000120529 001__ 120529
000120529 005__ 20190316234159.0
000120529 02470 $$2DAR$$a10902
000120529 02470 $$2ISI$$a000248600000002
000120529 0247_ $$2doi$$a10.1029/2006JD008344
000120529 037__ $$aARTICLE
000120529 245__ $$aA satellite- and model-based assessment of the 2003 Russian fires: Impact on the Arctic region
000120529 269__ $$a2007
000120529 260__ $$c2007
000120529 336__ $$aJournal Articles
000120529 520__ $$aIn this paper, we address the issues of the representation of boreal fires in a global chemistry and transport model (GEOS-Chem) as well as their contribution to the Arctic aerosol optical thickness and black carbon (BC) deposition, with a focus on the 2003 Russian fires. We use satellite observations from the MOPITT, POLDER and MODIS sensors to evaluate the model performances in simulating the fire pollution export over the North Pacific. Our results show that aerosol and carbon monoxide (CO) outflow is best reproduced in our model when fire emissions are increased to 72 Tg for CO, 0.5 Tg C for BC, and 5.3 Tg C for organic carbon over the entire fire season; prescribed on a daily basis; and injected up to 4.5 km in July and August. The use of daily, rather than monthly, biomass burning emission inventories improves significantly the representation of the aerosol outflow, but has little impact on CO. The injection of fire emissions above the boundary layer influences both the CO and aerosol columns but only during the late fire season. The model improvements with respect to the standard configuration induce an increase of a factor up to 2 on the aerosol optical thickness and the mass of BC deposited in the Northern Hemisphere. According to our improved simulation, the 2003 Russian fires contributed to 16–33% of the aerosol optical thickness and to 40–56% of the mass of BC deposited, north of 75°N in spring and summer. They contribute to the aerosol optical thickness by more than 30% during the days of Arctic haze events in spring and summer.
000120529 6531_ $$asatellite
000120529 6531_ $$amodel-based assesment
000120529 6531_ $$afire
000120529 6531_ $$aimpact
000120529 700__ $$0240357$$g168560$$aGeneroso, S.
000120529 700__ $$0240356$$g139097$$aBey, I.
000120529 700__ $$aAttie, J.-L.
000120529 700__ $$aBréon, F.M.
000120529 773__ $$j112$$tJournal of Geophysical Research$$kD15302
000120529 8564_ $$uhttp://lmca.epfl.ch/publications.en.php$$zURL
000120529 909C0 $$0252117$$pLMCA
000120529 909CO $$ooai:infoscience.tind.io:120529$$qGLOBAL_SET$$particle
000120529 937__ $$aLMCA-ARTICLE-2008-001
000120529 973__ $$rREVIEWED$$sPUBLISHED$$aEPFL
000120529 980__ $$aARTICLE