Changes in forest cover could affect climate as much as greenhouse gases in some areas
Rhett A. Butler, mongabay.com
December 9, 2005
Deforestation, the growth of forests, and other changes in land cover could produce local temperature changes comparable to those caused by greenhouse gases according to new simulations from the National Center for Atmospheric Research (NCAR).
Using computer simulations, a team of scientists found that changes in vegetation could have a significant impact on land temperatures. In the Amazon, where moisture-producing forest is replaced with less productive pasture, temperatures are expected to rise. The opposite is true in temperate regions where converting midlatitude forests and grasses to cropland tends to act as a cooling influence, because the crops tend to reflect more sunlight and release more moisture into the air. Temperate forests, unlike tropical rainforests, appear to have an overall warming effect since they absorb heat and release relatively little moisture compared with tropical forests.
The research is announced in the NCAR news release that follows.
Changes to land cover may enhance global warming in Amazon, reduce it in midlatitudes
National Center for Atmospheric Research/University Corporation for Atmospheric Research release
Lead author Johannes Feddema (University of Kansas) carried out the modeling work with six coauthors from NCAR while on sabbatical at the center. The team linked NCAR’s Land Surface Model with the global-scale Parallel Climate Model, developed by scientists at NCAR and the U.S. Department of Energy under DOE sponsorship. This marks the first time a simulation of 21st-century warming includes not only interactive ocean and atmosphere components but also changes in land cover caused by agriculture, deforestation, and other human activities.
“The choices humans make about future land use could have a significant impact on regional and seasonal climates,” says Feddema.
Taken together, the impacts of greenhouse gases around the globe should far outweigh the regional effects of land-cover change, according to Feddema. However, the regions with extensive agriculture and deforestation also tend to be highly populated, so the effects of land-cover change are often focused where people live.
“Compared to global warming, land use is a relatively small influence. However, there are regions where it’s really important,” he says.
To bracket a range of possibilities, the group examined two contrasting scenarios for greenhouse emissions and land cover put forth by the Intergovernmental Panel on Climate Change. The more pessimistic scenario assumed that emissions will increase steadily, while the more optimistic scenario assumes rapid gains in energy efficiency.
 Related articles Future forests may absorb more carbon dioxide than current forests | 12/08/05 Forests of the future may grow faster and absorb more carbon in a carbon dioxide enriched environment according to a new study by researchers at the Department of Energy (DOE). Scientists at the DOE’s Oak Ridge National Laboratory and 10 other institutions in the United States and Europe, found that forests grown in plots experimentally enriched with carbon dioxide have higher productivity than forest plots in the current atmosphere. This suggests that future forests may absorb more carbon than forests of today, helping to partially offset rising carbon dioxide levels. Temperate forests may worsen global warming, tropical forests fight higher temperatures | 12/05/2005 Growing a forest might sound like a good idea to combat global warming, since trees draw carbon dioxide from the air and release cool water from their leaves. But they also absorb sunlight, warming the air in the process. According to a new study from the Carnegie Institution’s Department of Global Ecology and Lawrence Livermore National Laboratory, planting forests at certain latitudes could make the Earth warmer. 70 years after logging, forests don’t hold as much carbon as original forests | 12/05/2005 New research out of Ohio State University suggests that following logging, temperate forests take long periods of time to recover their carbon storing capacity. The scientists examined forests of of the upper Great Lakes region, which were 90% logged at the turn of the century, and found that they store only half the carbon the original forests contained. Poor forest management is blamed for the shortfall. Elevated atmospheric CO2 increases soil carbon | 12/05/2005 An article in the current issue of Global Change Biology indicates that soils in temperate ecosystems might contribute more to partially offsetting the effects of rising atmospheric CO2 concentrations than earlier studies have suggested. Vegetation growth in Arctic could add to global warming | 9/8/05 |
The results for the first scenario show that deforestation adds 2°C (3.6°F) or more to surface temperature across the Amazon by 2100. Cooling occurs in the nearby Pacific and Atlantic waters with a weakening of the large-scale Hadley circulation that drives tropical and subtropical climate. In turn, moisture penetrates further north and produces a cooling, moistening influence across the U.S. Southwest during that region’s summer monsoon.
While deforestation acts to warm the tropics by replacing forests with less productive pasture, converting midlatitude forests and grasses to cropland tends to act as a cooling influence, because the crops tend to reflect more sunlight and release more moisture into the air. Feddema and colleagues found that expanded agriculture tends to counteract global warming by as much as 50% across parts of North America, Europe, and Asia. In Canada and Russia, boreal forests add to regional warming as they spread north over time.
Although the two IPCC scenarios studied agree on the impacts of land use in some regions, they produce contrasting results in others. The next step for Feddema and colleagues is to utilize the NCAR-based Community Climate System Model, which will provide higher-resolution results. They also hope to incorporate the effects of urban areas on regional climate.
“Our results suggest that more research efforts should be devoted to producing viable scenarios of land-cover change in the future,” says coauthor Linda Mearns, director of the NCAR Institute for the Study of Society and Environment. “We very much hope that other climate modeling centers perform experiments similar to ours.”
“The purpose of our project is to include human processes more directly in global climate models,” adds Feddema. “This is the first step.”
The simulations were supported by the DOE, the National Science Foundation, and the University of Kansas. NSF is NCAR’s primary sponsor. Opinions, findings, conclusions, or recommendations expressed in this publication do not necessarily reflect the views of NSF.
This story includes a modified news release (“Changes to land cover may enhance global warming in Amazon, reduce it in midlatitudes”) from the National Center for Atmospheric Research/University Corporation for Atmospheric Research
