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This layer has been updated in 2016 This shapefile represents the watersheds present within the Crown of the Continent Ecosystem (CCE) boundary.(Note: a different CCE boundary layer was used at the time of creation, so the area amounts within the CCE may not be accurate)This dataset was developed by the Crown Managers Partnership, as part of a transboundary collaborative management initiative for the Crown of the Continent Ecosystem, based on commonly identified management priorities that are relevant at the landscape scale. The CMP is collaborative group of land managers, scientists, and stakeholder in the CCE. For more information on the CMP and its collaborators, programs, and projects please visit: http://crownmanagers.org/
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This data set includes geospatial data and tables providing location, environmental, and vegetation data collected in 2017 and 2018 at the Little Saint Francis River chat pile restoration site, Fredericktown, Madison County, Missouri. Restoration actions are being implemeneted as part of the settlement for the Madison County Mines Superfund site to compensate the public for losses of natural resources and the services they provide as part of the Natural Resource Damage Assessment and Restoration Southeast Missouri Lead Mining District case. Data were collected prior to and during the early stages of restoration actions to restore bottomland forest habitat, reduce invasive plant species abundance, and improve upland...
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Average Winter (Jan-Mar) Temperature (2045-2060) simulated by RegCM3 with GENMOM projections as boundary conditions. Units are degrees Celsius. These data were generated by the regional climate model RegCM3 with boundary conditions from a GCM future climate projections. The data were downscaled statistically by calculating differences (anomalies) between the RegCM3 results with GCM-driven boundary conditions for 1968-99 and those for a future period, in this case 2015-2030. The anomalies were added (temperatures) or multiplied (precipitation) to a climate baseline from PRISM (Parameter-elevation Regressions on Indepenent Slopes Model - prism.oregonstate.edu) data based on historical observations. The PRISM baseline...
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Difference of Spring (Apr-Jun) Precipitation (2045-2060 vs 1968-1999) simulated by RegCM3 with ECHAM5 projections as boundary conditions. Units are millimeters. These data were generated by the regional climate model RegCM3 with boundary conditions from a GCM future climate projections. The data were downscaled statistically by calculating differences (anomalies) between the RegCM3 results with GCM-driven boundary conditions for 1968-99 and those for a future period, in this case 2015-2030. The anomalies were added (temperatures) or multiplied (precipitation) to a climate baseline from PRISM (Parameter-elevation Regressions on Indepenent Slopes Model - prism.oregonstate.edu) data based on historical observations....
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Potential Evapotranspiration simulated by the biogeography model MAPSS using RegCM3 climate with GFDL projections as boundary conditions. Units are millimeters of water. MAPSS (Mapped Atmosphere-Plant-Soil System) is a static biogeography model that projects potential vegetation distribution and hydrological flows on a grid (http://www.databasin.org/climate-center/features/mapss-model). MAPSS has been used widely for various climate change assessments including the 2000 National Assessment Synthesis Team's report. MAPSS uses long term, average monthly climate data (mean monthly temperature, vapor pressure, wind speed, and precipitation) as well as soils information (texture, depth). Based on a set of climatic thresholds,...
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Average Summer (Jul-Sep) Precipitation (2045-2060) simulated by RegCM3 with ECHAM5 projections as boundary conditions. Units are millimeters. These data were generated by the regional climate model RegCM3 with boundary conditions from a GCM future climate projections. The data were downscaled statistically by calculating differences (anomalies) between the RegCM3 results with GCM-driven boundary conditions for 1968-99 and those for a future period, in this case 2015-2030. The anomalies were added (temperatures) or multiplied (precipitation) to a climate baseline from PRISM (Parameter-elevation Regressions on Indepenent Slopes Model - prism.oregonstate.edu) data based on historical observations. The PRISM baseline...
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5th Code HUC reporting units for the Colorado Plateau Ecoregion Used as analytical reporting units for aquatic conservation elements.
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Difference of Average Winter (Jan-Mar) Temperature (2045-2060 vs 1968-1999) simulated by RegCM3 with GENMOM projections as boundary conditions. Units are degrees Celsius. These data were generated by the regional climate model RegCM3 with boundary conditions from a GCM future climate projections. The data were downscaled statistically by calculating differences (anomalies) between the RegCM3 results with GCM-driven boundary conditions for 1968-99 and those for a future period, in this case 2015-2030. The anomalies were added (temperatures) or multiplied (precipitation) to a climate baseline from PRISM (Parameter-elevation Regressions on Indepenent Slopes Model - prism.oregonstate.edu) data based on historical observations....
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This dataset provides an estimate of aquatic biodiversity sites, based on protected and conservation lands superimposed on the NHD flowlines dataset. Caution is warrented in interpreting this dataset. While measures of aquatic biodiversity exist, they are based on localized samples that cannot be extrapolated beyond the sampling domain. These measures were not included in this dataset. Instead, it was assumed that areas within TNC Portfolio areas were identified for factors that include high aquatic biodiversity. Furthermore, it is assumed that aquatic biodiversity is higher in protected areas due to stricter controls over land and water management. However, this assumption may not be valid for stream reaches that...
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This dataset provides an estimate of water-based recreation travel corridors, based on a combination of wild and scenic rivers, and major rivers selected from NHD that were listed on the BLM rivers website. All reaches of these rivers were selected, as insufficient information exists to determine what segments may or may not be open to recreation. Other areas may be open to water-based recreation travel than are represented in this dataset.
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5th Code HUC reporting units for the Colorado Plateau Ecoregion Used as analytical reporting units for aquatic conservation elements.
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The distribution and abundance of Colorado River cutthroat trout (Oncorhynchus clarkii pleuriticus; CRCT) have declined from historical levels over their entire range. For this CRCT assessment we used existing information provided by 48 fisheries professionals applied through a consistent methodology to assess the extent of CRCT historical range, their current distribution, including genetic status, and evaluated the foreseeable risks to 285 populations designated as "conservation populations" by management agencies. We estimated CRCT historically occupied about 21,386 miles of habitat in the western U.S. CRCT currently occupy about 3,022 miles of habitat in 51 of the 61 4th level HUCs historically occupied. Of...
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Two future climate change scenarios at a resolution of 0.5 degree latitude/longitude for the conterminous United States were used in the Vegetation Ecosystems Modelling Analysis Project (VEMAP): a moderately warm scenario produced by the general circulation model from the Hadley Climate Centre [Johns et al., 1997; Mitchell and Johns, 1997], HADCM2SUL (up to a 2.8oC increase in average annual U.S. temperature in 2100) and a warmer scenario (up to a 5.8oC increase in average annual U.S. temperature in 2100), CGCM1, from the Canadian Climate Center [Boer et al., 1999a, 1999b; Flato et al., 1999]. Both general circulation models (GCMs) included sulfate aerosols and a fully dynamic 3-D ocean. Both transient scenarios...
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This is a first cut at a statewide 1:63,360 coastline. The entire coasline, however, is not 1:63.360; only where data was available as of January 1998. It is a mixture of sources ranging from the Department of Natural Resources, Land Records Information Section hydrography database to the Exxon Valdez Oil Spill Environmentally Sensitive Index coastline (no ESI attributes included) to the US Geologic Survey hydrography to US Forest Service (in Prince William Sound). Where the 1:63,360 data was unavailable the 1:250,000 coastline was used to fill in. This information does not include lakes or streams. All streams are cut off at the mouth with a straight line. It excludes small islands that are difficult to visually...
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The National Hydrography Dataset (NHD) and Watershed Boundary Dataset (WBD) are used to portray surface water on The National Map. The NHD represents the drainage network with features such as rivers, streams, canals, lakes, ponds, coastline, dams, and streamgages. The WBD represents drainage basins as enclosed areas in eight different size categories. Both datasets represent the real world at a nominal scale of 1:24,000-scale, which means that one inch of The National Map data equals 2,000 feet on the ground. To maintain mapping clarity not all water features are represented and those that are use a moderate level of detail. The NHD and WBD are digital vector datasets used by geographic information systems (GIS)....
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Large and small connected lakes throughout the CYR study area support a rich biodiversity of aquatic organisms and represent important foraging and breeding habitat for fish, waterfowl, and shorebirds. Additionally, lakes provide important recreational opportunities and food resources for local residents (e.g., subsistence harvest of fish and wildlife). Small and large lakes were identified based on the definition used in Arp and Jones (2009) to differentiate small (less than 0.1 sq km) from medium and large lakes (greater than 0.1 km2). Lake connections, especially for smaller lakes, can vary greatly and change throughout the open-water season, with ephemeral connections commonly occurring during high flows in...
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Two future climate change scenarios at a resolution of 0.5 degree latitude/longitude for the conterminous United States were used in the Vegetation Ecosystems Modelling Analysis Project (VEMAP): a moderately warm scenario produced by the general circulation model from the Hadley Climate Centre [Johns et al., 1997; Mitchell and Johns, 1997], HADCM2SUL (up to a 2.8oC increase in average annual U.S. temperature in 2100) and a warmer scenario (up to a 5.8oC increase in average annual U.S. temperature in 2100), CGCM1, from the Canadian Climate Center [Boer et al., 1999a, 1999b; Flato et al., 1999]. Both general circulation models (GCMs) included sulfate aerosols and a fully dynamic 3-D ocean. Both transient scenarios...
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Difference of Leaf Area Index (2045-2060 vs 1968-1999) simulated by the biogeography model MAPSS using RegCM3 climate with ECHAM5 projections as boundary conditions. MAPSS (Mapped Atmosphere-Plant-Soil System) is a static biogeography model that projects potential vegetation distribution and hydrological flows on a grid (http://www.databasin.org/climate-center/features/mapss-model). MAPSS has been used widely for various climate change assessments including the 2000 National Assessment Synthesis Team's report. MAPSS uses long term, average monthly climate data (mean monthly temperature, vapor pressure, wind speed, and precipitation) as well as soils information (texture, depth). Based on a set of climatic thresholds,...


map background search result map search result map Major Lakes Crown of the Continent Ecosystem (CCE) z_Archive Watersheds in the CCE Pre-restoration vegetation data, Little Saint Francis River chat pile site, Missouri, USA, 2017 and 2018 BLM REA COP 2010 Projected annual average precipitation (mm) under HAD future climate scenario 2070-2099 for the Colorado Plateau ecoregion, USA BLM REA COP 2010 Difference of Leaf Area Index (2045-2060 vs 1968-1999) Simulated by MAPSS using RegCM3 Climate with ECHAM5 Projections as Boundary Conditions (Western US) BLM REA COP 2010 Difference of Spring (Apr-Jun) Precipitation (2045-2060 vs 1968-1999) Simulated by RegCM3 with ECHAM5 Projections as Boundary Conditions (Western US) BLM REA COP 2010 Average Winter (Jan-Mar) Temperature (2045-2060) Simulated by RegCM3 with GENMOM Projections as Boundary Conditions (Western US) BLM REA COP 2010 Potential Evapotranspiration (2045-2060) Simulated by MAPSS using RegCM3 Climate with GFDL Projections as Boundary Conditions (Western US) BLM REA COP 2010 Average Summer (Jul-Sep) Precipitation (2045-2060) Simulated by RegCM3 with ECHAM5 Projections as Boundary Conditions (Western US) BLM REA COP 2010 AT C Reservoir DN HUC5 poly BLM REA COP 2010 Potential Aquatic Biodiversity Areas BLM REA COP 2010 Water-Based Recreation Travel Corridors BLM REA COP 2010 AT C NAS DN HUC5 poly BLM REA COP 2010 Difference of Average Winter (Jan-Mar) Temperature (2045-2060 vs 1968-1999) Simulated by RegCM3 with GENMOM Projections as Boundary Conditions (Western US) BLM REA COP 2010 Range-Wide Status of Colorado River Cutthroat Trout (Oncorhynchus clarkii pleuriticus) - Streams BLM REA COP 2010 Wild and Scenic Rivers BLM REA COP 2010 Historic annual average precipitation (mm) 1961-1990 (VEMAP version) for the Colorado Plateau ecoregion, USA BLM REA CYR 2013 National Hydrography Dataset Alaska: Flowlines BLM REA CYR 2013 Alaska Coastline 1:63,360 Excluding Small Islands BLM REA CYR 2013 Connected Small Lakes Pre-restoration vegetation data, Little Saint Francis River chat pile site, Missouri, USA, 2017 and 2018 BLM REA COP 2010 Wild and Scenic Rivers BLM REA COP 2010 Range-Wide Status of Colorado River Cutthroat Trout (Oncorhynchus clarkii pleuriticus) - Streams z_Archive Watersheds in the CCE BLM REA COP 2010 Water-Based Recreation Travel Corridors BLM REA COP 2010 Potential Aquatic Biodiversity Areas BLM REA COP 2010 AT C Reservoir DN HUC5 poly BLM REA COP 2010 AT C NAS DN HUC5 poly BLM REA COP 2010 Difference of Leaf Area Index (2045-2060 vs 1968-1999) Simulated by MAPSS using RegCM3 Climate with ECHAM5 Projections as Boundary Conditions (Western US) BLM REA COP 2010 Difference of Spring (Apr-Jun) Precipitation (2045-2060 vs 1968-1999) Simulated by RegCM3 with ECHAM5 Projections as Boundary Conditions (Western US) BLM REA COP 2010 Average Winter (Jan-Mar) Temperature (2045-2060) Simulated by RegCM3 with GENMOM Projections as Boundary Conditions (Western US) BLM REA COP 2010 Potential Evapotranspiration (2045-2060) Simulated by MAPSS using RegCM3 Climate with GFDL Projections as Boundary Conditions (Western US) BLM REA COP 2010 Average Summer (Jul-Sep) Precipitation (2045-2060) Simulated by RegCM3 with ECHAM5 Projections as Boundary Conditions (Western US) BLM REA COP 2010 Difference of Average Winter (Jan-Mar) Temperature (2045-2060 vs 1968-1999) Simulated by RegCM3 with GENMOM Projections as Boundary Conditions (Western US) BLM REA COP 2010 Projected annual average precipitation (mm) under HAD future climate scenario 2070-2099 for the Colorado Plateau ecoregion, USA BLM REA COP 2010 Historic annual average precipitation (mm) 1961-1990 (VEMAP version) for the Colorado Plateau ecoregion, USA BLM REA CYR 2013 Connected Small Lakes BLM REA CYR 2013 National Hydrography Dataset Alaska: Flowlines Major Lakes Crown of the Continent Ecosystem (CCE) BLM REA CYR 2013 Alaska Coastline 1:63,360 Excluding Small Islands