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This is aggregated results from a run of the MC1 model (MC1_GLOBAL version). The GCM data were downscaled to a half degree grid resolution using an anomaly approach. The baseline historical data was based on CRU TS 2.0 climate. For this map percent change was calculated as: (((Future – Historical)/Historical)*100) Where Future is the average value for 2050-2099 and Historical is the average value for 1950-1999. See related datasets: http://app.databasin.org/app/pages/galleryPage.jsp?id=f7eee62457f641dd85016b7fec7e7c67
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This is aggregated results from a run of the MC1 model (MC1_GLOBAL version). The GCM data were downscaled to a half degree grid resolution using an anomaly approach. The baseline historical data was based on CRU TS 2.0 climate. For this map percent change was calculated as: (((Future – Historical)/Historical)*100) Where Future is the average value for 2050-2099 and Historical is the average value for 1950-1999. See related datasets: http://app.databasin.org/app/pages/galleryPage.jsp?id=f7eee62457f641dd85016b7fec7e7c67
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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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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 is aggregated results from a run of the MC1 model (MC1_GLOBAL version). The GCM data were downscaled to a half degree grid resolution using an anomaly approach. The baseline historical data was based on CRU TS 2.0 climate. For this map percent change was calculated as: (((Future – Historical)/Historical)*100) Where Future is the average value for 2050-2099 and Historical is the average value for 1950-1999. See related datasets: http://app.databasin.org/app/pages/galleryPage.jsp?id=f7eee62457f641dd85016b7fec7e7c67
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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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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 is from the NA8K version of the MC1 model. 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...
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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 is aggregated results from a run of the MC1 model (MC1_GLOBAL version). The GCM data were downscaled to a half degree grid resolution using an anomaly approach. The baseline historical data was based on CRU TS 2.0 climate. For this map percent change was calculated as: (((Future – Historical)/Historical)*100) Where Future is the average value for 2050-2099 and Historical is the average value for 1950-1999. See related datasets: http://app.databasin.org/app/pages/galleryPage.jsp?id=f7eee62457f641dd85016b7fec7e7c67
thumbnail
This is aggregated results from a run of the MC1 model (MC1_GLOBAL version). The GCM data were downscaled to a half degree grid resolution using an anomaly approach. The baseline historical data was based on CRU TS 2.0 climate. For this map percent change was calculated as: (((Future – Historical)/Historical)*100) Where Future is the average value for 2050-2099 and Historical is the average value for 1950-1999. See related datasets: http://app.databasin.org/app/pages/galleryPage.jsp?id=f7eee62457f641dd85016b7fec7e7c67
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This is aggregated results from a run of the MC1 model (MC1_GLOBAL version). The baseline historical data was based on CRU TS 2.0 climate. See related datasets: http://app.databasin.org/app/pages/galleryPage.jsp?id=f7eee62457f641dd85016b7fec7e7c67
thumbnail
This is aggregated results from a run of the MC1 model (MC1_GLOBAL version). The GCM data were downscaled to a half degree grid resolution using an anomaly approach. The baseline historical data was based on CRU TS 2.0 climate. For this map percent change was calculated as: (((Future – Historical)/Historical)*100) Where Future is the average value for 2050-2099 and Historical is the average value for 1950-1999. See related datasets: http://app.databasin.org/app/pages/galleryPage.jsp?id=f7eee62457f641dd85016b7fec7e7c67
thumbnail
This is aggregated results from a run of the MC1 model (MC1_GLOBAL version). The GCM data were downscaled to a half degree grid resolution using an anomaly approach. The baseline historical data was based on CRU TS 2.0 climate. For this map percent change was calculated as: (((Future – Historical)/Historical)*100) Where Future is the average value for 2050-2099 and Historical is the average value for 1950-1999. See related datasets: http://app.databasin.org/app/pages/galleryPage.jsp?id=f7eee62457f641dd85016b7fec7e7c67
thumbnail
This is aggregated results from a run of the MC1 model (MC1_GLOBAL version). The GCM data were downscaled to a half degree grid resolution using an anomaly approach. The baseline historical data was based on CRU TS 2.0 climate. For this map percent change was calculated as: (((Future – Historical)/Historical)*100) Where Future is the average value for 2050-2099 and Historical is the average value for 1950-1999. See related datasets: http://app.databasin.org/app/pages/galleryPage.jsp?id=f7eee62457f641dd85016b7fec7e7c67
thumbnail
This is aggregated results from a run of the MC1 model (MC1_GLOBAL version). The GCM data were downscaled to a half degree grid resolution using an anomaly approach. The baseline historical data was based on CRU TS 2.0 climate. For this map percent change was calculated as: (((Future – Historical)/Historical)*100) Where Future is the average value for 2050-2099 and Historical is the average value for 1950-1999. See related datasets: http://app.databasin.org/app/pages/galleryPage.jsp?id=f7eee62457f641dd85016b7fec7e7c67
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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...


    map background search result map search result map 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 CSIRO Mk3.0 GCM for the SRES A1B 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 CSIRO Mk3.0 GCM for the SRES A2 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 HADCM3 GCM for the SRES A1B 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 A2 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. 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 A1B 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 A2 emission scenario. Average Biomass Consumed by Fire for the United States and Canada Simulated for Historical data for the years 1950-1999 by the MC1 Model Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with MIROC 3.2 medres climate projections under the B1 anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with CSIRO Mk3.0 climate projections under the A1B anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with MIROC 3.2 medres climate projections under the A2 anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with HADCM3 climate projections under the B1 anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with HADCM3 climate projections under the A1B anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with HADCM3 climate projections under the A2 anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with CSIRO Mk3.0 climate projections under the A1B anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with CSIRO Mk3.0 climate projections under the A2 anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with CSIRO Mk3.0 climate projections under the B1 anthropogenic emission scenario at a half degree spatial grain over the globe. Average biomass consumed by fire for years 1950-1999 simulated using the MC1 model with Historic climate at a half degree spatial grain over the globe. 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 CSIRO Mk3.0 GCM for the SRES A1B 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 CSIRO Mk3.0 GCM for the SRES A2 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 HADCM3 GCM for the SRES A1B 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 A2 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. 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 A1B 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 A2 emission scenario. Average Biomass Consumed by Fire for the United States and Canada Simulated for Historical data for the years 1950-1999 by the MC1 Model Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with MIROC 3.2 medres climate projections under the B1 anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with CSIRO Mk3.0 climate projections under the A1B anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with MIROC 3.2 medres climate projections under the A2 anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with HADCM3 climate projections under the B1 anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with HADCM3 climate projections under the A1B anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with HADCM3 climate projections under the A2 anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with CSIRO Mk3.0 climate projections under the A1B anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with CSIRO Mk3.0 climate projections under the A2 anthropogenic emission scenario at a half degree spatial grain over the globe. Percent change in biomass consumed by fire for years 2050-2099 versus 1950-1999 simulated using the MC1 model with CSIRO Mk3.0 climate projections under the B1 anthropogenic emission scenario at a half degree spatial grain over the globe. Average biomass consumed by fire for years 1950-1999 simulated using the MC1 model with Historic climate at a half degree spatial grain over the globe.