Hello Oliver,

Thank you for the correction. Apologies! 

I must have muddled-up the authorships of the various papers.

All Best Wishes from yr semi-senile friend,    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 O Morton [omeconom...@gmail.com]
Sent: 02 April 2013 22:25
To: geoengineering@googlegroups.com
Cc: omeconom...@gmail.com
Subject: Re: [geo] SRM and droughts in the Sahel - rectification

Dear John

In my piece I didn't use the term SRM, which I try to avoid, and specifically 
addressed the application of cloud brightening in such a scenario

Best

o

On Tuesday, 2 April 2013 20:09:16 UTC+1, JohnLatham wrote:
SRM and droughts in the Sahel,

Hello Oliver, Jim, Andy, and All,

Good to read the several interesting results and arguments,
hopefully to be developed further.

However, I’d like to request rectification of a common
tendency for the terms SRM, and sometimes climate
geoengineering to be regarded as synonymous with
stratospheric sulphur seeding. The latter is without
question the best known SRM technique, and clearly
has a significant likelihood of proving useful, but
other SRM ideas, including Marine Cloud Brightening
(MCB) and Russell Seitz’s microbubble technique also
have promise and should not be disregarded at this stage.

Bala, Caldeira et al. found that extensive oceanic
cloud seeding via MCB did not significantly reduce
rainfall over land. Jones et al. found that – with
geographically more limited seeding - the occurrence of
rainfall reduction over land via MCB did or did not occur
dependent on the choice of seeding locations. Our own
work on MCB, with larger seeding areas, gave results
similar to those of Bala et al. So it is too sweeping and
also misleading  to say that SRM would cause droughts in
the Sahel.

Although designed to produce global effects MCB, in
principle, could also be used to address much smaller-scale
issues, such as hurricane weakening and coral reef
preservation: and could perhaps prove helpful regarding
the prevention of polar sea-ice loss

Best Wishes,     John.


John Latham
Address: P.O. Box 3000,MMM,NCAR,Boulder,CO 80307-3000
Email: lat...@ucar.edu  or john.l...@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: geoengi...@googlegroups.com [geoengi...@googlegroups.com] on behalf of O 
Morton [omeco...@gmail.com]
Sent: 02 April 2013 14:53
To: geoengi...@googlegroups.com
Subject: [geo] SRM and droughts in the Sahel

Asymmetric forcing from stratospheric aerosols impacts Sahelian rainfall

  *   Jim M. 
Haywood<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#auth-1>,
  *   Andy 
Jones<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#auth-2>,
  *   Nicolas 
Bellouin<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#auth-3>
  *   & David 
Stephenson<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#auth-4>

Nature Climate Change
(2013)
doi:10.1038/nclimate1857

Received
23 October 2012
Accepted
22 February 2013
Published online
31 March 2013
Article tools

The Sahelian drought of the 1970s–1990s was one of the largest humanitarian 
disasters of the past 50 years, causing up to 250,000 deaths and creating 10 
million 
refugees1<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#ref1>.
 It has been attributed to natural 
variability2<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#ref2>,
 
3<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#ref3>,
 
4<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#ref4>,
 
5<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#ref5>,
 
over-grazing6<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#ref6>
 and the impact of industrial emissions of sulphur 
dioxide7<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#ref7>,
 
8<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#ref8>.
 Each mechanism can influence the Atlantic sea surface temperature gradient, 
which is strongly coupled to Sahelian 
precipitation2<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#ref2>,
 
3<http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html#ref3>.
 We suggest that sporadic volcanic eruptions in the Northern Hemisphere also 
strongly influence this gradient and cause Sahelian drought. Using de-trended 
observations from 1900 to 2010, we show that three of the four driest Sahelian 
summers were preceded by substantial Northern Hemisphere volcanic eruptions. We 
use a state-of-the-art coupled global atmosphere–ocean model to simulate both 
episodic volcanic eruptions and geoengineering by continuous deliberate 
injection into the stratosphere. In either case, large asymmetric stratospheric 
aerosol loadings concentrated in the Northern Hemisphere are a harbinger of 
Sahelian drought whereas those concentrated in the Southern Hemisphere induce a 
greening of the Sahel. Further studies of the detailed regional impacts on the 
Sahel and other vulnerable areas are required to inform policymakers in 
developing careful consensual global governance before any practical solar 
radiation management geoengineering scheme is implemented.

Full article at 
http://www.nature.com/nclimate/journal/vaop/ncurrent/full/nclimate1857.html

Blogpost by me at 
http://heliophage.wordpress.com/2013/03/31/climate-geoengineering-for-natural-disasters/

Extract: One implication is that climate geoengineering deployed in just the 
northern hemisphere looks like a very bad idea. Programmes in just the north 
have been considered and studied, in part because of the worries people have 
about something suddenly going wrong in the Arctic, something that needs 
“fixing” quickly. This research makes such approaches look dangerous.
More interesting, and more novel, is the implication that geoengineering might 
be used to avert a Sahelian drought caused by a volcano. If the stratospheric 
sulphates released in a major northern eruption were promptly countered by a 
deliberate release of sulphates into the southern hemisphere, both hemispheres 
would cool. The ITCZ would stay put, and a drought might well be averted. For a 
major drought, that would be a big win. The drought in the 1980s, which 
followed on the 1982 eruption of El Chichon in Mexico, killed about a quarter 
of a million people and turned millions more into refugees.
...
And if the Earth is left to its own devices, such droughts will happen again. 
Last century there were two eruptions that cooled the north and were followed 
by drought in the Sahel. The north is better endowed with volcanoes than the 
south, since the Pacific “ring of fire” is more a horseshoe of fire, with a gap 
in the south but a continuous arc in the north. The odds of at least one 
eruption in the Pinatubo-to-Krakatoa range somewhere of the Earth in this 
century are better than even. The chances of one happening in the north are 
obviously lower; but the odds are hardly long.
If humans had had the technological wherewithal to stop the 1980s Sahel drought 
in its tracks, would people have wanted to use it? It seems likely that there 
would have been a constituency for it, not least in the Sahel. And many of the 
reasons people have for objecting to geoengineering as an inappropriate 
“technical fix” to man-made climate change might apply with rather less force 
if the technology was being used to forestall a natural disaster on a 
continental scale.

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