Source: Bulletin of the American Meteorological Society:;2017:;volume( 098 ):;issue: 009:;page 1857
Author(s): Reddington, C. L.; Carslaw, K. S.; Stier, P.; Schutgens, N.; Coe, H.; Liu, D.; Allan, J.; Browse, J.; Pringle, K. J.; Lee, L. A.; Yoshioka, M.; Johnson, J. S.; Regayre, L. A.; Spracklen, D. V.; Mann, G. W.; Clarke, A.; Hermann, M.; Henning, S.; Wex, H.; Kristensen, T. B.; Leaitch, W. R.; Pöschl, U.; Rose, D.; Andreae, M. O.; Schmale, J.; Kondo, Y.; Oshima, N.; Schwarz, J. P.; Nenes, A.; Anderson, B.; Roberts, G. C.; Snider, J. R.; Leck, C.; Quinn, P. K.; Chi, X.; Ding, A.; Jimenez, J. L.; Zhang, Q.
Publisher: American Meteorological Society
Abstract: he largest uncertainty in the historical radiative forcing of climate is caused by changes in aerosol particles due to anthropogenic activity. Sophisticated aerosol microphysics processes have been included in many climate ...
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