Is there evidence for an aerosol indirect effect during the recent aerosol optical depth decline in Europe?

Abstract

Aerosol indirect effects are some of the largest uncertainties of anthropogenic climate change. To estimate the first aerosol indirect radiative effect (or cloud albedo effect), we analyzed global solar irradiance measurements under completely overcast skies during the recent period of aerosol optical depth decline in Europe. Although measurements from 15 Swiss and 8 northern German sites show clear evidence for an aerosol direct radiative effect under cloud‐free skies, trends of transmitted solar irradiance (SWtran) under overcast skies are ambiguous. Time series from 1981 to 2005 of SWtran for all overcast conditions show slightly negative, but nonsignificant trends. SWtran under overcast conditions with “thick” clouds (SWtran smaller than the long‐term mean) exhibit on average an increasing trend of +0.29 [+0.01 to +0.57] W m−2/decade. The increase of SWtran under “thick” overcast skies, however, is about nine times smaller than the increase under cloud‐free skies. Since cirrus clouds are generally excluded from and low‐level stratiform clouds are more frequently represented by “thick” overcast skies, the slight increase in SWtran may possibly result from a weak aerosol indirect effect. Alternatively, the increase in SWtran may be due to a decreasing trend in low‐level stratiform cloud amount under overcast conditions observed for these sites. We further find that solar irradiance changes caused by decreasing aerosol direct effect and increasing sunshine duration can account for most of the observed increasing all‐sky solar radiation trend. This suggests that the first aerosol indirect effect makes little contribution to surface solar radiation changes over Europe.