Andy

Sorry but I do not find this an effective way to debate these topics, 
particularly in this case when I am responding to a summary that does not 
accurately reflect what I said. I would rather put the energy into writing a 
paper or discussing these topics in smaller groups. I would be very happy to 
chat more over the next couple days.

I do think there is some utility in this blog but I do not now look at it 
routinely. It may be that I am just old-fashioned, but I find that the 24-hour 
blogging culture tends to overemphasize emphasize spurious disagreement fueled 
by jumbled factoids in a way that makes it hard to identify substantive 
disagreements about facts and values. This is particularly true in a 
single-threaded format like this.

But this may simply be my old-fashioned taste: many folks do contribute smart, 
relevant and thoughtful posts and are clearly having a lot of fun doing it.

Cheers,
David


From: Andrew Lockley [mailto:[email protected]]
Sent: Tuesday, August 6, 2013 10:38 AM
To: Keith, David; geoengineering
Subject: Response to D Keith lecture at Harvard


David

Below are a few questions and comments from your interesting lecture today. I'm 
copying to the Google group to invite wider comment on the important issues 
your raised.

It would be great to hear any comments you have, if you are able to respond.

Thanks

A

Ramp up
You considered a linear and shallow ramp up of SRM intervention. This perhaps 
works particularly well for a linear climate response. Should we not instead be 
looking at more rapid temperature reductions, to reduce risks of crossing 
tipping points (Greenland, permafrost, etc)?

Health impacts
You assume quantifiable health impacts from particulate rain out. However, the 
aerosol rain out would be well distributed, with much occurring in depopulated 
areas. Are the health impacts of distributed particulates comparable to those 
from concentrated loading patterns (eg focussed on harbours and cities)?  I 
assume the calculated risks were derived from these concentrated loading 
patterns. Will the health risks  be reduced because rain out will likely mix 
with, or condensate, raindrops -  hence diluting them to destruction.

Delivery mechanism
Previously you considered homogeneous condensation of H2SO4, and today you 
discussed in-situ high-altitude combustion of solid S to release SO2. In 
response to my verbal question, you stated that particle size distribution 
issues only kick in around 'a few' MT. However, having a constant delivery 
mechanism reduces the risk of 'nasty surprises' on switching, despite increased 
lofting costs in earlier stages. Is there an argument for 'starting as you mean 
to carry on'?

Distribution pattern
Particularly with high aerosol loads, there may be advantages to a temporally 
bound injection regime (when using precursor gases instead of direct 
particulate injection). This is due to the benefit of constrained particle 
growth. (See reference below) Does a potential requirement for a 
temporally-concentrated injection regime mean that the use of aircraft becomes 
problematic from a cost point of view? EG to do all the injection in a month 
per year, you'd likely need up to 12x as many aircraft.
You also considered the spatial distribution pattern. A 30N to 30S injection 
regime may take advantage of the Brewer Dobson circulation. However, is there 
not a risk of particle size growth and rain out. See
Heckendorn et al ( http://m.iopscience.iop.org/1748-9326/4/4/045108 ), who 
discussed particle growth, and I recall this paper may also have discussed 
spatial (vertical and latitude) and temporal distribution patterns, and 
advocated a more spatially varied injection regime.

Smart particles
You touched on the concept of 'smart particles'. Is there a risk that these can 
be weaponised to make a solar concentrator, capable of burning buildings on the 
ground?

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