TY - JOUR
T1 - Direct impacts on local climate of sugar-cane expansion in Brazil
AU - Loarie, Scott R.
AU - Lobell, David B.
AU - Asner, Gregory P.
AU - Mu, Qiaozhen
AU - Field, Christopher B.
N1 - Funding Information:
This work was made possible through the support of the Stanford University Global Climate and Energy Project.
PY - 2011/5
Y1 - 2011/5
N2 - The increasing global demand for biofuels will require conversion of conventional agricultural or natural ecosystems. Expanding biofuel production into areas now used for agriculture reduces the need to clear natural ecosystems, leading to indirect climate benefits through reduced greenhouse-gas emissions and faster payback of carbon debts. Biofuel expansion may also cause direct, local climate changes by altering surface albedo and evapotranspiration, but these effects have been poorly documented. Here we quantify the direct climate effects of sugar-cane expansion in the Brazilian Cerrado, on the basis of maps of recent sugar-cane expansion and natural-vegetation clearance combined with remotely sensed temperature, albedo and evapotranspiration over a 1.9 million km 2 area. On a regional basis for clear-sky daytime conditions, conversion of natural vegetation to a crop/pasture mosaic warms the cerrado by an average of 1.55 (1.45-1.65)C, but subsequent conversion of that mosaic to sugar cane cools the region by an average of 0.93 (0.78-1.07)C, resulting in a mean net increase of 0.6C. Our results indicate that expanding sugar cane into existing crop and pasture land has a direct local cooling effect that reinforces the indirect climate benefits of this land-use option.
AB - The increasing global demand for biofuels will require conversion of conventional agricultural or natural ecosystems. Expanding biofuel production into areas now used for agriculture reduces the need to clear natural ecosystems, leading to indirect climate benefits through reduced greenhouse-gas emissions and faster payback of carbon debts. Biofuel expansion may also cause direct, local climate changes by altering surface albedo and evapotranspiration, but these effects have been poorly documented. Here we quantify the direct climate effects of sugar-cane expansion in the Brazilian Cerrado, on the basis of maps of recent sugar-cane expansion and natural-vegetation clearance combined with remotely sensed temperature, albedo and evapotranspiration over a 1.9 million km 2 area. On a regional basis for clear-sky daytime conditions, conversion of natural vegetation to a crop/pasture mosaic warms the cerrado by an average of 1.55 (1.45-1.65)C, but subsequent conversion of that mosaic to sugar cane cools the region by an average of 0.93 (0.78-1.07)C, resulting in a mean net increase of 0.6C. Our results indicate that expanding sugar cane into existing crop and pasture land has a direct local cooling effect that reinforces the indirect climate benefits of this land-use option.
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U2 - 10.1038/nclimate1067
DO - 10.1038/nclimate1067
M3 - Article
AN - SCOPUS:80052202529
SN - 1758-678X
VL - 1
SP - 105
EP - 109
JO - Nature Climate Change
JF - Nature Climate Change
IS - 2
ER -