Dear Stephen,

I would just like to clarify that your statement is not quite correct 'that all monsoon areas show reduced precipitation in all models'.

The EOS paper states:
'All monsoon areas show reduced precipitation, manifested as reduced numbers of intense precipitation events.'

Precipitation and evaporation are reduced over land for most of the monsoonal regions in summer, however, not for all (Australia) and not for all the models, considering a G1 experiment (very strong forcing). All the models agree on the sign of change for East Asia and North and South America, as found in Tilmes et al., 2013, (in revision). But it is true that months with largest precipitation show a reduction for all monsoonal regions in summer.

The reduction of precipitation in applying SRM is coupled to the fast response, controlled by changes in stability, clouds, stomatal resistance, etc. in the models. I don't see how you would design an idealize experiment that would take the phase of the monsoon into account to improve the reduction of the hydrological cycle?

Simone


Dear Alan

Thank you for an interesting paper.  I note that you used uniform solar
reduction and found that all monsoon areas show reduced precipitation in
all models.

I hope that your next paper will study non-uniform solar reduction
planned according to the phase of the monsoon, the state of the el Nino
la Nina oscillation and sensitive regions.

Stephen

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Emeritus Professor of Engineering Design School of Engineering
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On 14/08/2013 00:14, Alan Robock wrote:
Kravitz, Ben, Alan Robock, and Peter Irvine, 2013:Robust results from
climate model simulations of geoengineering, /Eos/, *94*, 292,
doi:10.1002/2013EO330005.
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Alan Robock

Alan Robock, Distinguished Professor
   Editor, Reviews of Geophysics
   Director, Meteorology Undergraduate Program
   Associate Director, Center for Environmental Prediction
Department of Environmental Sciences              Phone: +1-848-932-5751
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