Articles | Volume 12, issue 2
https://doi.org/10.5194/bg-12-557-2015
https://doi.org/10.5194/bg-12-557-2015
Research article
 | 
29 Jan 2015
Research article |  | 29 Jan 2015

Global analysis of radiative forcing from fire-induced shortwave albedo change

G. López-Saldaña, I. Bistinas, and J. M. C. Pereira

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Cited articles

Aragão, L. E. O. C. and Shimabukuro, Y. E.: The incidence of fire in Amazonian forests with implications for REDD, Science, 328, 1275–1278, 2010.
Australian Government: http://www.bom.gov.au/climate/enso/enlist/, last access: 30 April 2014.
Boisier, J. P., de Noblet-Ducoudré, N., and Ciais, P.: Inferring past land use-induced changes in surface albedo from satellite observations: a useful tool to evaluate model simulations, Biogeosciences, 10, 1501–1516, https://doi.org/10.5194/bg-10-1501-2013, 2013.
Bond, T. C., Streets, D., Yarber, K. F., Nelson, S. M., Woo, J.-H., and Klimont, Z.: A technology-based global inventory of black and organic carbon emissions from combustion, J. Geophys. Res., 109, D14203, https://doi.org/10.1029/2003JD003697, 2004.
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Short summary
Land surface albedo is a key parameter to derive Earth’s surface energy balance. Any changes in the albedo have repercussions in the amount of energy that is retained by the Earth. Fire modifies albedo because it removes vegetation from the land surface; therefore, investigating these changes on a global scale can help to understand the role of fire within the Earth system.
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