Search Results
condition for the historical experiment ( Taylor et al. 2012 ). The signal of aerosols is very clear over much of the land area from southern Canada southward. The reduced net surface radiation is mainly a product of the increased shortwave optical depth in the CMIP5 models from the preindustrial to the historical run, whose effect is evident during winter as well ( Dirmeyer et al. 2013 ). However, in regions of expanding agriculture like the Great Plains, there is a warm season surface albedo change
condition for the historical experiment ( Taylor et al. 2012 ). The signal of aerosols is very clear over much of the land area from southern Canada southward. The reduced net surface radiation is mainly a product of the increased shortwave optical depth in the CMIP5 models from the preindustrial to the historical run, whose effect is evident during winter as well ( Dirmeyer et al. 2013 ). However, in regions of expanding agriculture like the Great Plains, there is a warm season surface albedo change
