NOAA Office for Coastal Management

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Web Service, OGC Web Map Service 1.3.0
Keywords
Oceans, Marine, National, renewable energy, offshore, renewables, energy, artificial, reefs, radar, pinniped, haul out, rookeries, bathymetry, contours, bathymetric, sediment thickness, groundfish, EFH, gray whale migration, seafloor geology
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Data provider

NOAA Office for Coastal Management (unverified)

Contact information:

MarineCadastre.gov Data Steward

NOAA Office for Coastal Management

Physical and mailing:
2234 South Hobson Ave, 29405 Charleston, USA

Email: 

Phone: (843) 740-1202

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

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MarineCadastre.gov themed service for public consumption featuring layers from the Physical and Oceanographic and Marine Habitat bins featured in the National Viewer.

Available map layers (15)

Weather Radar Impact Zones (0)

These data represent an inventory of the national impacts of wind turbine interference with NEXRAD radar stations. This inventory was developed by the NOAA Radar Operations Center (ROC) to establish variable zones that delineate the possible impacts that wind turbines may have on radar operations. The inventory scheme includes four zones that take in to account terrain, distance, and the number of elevation angles impacted. ROC requests various degrees of consultation with the developer depending on the zone. No Build - No wind turbines permitted. Mitigation Zone - Significant impacts likely. Consultation Zone - Significant impacts possible. Notification Zone - Impacts not likely.

National Seafloor Geology (GLORIA) (1)

In 1984, the U.S. Geological Survey (USGS) began a program to map deep water portions of the Exclusive Economic Zone (EEZ) by selecting the long-range side scan sonar system GLORIA (Geological Long-Range Inclined ASDIC). The USGS selected side-scan sonar as the mapping tool because it could be used to obtain information on geologic processes. The intensity of back-scattered sound from the seafloor is a function of the gradient or slope of the seafloor, surface roughness, and sediment characteristics such as texture. The darkness or brightness of a feature or an area on the sonographs and completed mosaics is therefore a function of how much sound is reflected from the seafloor. The recorded digital data are processed and used to construct digital maps of the seafloor.

Pacific Groundfish EFH Areas with Fishing Restrictions (2)

This layer depicts Essential Fish Habitat (EFH) Areas with fishing restriction to protect Pacific Coast groundfish habitat. There are different gear restrictions within these areas, please use the identify tool to see the gear types associated with an individual closure. See NOAA Fisheries Service Final Rule, 71 FR 27408, for complete description of closed areas. More information can also be found within the source info link.

Gray Whale Migration (California, Graphical Representation Only, Not Official) (3)

Approximated area in which gray whale migration may occur. Not for official use.

Critical Habitat Designations (4)

The Endangered Species Act (ESA) requires the Federal government to designate "critical habitat" for any species it lists under the ESA. This dataset combines both the NOAA National Marine Fisheries Service species listed as critical habitat as well as the coastal species from US Fish & Wildlife Service. Critical habitat is defined as: 1. Specific areas within the geographical area occupied by the species at the time of listing, if they contain physical or biological features essential to conservation, and those features may require special management considerations or protection; and 2. Specific areas outside the geographical area occupied by the species if the agency determines that the area itself is essential for conservation.

High Frequency Radar Radial Ranges (5)

This dataset show the generalized coverage area (as of October 2014), of High Frequency (HF) radar systems across the US. HF radars measure the speed and direction of ocean surface currents in near real time. These radars can measure currents over a large region of the coastal ocean, from a few kilometers offshore up to 200 km, and can operate under any weather conditions. They are located near the water’s edge, and need not be situated atop a high point of land. Dozens of institutions own and operate HF radars within the United States, and a majority are coordinated through the US Integrated Ocean Observing System. Ocean surface current data from these radars are shared on national servers -- the National Data Buoy Center and Scripps Institution of Oceanography -- who deliver the data to anyone who needs it. A process is currently underway to further define the spatial footprint of each radar based on local factors such as nearby obstructions, local wind-wave environment, etc. When available, this data will be integrated into MarineCadastre.gov. In the meantime, if specific information regarding a local radar system is required, please contact Dr. Jack Harlan, Project Manager for the HF Radar Ocean Remote Sensing, US IOOS Program Office.

Ocean Sediment Thickness Contours (6)

Ocean sediment thickness contours in 200 meter intervals for water depths ranging from 0 – 18,000 meters. These contours were derived from a global sediment thickness grid distributed by the National Geophysical Data Center (NGDC). The NGDC grid was compiled from various existing sediment thickness maps and drilling cores, and has a cell resolution of 5 arc seconds. Sediment thickness data is typically acquired through two methods. Seismic (or sub-bottom) profile technologies rely on powerful pulses of low-frequency sound which penetrate the substrate and return information about substrate thickness, character, and stratification. The data are collected along transect lines and require interpolation to create comprehensive maps. Sediment thickness is also determined by direct measurement through coring, which provides more detailed information but only at discrete sites. Coring data can also be interpolated to form area maps, and to help interpret the seismic data.

Bathymetric Contours (7)

Coastal bathymetric depth, measured in meters at depth values of: -10, -20, -30, -40, -50, -60, -70, -80, -90, -100, -150 -200, -400, -600

National Seafloor Sediment (usSEABED) (8)

The usSEABED database contains data for the entire U.S. Exclusive Economic Zone and is an ongoing task of the Marine Aggregates Resources and Processes and National Benthic Habitats Studies (Pacific) projects, USGS Coastal and Marine Geology teams in Santa Cruz, CA, Woods Hole, MA, and St. Petersburg, FL, and the University of Colorado. This data layer is a point coverage of known sediment samplings, inspections and probings from the usSEABED data collection and integrated using the software system dbSEABED. This data layer represents the extracted (EXT) output of the dbSEABED mining software. The EXT data is usually based on instrumental analyses (probe or laboratory) but may apply to just a subsample of the sediment (eg. no large shells).

Pinniped Rookeries (California) (9)

Areas in which the pinnipeds repeatedly haul out and breed.

Pinniped Haul Outs (California) (10)

Seal and sea lion haul-out sites in California, including offshore islands.

Weather Radar Stations (Federal) (11)

These data represent Next-Generation Radar (NEXRAD) and Terminal Doppler Weather Radar (TDWR) stations within the US. The NEXRAD radar stations are maintained and operated by the National Oceanic and Atmospheric Administration (NOAA). The TDWR radar stations are maintained and operated by the Federal Aviation Administration (FAA). Both radar's are pulsed Doppler types that measure reflectivity out to 460km, and radial velocity and spectrum width out to 300km (NEXRAD) and 90km (TDWR). Both radars automatically scan the atmosphere from the surface to 70,000ft using a rotating parabolic antenna.

High Frequency Radar Locations (12)

This dataset show the point locations (as of October 2014), of High Frequency (HF) radar systems across the US. HF radars measure the speed and direction of ocean surface currents in near real time. These radars can measure currents over a large region of the coastal ocean, from a few kilometers offshore up to 200 km, and can operate under any weather conditions. They are located near the water’s edge, and need not be situated atop a high point of land. Dozens of institutions own and operate HF radars within the United States, and a majority are coordinated through the US Integrated Ocean Observing System. Ocean surface current data from these radars are shared on national servers -- the National Data Buoy Center and Scripps Institution of Oceanography -- who deliver the data to anyone who needs it.

Artificial Reefs (13)

An artificial reef is a human-made underwater structure, typically built to promote marine life in areas with a generally featureless bottom, control erosion, block ship passage, or improve surfing. Many reefs are built using objects that were built for other purposes, for example by sinking oil rigs (through the Rigs-to-Reefs program), scuttling ships, or by deploying rubble or construction debris. Other artificial reefs are purpose built (e.g. the reef balls) from PVC or concrete. Shipwrecks may become artificial reefs when preserved on the sea floor. Regardless of construction method, artificial reefs generally provide hard surfaces where algae and invertebrates such as barnacles, corals, and oysters attach; the accumulation of attached marine life in turn provides intricate structure and food for assemblages of fish. This is NOT a complete collection of artificial reefs on the seafloor, nor are the locations to be considered exact. The presence and location of the artificial reefs have been derived from multiple state websites. These data are intended for coastal and ocean planning.

Undersea Feature Place Names (14)

There are approximately 5100 undersea features with names approved by the United States Board on Geographic Names (BGN). The BGN approves undersea feature names based on the recommendation of the Advisory Committee on Undersea Features (ACUF). ACUF is charged with recommending BGN policy for totally-submerged undersea features which lie outside the territorial sea (as recognized by the United Nations Convention on the Law of the Sea) of all coastal states. Undersea features within the territorial sea of the United States are handled by the BGN Domestic Names Committee (DNC) in coordination with ACUF. Some of these names will have overlaps with the Esri Oceans basemap. Please select a different basemap if you want to view this layer without interference with Esri Oceans basemap reference information.

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