Springtime warming and reduced snow cover from carbonaceous particles

Springtime warming and reduced snow cover from carbonaceous particles

Boreal spring climate is uniquely susceptible to solar warming mechanisms because it has expansive snow cover and receives relatively strong insolation. Carbonaceous particles can influence snow coverage by warming the atmosphere, reducing surface-incident solar energy (<i>dimming&...

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Bibliographic Details
Main Authors:	M. G. Flanner, C. S. Zender, P. G. Hess, N. M. Mahowald, T. H. Painter, V. Ramanathan, P. J. Rasch
Format:	Article
Language:	English
Published:	Copernicus Publications 2009-04-01
Series:	Atmospheric Chemistry and Physics
Online Access:	http://www.atmos-chem-phys.net/9/2481/2009/acp-9-2481-2009.pdf

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