If the
aerosols are
dispersed primarily in the Northern Hemisphere, the greater cooling in this hemisphere
can also diminish the summertime heating that drives the northward migration of monsoon winds over Africa up to the Ethiopian highlands where the Blue Nile is supplied with its summer floodwaters.
It hardly takes imagination to posit that while initial
aerosol dimming might depress temperatures, the
aerosols and atmosphere might react in ways that change heat balance in other directions as they
disperse, through stratospheric chemistry, and the fact that, unsurprisingly, there is a difference in
aerosol behaviour depending on day vs night (you can't reduce the sunlight that reaches the south pole on June 23rd....).