Thursday, 31 May 2012: 11:30 AM
Press Room (Omni Parker House)
We use 2005-2009 observations of formaldehyde (HCHO) columns from OMI to infer biogenic isoprene emissions at monthly 1°x1° resolution over the African continent. Our work includes new approaches to remove biomass burning influences using OMI absorbing aerosol optical depth data (to account for transport of fire plumes), as well as anthropogenic influences using AATSR satellite data for small-flame fires (gas flaring). The resulting biogenic HCHO columns (WHCHO) follow closely the distribution of vegetation patterns in Africa. We infer isoprene emission (EISOP) from the local sensitivity S = DWHCHO/DEISOP derived with the GEOS-Chem chemical transport model using two alternate isoprene oxidation mechanisms, and verify the validity of this approach using AMMA aircraft observations over West Africa and a longitudinal transect across central Africa. Displacement error (smearing) is diagnosed by anomalously high values of S and the corresponding data are removed. We find significant sensitivity of S to NOx under low-NOx conditions and fit it to a linear function of tropospheric column NO2 from OMI. We estimate a 40% error in our inferred isoprene emissions for the high-NOx regime (16% of area in Africa retained after filtering), and 40-90% for the low-NOx regime with the error increasing with decreasing NOx. Most of the error is due to smearing. Comparison to the state-of-science MEGAN inventory indicates large overestimates in that inventory for the central African rainforest and adjacent broadleaf trees.
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