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: [email protected] <javascript:>  or 
> [email protected]<javascript:> 
> 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: [email protected] <javascript:> [
> [email protected] <javascript:>] on behalf of O Morton [
> [email protected] <javascript:>] 
> Sent: 02 April 2013 14:53 
> To: [email protected] <javascript:> 
> 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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