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Confini amministrativi dei comuni della Provincia di Venezia (geonode:ve_comuni)

No abstract provided

Tempo di residenza (WRT) della laguna di Venezia con le strutture fisse del mose (geonode:wrt_zoo)

Il tempo di residenza è stato calcolato sulla base della circolazione della laguna di Venezia, con le strutture fisse del mose, riprodotta da un modello idrodinamico (SHYFEM) applicato nella sua versione tridimensionale barotropica sottoposto a di forzanti di marea e vento reali. La mappa riporta il tempo di residenza calcolato su tutti i livelli, l'unità di misura è il giorno.

Clorofilla Golfo Manfredonia 2012 (geonode:clorofilla_tin_2012)

Valori di clorofilla del Golfo di Manfredonia ottenuti da interpolazione di valori di cmapionamento del 2012

Lesina - Acquiferi_Piano_Tutela_Acque_2009_data_digitized (geonode:lesina_acquiferi_piano_tutela_acque_2009)

The Gargano aquifer consists of large, deep carbonate aquifers (of Jurassic-Oligocene and mainly Mesozoic age), and the predominant rock material is either limestone or limestone-dolomite. The aquifer is punctuated by karst and fractured phenomena; well below sea level. As is often the case in coastal lagoons, seawater underlies fresh groundwater due to density differences, and a freshwater lens is found. Aquifers underlying the Gargano Promontory are artesian, and have a pressure head above sea level except on a restricted coastline strip. The maximum piezometric head is about 50 m asl (Polemio et al. 2010). Sinking of the carbonate platform is observed along the borders between Tavoliere and Gargano. Successive layers of Pleio-Pleistocene clays, marly clays, sandstones and sands make up the base of the promontory. Other two aquifer lie in the lagoon area but contrary to the Gargano aquifer, they consist of alluvial material and the westernmost aquifer is fed by the Fortore River. All the springs in the eastern area of the lagoon belongs to the karst aquifer circulation of the Gargano aquifer Oblong aquifers in a NE-SW orientation are predominantly reported in the sandy layers of this succession (Balduzzi et al. 1982). Groundwater flowing through these 'intermediate" aquifers is generally of artesian nature, and is subject to high pressure due to the confining action of the clay layers (Cotecchia and Magri 1996). This succession overlies a third deeper carbonate aquifer, which is a sunken carbonate platform. Data fromRegione Puglia 2007. Adozione, ai sensi dell’art.121 del D. Lgs. n.152/2006, del Progetto di Piano di Tutela delle Acque della Regione Puglia 2007 Regione Puglia (soc. Terna) 2009. Valutazione Ambientale del Piano di Sviluppo 2009 Rapporto Ambientale.

Livello piezometrico 2012, 2° acquifero (geonode:2_aq_2012_clip_idw_4_pseudomercator)

Valore interpolato della falda artesiana del secondo acquifero nell'anno 2012.

Uso_Suolo (wms_esterni:IMAGES_USO_SUOLO.ECW)

Livello piezometrico 1991, 2° acquifero (geonode:1991_aq2_idw4_clip_pseudomercator)

Valore interpolato della falda artesiana del secondo acquifero nell'anno 1991.

venice_wrt_spatialized_difference_merc (ismar:venice_wrt_spatialized_difference_merc)

No abstract provided

Lesina_Nutrienti_Marzo_1995_Data_digitized_from_SOGESID (geonode:nutrients_march_1995_data_sogesid)

Campagna di campionamento condotta nel marzo 1995 dalla SOGESID (Bari) per la Regione Puglia (Report: Sogesid 2002, Regione Puglia, Commissario delegato per l’emergenza ambientale, Presidente della Regione Puglia 2002. (Ordinanza del Ministro dell'Interno n° 3184 del 22/3/2002). Attivita’ connesse alla redazione del apiano di tutela delle acque (D. Lgs. 152/99 e successive modifiche ed integrazioni). Piano direttore a stralcio del piano di tutela della acque- Piano Generale). Parametri misurati: T (°C), Salinity (I), Dissolved Oxygen (ppm),pH, NH4 (µg/l), NO2(µg/l), NO3(µg/l);PO4(µg/l), Ptot(µg/l), Esaclorobenzene(µg/l), Lindano(µg/l), p p-DDT(µg/l), p p-DDE(µg/l), PCB 1260(µg/l), BHC(µg/l); Suspended solids (mg/l), solid sediment (ml/l), Tot COliform (MPN/100 ml), Fecal Cliform (MPN/100 ml), Tot Strept. (MPN/100 ml), fecal Strept. (MPN/100 ml), Chlorophyl A (µg/l]

Livello piezometrico 1991, 5° acquifero (geonode:1991_aq5_idw4_clip_pseudomercator)

Valore interpolato della falda artesiana del quinto acquifero nell'anno 1991.

Lesina_Indice_Biocenotico_Aprile1997_data_digitized_from_Piscitelli_et_al_2000 (geonode:lesina_indice_biocenotico_aprile1997_data_digitize)

Nella tabella .dbf: Number of repeated samples; Number of Species; Density ind/m2; Biomass g/m2; Dominanza ind; Dominanza biomass; Shannon Diversity Index individual (H); H min - H max; Pielou Index (J). Variazione spazio-temporale delle comunitá macrozoobentiche della Laguna di Lesina. Campionamenti In Aprile 1997 in 3 siti. Piscitelli et al. 2000. Macrobenthos of soft bottoms of the Lesina lagoon. Biol. Mar. Medit. (2000), 7(1): 723-727

Lesina-Trophic_Index_2009_data_digitized_from_Lugoli_et_al_2012 (geonode:lesina_trophic_index_2004)

Nella Tabella .dbf: Temperatura (T °C); Salinità (ppt); Oxygen saturation (%); DIN (µM); DIP (µM); Total Chl a (µg/l); Taxon (no.); Weight (pgC/cell); TRIX The lagoon of Lesina is classified into different categories depending on which trophic state indices are applied. These indices all describe conditions governed by the temporal and spatial variability of the system, and highlight distinctive properties of the areas near the freshwater inputs (Roselli et al. 2009). Lugoli et al. (2012) applied a new multimetric phytoplankton index, which integrates simple size spectra metrics, size class sensitivity to anthropogenic disturbance, phytoplankton biomass (Chl-a) and taxonomic richness thresholds. ISS-Phyto was originally developed for transitional waters but it can also be an adequate assessment tool of ecological status in coastal marine waters to describe within ecosystem disturbance gradients. The fact that it is mainly based on the phytoplankton size rather than taxonomic studies makes it an effective tool to assess the ecological status of transitional water. data from Lugoli F., Garmendiad M., Lehtinenb S., Kauppilab P., Monchevac S., Revillad M., Roselli L., Slabakovac N., Valenciad V., Dromphe K.M., Basset A. 2012. Application of a new multimetric phytoplankton index to the assessment of ecological status in marine and transitional waters. Ecological Indicators 23, 338–355.

Lesina - metalli campioni acque 2004_data_digitized_from_D_Adamo_et_al_2008 (geonode:metalli_acque_2004)

Campionamenti nella colonna d´acqua nel 2004. The Lesina lagoon is located on the southern Adriatic coast of Italy; many marine species, such as the shrimp M. kerathurus, use the Lesina lagoon as a nursery, spending their initial growth phase there. In order to assess the usefulness of migratory species as biomonitors of the environmental quality of this nursery area, we evaluated the metal content of the M. kerathurus juveniles at the end of their growth phase in the lagoon (October), when they are assumed to have bioaccumulated the maximum level of metals from the lagoon environment. The concentrations of Cr, Cd, Pb, Zn, Mn and Cu were measured in the muscle and exoskeleton of the shrimp, and in the sediments and waters of three areas of the Lesina Lagoon. Both the water and sediment levels of the investigated metals tended to fall within the ranges recorded for other lagoon environments characterized by similar anthropic impact and texturally similar sediment; the juveniles of the shrimp M. kerathurus proved to be strong bioaccumulators of heavy metals such as Zn and Cu (biota-sediment accumulation factors – BSAFs – 6.01 and 25.0 respectively), which derive from agricultural activities; therefore, at the end of their growing phase in the lagoon they can be considered useful biomonitors of metal contamination of agricultural origin in their nursery area. D´Adamo et al. 2008 DOI 10.1007/s10661-007-9944-3

Lesina_Indice_Biocenotico_Nov1997_dati_digitalizzati_da_Piscitelli_et_al_2000 (geonode:lesina_macrobenthos_nov1997_data_digitized_from_pi)

Nella tabella .dbf: Number of repeated samples; Number of Species; Density ind/m2; Biomass g/m2; Dominanza ind; Dominanza biomass; Shannon Diversity Index individual (H); H min - H max; Pielou Index (J). Variazione spazio-temporale delle comunitá macrozoobentiche della Laguna di Lesina. Campionamenti In Aprile 1997 in 3 siti. Piscitelli et al. 2000. Macrobenthos of soft bottoms of the Lesina lagoon. Biol. Mar. Medit. (2000), 7(1): 723-727

aisstat_track (geonode:aisstat_track)

No abstract provided

Lesina_Benthic_ciliates_MayJune2004_Data_digitized_from_Madoni2006 (geonode:lesina_benthic_ciliates_mayjune2004_data_digitized)

Sample collections were made during early May and the end of July 2004 at Lesina lagoon. During the investigation period, 63 ciliate taxa belonging to 41 genera were found: 38 were observed at Sacca di Goro stations, 33 were observed at Lesina stations, and 8 were common to the two lagoons. In the .dbf Table data refer to sediments collected in Spring and Summer: Porosity (ml/ml); Density (g/cm3); Redox (mV); Bacterial biomass (µgC/g); Chlorophyll a (µg/g) and Ciliates. Data digitized from Madoni 2006. Benthic ciliates in Adriatic Sea lagoons. European Journal of Protistology 42 (2006) 165–173

Lesina_Indice_Biocenotico_Aprile1997_data_digitized_from_Piscitelli_et_al_2000 (geonode:lesina_macrobenthos_february1997_data_digitized_fr)

Nella tabella .dbf: Number of repeated samples; Number of Species; Density ind/m2; Biomass g/m2; Dominanza ind; Dominanza biomass; Shannon Diversity Index individual (H); H min - H max; Pielou Index (J). Variazione spazio-temporale delle comunitá macrozoobentiche della Laguna di Lesina. Campionamenti In Aprile 1997 in 3 siti. Piscitelli et al. 2000. Macrobenthos of soft bottoms of the Lesina lagoon. Biol. Mar. Medit. (2000), 7(1): 723-727

puglia (wms_esterni:ECW_PUGLIA)

Lesina-Macrofitobenthos_2001_data_digitized_from_Marzano_et_al_2003 (geonode:macrophytobenthos_2001)

Nella Tabella .dbf: Macrophytobenthos; Bottom Type. The benthic community of the lagoon of Lesina was studied from July 2000 to June 2001. The distribution of the main macrophytobenthic species was recorded by visual census at 24 stations in July 2000. The macrofauna, from both hard and soft substrates, was analyzed at five stations with seasonal frequency; in addition, themain hydrologic parameters were recorded monthly. The lagoon was mainly characterized by brackish water, with salinity values decreasing from west to east (annual mean: 23.3 psu). It showed mild water temperatures throughout the year (annual mean: 19.8 °C) and moderately high values of dissolved oxygen (annual mean: 9.9 ppm). No dystrophic crises were observed during the period of study. In the eastern basin, Zostera noltii Hornemann, Lissara and Ruppia cirrhosa (Patagna) Grande were the most abundant species of macrophytobenthos. Their distributional pattern was coherent with literature data. Soft bottoms of the western basin were largely occupied by the benthopleustophytic alga Valonia aegagropila C. Agardh, which during the last decade had almost completely replaced Cladophora prolifera (Roth) Kützing and Gracilaria confervoides Greville, the latter of which was previously very abundant in the lagoon. Macrozoobenthos consisted of 53 species (1 sponge, 2 cnidarians, 11 molluscs, 14 annelids, 21 crustaceans, 1 insect, 1 bryozoan, 1 echinoderm, 1 tunicate), most of which are typical of brackish water. Highest abundances were found in the eastern area of the basin. Some marine species were recorded in the western area. In contrast with the dramatic changes observed in the floral assemblage, a large amount of species had already been recorded in the lagoon during the last 10 years, pointing out the persistence of the macrozoobenthic community. Nevertheless, the distribution of benthic macrofauna seemed to be greatly influenced by the presence of Valonia aegagropila, as shown in an ordination model, where station-points were segregated by the presence of the alga rather than by hydrologic parameters. The impact of biotic factors on the community, such as non-indigenous species invasions, was suggested as constraints inducing the temporal variations of benthos. Data digitized from Marzano et al. 2003. Distribution, persistence and change in the macrobenthos of the lagoon of Lesina (Apulia, southern Adriatic Sea). Oceanologica Acta 26 (2003) 57–66 DOI:10.1016/S0399-1784(02)01229-X

Siti Osservativi fissi nel Golfo di Manfredonia Test del Gargano (geonode:siti_osservativi_fissi_nel_golfo_di_manfredonia_te)

Meda Gargano e Antenne H/F in SSD Pesca

Lesina-Metals_Muscles_M_kerathurus_data_digitized_D_Adamo_et_al_2008 (geonode:lesina_metals_muscles_m_kerathurus_data_digitized__1)

In order to assess the usefulness of migratory species as biomonitors of the environmental quality of this nursery area, we evaluated the metal content of the M. kerathurus juveniles at the end of their growth phase in the lagoon (October), when they are assumed to have bioaccumulated the maximum level of metals from the lagoon environment. The concentrations of Cr, Cd, Pb, Zn, Mn and Cu were measured in the muscle and exoskeleton of the shrimp, and in the sediments and waters of three areas of the Lesina Lagoon. Concentrations of metals represent the mean value over the numer of samples at the same site.

falde_2012 (falde_2012)

Lesina_Indice_Biocenotico_Luglio1997_data_digitized_from_Piscitelli_et_al_2000 (geonode:lesina_macrobenthos_july1997_data_digitized_from_p)

Nella tabella .dbf: Number of repeated samples; Number of Species; Density ind/m2; Biomass g/m2; Dominanza ind; Dominanza biomass; Shannon Diversity Index individual (H); H min - H max; Pielou Index (J). Variazione spazio-temporale delle comunitá macrozoobentiche della Laguna di Lesina. Campionamenti In Aprile 1997 in 3 siti. Piscitelli et al. 2000. Macrobenthos of soft bottoms of the Lesina lagoon. Biol. Mar. Medit. (2000), 7(1): 723-727

GEOLOGIA_SUPERFICIALE (wms_esterni:GEOLOGIA_SUPERFICIALE)

GEOLOGIA_SUPERFICIALE

PugliaCoste_2010 (wms_esterni:IMAGES_PUGLIACOSTE_2010.ECW)

Polygonal watersheds (Lagoon of Venice) (geonode:polygonal_watersheds_lagoon_of_venice)

No abstract provided

Lesina-rischio_intrusione_salina_ dati_digitalizzati_da_Piano_Tutela_Acque (geonode:lesina_salt_water_intrusion)

Clean drinking water is provided to the settlements along the lagoon through pipes from the Occhito dam, which also supplies agriculture and small industries. However, a huge density of wells is recorded in the area but they are mostly used for agriculture, especially during drought periods. The presence of numerous karst springs has also contributed to the development of inland aquaculture farms, which utilize groundwater for their pools. Data from: Regione Puglia 2007. Adozione, ai sensi dell’art.121 del D. Lgs. n.152/2006, del Progetto di Piano di Tutela delle Acque della Regione Puglia 2007 Regione Puglia (soc. Terna) 2009. Valutazione Ambientale del Piano di Sviluppo 2009 Rapporto Ambientale.

Lesina_Canali_Data_Fidelibus_et_al_2011 (geonode:lesina_old_inlets_data_fidelibus_et_al_2011)

Nella Tabella .dbf: Nome del canale (Name); Fonte dati (Source). Canali che precedentemente collegavano la laguna di Lesina al mare ed ora interrati. Data da Fidelibus et al. 2011 (Human-induced hydrogeological changes and sinkholes in the coastal gypsum karst of Lesina Marina area) doi:10.1016/j.enggeo.2010.12.003

Marea modellata in Laguna di Venezia (shyfem:shyfem_shyfemoutput_raster)

Livello di marea all'interno della laguna di Venezia calcolato tramite il modello idrodinamico agli elementi finiti SHYFEM. La mappa viene aggiornata ogni trenta minuti, utilizzando le ultime osservazioni disponibili per forzare il modello.

Livello piezometrico 1991, 4° acquifero (geonode:1991_aq4_idw4_clip_pseudomercator)

Valore interpolato della falda artesiana del quarto acquifero nell'anno 1991.

Curve di Livello transetto Manfredonia (geonode:curve_di_livello_transetto_manfredonia)

Curve di livello ottenute dall'interpolazione della profondità relativa alle 12 stazioni del transetto per il campionamento di benthos e sedimenti.

tempi_residenza_senza_mose (ismar:tempi_residenza_senza_mose)

No abstract provided

Lesina_Campionamenti2008_2009_Data_digitized_from_Borja_et_al_2011 (geonode:lesina_samples2008_2009_data_digitized_from_borja_)

Caratteristiche chimico fisiche dei siti di campionamento. Le stazioni sono in ordine di distanza dalla sorgente di pressione antropica. NA – informazini non disponibili. TOC – Carbonio Organico Totale. In the .dbf Table: Depth (m); Distance to the pressure (km); Salinity; Redox potential (mV); Gravel (%); Sand (%); Mud (%); Organic content (%) Data digitized from A. Borja et al. 2011. Response of single benthic metrics and multi-metric methods to anthropogenic pressure gradients, in five distinct European coastal and transitional ecosystems. Marine Pollution Bulletin 62 (2011) 499–513

Livello piezometrico 1975, 4° acquifero (geonode:1975_aq4_pseudomercator)

Valore interpolato della falda artesiana del quarto acquifero nell'anno 1975.

Differenza batimetrie 1990-1970 (geonode:differenza_batimetrie_1990_1970)

Differenza delle carte batimetriche elaborate per gli anni 1990 e 1970

Tempo di residenza (WRT) della laguna di Venezia con le strutture fisse del mose (ismar:venice_wrt_spatialized_with_mose_merc)

Il tempo di residenza è stato calcolato sulla base della circolazione della laguna di Venezia, con le strutture fisse del mose, riprodotta da un modello idrodinamico (SHYFEM) applicato nella sua versione tridimensionale barotropica sottoposto a di forzanti di marea e vento reali. La mappa riporta il tempo di residenza calcolato su tutti i livelli, l'unità di misura è il giorno.

Rete Monitoraggio pozzi artesiani (geonode:retepozzi)

Identificazione e attributi dei pozzi appartenenti alla rete di monitoraggio della falda artesiana. La rete è stata istituita già nel 1970 al fine di poter seguire l’evoluzione delle pressioni di strato e, in caso di nuovi abbattimenti piezometrici, poter intervenire per tempo e prevenire nuovi conseguenti abbassamenti del suolo.

Superficie di Trasgressione (wms_esterni:Superficie di Trasgressione)

Superficie di Trasgressione

Differenza della pressione di falda del 5° acquifero 2012 1975 (geonode:5_aq_2012diff1975)

Differenza della pressione di falda interpolata con i valori misurati del 2012 e 1975 nel quinto acquifero.

Livello piezometrico 2012, 5° acquifero (geonode:5_aq_2012_clip_idw_4_pseudomercator)

Valore interpolato della falda artesiana del quinto acquifero nell'anno 2012.

aisstat_voyage (geonode:aisstat_voyage)

Lesina - Piezometria Cotecchia 1996_data_digitized (geonode:lesina_piezometria_cotecchia_1996)

The Gargano aquifer consists of large, deep carbonate aquifers (of Jurassic-Oligocene and mainly Mesozoic age), and the predominant rock material is either limestone or limestone-dolomite. The aquifer is punctuated by karst and fractured phenomena; well below sea level. As is often the case in coastal lagoons, seawater underlies fresh groundwater due to density differences, and a freshwater lens is found. Aquifers underlying the Gargano Promontory are artesian, and have a pressure head above sea level except on a restricted coastline strip. The maximum piezometric head is about 50 m asl (Polemio et al. 2010). Sinking of the carbonate platform is observed along the borders between Tavoliere and Gargano. Successive layers of Pleio-Pleistocene clays, marly clays, sandstones and sands make up the base of the promontory. Other two aquifer lie in the lagoon area but contrary to the Gargano aquifer, they consist of alluvial material and the westernmost aquifer is fed by the Fortore River. Oblong aquifers in a NE-SW orientation are predominantly reported in the sandy layers of this succession (Balduzzi et al. 1982). Groundwater flowing through these 'intermediate" aquifers is generally of artesian nature, and is subject to high pressure due to the confining action of the clay layers (Cotecchia and Magri 1996). This succession overlies a third deeper carbonate aquifer, which is a sunken carbonate platform. Data from Cotecchia V. and Magri G. 1966. Idrogeologia del Gargano. Geol. Appl. e Idrogeol. 1, pp. 1-80.

point_competenza_gr_pg (geonode:point_competenza_gr_pg)

Operational Lagoonal Units - Lagoon of Venice (geonode:operational_lagoonal_units_lagoon_of_venice)

No abstract provided

batimetrie Laguna-Ve 2002 (geonode:lag02_okart_export)

Batimetria della Laguna di Venezia. Anno 2002

Prova (geonode:prova)

No abstract provided

venice_wrt_spatialized_without_mose_merc (ismar:venice_wrt_spatialized_without_mose_merc)

Il tempo di residenza è stato calcolato sulla base della circolazione della laguna di Venezia riprodotta da un modello idrodinamico (SHYFEM) applicato nella sua versione tridimensionale barotropica sottoposto a di forzanti di marea e vento reali. La mappa riporta il tempo di residenza calcolato su tutti i livelli, l'unità di misura è il giorno. In questo caso il modello idrodinamico simula il tempo di residenza alla situazione antecedente la costruzione delle nuove strutture fisse del MOSE ed in particolare alle modifiche delle bocche di porto.

Lesina - Flooding risk_data_digitized_from_Piano_tutela_Acque (geonode:lesina_flooding_risk)

According to the Piano territioriale di Coordinamento Provinciale 2006 prepared by the Provincia di Foggia, the western part of the municipality of Lesina is included in an area that is at serious risk of flooding, because of the torrential regime of the river Fortore during exceptional precipitation events when the Occhito dam is not enough to contain the surplus of water. Therefore, the lagoon represents a natural detention basin and can be considered to provide a benefit by preventing flooding in the reclaimed areas situated below the sea level (preventive benefit or provisioning services). Data from: Regione Puglia 2007. Adozione, ai sensi dell’art.121 del D. Lgs. n.152/2006, del Progetto di Piano di Tutela delle Acque della Regione Puglia 2007 Regione Puglia (soc. Terna) 2009. Valutazione Ambientale del Piano di Sviluppo 2009 Rapporto Ambientale.

GEBCO_08 Grid (wms_esterni:GEBCO_08_Grid)

Lesina-metalli sedimenti_2004_data_digitized_from_D_Adamo_et_al_2008 (geonode:lesina_metalli_sedimenti_2004)

Nella Tabella .dbf: Cd (µg/g); Pb (µg/g); Cu (µg/g); Mn (µg/g); Zn (µg/g); Cr (µg/g); Name of the station sampled. The distribution of Cd (0.4–1.3 μg/g) and Mn (63–160 μg/g in the sediment was found to be relatively homogeneous across sampling sites and the main source of these metals could not be identified. Cr (0.4–31 μg/g) and Zn (2–23 μg/g) were mainly recorded near the mouths of the channels, while Pb (0.6–28 μg/g) and Cu (0.4–14 μg/g) were found mainly in the central area of the lagoon and near the points of entry of urban and agricultural runoff. Higher concentrations of metals are found in sediments compared to within the cell structure of Melicertus kerathurus. Concentrations of most metals have not changed markedly in the last decade (i.e., from the study of De Benedictis 1996 to the most recent), while Zn levels (255–1,155 μg/g) have considerably decreased. Metals in sediments are relatively conservative and therefore one can compare changes in time with more certainty than when looking at nutrient variation (D’Adamo 2008). Also in the more current study, metal content of the sediments proved to be lower than concentrations in water. And these values remain lower than or similar to those recorded by other authors for similar environments (Vazquez et al. 1999; Chou et al. 2004). Results of the investigations showed that the concentrations of all the investigated metals in the sampled sites of the Lesina lagoon were found to be independent of salinity. Data digitized from D’Adamo R., Di Stasio M., Fabbrocini A., Petitto F., Roselli L., Volpe M.G. 2008. Migratory crustaceans as biomonitors of metal pollution in their nursery areas. The Lesina lagoon (SE Italy) as a case study. Environ Monit Assess 143,15–24. doi10.1007/s10661-007-9944-3.

Campo di velocità in laguna di Venezia (geonode:velist_zoo)

La velocità istantanea è espressa in metri al secondo ed è stata calcolata in ogni punto della griglia all'interno della Laguna di Venezia e nella zona di mare antistante. Questi valori sono stati prodotti nel corso di uno studio modellistico della laguna utilizzando un modello di circolazione forzato con dati di livello e vento reali.