@article {800,
	title = {Satellite monitoring of the biomass-burning aerosols during the wildfires of August 2007 in Greece: Climate implications},
	journal = {Atmospheric Environment},
	volume = {45},
	number = {3},
	year = {2011},
	note = {Atmos. Environ.Cited By (since 1996):12Export Date: 13 October 2014CODEN: AENVECorrespondence Address: Kaskaoutis, D.G.; Atmospheric Research Team, Institute for Environmental Research and Sustainable Development, National Observatory of Athens, Lofos Nymphon, P.O. Box 20048, GR-11810 Athens, Greece; email: dkask@meteo.noa.grReferences: OMI algorithm theoretical basis document (2002) Clouds, Aerosols, and Surface UV Irradiance, 3. , ATBD-OMI-03, Version 2.0, P. Stammes, R. 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	pages = {716-726},
	abstract = {Biomass burning and associated emissions of aerosols into the atmosphere play a vital role in atmospheric composition and climate change. During summer of 2007, Greece faced the worst natural disaster recorded in recent decades in terms of human losses, number of fire outbreaks and extent of the estimated burned area (more than 12\% of the total forested areas in Greece). The present study aims at analyzing the impact of these fire events in western Peloponnese on atmospheric aerosol concentrations using satellite data. MODIS-derived Aerosol Optical Depth (AOD), effective radius, Γ{\textellipsis}ngstrΓ{\textparagraph}m exponent, mass concentration, cloud-condensation nuclei (CCN) and OMI Aerosol Index (AI), single scattering albedo, absorption and extinction optical depths were analyzed. MODIS data showed smoke plumes traversing thousands of kilometers southwards influencing the central Mediterranean as well as the north African coastal regions. These thick smoke plumes dramatically affected AOD and aerosol-mass concentrations over the region and altered the microphysical aerosol properties, such as the effective radius and absorption coefficient. Model calculations suggested that the shortwave radiation at the ground was reduced by βΌ50 Wm2, while that at the top of the atmosphere was reduced by βΌ20 Wm2 resulting in atmospheric heating of βΌ30 Wm2 over the areas affected by the smoke plumes. Β{\textcopyright} 2010 Elsevier Ltd.},
	keywords = {Absorption, absorption coefficient, aerosol, aerosol property, article, Atmospheric aerosols, Atmospheric chemistry, Atmospheric composition, atmospheric plume, atmospheric radioactivity, Biomass, Biomass burning, Biomass-burning, Climate change, cloud condensation nucleus, Coastal zones, data set, Deforestation, Environmental Monitoring, fire, Fires, Fluid dynamics, fogo selvagem, forest fire, Forest fires, Greece, Heating, Mediterranean Sea, MODIS, natural disaster, North Africa, optical depth, Peloponnese, plume, priority journal, radiative forcing, Radiative forcings, Radiometers, remote sensing, satellite, satellite data, Satellite imagery, Smoke, space flight, wildfire},
	isbn = {13522310 (ISSN)},
	url = {http://www.sciencedirect.com/science/article/pii/S1352231010008198},
	author = {Kaskaoutis, D. G. and Kharol, S. K. and Sifakis, N. and Nastos, P. T. and Sharma, A. R. and Badarinath, K. V. S. and Kambezidis, H. D.}
}
