Re the more detailed model: Both high haze and MCB have a problem, that of 
uneven application and its probable consequences.

Big perturbations in seasonal delivery of moisture to a region result in 
drought and/or deluge. Indeed, one states' drought may be another state's 
deluge, simply because of a detour in the precip pipeline. What can cause a 
detour? 

The current example comes from the land warming twice as fast as the ocean 
surface, the excess high pressure systems over land forcing a rearrangement 
in flow patterns. *Uneven *external forcing is another way, cooling one 
region to create denser air while not doing the same to its neighbors. 
Winds rearrange.

Thus my concern about uneven application of shadows. But shadows have 
penumbrias that vary with the length of the shadow. In our eyes, shadows 
caused by debris floating around can be seen only if the obstruction is 
close to the retina. If the debris is halfway back to the lens, its 
shadow will be too fuzzy to register.

Thus I see *uniform *sunlight reduction as necessary to avoid additional 
drought and deluge, and see the most likely way of achieving uniformity to 
involve sunscreens that are far above the atmosphere.

Of course, success in reducing solar input would do nothing for reducing 
ocean acidification since dimming will not get rid of the growing excess 
of CO2. Air capture of CO2 is the only thing I know that could back us out 
of the danger zone for extreme weather and acidification.

Cheers,
-Bill

On Monday, September 2, 2013 7:49:54 AM UTC-7, Mike MacCracken wrote:
>
> A new paper by myself, Ho-Jeong Shin, Ken Caldeira, and George Ban-Weiss 
> that provides a conceptual look at the notion of polar SRM is available 
> for 
> free download at http://www.earth-syst-dynam.net/4/301/2013/ 
>
> The results suggest that a much more detailed model evaluation of this 
> possible approach to limiting the amplified climate change in high 
> latitudes 
> is merited. 
>
> Mike MacCracken 
>
>
>

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