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This dataset presents the current potential distribution of lowland leopard frog in the context of current and near-term aquatic intactness, and long-term potential for climate change at the watershed (HUC5) scale. Current aquatic intactness is based on current measures of landscape development, water quality, hydrologic impacts, and road impacts. Near-term intactness includes estimates of urban growth. Long-term potential for climate change is based on absolute changes in runoff, precipitation, temperature, and vegetation change estimated using climate projections (RegCM3 regional climate model based on ECHAM5 boundary conditions) and a biogeography model (MAPSS) for the period 2045-2060. The aquatic intactness...
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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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5th Code HUC reporting units for the Sonoran Desert Ecoregion Used as analytical reporting units for aquatic conservation elements.
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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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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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Runoff simulated by the biogeography model MAPSS using RegCM3 climate with ECHAM5 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, the model...
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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,...
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5th Code HUC reporting units for the Sonoran Desert Ecoregion Used as analytical reporting units for aquatic conservation elements.
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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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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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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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The National Hydrography Dataset (NHD) is a feature-based database that interconnects and uniquely identifies the stream segments or reaches that make up the nation's surface water drainage system. NHD data was originally developed at 1:100,000-scale and exists at that scale for the whole country. This high-resolution NHD, generally developed at 1:24,000/1:12,000 scale, adds detail to the original 1:100,000-scale NHD. (Data for Alaska, Puerto Rico and the Virgin Islands was developed at high-resolution, not 1:100,000 scale.) Local resolution NHD is being developed where partners and data exist. The NHD contains reach codes for networked features, flow direction, names, and centerline representations for areal water...
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Relative effects of the co-occurrence of CAs and CEs are addressed in part by evaluating ecological status of CEs within a given assessment scenario (e.g., current conditions). The approach to evaluating ecological status was based on existing methods for gauging relative ecological integrity . “Ecological integrity” is variously defined as the ability of an ecological system to support and maintain a community of organisms that have the species composition, diversity, and functional organization comparable to those of natural habitats within the ecoregion. Therefore, one of the early tasks in the assessment was to characterize reference conditions for each CE, including natural composition, structure, and dynamic...
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Riparian and wetland systems were determined from NHD waterbodies, SWReGAP riparian landcover types, and LANDFIRE riparian existing vegetation types. Potential for change (PFC) was determined by calculating the maximum potential for change among all change agents within each 1 km reporting unit. Current and future landscape intactness (LCM_C_FZ and LCM_N_FZ) are based on measures of landscape development and invasive species. Current vegetation departure (VDEP) is based on LANDFIRE vegetation departure and characterizes the departure of current vegetation from historic reference vegetation conditions. Current and future human development (DEV_C_FZ and DEV_N_FZ) represent human development intensity values modeled...
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To support the BLM's San Luis Valley-Taos Plateau Landscape Assessment. This dataset presents current and future change agent models and combined future potential for change (PFC) within USGS HUC12 boundaries.This dataset presents current and future change agent models and combined future potential for climate change (PFC). Potential for change (PFC) was determined by calculating the maximum potential for change among all change agents within each 1 km reporting unit. Current and future landscape intactness (LCM_C_FZ and LCM_N_FZ) are based on measures of landscape development and invasive species. Current vegetation departure (VDEP) is based on LANDFIRE vegetation departure and characterizes the departure of current...
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To support the BLM's San Luis Valley-Taos Plateau Landscape Assessment. This dataset presents current and future change agent models and combined future potential for change (PFC) within USGS HUC12 boundaries.This dataset presents current and future change agent models and combined future potential for climate change (PFC). Potential for change (PFC) was determined by calculating the maximum potential for change among all change agents within each 1 km reporting unit. Current and future landscape intactness (LCM_C_FZ and LCM_N_FZ) are based on measures of landscape development and invasive species. Current vegetation departure (VDEP) is based on LANDFIRE vegetation departure and characterizes the departure of current...
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The 303(d) Listed Impaired Waters program system provides impaired water data and impaired water features reflecting river segments, lakes, and estuaries designated under Section 303(d) of the Clean Water Act. Each State will establish Total Maximum Daily Loads (TMDLs) for these waters. Note the CWA Section 303(d) list of impaired waters does not represent waters that are impaired but have an EPA-approved TMDL established, impaired waters for which other pollution control mechanisms are in place and expected to attain water quality standards, or waters impaired as a result of pollution and is not caused by a pollutant. Therefore, the "Impaired Waters" layers do not represent all impaired waters reported in a state's...
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To support the BLM's San Luis Valley-Taos Plateau Landscape Assessment. This dataset presents current and future change agent models and combined future potential for change (PFC) within USGS HUC12 boundaries.This dataset presents current and future change agent models and combined future potential for climate change (PFC). Potential for change (PFC) was determined by calculating the maximum potential for change among all change agents within each 1 km reporting unit. Current and future landscape intactness (LCM_C_FZ and LCM_N_FZ) are based on measures of landscape development and invasive species. Current vegetation departure (VDEP) is based on LANDFIRE vegetation departure and characterizes the departure of current...
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Riparian and wetland systems were determined from NHD waterbodies, SWReGAP riparian landcover types, and LANDFIRE riparian existing vegetation types. Potential for change (PFC) was determined by calculating the maximum potential for change among all change agents within each 1 km reporting unit. Current and future landscape intactness (LCM_C_FZ and LCM_N_FZ) are based on measures of landscape development and invasive species. Current vegetation departure (VDEP) is based on LANDFIRE vegetation departure and characterizes the departure of current vegetation from historic reference vegetation conditions. Current and future human development (DEV_C_FZ and DEV_N_FZ) represent human development intensity values modeled...
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The NHDPlus Version 1.0 is an integrated suite of application-ready geospatial data sets that incorporate many of the best features of the National Hydrography Dataset (NHD) and the National Elevation Dataset (NED). The NHDPlus includes a stream network (based on the 1:100,000-scale NHD), improved networking, naming, and "value-added attributes" (VAA's). NHDPlus also includes elevation-derived catchments (drainage areas) produced using a drainage enforcement technique first broadly applied in New England, and thus dubbed "The New-England Method". This technique involves "burning-in" the 1:100,000-scale NHD and when available building "walls" using the national Watershed Boundary Dataset (WBD). The resulting modified...


map background search result map search result map BLM REA COP 2010 Runoff (2015-2030) Simulated by MAPSS using RegCM3 Climate with ECHAM5 Projections as Boundary Conditions (Western US) 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 Range-Wide Status of Colorado River Cutthroat Trout (Oncorhynchus clarkii pleuriticus) - Streams BLM REA SOD 2010 AT C 303d Waterbodies DN HUC5 Poly BLM REA SOD 2010 AT C 303d Streams DN HUC5 Poly BLM REA SOD 2010 Lowland Leopard Frog: Current and Near-Term Status and Long-Term Potential For Change BLM REA MAR 2012 NHDPointEventFC - MAR BLM REA SLV 2013 Riparian Wetland PFC BLM REA SLV 2013 AE Hydrology PFC HUC12 Poly Climate BLM REA SLV 2013 AE Hydrology PFC HUC12 Poly Fire BLM REA SLV 2013 EPA 303d ln BLM REA SLV 2013 AE Hydrology PFC HUC12 Poly Near Term Human Development BLM REA SLV 2013 Riparian Wetland PFC Fire BLM REA MBR 2010 National Hydrography Dataset Plus - NHDPlus Pt BLM REA SNK 2010 Aquatic Coarse Filter CE Scorecard - Hot Springs - DITCHES BLM REA SLV 2013 EPA 303d ln BLM REA SLV 2013 Riparian Wetland PFC BLM REA SLV 2013 Riparian Wetland PFC Fire BLM REA SLV 2013 AE Hydrology PFC HUC12 Poly Climate BLM REA SLV 2013 AE Hydrology PFC HUC12 Poly Fire BLM REA SLV 2013 AE Hydrology PFC HUC12 Poly Near Term Human Development BLM REA MAR 2012 NHDPointEventFC - MAR BLM REA COP 2010 Range-Wide Status of Colorado River Cutthroat Trout (Oncorhynchus clarkii pleuriticus) - Streams BLM REA MBR 2010 National Hydrography Dataset Plus - NHDPlus Pt BLM REA SOD 2010 AT C 303d Waterbodies DN HUC5 Poly BLM REA SOD 2010 AT C 303d Streams DN HUC5 Poly BLM REA SOD 2010 Lowland Leopard Frog: Current and Near-Term Status and Long-Term Potential For Change BLM REA COP 2010 Runoff (2015-2030) Simulated by MAPSS using RegCM3 Climate with ECHAM5 Projections as Boundary Conditions (Western US) 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 SNK 2010 Aquatic Coarse Filter CE Scorecard - Hot Springs - DITCHES