Re: [geo] Re: Asymmetric forcing from stratospheric aerosols impacts Sahelian rainfall : Nature Climate Change

2013-04-06 Thread RAU greg
Thanks Oliver.
Just to clarify from the link, ETC's stated Plan A is:

 pull out and dust off the many practical proposals that have been around 
for decades that would plant trees, push back the Sahara, and support 
sustainable agricultural strategies in the region. And, if that’s not enough in 
a dire emergency, then make sure there is sufficient food aid. 

I'd also suggest throwing in some significant family planning aid.  Apparently 
sufficient food aid will be required because the planted trees will be 
occupying otherwise arable land(?)

In any case sounds like some serious social, bio,  and geo engineering to me, 
which I'm all for carefully considering.  But how is this immune from the same 
criticism as GE with regard to effectiveness and unintended consequences, and 
especially what is the likelihood of achieving Plan A goals given African 
social 
and political instability, not to mention lack of global will? This is why it's 
dangerous at this stage to dismiss any Plan B option until it is proven that it 
is not needed, and why ETC's vehement opposition to such seems so irrational. 
 This is making a big assumption that their true agenda is to maintain earth 
habitability.
-Greg




From: O Morton omeconom...@gmail.com
To: geoengineering@googlegroups.com
Sent: Sat, April 6, 2013 2:27:49 AM
Subject: [geo] Re: Asymmetric forcing from stratospheric aerosols impacts 
Sahelian rainfall : Nature Climate Change

Opps: forgot teh URL of Jim's post 
http://www.etcgroup.org/content/normalizing-geoengineering-foreign-aid

On Monday, 1 April 2013 11:17:28 UTC+1, andrewjlockley  wrote:
Posters note: a discussion of the policy implications of this paper can be 
found 
at http://m.guardian.co.uk/ environment/2013/mar/31/earth- 
cooling-schemes-global-signoff , pasted below.
http://www.nature.com/ nclimate/journal/vaop/ ncurrent/full/nclimate1857. html
Asymmetric forcing from stratospheric aerosols impacts Sahelian rainfall
Jim M. Haywood, Andy Jones, Nicolas Bellouin  David Stephenson
Nature Climate Change (2013) doi:10.1038/ nclimate1857
Received 23 October 2012 
Accepted 22 February 2013 
Published online 31 March 2013
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 refugees. It has been attributed to natural variability, 
over-grazing and the impact of industrial emissions of sulphur dioxide. Each 
mechanism can influence the Atlantic sea surface temperature gradient, which 
is 
strongly coupled to Sahelian precipitation. 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.

Comment piece below, http://m.guardian.co.uk/ environment/2013/mar/31/earth- 
cooling-schemes-global-signoff
Guardian, Sunday 31 March 2013 17.59 BST 
AIan Sample, science correspondent
Earth-cooling schemes need global sign-off, researchers say
World's most vulnerable people need protection from huge and unintended 
impacts 
of radical geoengineering projects.
Controversial geoengineering projects that may be used to cool the planet must 
be approved by world governments to reduce the danger of catastrophic 
accidents, 
British scientists said.Met Office researchers have called for global 
oversight 
of the radical schemes after studies showed they could have huge and 
unintended 
impacts on some of the world's most vulnerable people.The dangers arose in 
projects that cooled the planet unevenly. In some cases these caused 
devastating 
droughts across Africa; in others they increased rainfall in the region but 
left 
huge areas of Brazil parched.The massive complexities associated with 
geoengineering, and the potential for winners and losers, means that some form 
of global governance is essential, said Jim Haywood at the Met Office's 
Hadley 
Centre in Exeter.The warning builds on work by scientists and engineers to 
agree 
a regulatory framework that would ban full-scale geoengineering projects, at 
least temporarily, but allow smaller research projects to go 
ahead.Geoengineering 

Re: [geo] Re: Asymmetric forcing from stratospheric aerosols impacts Sahelian rainfall : Nature Climate Change

2013-04-06 Thread Emily L-B
Hi all,

One thing that perturbed me last year was the etc work at the un fao csm conf 
on food security where they are highly respected in the civil society movement. 
A move in civil society to oppose Genetic engineering was mutated to a call for 
a ban on Geo engineering. 
If this move had been successful, and put to the unfao on behalf of the large 
and wide group of civil society organisations, it could have precipitated 
another un body opposing geo engineering, which I don't think had been the 
intention of most of the organisations being represented. 
I was glad this move was retracted when I challenged it, but I suppose it will 
be tried again.
It is a shame to me that this kind of tricky tactic is being used. 

Civil society will need to be vigilant that they do not end up calling for a 
ban on the wrong thing!

In terms of the paper cited below, an EIA of geo-eng would compare the risk of 
potential impacts from any geo-eng project in the future against the expected 
status in the future, not the current status. Ie if the Sahel is due to dry 
with climate change and is also due to dry with a proposed SRM project, this 
would mean the drying needs to mitigated (ameliorated) whether the SRM takes 
place or not.

In good faith,
Emily.



Sent from my BlackBerry

-Original Message-
From: RAU greg gh...@sbcglobal.net
Sender: geoengineering@googlegroups.com
Date: Sat, 6 Apr 2013 10:31:59 
To: omeconom...@gmail.com; geoengineering@googlegroups.com
Reply-To: gh...@sbcglobal.net
Cc: j...@etcgroup.org
Subject: Re: [geo] Re: Asymmetric forcing from stratospheric aerosols impacts
 Sahelian rainfall : Nature Climate Change

Thanks Oliver.
Just to clarify from the link, ETC's stated Plan A is:

 pull out and dust off the many practical proposals that have been around 
for decades that would plant trees, push back the Sahara, and support 
sustainable agricultural strategies in the region. And, if that’s not enough in 
a dire emergency, then make sure there is sufficient food aid. 

I'd also suggest throwing in some significant family planning aid.  Apparently 
sufficient food aid will be required because the planted trees will be 
occupying otherwise arable land(?)

In any case sounds like some serious social, bio,  and geo engineering to me, 
which I'm all for carefully considering.  But how is this immune from the same 
criticism as GE with regard to effectiveness and unintended consequences, and 
especially what is the likelihood of achieving Plan A goals given African 
social 
and political instability, not to mention lack of global will? This is why it's 
dangerous at this stage to dismiss any Plan B option until it is proven that it 
is not needed, and why ETC's vehement opposition to such seems so irrational. 
 This is making a big assumption that their true agenda is to maintain earth 
habitability.
-Greg




From: O Morton omeconom...@gmail.com
To: geoengineering@googlegroups.com
Sent: Sat, April 6, 2013 2:27:49 AM
Subject: [geo] Re: Asymmetric forcing from stratospheric aerosols impacts 
Sahelian rainfall : Nature Climate Change

Opps: forgot teh URL of Jim's post 
http://www.etcgroup.org/content/normalizing-geoengineering-foreign-aid

On Monday, 1 April 2013 11:17:28 UTC+1, andrewjlockley  wrote:
Posters note: a discussion of the policy implications of this paper can be 
found 
at http://m.guardian.co.uk/ environment/2013/mar/31/earth- 
cooling-schemes-global-signoff , pasted below.
http://www.nature.com/ nclimate/journal/vaop/ ncurrent/full/nclimate1857. html
Asymmetric forcing from stratospheric aerosols impacts Sahelian rainfall
Jim M. Haywood, Andy Jones, Nicolas Bellouin  David Stephenson
Nature Climate Change (2013) doi:10.1038/ nclimate1857
Received 23 October 2012 
Accepted 22 February 2013 
Published online 31 March 2013
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 refugees. It has been attributed to natural variability, 
over-grazing and the impact of industrial emissions of sulphur dioxide. Each 
mechanism can influence the Atlantic sea surface temperature gradient, which 
is 
strongly coupled to Sahelian precipitation. 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