Skip to main content
Advanced Search

Filters: Tags: gcm (X)

545 results (134ms)   

Filters
Date Range
Extensions
Types
Contacts
Categories
Tag Types
Tag Schemes
View Results as: JSON ATOM CSV
thumbnail
Using the simple anomaly method (modifying a historical baseline with differences or ratios projected by General Circulation Models), scientists from the California Academy of Sciences downscaled monthly average temperature and monthly total precipitation from 16 different global circulation models (GCMs). The GCMs were described in the latest Intergovernmental Panel for Climate Change (IPCC 2007) and archived at the WCRP PCMDI (http://www-pcmdi.llnl.gov/ipcc/about_ipcc.php). Monthly maximum temperature and monthly minimum temperatures were downscaled from the only 6 GCMs that archived these particular variables. Scientists used Worldclim v.1.4 (Hijmans et al 2005) at 5 arc-minute (~10km) spatial grain as the current...
thumbnail
Using the simple anomaly method (modifying a historical baseline with differences or ratios projected by General Circulation Models), scientists from the California Academy of Sciences downscaled monthly average temperature and monthly total precipitation from 16 different global circulation models (GCMs). The GCMs were described in the latest Intergovernmental Panel for Climate Change (IPCC 2007) and archived at the WCRP PCMDI (http://www-pcmdi.llnl.gov/ipcc/about_ipcc.php). Monthly maximum temperature and monthly minimum temperatures were downscaled from the only 6 GCMs that archived these particular variables. Scientists used Worldclim v.1.4 (Hijmans et al 2005) at 5 arc-minute (~10km) spatial grain as the current...
thumbnail
Using the simple anomaly method (modifying a historical baseline with differences or ratios projected by General Circulation Models), scientists from the California Academy of Sciences downscaled monthly average temperature and monthly total precipitation from 16 different global circulation models (GCMs). The GCMs were described in the latest Intergovernmental Panel for Climate Change (IPCC 2007) and archived at the WCRP PCMDI (http://www-pcmdi.llnl.gov/ipcc/about_ipcc.php). Monthly maximum temperature and monthly minimum temperatures were downscaled from the only 6 GCMs that archived these particular variables. Scientists used Worldclim v.1.4 (Hijmans et al 2005) at 5 arc-minute (~10km) spatial grain as the current...
thumbnail
Using the simple anomaly method (modifying a historical baseline with differences or ratios projected by General Circulation Models), scientists from the California Academy of Sciences downscaled monthly average temperature and monthly total precipitation from 16 different global circulation models (GCMs). The GCMs were described in the latest Intergovernmental Panel for Climate Change (IPCC 2007) and archived at the WCRP PCMDI (http://www-pcmdi.llnl.gov/ipcc/about_ipcc.php). Monthly maximum temperature and monthly minimum temperatures were downscaled from the only 6 GCMs that archived these particular variables. Scientists used Worldclim v.1.4 (Hijmans et al 2005) at 5 arc-minute (~10km) spatial grain as the current...
thumbnail
Using the simple anomaly method (modifying a historical baseline with differences or ratios projected by General Circulation Models), scientists from the California Academy of Sciences downscaled monthly average temperature and monthly total precipitation from 16 different global circulation models (GCMs). The GCMs were described in the latest Intergovernmental Panel for Climate Change (IPCC 2007) and archived at the WCRP PCMDI (http://www-pcmdi.llnl.gov/ipcc/about_ipcc.php). Monthly maximum temperature and monthly minimum temperatures were downscaled from the only 6 GCMs that archived these particular variables. Scientists used Worldclim v.1.4 (Hijmans et al 2005) at 5 arc-minute (~10km) spatial grain as the current...
thumbnail
Using the simple anomaly method (modifying a historical baseline with differences or ratios projected by General Circulation Models), scientists from the California Academy of Sciences downscaled monthly average temperature and monthly total precipitation from 16 different global circulation models (GCMs). The GCMs were described in the latest Intergovernmental Panel for Climate Change (IPCC 2007) and archived at the WCRP PCMDI (http://www-pcmdi.llnl.gov/ipcc/about_ipcc.php). Monthly maximum temperature and monthly minimum temperatures were downscaled from the only 6 GCMs that archived these particular variables. Scientists used Worldclim v.1.4 (Hijmans et al 2005) at 5 arc-minute (~10km) spatial grain as the current...
thumbnail
Using the simple anomaly method (modifying a historical baseline with differences or ratios projected by General Circulation Models), scientists from the California Academy of Sciences downscaled monthly average temperature and monthly total precipitation from 16 different global circulation models (GCMs). The GCMs were described in the latest Intergovernmental Panel for Climate Change (IPCC 2007) and archived at the WCRP PCMDI (http://www-pcmdi.llnl.gov/ipcc/about_ipcc.php). Monthly maximum temperature and monthly minimum temperatures were downscaled from the only 6 GCMs that archived these particular variables. Scientists used Worldclim v.1.4 (Hijmans et al 2005) at 5 arc-minute (~10km) spatial grain as the current...
thumbnail
Using the simple anomaly method (modifying a historical baseline with differences or ratios projected by General Circulation Models), scientists from the California Academy of Sciences downscaled monthly average temperature and monthly total precipitation from 16 different global circulation models (GCMs). The GCMs were described in the latest Intergovernmental Panel for Climate Change (IPCC 2007) and archived at the WCRP PCMDI (http://www-pcmdi.llnl.gov/ipcc/about_ipcc.php). Monthly maximum temperature and monthly minimum temperatures were downscaled from the only 6 GCMs that archived these particular variables. Scientists used Worldclim v.1.4 (Hijmans et al 2005) at 5 arc-minute (~10km) spatial grain as the current...
thumbnail
The Nature Conservancy (TNC) has derived climate suitability forecasts for most species of trees and shrubs considered to be ecological dominants of terrestrial Californian habitat types. Our plant projections are compiled as decision support tools to help Conservancy project staff, as well as our external partners, develop the necessary plans, priorities and strategies to successfully adapt to uncertain changes in future climate. In the recently completed Southern Sierra Partnership's 2010 Climate-Adapted Conservation Plan for the Southern Sierra Nevada and Tehachapi Mountains, species and habitat forecasts shown here informed the development of a regional conservation design that explicitly incorporates long-term...
thumbnail
The Nature Conservancy (TNC) has derived climate suitability forecasts for most species of trees and shrubs considered to be ecological dominants of terrestrial Californian habitat types. Our plant projections are compiled as decision support tools to help Conservancy project staff, as well as our external partners, develop the necessary plans, priorities and strategies to successfully adapt to uncertain changes in future climate. In the recently completed Southern Sierra Partnership's 2010 Climate-Adapted Conservation Plan for the Southern Sierra Nevada and Tehachapi Mountains, species and habitat forecasts shown here informed the development of a regional conservation design that explicitly incorporates long-term...
thumbnail
The Nature Conservancy (TNC) has derived climate suitability forecasts for most species of trees and shrubs considered to be ecological dominants of terrestrial Californian habitat types. Our plant projections are compiled as decision support tools to help Conservancy project staff, as well as our external partners, develop the necessary plans, priorities and strategies to successfully adapt to uncertain changes in future climate. In the recently completed Southern Sierra Partnership's 2010 Climate-Adapted Conservation Plan for the Southern Sierra Nevada and Tehachapi Mountains, species and habitat forecasts shown here informed the development of a regional conservation design that explicitly incorporates long-term...
thumbnail
The Nature Conservancy (TNC) has derived climate suitability forecasts for most species of trees and shrubs considered to be ecological dominants of terrestrial Californian habitat types. Our plant projections are compiled as decision support tools to help Conservancy project staff, as well as our external partners, develop the necessary plans, priorities and strategies to successfully adapt to uncertain changes in future climate. In the recently completed Southern Sierra Partnership's 2010 Climate-Adapted Conservation Plan for the Southern Sierra Nevada and Tehachapi Mountains, species and habitat forecasts shown here informed the development of a regional conservation design that explicitly incorporates long-term...
thumbnail
The Nature Conservancy (TNC) has derived climate suitability forecasts for most species of trees and shrubs considered to be ecological dominants of terrestrial Californian habitat types. Our plant projections are compiled as decision support tools to help Conservancy project staff, as well as our external partners, develop the necessary plans, priorities and strategies to successfully adapt to uncertain changes in future climate. In the recently completed Southern Sierra Partnership's 2010 Climate-Adapted Conservation Plan for the Southern Sierra Nevada and Tehachapi Mountains, species and habitat forecasts shown here informed the development of a regional conservation design that explicitly incorporates long-term...
thumbnail
The Nature Conservancy (TNC) has derived climate suitability forecasts for most species of trees and shrubs considered to be ecological dominants of terrestrial Californian habitat types. Our plant projections are compiled as decision support tools to help Conservancy project staff, as well as our external partners, develop the necessary plans, priorities and strategies to successfully adapt to uncertain changes in future climate. In the recently completed Southern Sierra Partnership's 2010 Climate-Adapted Conservation Plan for the Southern Sierra Nevada and Tehachapi Mountains, species and habitat forecasts shown here informed the development of a regional conservation design that explicitly incorporates long-term...
thumbnail
The Nature Conservancy (TNC) has derived climate suitability forecasts for most species of trees and shrubs considered to be ecological dominants of terrestrial Californian habitat types. Our plant projections are compiled as decision support tools to help Conservancy project staff, as well as our external partners, develop the necessary plans, priorities and strategies to successfully adapt to uncertain changes in future climate. In the recently completed Southern Sierra Partnership's 2010 Climate-Adapted Conservation Plan for the Southern Sierra Nevada and Tehachapi Mountains, species and habitat forecasts shown here informed the development of a regional conservation design that explicitly incorporates long-term...
thumbnail
The Nature Conservancy (TNC) has derived climate suitability forecasts for most species of trees and shrubs considered to be ecological dominants of terrestrial Californian habitat types. Our plant projections are compiled as decision support tools to help Conservancy project staff, as well as our external partners, develop the necessary plans, priorities and strategies to successfully adapt to uncertain changes in future climate. In the recently completed Southern Sierra Partnership's 2010 Climate-Adapted Conservation Plan for the Southern Sierra Nevada and Tehachapi Mountains, species and habitat forecasts shown here informed the development of a regional conservation design that explicitly incorporates long-term...
thumbnail
The Nature Conservancy (TNC) has derived climate suitability forecasts for most species of trees and shrubs considered to be ecological dominants of terrestrial Californian habitat types. Our plant projections are compiled as decision support tools to help Conservancy project staff, as well as our external partners, develop the necessary plans, priorities and strategies to successfully adapt to uncertain changes in future climate. In the recently completed Southern Sierra Partnership's 2010 Climate-Adapted Conservation Plan for the Southern Sierra Nevada and Tehachapi Mountains, species and habitat forecasts shown here informed the development of a regional conservation design that explicitly incorporates long-term...
thumbnail
The Nature Conservancy (TNC) has derived climate suitability forecasts for most species of trees and shrubs considered to be ecological dominants of terrestrial Californian habitat types. Our plant projections are compiled as decision support tools to help Conservancy project staff, as well as our external partners, develop the necessary plans, priorities and strategies to successfully adapt to uncertain changes in future climate. In the recently completed Southern Sierra Partnership's 2010 Climate-Adapted Conservation Plan for the Southern Sierra Nevada and Tehachapi Mountains, species and habitat forecasts shown here informed the development of a regional conservation design that explicitly incorporates long-term...
thumbnail
Ken Ferschweiler (CBI) used climate data from the PRISM group (Chris Daly, Oregon State University) at 4kmx4km spatial grain across the conterminous USA to generate a climatology or baseline. He then created future climate change scenarios using statistical downscaling and created anomalies from the Hadley CM3 General Circulation Model (GCM) run through the A2 emission scenario (SRES - special report on emission scenarios published in 2000). To run the MAPSS model (Neilson 1995), average monthly precipitation values were calculated for the period 2045-2060. This dataset shows the standard deviation of the annual precipitation for that period.
thumbnail
Using the simple anomaly method (modifying a historical baseline with differences or ratios projected by General Circulation Models), scientists from the California Academy of Sciences downscaled monthly average temperature and monthly total precipitation from 16 different global circulation models (GCMs). The GCMs were described in the latest Intergovernmental Panel for Climate Change (IPCC 2007) and archived at the WCRP PCMDI (http://www-pcmdi.llnl.gov/ipcc/about_ipcc.php). Monthly maximum temperature and monthly minimum temperatures were downscaled from the only 6 GCMs that archived these particular variables. Scientists used Worldclim v.1.4 (Hijmans et al 2005) at 5 arc-minute (~10km) spatial grain as the current...


map background search result map search result map Standard Deviation of Annual Precipitation (2045-2060) from HadCM3 GCM under A2 scenario (Western USA) Calculated change (Celsius) in seasonal temperature maximum (Spring: 2020-2039), under A2 emission scenario Calculated change (Celsius) in seasonal temperature maximum (Fall: 2080-2099), under B1 emission scenario Calculated change (Celsius) in seasonal temperature minimum (Winter: 2020-2039), under B1 emission scenario Calculated change (mm) in seasonal precipitation average (Winter: 2060-2079), under B1 emission scenario Calculated change (Celsius) in seasonal temperature maximum (Summer: 2020-2039), under A2 emission scenario Calculated change (Celsius) in seasonal temperature maximum (Spring: 2080-2099), under A2 emission scenario Calculated change (Celsius) in seasonal temperature average (Summer: 2020-2039), under A2 emission scenario Calculated change in seasonal precipitation average (Summer: 2080-2099), under A2 emission scenario Calculated change (mm) in seasonal precipitation average (Spring: 2060-2079), under A2 emission scenario Hot, dry scenario forecast of climate suitability for joshua tree (Yucca brevifolia) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 MIROC3.2 A2  projections Warm, dry scenario forecast of climate suitability for spineless horsebrush (Tetradymia canescens) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 MRI-CGCM2.3.2 A2  projections Warm, dry scenario forecast of climate suitability for California black oak (Quercus kelloggii) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 MRI-CGCM2.3.2 A2 projections Warm, dry scenario forecast of climate suitability for Douglas-fir (Pseudotsuga menziesii) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 MRI-CGCM2.3.2 A2  projections Hot, wet scenario forecast of climate suitability for California sycamore (Platanus racemosa) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 IPSL-CM4 A2 projections Warm, dry scenario forecast of climate suitability for sugar pine (Pinus lambertiana) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 MRI-CGCM2.3.2 A2  projections Hot, wet scenario forecast of climate suitability for lodgepole pine (Pinus contorta murrayana) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 IPSL-CM4 A2 projections Hot, dry scenario forecast of climate suitability for mountain mahogany (Cercocarpus betuloides) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 MIROC3.2 A2  projections Hot, wet scenario forecast of climate suitability for common chamise (Adenostoma fasciculatum) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 IPSL-CM4 A2 projections Hot, wet scenario forecast of climate suitability for white fir (Abies concolor) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 IPSL-CM4 A2 projections Hot, dry scenario forecast of climate suitability for joshua tree (Yucca brevifolia) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 MIROC3.2 A2  projections Warm, dry scenario forecast of climate suitability for spineless horsebrush (Tetradymia canescens) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 MRI-CGCM2.3.2 A2  projections Warm, dry scenario forecast of climate suitability for California black oak (Quercus kelloggii) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 MRI-CGCM2.3.2 A2 projections Warm, dry scenario forecast of climate suitability for Douglas-fir (Pseudotsuga menziesii) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 MRI-CGCM2.3.2 A2  projections Hot, wet scenario forecast of climate suitability for California sycamore (Platanus racemosa) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 IPSL-CM4 A2 projections Warm, dry scenario forecast of climate suitability for sugar pine (Pinus lambertiana) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 MRI-CGCM2.3.2 A2  projections Hot, wet scenario forecast of climate suitability for lodgepole pine (Pinus contorta murrayana) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 IPSL-CM4 A2 projections Hot, dry scenario forecast of climate suitability for mountain mahogany (Cercocarpus betuloides) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 MIROC3.2 A2  projections Hot, wet scenario forecast of climate suitability for common chamise (Adenostoma fasciculatum) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 IPSL-CM4 A2 projections Hot, wet scenario forecast of climate suitability for white fir (Abies concolor) in the southern Sierra Nevada and Tehachapi Mountains (California, USA) based upon downscaled 2045-2065 IPSL-CM4 A2 projections Standard Deviation of Annual Precipitation (2045-2060) from HadCM3 GCM under A2 scenario (Western USA) Calculated change (mm) in seasonal precipitation average (Winter: 2060-2079), under B1 emission scenario Calculated change (Celsius) in seasonal temperature average (Summer: 2020-2039), under A2 emission scenario Calculated change in seasonal precipitation average (Summer: 2080-2099), under A2 emission scenario Calculated change (mm) in seasonal precipitation average (Spring: 2060-2079), under A2 emission scenario Calculated change (Celsius) in seasonal temperature maximum (Spring: 2020-2039), under A2 emission scenario Calculated change (Celsius) in seasonal temperature maximum (Fall: 2080-2099), under B1 emission scenario Calculated change (Celsius) in seasonal temperature minimum (Winter: 2020-2039), under B1 emission scenario Calculated change (Celsius) in seasonal temperature maximum (Summer: 2020-2039), under A2 emission scenario Calculated change (Celsius) in seasonal temperature maximum (Spring: 2080-2099), under A2 emission scenario