Hasn't observational data from Pinatubo constrained this variable
reasonably well? It would be surprising if there was "hidden" cooling of
such magnitude. This would also presumably apply to Tambora, etc. which
have left temperature (measured and proxy) and ash records.
A
On 5 Feb 2018 18:28, "Da
After a volcanic eruption, together with SO2, there’s also a large amount of
ash injected in the upper troposphere that might favor heterogeneous nucleation
against homogeneous. This is mostly the reason why after volcanic eruption a
slight increase in citrus coverage is found.
On the other hand
