Not exact matches
What about the
cooling in the Maunder Minimum or just after
volcanic episodes?
We have poor direct information on aerosols, but the fossil fuel consumption rate is low, and there is only one major
volcanic episode, so we can assume aerosol
cooling is not significant.
We can see the temperature forcing of El Nino
episodes driven by the surface
cooling from large stratospheric
volcanic events, and some research suggests that near permanent El Nino conditions existed during full glaciation ~ 20kyrs ago.
The
cooling of the stratosphere (lower strato) following each of the
volcanic dusts
episodes may be related to the automatic
cooling of the lower stratosphere when the temperature of the surface increases: this obvious mechanical compensation is described and explained in the old V. A. Belinskii Dynamic Meteorology Ogiz Moscow 1948, The Israël program for scientific translations 1961, 592 pages.