While Alan Robock is right re "the best analog", this does not
mean it is a good analog (because of timescale differences).
This is an unresolved issue -- and some of the studies that have
begun to address this issue are of very limited value because
the GCMs used are very poor at simulating the present-day monsoon.
An a priori requirement for using a GCM in this context is that
it gives a good simulation of the present-day monsoon. I do not
know of any studies that have checked this -- if I'm wrong, please
let me know.

Tropospheric aerosols are not a good or useful analog. The
response to tropospheric aerosols depends on the emissions
pattern. (There are many other reasons why trop aerosols are
a useless analog.)

Tom.

++++++++++++++++++++++++++

Manu Sharma wrote:
> On Tue, Sep 8, 2009 at 3:38 AM, Alan Robock <rob...@envsci.rutgers.edu 
> <mailto:rob...@envsci.rutgers.edu>> wrote:
> 
> 
>     However the effects of volcanic eruptions on the monsoon are not
>     equivocal, and they are the best natural analog we have for SRM
> 
> 
> Perhaps the best analog to SRM is the phenomenon of global dimming and 
> its links [1] with the Ethiopia famine of mid 80's that was caused due 
> to shifting rainfall and killed a million people. 
> 
> It seems to me that this list is in denial of possible adverse impacts 
> of SRM on rainfall patterns.  
> 
> Manu
> 
> 1. Rotstayn and Lohmann, 2002: Tropical Rainfall Trends and the Indirect 
> Aerosol Effect 
> <http://ams.allenpress.com/amsonline/?request=get-abstract&issn=1520-0442&volume=015&issue=15&page=2103>
>  
> 
> 
> 
> > 



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