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Climate data (Average Annual Temperature for 1968-1999) were created by PRISM (Parameter-elevation Regressions on Indepenent Slopes Model - prism.oregonstate.edu) on a 2.5 arc-minute lat-lon grid. They are based on historical observations from 1968-1999. We created mean monthly climatologies for that period from the PRISM data, and reprojected the results to the BLM Albers 4km grid. We used these results as a historical baseline climate to de-bias RegCM3 projections. We also compiled annual and seasonal summaries of precipitation and temperature from the PRISM data to allow for simple comparisons with other climatologies. Units are degrees celsius.
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Average Winter (Jan-Mar) Temperature (2045-2060) simulated by RegCM3 with ECHAM5 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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Average Annual Temperature (2015-2030) 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 was calculated...
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Runoff simulated by the biogeography model MAPSS using RegCM3 climate with GENMOM 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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Average Annual Temperature (2015-2030) simulated by RegCM3 with ECHAM5 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 was calculated...
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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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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 Summer (Jul-Sep) Temperature (2015-2030) simulated by RegCM3 with ECHAM5 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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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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Potential Natural Vegetation Class simulated by the biogeography model MAPSS using RegCM3 climate with GFDL 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, the model defines...
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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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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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Leaf Area Index 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, the model defines the following plant...
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Some of the YKL rasters intentionally do not align or have the same extent. These rasters were not snapped to a common raster per the authors' discretion. Please review selected rasters prior to use. These varying alignments are a result of the use of differing source data sets and all products derived from them. We recommend that users snap or align rasters as best suits their own projects. - This file includes a downscaled projection of decadal cliomes for the decade 2060-2069 at 2km spatial resolution. "Cliomes" can be considered to be assemblages of species and aggregated communities that might be expected to occur based on linkages with prevailing climate conditions. They are not the same as actual biomes,...
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Some of the YKL rasters intentionally do not align or have the same extent. These rasters were not snapped to a common raster per the authors' discretion. Please review selected rasters prior to use. These varying alignments are a result of the use of differing source data sets and all products derived from them. We recommend that users snap or align rasters as best suits their own projects. - This set of files includes downscaled projections of decadal means of annual length of growing season (number of days, 0-365) for the decades 2010-2019, 2020-2029, 2050-2059, and 2060-2069 at 771x771 meter spatial resolution. Each file represents a decadal mean of an annual mean calculated from mean monthly data. The spatial...
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Some of the CYR rasters intentionally do not align or have the same extent. These rasters were not snapped to a common raster per the authors' discretion. Please review selected rasters prior to use. These varying alignments are a result of the use of differing source data sets and all products derived from them. We recommend that users snap or align rasters as best suits their own projects. - Projections show a relatively steady increase in mean annual ground temperature (MAGT) across the region over time, with acceleration as the century progresses. Because permafrost conditions are highly site-specific at fine resolution, actual conditions are likely to vary within pixels. Thus, these outputs must be viewed at...
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Some of the CYR rasters intentionally do not align or have the same extent. These rasters were not snapped to a common raster per the authors' discretion. Please review selected rasters prior to use. These varying alignments are a result of the use of differing source data sets and all products derived from them. We recommend that users snap or align rasters as best suits their own projects. - This file includes a downscaled projection of decadal Active Layer Thickness (in meters) for the decades 2010-2019, 2020-2029, and 2060-2069 at 2km spatial resolution, using the A2 emissions scenario. The raster contains both negative and positive values. Positive values relate to the active layer thickness, or depth of summer...
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Leaf Area Index simulated by the biogeography model MAPSS using RegCM3 climate with GFDL 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, the model defines the following plant...


map background search result map search result map BLM REA COP 2010 Runoff (2045-2060) Simulated by MAPSS using RegCM3 Climate with GENMOM Projections as Boundary Conditions (Western US) 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 Potential Natural Vegetation Class (2045-2060) Simulated by MAPSS using RegCM3 Climate with GFDL 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 Average Summer (Jul-Sep) Temperature (2015-2030) Simulated by RegCM3 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 Average Annual Temperature (2015-2030) Simulated by RegCM3 with ECHAM5 Projections as Boundary Conditions (Western US) BLM REA SOD 2010 Average Annual Temperature (1968-1999) from PRISM (Western US) BLM REA SOD 2010 Leaf Area Index (2045-2060) Simulated by MAPSS using RegCM3 Climate with ECHAM5 Projections as Boundary Conditions (Western US) BLM REA SOD 2010 Leaf Area Index (2045-2060) Simulated by MAPSS using RegCM3 Climate with GFDL Projections as Boundary Conditions (Western US) BLM REA SOD 2010 Average Winter (Jan-Mar) Temperature (2045-2060) Simulated by RegCM3 with ECHAM5 Projections as Boundary Conditions (Western US) BLM REA SOD 2010 Average Annual Temperature (2015-2030) Simulated by RegCM3 with GENMOM Projections as Boundary Conditions (Western US) BLM REA CYR 2013 Permafrost Thaw at 1 m Depth from the 2010s to 2060s BLM REA CYR 2013 Near-term Future (2020s) Active Layer Thickness and Seasonal Soil Freeze Thaw Depth BLM REA SOD 2010 Average Annual Temperature (1968-1999) from PRISM (Western US) BLM REA SOD 2010 Leaf Area Index (2045-2060) Simulated by MAPSS using RegCM3 Climate with ECHAM5 Projections as Boundary Conditions (Western US) BLM REA SOD 2010 Leaf Area Index (2045-2060) Simulated by MAPSS using RegCM3 Climate with GFDL Projections as Boundary Conditions (Western US) BLM REA SOD 2010 Average Winter (Jan-Mar) Temperature (2045-2060) Simulated by RegCM3 with ECHAM5 Projections as Boundary Conditions (Western US) BLM REA SOD 2010 Average Annual Temperature (2015-2030) Simulated by RegCM3 with GENMOM Projections as Boundary Conditions (Western US) BLM REA COP 2010 Runoff (2045-2060) Simulated by MAPSS using RegCM3 Climate with GENMOM Projections as Boundary Conditions (Western US) 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 Potential Natural Vegetation Class (2045-2060) Simulated by MAPSS using RegCM3 Climate with GFDL 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 Average Summer (Jul-Sep) Temperature (2015-2030) Simulated by RegCM3 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 Average Annual Temperature (2015-2030) Simulated by RegCM3 with ECHAM5 Projections as Boundary Conditions (Western US) BLM REA CYR 2013 Permafrost Thaw at 1 m Depth from the 2010s to 2060s BLM REA CYR 2013 Near-term Future (2020s) Active Layer Thickness and Seasonal Soil Freeze Thaw Depth