDM_250_DLR (geonode:cht_csm_bth_m01_was_hrc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month January. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M02_WAS_ERC_BDM_250_DLR (geonode:cht_csm_bth_m02_was_erc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M02_WAS_ERE_BDM_250_DLR (geonode:cht_csm_bth_m02_was_ere_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M02_WAS_ERM_BDM_250_DLR (geonode:cht_csm_bth_m02_was_erm_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M02_WAS_HRC_BDM_250_DLR (geonode:cht_csm_bth_m02_was_hrc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month February. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M03_WAS_ERC_BDM_250_DLR (geonode:cht_csm_bth_m03_was_erc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M03_WAS_ERE_BDM_250_DLR (geonode:cht_csm_bth_m03_was_ere_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M03_WAS_ERM_BDM_250_DLR (geonode:cht_csm_bth_m03_was_erm_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M03_WAS_HRC_BDM_250_DLR (geonode:cht_csm_bth_m03_was_hrc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month March. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M04_WAS_ERC_BDM_250_DLR (geonode:cht_csm_bth_m04_was_erc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M04_WAS_ERE_BDM_250_DLR (geonode:cht_csm_bth_m04_was_ere_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M04_WAS_ERM_BDM_250_DLR (geonode:cht_csm_bth_m04_was_erm_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M04_WAS_HRC_BDM_250_DLR (geonode:cht_csm_bth_m04_was_hrc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month April. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M05_WAS_ERC_BDM_250_DLR (geonode:cht_csm_bth_m05_was_erc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M05_WAS_ERE_BDM_250_DLR (geonode:cht_csm_bth_m05_was_ere_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M05_WAS_ERM_BDM_250_DLR (geonode:cht_csm_bth_m05_was_erm_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M05_WAS_HRC_BDM_250_DLR (geonode:cht_csm_bth_m05_was_hrc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month May. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M06_WAS_ERC_BDM_250_DLR (geonode:cht_csm_bth_m06_was_erc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M06_WAS_ERE_BDM_250_DLR (geonode:cht_csm_bth_m06_was_ere_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M06_WAS_ERM_BDM_250_DLR (geonode:cht_csm_bth_m06_was_erm_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M06_WAS_HRC_BDM_250_DLR (geonode:cht_csm_bth_m06_was_hrc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month June. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M07_WAS_ERC_BDM_250_DLR (geonode:cht_csm_bth_m07_was_erc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M07_WAS_ERE_BDM_250_DLR (geonode:cht_csm_bth_m07_was_ere_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M07_WAS_ERM_BDM_250_DLR (geonode:cht_csm_bth_m07_was_erm_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M07_WAS_HRC_BDM_250_DLR (geonode:cht_csm_bth_m07_was_hrc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month July. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M08_WAS_ERC_BDM_250_DLR (geonode:cht_csm_bth_m08_was_erc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M08_WAS_ERE_BDM_250_DLR (geonode:cht_csm_bth_m08_was_ere_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M08_WAS_ERM_BDM_250_DLR (geonode:cht_csm_bth_m08_was_erm_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M08_WAS_HRC_BDM_250_DLR (geonode:cht_csm_bth_m08_was_hrc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month August. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M09_WAS_ERC_BDM_250_DLR (geonode:cht_csm_bth_m09_was_erc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M09_WAS_ERE_BDM_250_DLR (geonode:cht_csm_bth_m09_was_ere_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M09_WAS_ERM_BDM_250_DLR (geonode:cht_csm_bth_m09_was_erm_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M09_WAS_HRC_BDM_250_DLR (geonode:cht_csm_bth_m09_was_hrc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month September. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M10_WAS_ERC_BDM_250_DLR (geonode:cht_csm_bth_m10_was_erc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M10_WAS_ERE_BDM_250_DLR (geonode:cht_csm_bth_m10_was_ere_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M10_WAS_ERM_BDM_250_DLR (geonode:cht_csm_bth_m10_was_erm_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M10_WAS_HRC_BDM_250_DLR (geonode:cht_csm_bth_m10_was_hrc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month October. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M11_WAS_ERC_BDM_250_DLR (geonode:cht_csm_bth_m11_was_erc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M11_WAS_ERE_BDM_250_DLR (geonode:cht_csm_bth_m11_was_ere_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M11_WAS_ERM_BDM_250_DLR (geonode:cht_csm_bth_m11_was_erm_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M11_WAS_HRC_BDM_250_DLR (geonode:cht_csm_bth_m11_was_hrc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month November. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M12_WAS_ERC_BDM_250_DLR (geonode:cht_csm_bth_m12_was_erc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M12_WAS_ERE_BDM_250_DLR (geonode:cht_csm_bth_m12_was_ere_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M12_WAS_ERM_BDM_250_DLR (geonode:cht_csm_bth_m12_was_erm_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_CSM_BTH_M12_WAS_HRC_BDM_250_DLR (geonode:cht_csm_bth_m12_was_hrc_bdm_250_dlr)

This layer displays the relative change in volumetric soil moisture within the Chiba test site for the future (2041-2070) and reference (1971-2000) period. It represents month December. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_BTH_M30_WAS_TND_BDM_250_DLR (geonode:cht_dit_bth_m30_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the drought index within the Chiba test site. It represents month NA. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_FUT_M30_SWA_ERC_BDM_50m_CERTE (geonode:cht_dit_fut_m30_swa_erc_bdm_50m_certe)

This layer displays the drought index within the Chiba test site for the future period: 2041-2070. The involved hydrological model was SWAT, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 50m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_FUT_M30_SWA_ERE_BDM_50m_CERTE (geonode:cht_dit_fut_m30_swa_ere_bdm_50m_certe)

This layer displays the drought index within the Chiba test site for the future period: 2041-2070. The involved hydrological model was SWAT, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 50m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_FUT_M30_SWA_ERM_BDM_50m_CERTE (geonode:cht_dit_fut_m30_swa_erm_bdm_50m_certe)

This layer displays the drought index within the Chiba test site for the future period: 2041-2070. The involved hydrological model was SWAT, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 50m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_FUT_M30_SWA_HRC_BDM_50m_CERTE (geonode:cht_dit_fut_m30_swa_hrc_bdm_50m_certe)

This layer displays the drought index within the Chiba test site for the future period: 2041-2070. The involved hydrological model was SWAT, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 50m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_FUT_M30_WAS_COV_BDM_250_DLR (geonode:cht_dit_fut_m30_was_cov_bdm_250_dlr)

This layer displays the coefficient of variation for the drought index within the Chiba test site. It represents the future period: 2041-2070. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_FUT_M30_WAS_ERC_BDM_250_DLR (geonode:cht_dit_fut_m30_was_erc_bdm_250_dlr)

This layer displays the drought index within the Chiba test site for the future period: 2041-2070. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_FUT_M30_WAS_ERE_BDM_250_DLR (geonode:cht_dit_fut_m30_was_ere_bdm_250_dlr)

This layer displays the drought index within the Chiba test site for the future period: 2041-2070. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_FUT_M30_WAS_ERM_BDM_250_DLR (geonode:cht_dit_fut_m30_was_erm_bdm_250_dlr)

This layer displays the drought index within the Chiba test site for the future period: 2041-2070. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_FUT_M30_WAS_HRC_BDM_250_DLR (geonode:cht_dit_fut_m30_was_hrc_bdm_250_dlr)

This layer displays the drought index within the Chiba test site for the future period: 2041-2070. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_REF_M30_SWA_ERC_BDM_50m_CERTE (geonode:cht_dit_ref_m30_swa_erc_bdm_50m_certe)

This layer displays the drought index within the Chiba test site for the reference period: 1971-2000. The involved hydrological model was SWAT, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 50m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_REF_M30_SWA_ERE_BDM_50m_CERTE (geonode:cht_dit_ref_m30_swa_ere_bdm_50m_certe)

This layer displays the drought index within the Chiba test site for the reference period: 1971-2000. The involved hydrological model was SWAT, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 50m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_REF_M30_SWA_ERM_BDM_50m_CERTE (geonode:cht_dit_ref_m30_swa_erm_bdm_50m_certe)

This layer displays the drought index within the Chiba test site for the reference period: 1971-2000. The involved hydrological model was SWAT, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 50m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_REF_M30_SWA_HRC_BDM_50m_CERTE (geonode:cht_dit_ref_m30_swa_hrc_bdm_50m_certe)

This layer displays the drought index within the Chiba test site for the reference period: 1971-2000. The involved hydrological model was SWAT, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 50m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_REF_M30_WAS_COV_BDM_250_DLR (geonode:cht_dit_ref_m30_was_cov_bdm_250_dlr)

This layer displays the coefficient of variation for the drought index within the Chiba test site. It represents the reference period: 1971-2000. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_REF_M30_WAS_ERC_BDM_250_DLR (geonode:cht_dit_ref_m30_was_erc_bdm_250_dlr)

This layer displays the drought index within the Chiba test site for the reference period: 1971-2000. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_REF_M30_WAS_ERE_BDM_250_DLR (geonode:cht_dit_ref_m30_was_ere_bdm_250_dlr)

This layer displays the drought index within the Chiba test site for the reference period: 1971-2000. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_REF_M30_WAS_ERM_BDM_250_DLR (geonode:cht_dit_ref_m30_was_erm_bdm_250_dlr)

This layer displays the drought index within the Chiba test site for the reference period: 1971-2000. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_DIT_REF_M30_WAS_HRC_BDM_250_DLR (geonode:cht_dit_ref_m30_was_hrc_bdm_250_dlr)

This layer displays the drought index within the Chiba test site for the reference period: 1971-2000. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_BTH_M01_WAS_TND_BDM_250_DLR (geonode:cht_eti_bth_m01_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the ratio of eta/etp within the Chiba test site. It represents month January. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_BTH_M02_WAS_TND_BDM_250_DLR (geonode:cht_eti_bth_m02_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the ratio of eta/etp within the Chiba test site. It represents month February. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_BTH_M03_WAS_TND_BDM_250_DLR (geonode:cht_eti_bth_m03_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the ratio of eta/etp within the Chiba test site. It represents month March. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_BTH_M04_WAS_TND_BDM_250_DLR (geonode:cht_eti_bth_m04_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the ratio of eta/etp within the Chiba test site. It represents month April. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_BTH_M05_WAS_TND_BDM_250_DLR (geonode:cht_eti_bth_m05_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the ratio of eta/etp within the Chiba test site. It represents month May. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_BTH_M06_WAS_TND_BDM_250_DLR (geonode:cht_eti_bth_m06_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the ratio of eta/etp within the Chiba test site. It represents month June. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_BTH_M07_WAS_TND_BDM_250_DLR (geonode:cht_eti_bth_m07_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the ratio of eta/etp within the Chiba test site. It represents month July. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_BTH_M08_WAS_TND_BDM_250_DLR (geonode:cht_eti_bth_m08_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the ratio of eta/etp within the Chiba test site. It represents month August. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_BTH_M09_WAS_TND_BDM_250_DLR (geonode:cht_eti_bth_m09_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the ratio of eta/etp within the Chiba test site. It represents month September. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_BTH_M10_WAS_TND_BDM_250_DLR (geonode:cht_eti_bth_m10_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the ratio of eta/etp within the Chiba test site. It represents month October. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_BTH_M11_WAS_TND_BDM_250_DLR (geonode:cht_eti_bth_m11_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the ratio of eta/etp within the Chiba test site. It represents month November. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_BTH_M12_WAS_TND_BDM_250_DLR (geonode:cht_eti_bth_m12_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the ratio of eta/etp within the Chiba test site. It represents month December. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M01_WAS_ERC_BDM_250_DLR (geonode:cht_eti_fut_m01_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M01_WAS_ERE_BDM_250_DLR (geonode:cht_eti_fut_m01_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M01_WAS_ERM_BDM_250_DLR (geonode:cht_eti_fut_m01_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M01_WAS_HRC_BDM_250_DLR (geonode:cht_eti_fut_m01_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month January. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M02_WAS_ERC_BDM_250_DLR (geonode:cht_eti_fut_m02_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M02_WAS_ERE_BDM_250_DLR (geonode:cht_eti_fut_m02_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M02_WAS_ERM_BDM_250_DLR (geonode:cht_eti_fut_m02_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M02_WAS_HRC_BDM_250_DLR (geonode:cht_eti_fut_m02_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month February. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M03_WAS_ERC_BDM_250_DLR (geonode:cht_eti_fut_m03_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M03_WAS_ERE_BDM_250_DLR (geonode:cht_eti_fut_m03_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M03_WAS_ERM_BDM_250_DLR (geonode:cht_eti_fut_m03_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M03_WAS_HRC_BDM_250_DLR (geonode:cht_eti_fut_m03_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month March. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M04_WAS_ERC_BDM_250_DLR (geonode:cht_eti_fut_m04_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M04_WAS_ERE_BDM_250_DLR (geonode:cht_eti_fut_m04_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M04_WAS_ERM_BDM_250_DLR (geonode:cht_eti_fut_m04_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M04_WAS_HRC_BDM_250_DLR (geonode:cht_eti_fut_m04_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month April. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M05_WAS_ERC_BDM_250_DLR (geonode:cht_eti_fut_m05_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M05_WAS_ERE_BDM_250_DLR (geonode:cht_eti_fut_m05_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M05_WAS_ERM_BDM_250_DLR (geonode:cht_eti_fut_m05_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M05_WAS_HRC_BDM_250_DLR (geonode:cht_eti_fut_m05_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month May. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M06_WAS_ERC_BDM_250_DLR (geonode:cht_eti_fut_m06_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M06_WAS_ERE_BDM_250_DLR (geonode:cht_eti_fut_m06_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M06_WAS_ERM_BDM_250_DLR (geonode:cht_eti_fut_m06_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M06_WAS_HRC_BDM_250_DLR (geonode:cht_eti_fut_m06_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month June. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M07_WAS_ERC_BDM_250_DLR (geonode:cht_eti_fut_m07_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M07_WAS_ERE_BDM_250_DLR (geonode:cht_eti_fut_m07_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M07_WAS_ERM_BDM_250_DLR (geonode:cht_eti_fut_m07_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M07_WAS_HRC_BDM_250_DLR (geonode:cht_eti_fut_m07_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month July. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M08_WAS_ERC_BDM_250_DLR (geonode:cht_eti_fut_m08_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M08_WAS_ERE_BDM_250_DLR (geonode:cht_eti_fut_m08_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M08_WAS_ERM_BDM_250_DLR (geonode:cht_eti_fut_m08_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M08_WAS_HRC_BDM_250_DLR (geonode:cht_eti_fut_m08_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month August. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M09_WAS_ERC_BDM_250_DLR (geonode:cht_eti_fut_m09_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M09_WAS_ERE_BDM_250_DLR (geonode:cht_eti_fut_m09_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M09_WAS_ERM_BDM_250_DLR (geonode:cht_eti_fut_m09_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M09_WAS_HRC_BDM_250_DLR (geonode:cht_eti_fut_m09_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month September. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M10_WAS_ERC_BDM_250_DLR (geonode:cht_eti_fut_m10_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M10_WAS_ERE_BDM_250_DLR (geonode:cht_eti_fut_m10_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M10_WAS_ERM_BDM_250_DLR (geonode:cht_eti_fut_m10_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M10_WAS_HRC_BDM_250_DLR (geonode:cht_eti_fut_m10_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month October. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M11_WAS_ERC_BDM_250_DLR (geonode:cht_eti_fut_m11_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M11_WAS_ERE_BDM_250_DLR (geonode:cht_eti_fut_m11_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M11_WAS_ERM_BDM_250_DLR (geonode:cht_eti_fut_m11_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M11_WAS_HRC_BDM_250_DLR (geonode:cht_eti_fut_m11_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month November. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M12_WAS_ERC_BDM_250_DLR (geonode:cht_eti_fut_m12_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M12_WAS_ERE_BDM_250_DLR (geonode:cht_eti_fut_m12_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M12_WAS_ERM_BDM_250_DLR (geonode:cht_eti_fut_m12_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_FUT_M12_WAS_HRC_BDM_250_DLR (geonode:cht_eti_fut_m12_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the future period: 2041-2070. It represents month December. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M01_WAS_ERC_BDM_250_DLR (geonode:cht_eti_ref_m01_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M01_WAS_ERE_BDM_250_DLR (geonode:cht_eti_ref_m01_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M01_WAS_ERM_BDM_250_DLR (geonode:cht_eti_ref_m01_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M01_WAS_HRC_BDM_250_DLR (geonode:cht_eti_ref_m01_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month January. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M02_WAS_ERC_BDM_250_DLR (geonode:cht_eti_ref_m02_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M02_WAS_ERE_BDM_250_DLR (geonode:cht_eti_ref_m02_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M02_WAS_ERM_BDM_250_DLR (geonode:cht_eti_ref_m02_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M02_WAS_HRC_BDM_250_DLR (geonode:cht_eti_ref_m02_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month February. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M03_WAS_ERC_BDM_250_DLR (geonode:cht_eti_ref_m03_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M03_WAS_ERE_BDM_250_DLR (geonode:cht_eti_ref_m03_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M03_WAS_ERM_BDM_250_DLR (geonode:cht_eti_ref_m03_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M03_WAS_HRC_BDM_250_DLR (geonode:cht_eti_ref_m03_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month March. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M04_WAS_ERC_BDM_250_DLR (geonode:cht_eti_ref_m04_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M04_WAS_ERE_BDM_250_DLR (geonode:cht_eti_ref_m04_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M04_WAS_ERM_BDM_250_DLR (geonode:cht_eti_ref_m04_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M04_WAS_HRC_BDM_250_DLR (geonode:cht_eti_ref_m04_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month April. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M05_WAS_ERC_BDM_250_DLR (geonode:cht_eti_ref_m05_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M05_WAS_ERE_BDM_250_DLR (geonode:cht_eti_ref_m05_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M05_WAS_ERM_BDM_250_DLR (geonode:cht_eti_ref_m05_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M05_WAS_HRC_BDM_250_DLR (geonode:cht_eti_ref_m05_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month May. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M06_WAS_ERC_BDM_250_DLR (geonode:cht_eti_ref_m06_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M06_WAS_ERE_BDM_250_DLR (geonode:cht_eti_ref_m06_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M06_WAS_ERM_BDM_250_DLR (geonode:cht_eti_ref_m06_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M06_WAS_HRC_BDM_250_DLR (geonode:cht_eti_ref_m06_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month June. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M07_WAS_ERC_BDM_250_DLR (geonode:cht_eti_ref_m07_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M07_WAS_ERE_BDM_250_DLR (geonode:cht_eti_ref_m07_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M07_WAS_ERM_BDM_250_DLR (geonode:cht_eti_ref_m07_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M07_WAS_HRC_BDM_250_DLR (geonode:cht_eti_ref_m07_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month July. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M08_WAS_ERC_BDM_250_DLR (geonode:cht_eti_ref_m08_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M08_WAS_ERE_BDM_250_DLR (geonode:cht_eti_ref_m08_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M08_WAS_ERM_BDM_250_DLR (geonode:cht_eti_ref_m08_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M08_WAS_HRC_BDM_250_DLR (geonode:cht_eti_ref_m08_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month August. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M09_WAS_ERC_BDM_250_DLR (geonode:cht_eti_ref_m09_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M09_WAS_ERE_BDM_250_DLR (geonode:cht_eti_ref_m09_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M09_WAS_ERM_BDM_250_DLR (geonode:cht_eti_ref_m09_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M09_WAS_HRC_BDM_250_DLR (geonode:cht_eti_ref_m09_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month September. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M10_WAS_ERC_BDM_250_DLR (geonode:cht_eti_ref_m10_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M10_WAS_ERE_BDM_250_DLR (geonode:cht_eti_ref_m10_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M10_WAS_ERM_BDM_250_DLR (geonode:cht_eti_ref_m10_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M10_WAS_HRC_BDM_250_DLR (geonode:cht_eti_ref_m10_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month October. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M11_WAS_ERC_BDM_250_DLR (geonode:cht_eti_ref_m11_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M11_WAS_ERE_BDM_250_DLR (geonode:cht_eti_ref_m11_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M11_WAS_ERM_BDM_250_DLR (geonode:cht_eti_ref_m11_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M11_WAS_HRC_BDM_250_DLR (geonode:cht_eti_ref_m11_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month November. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M12_WAS_ERC_BDM_250_DLR (geonode:cht_eti_ref_m12_was_erc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M12_WAS_ERE_BDM_250_DLR (geonode:cht_eti_ref_m12_was_ere_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M12_WAS_ERM_BDM_250_DLR (geonode:cht_eti_ref_m12_was_erm_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETI_REF_M12_WAS_HRC_BDM_250_DLR (geonode:cht_eti_ref_m12_was_hrc_bdm_250_dlr)

This layer displays the ratio of eta/etp within the Chiba test site for the reference period: 1971-2000. It represents month December. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_BTH_M01_WAS_TND_BDM_250_DLR (geonode:cht_etp_bth_m01_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the potential evapotranspiration within the Chiba test site. It represents month January. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_BTH_M02_WAS_TND_BDM_250_DLR (geonode:cht_etp_bth_m02_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the potential evapotranspiration within the Chiba test site. It represents month February. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_BTH_M03_WAS_TND_BDM_250_DLR (geonode:cht_etp_bth_m03_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the potential evapotranspiration within the Chiba test site. It represents month March. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_BTH_M04_WAS_TND_BDM_250_DLR (geonode:cht_etp_bth_m04_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the potential evapotranspiration within the Chiba test site. It represents month April. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_BTH_M05_WAS_TND_BDM_250_DLR (geonode:cht_etp_bth_m05_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the potential evapotranspiration within the Chiba test site. It represents month May. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_BTH_M06_WAS_TND_BDM_250_DLR (geonode:cht_etp_bth_m06_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the potential evapotranspiration within the Chiba test site. It represents month June. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_BTH_M07_WAS_TND_BDM_250_DLR (geonode:cht_etp_bth_m07_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the potential evapotranspiration within the Chiba test site. It represents month July. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_BTH_M08_WAS_TND_BDM_250_DLR (geonode:cht_etp_bth_m08_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the potential evapotranspiration within the Chiba test site. It represents month August. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

cht_etp_bth_m09_was_tnd_bdm_250_dlr (geonode:cht_etp_bth_m09_was_tnd_bdm_250_dlr)

No abstract provided

CHT_ETP_BTH_M10_WAS_TND_BDM_250_DLR (geonode:cht_etp_bth_m10_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the potential evapotranspiration within the Chiba test site. It represents month October. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_BTH_M11_WAS_TND_BDM_250_DLR (geonode:cht_etp_bth_m11_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the potential evapotranspiration within the Chiba test site. It represents month November. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_BTH_M12_WAS_TND_BDM_250_DLR (geonode:cht_etp_bth_m12_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the potential evapotranspiration within the Chiba test site. It represents month December. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M01_WAS_ERC_BDM_250_DLR (geonode:cht_etp_fut_m01_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M01_WAS_ERE_BDM_250_DLR (geonode:cht_etp_fut_m01_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M01_WAS_ERM_BDM_250_DLR (geonode:cht_etp_fut_m01_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M01_WAS_HRC_BDM_250_DLR (geonode:cht_etp_fut_m01_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month January. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M02_WAS_ERC_BDM_250_DLR (geonode:cht_etp_fut_m02_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M02_WAS_ERE_BDM_250_DLR (geonode:cht_etp_fut_m02_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M02_WAS_ERM_BDM_250_DLR (geonode:cht_etp_fut_m02_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M02_WAS_HRC_BDM_250_DLR (geonode:cht_etp_fut_m02_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month February. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M03_WAS_ERC_BDM_250_DLR (geonode:cht_etp_fut_m03_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M03_WAS_ERE_BDM_250_DLR (geonode:cht_etp_fut_m03_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M03_WAS_ERM_BDM_250_DLR (geonode:cht_etp_fut_m03_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M03_WAS_HRC_BDM_250_DLR (geonode:cht_etp_fut_m03_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month March. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M04_WAS_ERC_BDM_250_DLR (geonode:cht_etp_fut_m04_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M04_WAS_ERE_BDM_250_DLR (geonode:cht_etp_fut_m04_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M04_WAS_ERM_BDM_250_DLR (geonode:cht_etp_fut_m04_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M04_WAS_HRC_BDM_250_DLR (geonode:cht_etp_fut_m04_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month April. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M05_WAS_ERC_BDM_250_DLR (geonode:cht_etp_fut_m05_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M05_WAS_ERE_BDM_250_DLR (geonode:cht_etp_fut_m05_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M05_WAS_ERM_BDM_250_DLR (geonode:cht_etp_fut_m05_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M05_WAS_HRC_BDM_250_DLR (geonode:cht_etp_fut_m05_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month May. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M06_WAS_ERC_BDM_250_DLR (geonode:cht_etp_fut_m06_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M06_WAS_ERE_BDM_250_DLR (geonode:cht_etp_fut_m06_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M06_WAS_ERM_BDM_250_DLR (geonode:cht_etp_fut_m06_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M06_WAS_HRC_BDM_250_DLR (geonode:cht_etp_fut_m06_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month June. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M07_WAS_ERC_BDM_250_DLR (geonode:cht_etp_fut_m07_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M07_WAS_ERE_BDM_250_DLR (geonode:cht_etp_fut_m07_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M07_WAS_ERM_BDM_250_DLR (geonode:cht_etp_fut_m07_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M07_WAS_HRC_BDM_250_DLR (geonode:cht_etp_fut_m07_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month July. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M08_WAS_ERC_BDM_250_DLR (geonode:cht_etp_fut_m08_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M08_WAS_ERE_BDM_250_DLR (geonode:cht_etp_fut_m08_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M08_WAS_ERM_BDM_250_DLR (geonode:cht_etp_fut_m08_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M08_WAS_HRC_BDM_250_DLR (geonode:cht_etp_fut_m08_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month August. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M09_WAS_ERC_BDM_250_DLR (geonode:cht_etp_fut_m09_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M09_WAS_ERE_BDM_250_DLR (geonode:cht_etp_fut_m09_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M09_WAS_ERM_BDM_250_DLR (geonode:cht_etp_fut_m09_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M09_WAS_HRC_BDM_250_DLR (geonode:cht_etp_fut_m09_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month September. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M10_WAS_ERC_BDM_250_DLR (geonode:cht_etp_fut_m10_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M10_WAS_ERE_BDM_250_DLR (geonode:cht_etp_fut_m10_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M10_WAS_ERM_BDM_250_DLR (geonode:cht_etp_fut_m10_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M10_WAS_HRC_BDM_250_DLR (geonode:cht_etp_fut_m10_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month October. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M11_WAS_ERC_BDM_250_DLR (geonode:cht_etp_fut_m11_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M11_WAS_ERE_BDM_250_DLR (geonode:cht_etp_fut_m11_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M11_WAS_ERM_BDM_250_DLR (geonode:cht_etp_fut_m11_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M11_WAS_HRC_BDM_250_DLR (geonode:cht_etp_fut_m11_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month November. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M12_WAS_ERC_BDM_250_DLR (geonode:cht_etp_fut_m12_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M12_WAS_ERE_BDM_250_DLR (geonode:cht_etp_fut_m12_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M12_WAS_ERM_BDM_250_DLR (geonode:cht_etp_fut_m12_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_FUT_M12_WAS_HRC_BDM_250_DLR (geonode:cht_etp_fut_m12_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month December. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M01_WAS_ERC_BDM_250_DLR (geonode:cht_etp_ref_m01_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M01_WAS_ERE_BDM_250_DLR (geonode:cht_etp_ref_m01_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M01_WAS_ERM_BDM_250_DLR (geonode:cht_etp_ref_m01_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M01_WAS_HRC_BDM_250_DLR (geonode:cht_etp_ref_m01_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month January. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M02_WAS_ERC_BDM_250_DLR (geonode:cht_etp_ref_m02_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M02_WAS_ERE_BDM_250_DLR (geonode:cht_etp_ref_m02_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M02_WAS_ERM_BDM_250_DLR (geonode:cht_etp_ref_m02_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M02_WAS_HRC_BDM_250_DLR (geonode:cht_etp_ref_m02_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month February. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M03_WAS_ERC_BDM_250_DLR (geonode:cht_etp_ref_m03_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M03_WAS_ERE_BDM_250_DLR (geonode:cht_etp_ref_m03_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M03_WAS_ERM_BDM_250_DLR (geonode:cht_etp_ref_m03_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M03_WAS_HRC_BDM_250_DLR (geonode:cht_etp_ref_m03_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month March. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M04_WAS_ERC_BDM_250_DLR (geonode:cht_etp_ref_m04_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M04_WAS_ERE_BDM_250_DLR (geonode:cht_etp_ref_m04_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M04_WAS_ERM_BDM_250_DLR (geonode:cht_etp_ref_m04_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month April. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M04_WAS_HRC_BDM_250_DLR (geonode:cht_etp_ref_m04_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month April. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M05_WAS_ERC_BDM_250_DLR (geonode:cht_etp_ref_m05_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M05_WAS_ERE_BDM_250_DLR (geonode:cht_etp_ref_m05_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M05_WAS_ERM_BDM_250_DLR (geonode:cht_etp_ref_m05_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month May. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M05_WAS_HRC_BDM_250_DLR (geonode:cht_etp_ref_m05_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month May. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M06_WAS_ERC_BDM_250_DLR (geonode:cht_etp_ref_m06_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M06_WAS_ERE_BDM_250_DLR (geonode:cht_etp_ref_m06_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M06_WAS_ERM_BDM_250_DLR (geonode:cht_etp_ref_m06_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month June. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M06_WAS_HRC_BDM_250_DLR (geonode:cht_etp_ref_m06_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month June. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M07_WAS_ERC_BDM_250_DLR (geonode:cht_etp_ref_m07_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M07_WAS_ERE_BDM_250_DLR (geonode:cht_etp_ref_m07_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M07_WAS_ERM_BDM_250_DLR (geonode:cht_etp_ref_m07_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month July. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M07_WAS_HRC_BDM_250_DLR (geonode:cht_etp_ref_m07_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month July. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M08_WAS_ERC_BDM_250_DLR (geonode:cht_etp_ref_m08_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M08_WAS_ERE_BDM_250_DLR (geonode:cht_etp_ref_m08_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M08_WAS_ERM_BDM_250_DLR (geonode:cht_etp_ref_m08_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month August. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M08_WAS_HRC_BDM_250_DLR (geonode:cht_etp_ref_m08_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month August. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M09_WAS_ERC_BDM_250_DLR (geonode:cht_etp_ref_m09_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M09_WAS_ERE_BDM_250_DLR (geonode:cht_etp_ref_m09_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M09_WAS_ERM_BDM_250_DLR (geonode:cht_etp_ref_m09_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month September. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M09_WAS_HRC_BDM_250_DLR (geonode:cht_etp_ref_m09_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month September. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M10_WAS_ERC_BDM_250_DLR (geonode:cht_etp_ref_m10_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M10_WAS_ERE_BDM_250_DLR (geonode:cht_etp_ref_m10_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M10_WAS_ERM_BDM_250_DLR (geonode:cht_etp_ref_m10_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month October. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M10_WAS_HRC_BDM_250_DLR (geonode:cht_etp_ref_m10_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month October. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M11_WAS_ERC_BDM_250_DLR (geonode:cht_etp_ref_m11_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M11_WAS_ERE_BDM_250_DLR (geonode:cht_etp_ref_m11_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M11_WAS_ERM_BDM_250_DLR (geonode:cht_etp_ref_m11_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month November. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M11_WAS_HRC_BDM_250_DLR (geonode:cht_etp_ref_m11_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month November. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M12_WAS_ERC_BDM_250_DLR (geonode:cht_etp_ref_m12_was_erc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M12_WAS_ERE_BDM_250_DLR (geonode:cht_etp_ref_m12_was_ere_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M12_WAS_ERM_BDM_250_DLR (geonode:cht_etp_ref_m12_was_erm_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month December. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETP_REF_M12_WAS_HRC_BDM_250_DLR (geonode:cht_etp_ref_m12_was_hrc_bdm_250_dlr)

This layer displays the potential evapotranspiration within the Chiba test site for the reference period: 1971-2000. It represents the longterm monthly sum in mm for month December. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_BTH_M01_WAS_TND_BDM_250_DLR (geonode:cht_etr_bth_m01_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the real evapotranspiration within the Chiba test site. It represents month January. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_BTH_M02_WAS_TND_BDM_250_DLR (geonode:cht_etr_bth_m02_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the real evapotranspiration within the Chiba test site. It represents month February. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_BTH_M03_WAS_TND_BDM_250_DLR (geonode:cht_etr_bth_m03_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the real evapotranspiration within the Chiba test site. It represents month March. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_BTH_M04_WAS_TND_BDM_250_DLR (geonode:cht_etr_bth_m04_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the real evapotranspiration within the Chiba test site. It represents month April. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_BTH_M05_WAS_TND_BDM_250_DLR (geonode:cht_etr_bth_m05_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the real evapotranspiration within the Chiba test site. It represents month May. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_BTH_M06_WAS_TND_BDM_250_DLR (geonode:cht_etr_bth_m06_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the real evapotranspiration within the Chiba test site. It represents month June. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_BTH_M07_WAS_TND_BDM_250_DLR (geonode:cht_etr_bth_m07_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the real evapotranspiration within the Chiba test site. It represents month July. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_BTH_M08_WAS_TND_BDM_250_DLR (geonode:cht_etr_bth_m08_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the real evapotranspiration within the Chiba test site. It represents month August. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_BTH_M09_WAS_TND_BDM_250_DLR (geonode:cht_etr_bth_m09_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the real evapotranspiration within the Chiba test site. It represents month September. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_BTH_M10_WAS_TND_BDM_250_DLR (geonode:cht_etr_bth_m10_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the real evapotranspiration within the Chiba test site. It represents month October. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_BTH_M11_WAS_TND_BDM_250_DLR (geonode:cht_etr_bth_m11_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the real evapotranspiration within the Chiba test site. It represents month November. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_BTH_M12_WAS_TND_BDM_250_DLR (geonode:cht_etr_bth_m12_was_tnd_bdm_250_dlr)

This layer displays spatially distributed the congruence in the direction of climate induced change between the future (2041-2070) and reference (1971-2000) period for the real evapotranspiration within the Chiba test site. It represents month December. The involved hydrological model was WaSiM. The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_FUT_M01_WAS_ERC_BDM_250_DLR (geonode:cht_etr_fut_m01_was_erc_bdm_250_dlr)

This layer displays the real evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_FUT_M01_WAS_ERE_BDM_250_DLR (geonode:cht_etr_fut_m01_was_ere_bdm_250_dlr)

This layer displays the real evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_FUT_M01_WAS_ERM_BDM_250_DLR (geonode:cht_etr_fut_m01_was_erm_bdm_250_dlr)

This layer displays the real evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month January. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_FUT_M01_WAS_HRC_BDM_250_DLR (geonode:cht_etr_fut_m01_was_hrc_bdm_250_dlr)

This layer displays the real evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month January. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_FUT_M02_WAS_ERC_BDM_250_DLR (geonode:cht_etr_fut_m02_was_erc_bdm_250_dlr)

This layer displays the real evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_FUT_M02_WAS_ERE_BDM_250_DLR (geonode:cht_etr_fut_m02_was_ere_bdm_250_dlr)

This layer displays the real evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_FUT_M02_WAS_ERM_BDM_250_DLR (geonode:cht_etr_fut_m02_was_erm_bdm_250_dlr)

This layer displays the real evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month February. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_FUT_M02_WAS_HRC_BDM_250_DLR (geonode:cht_etr_fut_m02_was_hrc_bdm_250_dlr)

This layer displays the real evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month February. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_FUT_M03_WAS_ERC_BDM_250_DLR (geonode:cht_etr_fut_m03_was_erc_bdm_250_dlr)

This layer displays the real evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_FUT_M03_WAS_ERE_BDM_250_DLR (geonode:cht_etr_fut_m03_was_ere_bdm_250_dlr)

This layer displays the real evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 REMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_FUT_M03_WAS_ERM_BDM_250_DLR (geonode:cht_etr_fut_m03_was_erm_bdm_250_dlr)

This layer displays the real evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month March. The involved hydrological model was WaSiM, the considered climate model was ECHAM-5 RACMO, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.

CHT_ETR_FUT_M03_WAS_HRC_BDM_250_DLR (geonode:cht_etr_fut_m03_was_hrc_bdm_250_dlr)

This layer displays the real evapotranspiration within the Chiba test site for the future period: 2041-2070. It represents the longterm monthly sum in mm for month March. The involved hydrological model was WaSiM, the considered climate model was HadCM3 RCA, applied in the form: bias corrected and downscaled using multifractal cascades method (1km). The cell size of the target grid is 250m. The presented layer covers the total study site Chiba, Tunisia. Its visualization is based on subcatchment level.