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This set of 4 rasters shows precipitation as snow (mm) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America. These data, originally published here, were converted...
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This set of 4 rasters shows mean summer (May to Sep) precipitation (mm) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America. These data, originally published here,...
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This set of 4 rasters shows mean temperature of the coldest month (deg C * 10) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America. These data, originally published...
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This set of 4 rasters shows mean summer (May to Sep) precipitation (mm) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America.
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This set of 4 rasters shows mean temperature of the coldest month (deg C * 10) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America.
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This set of 4 rasters shows summer (Jun to Aug) precipitation (mm) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America. These data, originally published here, were...
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This set of 4 rasters shows winter (Dec to Feb) precipitation (mm) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America. These data, originally published here, were...
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MC1 is a dynamic vegetation model for estimating the distribution of vegetation and associated ecosystem fluxes of carbon, nutrients, and water. It was created to assess the potential impacts of global climate change on ecosystem structure and function at a wide range of spatial scales from landscape to global. The model incorporates transient dynamics to make predictions about the patterns of ecological change. MC1 was created by combining physiologically based biogeographic rules defined in the MAPSS model with a modified version of the biogeochemical model, CENTURY. MC1 includes a fire module, MCFIRE, that mechanistically simulates the occurrence and impacts of fire events. Climate input data sources for this...
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Percent change in biomass consumed by fire is calculated for 50 year periods for the historical period and for the future (2050-2099 versus 1951-2000. Percent change is calculated as ((future – historical/historical) x 100). These are results from the NA8K version of MC1. MC1 is a dynamic vegetation model for estimating the distribution of vegetation and associated ecosystem fluxes of carbon, nutrients, and water. It was created to assess the potential impacts of global climate change on ecosystem structure and function at a wide range of spatial scales from landscape to global. The model incorporates transient dynamics to make predictions about the patterns of ecological change. MC1 was created by combining physiologically...
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Percent change in biomass consumed by fire is calculated for 50 year periods for the historical period and for the future (2050-2099 versus 1951-2000. Percent change is calculated as ((future – historical/historical) x 100). These are results from the NA8K version of MC1. MC1 is a dynamic vegetation model for estimating the distribution of vegetation and associated ecosystem fluxes of carbon, nutrients, and water. It was created to assess the potential impacts of global climate change on ecosystem structure and function at a wide range of spatial scales from landscape to global. The model incorporates transient dynamics to make predictions about the patterns of ecological change. MC1 was created by combining physiologically...
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This set of 4 rasters shows mean annual temperature (deg C * 10) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America. These data, originally published here, were...
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This set of 4 rasters shows winter (Dec to Feb) mean temperature (deg C * 10) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America. These data, originally published...
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This set of 4 rasters shows mean temperature of the warmest month (deg C * 10) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America.
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This set of 4 rasters shows winter (Dec to Feb) precipitation (mm) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America.
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Percent change in biomass consumed by fire is calculated for 50 year periods for the historical period and for the future (2050-2099 versus 1951-2000. Percent change is calculated as ((future – historical/historical) x 100). These are results from the NA8K version of MC1. MC1 is a dynamic vegetation model for estimating the distribution of vegetation and associated ecosystem fluxes of carbon, nutrients, and water. It was created to assess the potential impacts of global climate change on ecosystem structure and function at a wide range of spatial scales from landscape to global. The model incorporates transient dynamics to make predictions about the patterns of ecological change. MC1 was created by combining physiologically...
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This set of 4 rasters shows summer (Jun to Aug) mean temperature (deg C * 10) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America. These data, originally published...
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MC1 is a dynamic vegetation model for estimating the distribution of vegetation and associated ecosystem fluxes of carbon, nutrients, and water. It was created to assess the potential impacts of global climate change on ecosystem structure and function at a wide range of spatial scales from landscape to global. The model incorporates transient dynamics to make predictions about the patterns of ecological change. MC1 was created by combining physiologically based biogeographic rules defined in the MAPSS model with a modified version of the biogeochemical model, CENTURY. MC1 includes a fire module, MCFIRE, that mechanistically simulates the occurrence and impacts of fire events. Climate input data sources for this...
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This set of 4 rasters shows mean temperature of the warmest month (deg C * 10) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America. These data, originally published...
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This set of 4 rasters shows summer (Jun to Aug) mean temperature (deg C * 10) for Western North America under the B1 Emissions Scenario from the Intergovernmental Panel on Climate Change (IPCC). One layer shows the historic period (1961 to 1990), and there are three layers of future climate projections representing the 2020s, the 2050s, and the 2080s. These future layers are ensemble averages across all 23 CMIP3 AOGCMs (Coupled Model Intercomparison Project 3 Atmosphere-Ocean General Circulation Models). All layers have a resolution of 1 km, and are designed to capture climate gradients, temperature inversions, and rain shadows in the mountainous landscape of western North America.
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This product is one of a set of mapped model simulation results generated for a project called "Global Climate Change and California: Potential Implications for Ecosystems, Health, and the Economy". The project was conducted by the Electrical Power Research Institute (EPRI) and funded by the California Energy Commission's Public Interest Energy Research (PIER) Program. The project was the most detailed study ever undertaken on the potential effect of climate change on California. The work examined a broad array of potentially affected sectors as well as the interactions between climate change and increased population, economic growth, and technological change. It considered a wide range of climate change scenarios,...


map background search result map search result map Mean Annual Temperature under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Mean Temperature of the coldest month under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Mean Summer (May to Sep) Precipitation under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Precipitation as Snow under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Summer (Jun to Aug) Mean Temperature under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Summer (Jun to Aug) Precipitation under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Winter (Dec to Feb) Mean Temperature under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Winter (Dec to Feb) Precipitation under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Mean Temperature of the Warmest Month under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Mean Temperature of the Warmest Month under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Winter (Dec to Feb) Precipitation under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Mean Temperature of the coldest month under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Summer (Jun to Aug) Mean Temperature under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Mean Summer (May to Sep) Precipitation under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) GFDL B1 future climate scenario: annual output of potential natural vegetation for California Percent change in biomass consumed by fire for the USA and Canada simulated by the MC1 model and based on climate projections from the CSIRO Mk3.0 GCM for the SRES B1 emission scenario. Percent change in biomass consumed by fire for the USA and Canada simulated by the MC1 model and based on climate projections from the HADCM3 GCM for the SRES B1 emission scenario. Percent change in biomass consumed by fire for the USA and Canada simulated by the MC1 model and based on climate projections from the MIROC 3.2 MEDRES GCM for the SRES B1 emission scenario. Vegetation Type for the United States and Canada Simulated for the years 2070-2099 as Simulated by the MC1 Model (NA8K version) and Based on Climate Projections from the MIROC 3.2 MEDRES GCM for the SRES B1 Emission Scenario Vegetation Type for the United States and Canada Simulated for the years 2070-2099 as Simulated by the MC1 Model (NA8K version) and Based on Climate Projections from the HADLEY for the SRES B1 Emission Scenario GFDL B1 future climate scenario: annual output of potential natural vegetation for California Mean Temperature of the Warmest Month under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Winter (Dec to Feb) Precipitation under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Mean Temperature of the coldest month under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Summer (Jun to Aug) Mean Temperature under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Mean Summer (May to Sep) Precipitation under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Mean Annual Temperature under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Mean Temperature of the coldest month under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Mean Summer (May to Sep) Precipitation under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Precipitation as Snow under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Summer (Jun to Aug) Mean Temperature under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Summer (Jun to Aug) Precipitation under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Winter (Dec to Feb) Mean Temperature under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Winter (Dec to Feb) Precipitation under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Mean Temperature of the Warmest Month under the B1 Emissions Scenario (Western North America, 23 AOGCM Ensemble) Percent change in biomass consumed by fire for the USA and Canada simulated by the MC1 model and based on climate projections from the CSIRO Mk3.0 GCM for the SRES B1 emission scenario. Percent change in biomass consumed by fire for the USA and Canada simulated by the MC1 model and based on climate projections from the HADCM3 GCM for the SRES B1 emission scenario. Percent change in biomass consumed by fire for the USA and Canada simulated by the MC1 model and based on climate projections from the MIROC 3.2 MEDRES GCM for the SRES B1 emission scenario. Vegetation Type for the United States and Canada Simulated for the years 2070-2099 as Simulated by the MC1 Model (NA8K version) and Based on Climate Projections from the MIROC 3.2 MEDRES GCM for the SRES B1 Emission Scenario Vegetation Type for the United States and Canada Simulated for the years 2070-2099 as Simulated by the MC1 Model (NA8K version) and Based on Climate Projections from the HADLEY for the SRES B1 Emission Scenario