A51B-3039:
Deforestation fires versus understory fires in the Amazon Basin: What can we learn from satellite-based CO measurements?

Friday, 19 December 2014
Sara Martinez-Alonso1, Merritt N Deeter1, Helen Marie Worden1, John C Gille1, Cathy Clerbaux2,3 and Maya George3,4, (1)National Center for Atmospheric Research, Boulder, CO, United States, (2)UPMC Univ. Paris 06; Université Versailles St-Quentin, LATMOS-IPSL, Paris, France, (3)CNRS/INSU, LATMOS-IPSL, Paris, France, (4)UPMC Univ. Paris 06; Université Versailles St-Quentin, Paris, France
Abstract:
Deforestation fires in the Amazon Basin abound during the dry season (July to October) and are mostly associated with “slash and burn” agricultural practices. Understory fires occur when fires escape from deforested areas into neighboring standing forests; they spread slowly below the canopy, affecting areas that may be comparable or even larger than clear-cut areas. The interannual variabilities of understory fires and deforestation rates appear to be uncorrelated. Areas burned in understory fires are particularly extensive during droughts. Because they progress below a canopy of living trees, understory fires and their effects are not as easily identifiable from space as deforestation fires.

Here we analyze satellite remote sensing products for CO and fire to investigate differences between deforestation fires and understory fires in the Amazon Basin under varying climatic conditions. The MOPITT (Measurements Of Pollution In The Troposphere) instrument on board NASA's Terra satellite has been measuring tropospheric CO since 2000, providing the longest global CO record to date. IASI (the Infrared Atmospheric Sounding Interferometer) A and B are two instruments on board METOP-A and -B, respectively, measuring, among others, CO since 2006 and 2012. MODIS (the Moderate Resolution Imaging Spectroradiometer) instruments on board NASA's Terra and Aqua satellites provide, among other products, a daily record of fires and their effects since 2000 and 2002, respectively. The temporal extent of all these datasets allows for the detailed analysis of drought versus non-drought years. Initial results indicate that MOPITT CO emissions during the dry season peaked in 2005, 2007, and 2010. Those were draught years and coincide with peaks in area affected by understory fires.