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June 09, 2004

NASA Data Shows Deforestation Affects Climate in the Amazon

NASA satellite data are giving scientists insight into how large-scale deforestation in the Amazon Basin in South America is affecting regional climate. Researchers found during the Amazon dry season last August, there was a distinct pattern of higher rainfall and warmer temperatures over deforested regions.

Researchers analyzed multiple years of data from NASA's Tropical Rainfall Measuring Mission (TRMM). They also used data from the Department of Defense Special Sensor Microwave Imager and the National Oceanic and Atmospheric Administration's Geostationary Operational Environmental Satellites.

The study is in a recent American Meteorological Society Journal of Climate. Lead authors, Andrew Negri and Robert Adler, are research meteorologists at NASA's Goddard Space Flight Center (GSFC), Greenbelt, Md. Other authors include Liming Xu, formerly with the University of Arizona, Tucson, and Jason Surratt, North Carolina State University, Raleigh.

"In deforested areas, the land heats up faster and reaches a higher temperature, leading to localized upward motions that enhance the formation of clouds and ultimately produce more rainfall," Negri said.

The researchers caution the rainfall increases were most pronounced in August, during the transition from dry to wet seasons. In this transition period, the effects of land cover, such as evaporation, are not overwhelmed by large- scale weather disturbances that are common during the rest of the year. While the study, based on satellite data analysis, focused on climate changes in the deforested areas, large increases in cloud cover and rainfall were also observed in the naturally un-forested savanna region and surrounding the urban area of Port Velho, Brazil, particularly in August and September.

Recent studies by Dr. Marshall Shepherd cited similar findings, including an average rain-rate increase of 28 percent downwind of urban areas and associated changes in the daily timing of cloud formation and precipitation. He is also a research meteorologist at GSFC.

This research confirmed the Amazon savanna region experienced a shift in the onset of cloudiness and rainfall toward the morning hours. The shift was likely initiated by the contrast in surface heating across the deforested and savanna region.

The varied heights of plants and trees in the region change the aerodynamics of the atmosphere, creating more circulation and rising air. When the rising air reaches the dew point in the cooler, upper atmosphere, it condenses into water droplets and forms clouds.

Negri acknowledged other factors are involved. The savanna in this study is approximately 100 kilometers (62 miles) wide, the perfect size to influence precipitation, such as rain showers and thunderstorms. Earlier studies hypothesized certain land surfaces, such as bands of vegetation 50 to 100 kilometers (31-62 miles) wide in semiarid regions, could result in enhanced precipitation.

This research is in agreement with the recent and sophisticated computer models developed by the Massachusetts Institute of Technology. The models concluded small-scale circulations, including the mixing and rising of air induced by local land surfaces, could enhance cloudiness and rainfall. Many earlier studies that relied on models developed in the 1990s or earlier concluded widespread deforestation of the Amazon Basin would lead to decreased rainfall.

"The effects here are rather subtle and appear to be limited to the dry season. The overall effect of this deforestation on annual and daily rainfall cycles is probably small and requires more study," Negri said. Future research will use numerical models for investigating the linkage between deforested land surface and the cloud-precipitation components of the water cycle.

NASA's Earth Science Enterprise is dedicated to understanding the Earth as an integrated system and applying Earth System Science to improve prediction of climate, weather, and natural hazards using the unique vantage point of space.

For more information and images about this research on the Internet, visit:
http://www.gsfc.nasa.gov/topstory/2004/0603amazondry.html

For information about NASA and agency programs on the internet, visit:
http://wwwgsfc.nasa.gov/

###
Contacts:

Gretchen Cook-Anderson
Headquarters, Washington
Phone: 202/358-0836

Rob Gutro/Mike Bettwy
Goddard Space Flight Center, Greenbelt, Md.
Phone: 301/286-4044

 



Tropical Rainforests

Tropical Rainforests
The tropical rainforest is a hot, moist biome where it rains all year long. It i s known for its dense canopies of vegetation that form three different layers. T he top layer or canopy contains giant trees that grow to heights of about 250 ft or more. This layer of vegetation prevents much of the sunlight from reaching t he ground. The middle layer is made up of vines, smaller trees, ferns, and palms . The bottom layer or floor of the rainforest is covered with wet leaves and lea f litter. CREDIT: NASA Earth Observatory

Looking at Deforestation by Satellite

Looking at Deforestation by Satellite
This black and white image was created from the visible channel of the Geosynch ronous Operational Environmental Satellite (GOES). Deforestated areas are depict ed in gray and white shading over Rondonia, Brazil. The lighter shaded area arou nd Porto Velho is a naturally occurring region of savanna and the urban area. CR EDIT: NASA & NOAA

Comparing the Size of Rondonia's Deforestation to Florida

Comparing the Size of Rondonia's Deforestation to Florida
This GOES image superimposed over the outline of the state of Florida makes it e asier to understand how much land (in gray and white) in Rondonia, Brazil has be en deforested. CREDIT: NASA & NOAA

Land Surface Temperature in Deforested Areas

Land Surface Temperature in Deforested Areas
This image shows the mean surface temperature at noon for August 2000. The outli nes of the deforestation are in white. A warming of 6 K (11 F) is observed over the non-forested regions with respect to the forested regions. CREDIT: NASA

Less Cloud Cover Over Deforested Areas

Less Cloud Cover Over Deforested Areas
This image shows the percent of convective cloud cover over the study area in Br azil during the afternoon hours of August 2000 and 2001. The white outline shows the deforested area, and the blue coloration indicates the smallest percentage of cloud cover, while the yellow color toward the top of the image indicates mor e cloud cover over a savannah. CREDIT: NASA

Rainfall Over Deforested Areas

Rainfall Over Deforested Areas
NASA's Tropical Rainfall Measuring Mission (TRMM) satellite was used to find the percent occurrence of rainfall over the study area. This image was captured dur ing the afternoon hours of August 2000 and 2001. Note the increased frequency of rain (red area) west of, or downwind of the naturally occurring savanna, the ur ban area of Porto Velho, as well as within the large region of deforestation (wh ite outline). CREDIT: NASA

This text derived from http://www.gsfc.nasa.gov/topstory/2004/0603amazondry.html

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