Hello Andrew et al,

Good to have yr comments Andrew on what was clearly a fine lecture
by David.

It is incorrect, however, to regard SRM as synonymous with 
stratospheric sulphur seeding. The latter is the most discussed
SRM technique, but it is not the only one. They will be synonymous
only if and when all other SRM techniques have been discarded.

All best,    John.



John Latham
Address: P.O. Box 3000,MMM,NCAR,Boulder,CO 80307-3000
Email: lat...@ucar.edu  or john.latha...@manchester.ac.uk
Tel: (US-Work) 303-497-8182 or (US-Home) 303-444-2429
 or   (US-Cell)   303-882-0724  or (UK) 01928-730-002
http://www.mmm.ucar.edu/people/latham
________________________________________
From: geoengineering@googlegroups.com [geoengineering@googlegroups.com] on 
behalf of Andrew Lockley [andrew.lock...@gmail.com]
Sent: 06 August 2013 17:37
To: David Keith; geoengineering
Subject: [geo] 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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