When analyzed together with
the aerosol loading over the same area at the same time, the outcome, says Koren, was a «textbook demonstration of the invigoration effect» of added aerosols on clouds.
Not exact matches
The Hadcm3 model has calculated the largest increase in temperature which may be attributed to the reduction of
aerosol load (40 %)
over the period 1990 - 1999 somewhere in NE Europe, other models do that more in Southern Europe.
The localized cooling between about 1950 and 1970
over industrial regions such as Europe and Southeast Asia, where anthropogenic sulfate
aerosol loadings were high, is consistent with the expected cooling effect of sulfate
aerosols.
The first part of this thesis compares the seasonal cycle and interannual variability of Advanced Very High Resolution Radiometer (AVHRR) and Total Ozone Mapping Spectrometer (TOMS) satellite retrievals
over the Northern Hemisphere subtropical Atlantic Ocean, where soil dust
aerosols make the largest contribution to the
aerosol load, and are assumed to dominate the variability of each data set.
Here's a paper (Sutton et al GRL 2007) Note, however, that they used 1 % pa CO2 runs and realistic
aerosol loading will (I expect) reduce this ratio by primarily cooling
over land.
There is also a fairly large increase in modelled sulfate
load over the Tropical North Atlantic from about 1960, which is presumably the main cause of modelled present day strong
aerosol forcing off the West African coast, as depicted in Booth et al. figure 4b.