16) The main cloud bands move more equatorward to regions where insolation is more intense and total global albedo increases once more due to longer lines of air mass mixing. (newclimatemodel.com)
6) The main cloud bands move more poleward to regions where solar insolation is less intense and total global albedo declines via a reduction in global cloud cover due to shorter lines of air mass mixing. (newclimatemodel.com)
3) The global albedo changes necessary to produce observed climate variability and the changes in solar energy input to the oceans can be explained by the latitudinal shifts (beyond normal seasonal variation) of all the air circulation systems and in particular the net latitudinal positions of the three main cloud bands namely the two generated by the mid latitude jet streams plus the Inter Tropical Convergence Zone (ITCZ). (newclimatemodel.com)