Abstract
Aerosol particles, such as sulfate aerosols, can act as cloud condensation nuclei (CCN). The CCN spectrum and the water vapor supply in a cloud determine the cloud droplet number concentration (CDNC) and hence the shortwave optical properties of low-level liquid clouds. The capability of anthropogenic aerosols to increase cloud reflectivity and thereby cool the Earth's surface is referred to as the indirect effect of anthropogenic aerosols. To obtain an estimate of this effect on climate, we empirically relate the CDNC, and thus the cloud optical properties, of two general circulation models (GCM) to the sulfate aerosol mass concentration derived from a chemical transport model. -from Authors
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CITATION STYLE
Boucher, O., & Lohmann, U. (1995). The sulfate-CCN-cloud albedo effect: a sensitivity study with two general circulation models. Tellus, Series B, 47 B(3), 281–300. https://doi.org/10.3402/tellusb.v47i3.16048
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