[geo] Re: tropospheric aerosol use

2012-03-18 Thread Nathan Currier
Thanks for the responses - though what I had in mind was actually more
in line with the tenor of Mike's latest comments about the 6-to-1
lifetime ratio for arctic sulfur SRM, stratospheric vs. tropospheric,
etc.

David’s early article is very impressive for how much it adumbrated
the current public discourse on geoengineering, though at the same
time, a bit of misunderstanding about what I was intending to ask –
and I was probably not expressing myself very well – possibly
underscores how something really has been shifting lately within the
geoengineering world, too. What I meant about tropospheric sulfur
injections was entirely in the newer sense of a more ‘localized
geoengineering’, which has been getting attention here in this group
lately (so much so that I forgot to mention what I meant in my
question), and which I think makes a world of difference in
considering its use. In a sense, stratospheric injections can’t be
effectively localized, and this newer local thinking - coming in
response to events on the ground - might bring out new ways of
considering tropospheric sulfur versus stratospheric sulfur, as Mike’s
comments from earlier today in that other thread show, and the issue
of sulfur's dangers, which are the main point in David's comments, are
clearly altered by the reduced scale of use.

In the BBC article that Andrew has just posted, Pete Wadhams is
talking about AMEG’s plans should the methane situation there
deteriorate a good deal further (which seems almost certain, if I had
to guess), and they focus on MCB alone. I think I had first seen
mention here of tropospheric sulfur injections in this context from
Mike, and this really took off in my imagination when I by chance
shortly afterward saw some work involving Eileen Matthews (Gauci et
al) showing how strongly just ordinary levels of acid rain will impede
methanogenesis in wetlands, with strong reductions, like 40% or so,
which play out through considerably longer time periods than the brief
atmospheric lifetime of the aerosols.

I think study of this combined methane-SRM effect for tropospheric
sulfur injection should really be done. Curiously, David, in what you
sent me, the abstract on intercontinental effects of SO2 don’t suggest
that Russia is particularly bad for that particular concern, less so
than Europe, for example. And curiously, I might add, despite what you
just wrote, in your early paper you had actually listed stratospheric
injections as more dangerous than tropospheric (although I assume for
entirely different reasons, related then to ozone loss concerns, etc).

But this is really something very different now from all that, or from
Budyko’s early comparisons of efficiency, lifetimes, etc. We’re
talking about a very limited area for treatment, almost nothing by
comparison with plans to geoengineer a global –1W/m2 or some such
thing. And currently one third of the land area of China is
experiencing acid rain, I recently read. How could it be acceptable to
add copious amounts of sulfur to one of the most densely populated
parts of the planet, which will clearly lead to considerable mortality
and sickness, and unacceptable to add any sulfur at all to a mostly
unpopulated area around the mouth of the Lena river, where there are
globally dangerous submarine methane hotspots and lots of wetlands,
thermokarst lakes, etc, emitting plenty of methane right nearby?

Could one not hope that there might be some effect from the sulfur on
the shelf floor itself, too? (I've cc-ed Vincent Gauci on this, and
maybe he could easily answer that).  After all, it is a complex
picture at the ESAS, probably with older methane stores and current
methanogenesis from thawing submarine permafrost driving the ambient
methane levels' rise there together. Indeed, the isotopic analysis
thus far points more to contemporary methane, which might
realistically be capable of being impacted – so it might be possible
to help push back against this spiraling situation in multiple
respects at once simply through tropospheric emissions of sulfur. That
is, with pinpointed and targeted ground level injections, there’s the
scattering effect – less efficient than in the stratosphere but still
certainly present – then the indirect effect (its ‘Twomey’ effect),
and then its methane-suppressing effects as well. Someone should try
to roughly calculate what might be possible totals in terms of local –
RF, given different options for release area, amount of release per
hour, estimates of what the wetlands near the hotspots are currently
emitting, etc.

Further, since it sounds from the BBC article as though MCB is the
main thing being considered by AMEG right now, another question of
mine would be for John, and that is how would the interaction of such
ground-level sulfur injection and the MCB compare to the rather
synergistic situation of MCB with stratospheric injections? (I noticed
that Wadhams is proposing MCB down around the Diomedes, though). I
realize that’s probably 

Re: [geo] Source on SRM causing warming

2012-03-18 Thread Andrew Lockley
For clarity, I've never used or advocated this 10C figure, just explained
where I think it was from.

I don't think CCN manipulation in the arctic is expected. From what I
understand It's proposed that any local cooling will be at lower latitudes,
on water headed to the arctic.

It's been pointed out to me that arctic geoengineering alone will risk
monsoon failure by moving the ITCZ. Perhaps one of the climatic modelers
can confirm?

A
 On Mar 18, 2012 1:29 AM, Mike MacCracken mmacc...@comcast.net wrote:

  The Robock et al simulations of an Arctic injection found that the
 lifetime of particles in the lower Arctic stratosphere was only two months.
 In that one would only need particles up during the sunlit season (say
 three months, for only really helps after the sea ice surface has melted
 and the sun is high in the sky). During the relatively calm weather of
 Arctic summer, the lifetime of tropospheric sulfate, for example—and quite
 possibly sea salt CCN--emitted above the inversion is likely 10 days or so.
 It is not at all clear to me that the 6 to 1 or so lifetime advantage of
 the lower stratosphere is really worth the effort to loft the aerosols.

 And on the temperature rise in the polar stratosphere, I would hope any
 calculation of the effects of the sulfate/dust injection only put it in
 during the sunlit season—obviously, there would be no effect on solar
 radiation during the polar night, so, with a two month lifetime of aerosols
 there, it makes absolutely no sense to be lofting anything for about two
 thirds of the year. And so likely no effect on winter temperatures
 (although warming the coldest part of the polar winter stratosphere might
 well help to prevent an ozone hole from forming).

 So, I think a tropospheric brightening approach is likely the better
 option. Whether it can be done with just CCN or might also need sulfate
 seems to me worth investigating (what one needs may well be not just cloud
 brightening, but also clear sky aerosol loading).

 Best, Mike

 *

 On 3/17/12 8:41 PM, Ken Caldeira kcalde...@carnegie.stanford.edu
 wrote:

 That is just misleading.  The third attachment is a top-of-atmosphere
 radiation balance on the email I am responding to shows shortwave radiation.

 The attached figure shows the corresponding temperature field from the
 same simulation for the same time period.  Note Arctic cooling.

 Also, we should not focus on individual regional blobs of color in an
 average of a single decade from a single simulation.

 The paper these figures came from is here:
 http://www.atmos-chem-phys.net/10/5999/2010/acp-10-5999-2010.pdf

 ___
 Ken Caldeira

 Carnegie Institution Dept of Global Ecology
 260 Panama Street, Stanford, CA 94305 USA
 +1 650 704 7212 kcalde...@carnegie.stanford.edu
 http://dge.stanford.edu/labs/caldeiralab  @kencaldeira

 *YouTube:
 * http://www.youtube.com/watch?v=a9LaYCbYCxo Climate change and the
 transition from coal to low-carbon electricity 
 http://www.youtube.com/watch?v=a9LaYCbYCxo
 Crop yields in a geoengineered climate 
 http://www.youtube.com/watch?v=-0LCXNoIu-c




 On Sat, Mar 17, 2012 at 1:31 PM, Andrew Lockley and...@andrewlockley.com
 wrote:


 Hi

 Here are some model outputs which Stephen sent me. These appear to show
 localized arctic warming in geoengineering simulations. This could be due
 to winter effects.

 I assume this is the source for the controversial figure in the BBC quote

 A



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Re: [geo] Re: We are top story on BBC environmental news

2012-03-18 Thread John Nissen
Hi Josh,

Before commenting on your question, I need to explain the recent activities
of AMEG, a group whose position Professor Salter supports.  Professor Peter
Wadhams and I gave evidence, on behalf of AMEG, to the first of two
hearings of the Environment Audit Committee (AEC) inquiry Protecting the
Arctic on 21st February.  We were given an opportunity to make a further
presentation of the AMEG case to the All-Party Parliamentary Climate Change
Group (APPCCG) on 13th March, i.e. last Tuesday, where we were joined by
Professor Salter and journalist, Jon Hughes.  Richard Black, of the BBC,
reported on the APPCCG meeting [1].  The second hearing of EAC was on 14th
March, at which the Met Office gave oral evidence, reported by the Guardian
[2] [3].

I am a great supporter of Stephen's cloud brightening approach, and we both
want it deployed as soon as possible.   Stephen is a supporter of Peter
Wadhams and the AMEG position, that geoengineering is urgently needed to
try to save the sea ice.  The sea ice is disappearing extraordinarily
rapidly as Richard Black reports from the APPCCG presentation [4] and you
can see from the graph of sea ice volume decline [5].  One can see from
this graph that, if we are unlucky and the sea ice volume declines this
summer as much as it did between the minimum in 2009 and 2010, i.e. ~2000
km-3, then it would halve the sea ice left this September.  Such a collapse
in volume is likely to be accompanied by a collapse in sea ice extent.
With less heat flux going into melting the ice, there could be a sudden
spurt in Arctic warming, making a reversal to restore the ice, by
geoengineered cooling, extremely difficult if not impossible.

A point of no return could be reached this summer.  Therefore we are in a
desperate situation.  As I pointed out to the EAC, beggars can't be
choosers, so we have to use available means to try and cool the Arctic
quickly, and avoid any actions which could make this daunting task more
difficult.  Thus for example, we urged EAC to recommend an immediate
halting of Arctic drilling because escape of methane (the main constituent
of natural gas) would have a warming effect on the Arctic.

Stephen was not at the EAC hearing on 21st February, but afterwards made it
clear to the committee that he supported the AMEG position.   Just before
the hearing, the committee had received an email [6] from some
geoengineering experts recommending research but suggesting that
development and deployment of geoengineering techniques was premature, thus
undermining the AMEG position.  The signatories had apparently included
Stephen Salter, but this was a mistake - he had not agreed to the wording
that was used.

On the other hand the APPCCG meeting last week was an opportunity for
Stephen to trumpet the advantages of cloud brightening over what is seen as
its main rival.  So I think you should take Stephen's strong statement as a
warning that, if used at the wrong time and place, stratospheric aerosols
could be counterproductive.  I'll let him produce his detailed argument,
which he submitted as written evidence to the EAC hearing.   We will no
doubt have to use a combination of techniques and measures to deal with the
desperate situation in the Arctic.

Cheers,

John

 [1] http://www.bbc.co.uk/news/science-environment-17400804

[2]
http://www.guardian.co.uk/business/2012/mar/14/oil-spill-arctic-exploration

[3]
http://www.guardian.co.uk/environment/2012/mar/14/met-office-arctic-sea-ice-loss-winter

[4]  Analysis from the University of Washington, in Seattle, using ice
thickness data from submarines and satellites, suggests that Septembers
could be ice-free within just a few years.

[5] http://neven1.typepad.com/.a/6a0133f03a1e37970b0153920ddd12970b-pitaken from
http://neven1.typepad.com/blog/2011/10/piomas-september-2011-volume-record-lower-still.html

[6] Email from Hue Coe to members of the AEC, 21st Feb, forwarded to the
geoengineering group on 23rd by Andrew Lockley.

---

On Sat, Mar 17, 2012 at 5:55 PM, Josh Horton joshuahorton...@gmail.comwrote:

 The idea of putting dust particles into the stratosphere to reflect
 sunlight, mimicking the cooling effect of volcanic eruptions, would in fact
 be disastrous for the Arctic, said Prof Salter, with models showing it
 would increase temperatures at the pole by perhaps 10C.

 That's a pretty strong statement--what's the evidence for this?

 Josh Horton



 On Saturday, March 17, 2012 6:25:22 AM UTC-4, Andrew Lockley wrote:

 http://www.bbc.co.uk/news/**science-environment-17400804http://www.bbc.co.uk/news/science-environment-17400804

 Climate 'tech fixes' urged for Arctic methane

 By Richard Black Environment correspondent, BBC News

 An eminent UK engineer is suggesting building cloud-whitening towers in
 the Faroe Islands as a technical fix for warming across the Arctic.

 Scientists told UK MPs this week that the possibility of a major methane
 release triggered by melting Arctic ice constitutes a planetary 

RE: [geo] Re: We are top story on BBC environmental news

2012-03-18 Thread John Latham
Hello John Nissen and All,

John N says:- 

   Just before the hearing, the committee had received an email [6] from 
some 
geoengineering experts recommending research but suggesting that development 
and deployment of geoengineering techniques was premature, thus undermining 
the AMEG position.

I was one of the signatories that John alluded to. I believe that each one of 
us feel 
it shameful and dangerous that that  research into promising SRM ideas has not 
been significantly financially supported. The major stages of the required 
research 
involve modelling, resolution of all technological questions, examination of - 
and 
international agreement on - possible adverse consequences of deployment, and 
the execution of (in the case of MCB, for example), of a limited area 
field-testing
experiment. If the required funding was available now I think I think all the 
above 
goals could be achieved in 5 years, perhaps even 3. 

At the moment these goals are far from being achieved. An attempt to 
successfully
deploy now any likely SRM  technique would be doomed to failure. The 
technological
questions have not been fully resolved - so it would not work - and there would 
be 
- in my opinion - an international outcry against deployment. 

We would be shooting ourselves in the foot, I think, if we tried to deploy now. 
If 
there was a major failure - which is likely - the response could be such as to 
prohibit 
further SRM work for a long time.We need to engage in crash programmes of 
research 
now, which means that we need immediately to obtain the required funding. [How, 
I
dont know, I'm afraid].

All Best,  John (Latham)

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 John Nissen [johnnissen2...@gmail.com]
Sent: Sunday, March 18, 2012 12:40 PM
To: joshuahorton...@gmail.com
Cc: geoengineering; John Nissen; P. Wadhams; Stephen Salter; JON HUGHES; Albert 
Kallio
Subject: Re: [geo] Re: We are top story on BBC environmental news

Hi Josh,

Before commenting on your question, I need to explain the recent activities of 
AMEG, a group whose position Professor Salter supports.  Professor Peter 
Wadhams and I gave evidence, on behalf of AMEG, to the first of two hearings of 
the Environment Audit Committee (AEC) inquiry Protecting the Arctic on 21st 
February.  We were given an opportunity to make a further presentation of the 
AMEG case to the All-Party Parliamentary Climate Change Group (APPCCG) on 13th 
March, i.e. last Tuesday, where we were joined by Professor Salter and 
journalist, Jon Hughes.  Richard Black, of the BBC, reported on the APPCCG 
meeting [1].  The second hearing of EAC was on 14th March, at which the Met 
Office gave oral evidence, reported by the Guardian [2] [3].

I am a great supporter of Stephen's cloud brightening approach, and we both 
want it deployed as soon as possible.   Stephen is a supporter of Peter Wadhams 
and the AMEG position, that geoengineering is urgently needed to try to save 
the sea ice.  The sea ice is disappearing extraordinarily rapidly as Richard 
Black reports from the APPCCG presentation [4] and you can see from the graph 
of sea ice volume decline [5].  One can see from this graph that, if we are 
unlucky and the sea ice volume declines this summer as much as it did between 
the minimum in 2009 and 2010, i.e. ~2000 km-3, then it would halve the sea ice 
left this September.  Such a collapse in volume is likely to be accompanied by 
a collapse in sea ice extent.  With less heat flux going into melting the ice, 
there could be a sudden spurt in Arctic warming, making a reversal to restore 
the ice, by geoengineered cooling, extremely difficult if not impossible.

A point of no return could be reached this summer.  Therefore we are in a 
desperate situation.  As I pointed out to the EAC, beggars can't be choosers, 
so we have to use available means to try and cool the Arctic quickly, and avoid 
any actions which could make this daunting task more difficult.  Thus for 
example, we urged EAC to recommend an immediate halting of Arctic drilling 
because escape of methane (the main constituent of natural gas) would have a 
warming effect on the Arctic.

Stephen was not at the EAC hearing on 21st February, but afterwards made it 
clear to the committee that he supported the AMEG position.   Just before the 
hearing, the committee had received an email [6] from some geoengineering 
experts recommending research but suggesting that development and deployment of 
geoengineering techniques was premature, thus undermining the AMEG position.  
The signatories had apparently included Stephen Salter, but this was a mistake 
- 

Re: [geo] Re: We are top story on BBC environmental news

2012-03-18 Thread Stephen Salter

Josh

My source is figure 2b of Jones Hayward Boucher Kravtitz and Robock of 
June 2010 in Atmospheric  Chemistry and Physics They reckon 5 million 
tonnes year will do a general world-wide coolling of 1.1 watt/m2 but 
will work the wrong way over the Arctic giving a warming of 4 to10 
watts/m2 above the methane releasing areas where last year there was a 
step up by a factor of 20.  I was caeful to say 10 watts not 10 C but 
other speakers had been talking in temperature which are already scary 
enough. Jon Egil Kristjansson at Oslo has some confirming results.   Can 
anyone predict the effects of a spike of methane lasting two years?  I 
will put figure 2b in my next email incase your spam filters disapprove 
of it.


The reason  for intense Arctic warming might be that in the summer 
stratospheric aerosol scatters energy from solar rays that might just 
have missed the earth and half the scattering is downwards.  At the 
summer solstice there is more solar energy hitting the North pole than 
the equator.


In winter there could be about 200 watts per square metre of longwave 
radiation trying to get out from the Arctic to deep space.  Aerosol at 
any height cannot tell up from down and will reflect some back like a 
blanket.  Low level cloud brightening would have exactly the same 
blanketing effect but the shorter life means that we have a much better 
chance of not getting any salt residues that far north.  Intercepting 
heat going from the tropics to the poles can be done anywhere  along the 
route. Cloud brightening anywhere away from the Arctic will cool it.  
Short life and local control is a very attractive feature.  Patchy and 
quick good, promiscuous and slow bad.


The cloud brightening community would greatly appreciate some 
distinction between our own low-level highly controlled activities and 
higher level, uncontrolled more acidic ones.


See if there is anything in your spam tray.

Stephen








Josh Horton wrote:
The idea of putting dust particles into the stratosphere to reflect 
sunlight, mimicking the cooling effect of volcanic eruptions, would in fact 
be disastrous for the Arctic, said Prof Salter, with models showing it 
would increase temperatures at the pole by perhaps 10C.


That's a pretty strong statement--what's the evidence for this?

Josh Horton



On Saturday, March 17, 2012 6:25:22 AM UTC-4, Andrew Lockley wrote:
  
http://www.bbc.co.uk/news/science-environment-17400804 


Climate 'tech fixes' urged for Arctic methane

By Richard Black Environment correspondent, BBC News

An eminent UK engineer is suggesting building cloud-whitening towers in 
the Faroe Islands as a technical fix for warming across the Arctic.


Scientists told UK MPs this week that the possibility of a major methane 
release triggered by melting Arctic ice constitutes a planetary emergency.


The Arctic could be sea-ice free each September within a few years.

Wave energy pioneer Stephen Salter has shown that pumping seawater sprays 
into the atmosphere could cool the planet.


The Edinburgh University academic has previously suggested whitening 
clouds using specially-built ships.


At a meeting in Westminster organised by the Arctic Methane Emergency 
Group (Ameg), Prof Salter told MPs that the situation in the Arctic was so 
serious that ships might take too long.


I don't think there's time to do ships for the Arctic now, he said.

We'd need a bit of land, in clean air and the right distance north... 
where you can cool water flowing into the Arctic.


Favoured locations would be the Faroes and islands in the Bering Strait, 
he said.


Towers would be constructed, simplified versions of what has been planned 
for ships.


In summer, seawater would be pumped up to the top using some kind of 
renewable energy, and out through the nozzles that are now being developed 
at Edinburgh University, which achieve incredibly fine droplet size.


In an idea first proposed by US physicist John Latham, the fine droplets 
of seawater provide nuclei around which water vapour can condense.


This makes the average droplet size in the clouds smaller, meaning they 
appear whiter and reflect more of the Sun's incoming energy back into 
space, cooling the Earth.


On melting ice

The area of Arctic Ocean covered by ice each summer has declined 
significantly over the last few decades as air and sea temperatures have 
risen.


For each of the last four years, the September minimum has seen about 
two-thirds of the average cover for the years 1979-2000, which is used a 
baseline. The extent covered at other times of the year has also been 
shrinking.


What more concerns some scientists is the falling volume of ice.

Analysis from the University of Washington, in Seattle, using ice 
thickness data from submarines and satellites, suggests that Septembers 
could be ice-free within just a few years.


Data for September suggests the Arctic Ocean could be free of sea ice in a 
few years


In 2007, the water [off northern 

Re: [geo] Source on SRM causing warming

2012-03-18 Thread Stephen Salter

Mike

I had thought that the plan was stratospheric aerosol to be released at 
low latitudes and would slowly migrate to the poles where is would 
gracefully descend.  If you can be sure that it will all have gone in 10 
days then my concerns vanish.  But if the air cannot get through the 
water surface how can the aerosol it carries get there?  It will form a 
blanket even if it is a very low one.


A short life would mean  that we do not have to worry about methane 
release.  But can we do enough to cool the rest of the planet?  Perhaps 
Jon Egil can tell us about blanket lifetime.


Stephen

Mike MacCracken wrote:

The Robock et al simulations of an Arctic injection found that the lifetime
of particles in the lower Arctic stratosphere was only two months. In that
one would only need particles up during the sunlit season (say three months,
for only really helps after the sea ice surface has melted and the sun is
high in the sky). During the relatively calm weather of Arctic summer, the
lifetime of tropospheric sulfate, for example‹and quite possibly sea salt
CCN--emitted above the inversion is likely 10 days or so. It is not at all
clear to me that the 6 to 1 or so lifetime advantage of the lower
stratosphere is really worth the effort to loft the aerosols.

And on the temperature rise in the polar stratosphere, I would hope any
calculation of the effects of the sulfate/dust injection only put it in
during the sunlit season‹obviously, there would be no effect on solar
radiation during the polar night, so, with a two month lifetime of aerosols
there, it makes absolutely no sense to be lofting anything for about two
thirds of the year. And so likely no effect on winter temperatures (although
warming the coldest part of the polar winter stratosphere might well help to
prevent an ozone hole from forming).

So, I think a tropospheric brightening approach is likely the better option.
Whether it can be done with just CCN or might also need sulfate seems to me
worth investigating (what one needs may well be not just cloud brightening,
but also clear sky aerosol loading).

Best, Mike

*

On 3/17/12 8:41 PM, Ken Caldeira kcalde...@carnegie.stanford.edu wrote:

  

That is just misleading.  The third attachment is a top-of-atmosphere
radiation balance on the email I am responding to shows shortwave radiation.

The attached figure shows the corresponding temperature field from the same
simulation for the same time period.  Note Arctic cooling.

Also, we should not focus on individual regional blobs of color in an average
of a single decade from a single simulation.

The paper these figures came from is here: 
http://www.atmos-chem-phys.net/10/5999/2010/acp-10-5999-2010.pdf


___
Ken Caldeira

Carnegie Institution Dept of Global Ecology
260 Panama Street, Stanford, CA 94305 USA
+1 650 704 7212 kcalde...@carnegie.stanford.edu
http://dge.stanford.edu/labs/caldeiralab  @kencaldeira

YouTube:
 http://www.youtube.com/watch?v=a9LaYCbYCxo Climate change and the
transition from coal to low-carbon electricity
http://www.youtube.com/watch?v=a9LaYCbYCxo
Crop yields in a geoengineered climate
http://www.youtube.com/watch?v=-0LCXNoIu-c




On Sat, Mar 17, 2012 at 1:31 PM, Andrew Lockley and...@andrewlockley.com
wrote:

Hi 


Here are some model outputs which Stephen sent me. These appear to show
localized arctic warming in geoengineering simulations. This could be due to
winter effects.

I assume this is the source for the controversial figure in the BBC quote

A 
  


  


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Re: [geo] Re: We are top story on BBC environmental news

2012-03-18 Thread John Nissen


Dear John,

How I wish we had the time.  We should have been doing what you suggest 
immediately after the crash in sea ice extent of September 2007 - a 
wake-up call.   We have just left it far too late, and have no option 
but to try anything that might reduce the chance of a collapse in sea 
ice extent this year.  If you just look at the PIOMAS graph of sea ice 
volume which is down 75% in three decades and compare it with the sea 
ice extent which is down 40%, it is obvious that the sea ice extent 
cannot hold out much longer while the ice continues thinning.  There 
must be a great deal of heat going into melting the ice - and much of 
this heat is from the heating of open water by the sun when the sea ice 
retreats - i.e. from the albedo flip effect.   After a collapse such 
that there's little sea ice left in September, there will be a spurt in 
Arctic warming, perhaps to double the current rate of warming.  And 
after we have a nearly sea ice free Arctic ocean for six months, the 
warming could increase to triple or quadruple the current rate.  
Meanwhile there is the methane to contend with.  There are already signs 
of an escalation of methane emissions from shallow seas of the 
continental shelf.  That by itself would be cause for concern, since the 
sea ice retreat is allowing the seabed to warm well above the thaw point 
for methane hydrates.


So I have three questions for you:

1.  Do you seriously recommend that nobody does anything for at least 
three years while there is more research into geoengineering?


2.  How can you say that geoengineering is doomed to failure?  Do you 
really lack confidence in your own modelling?


3.  What do I tell my wife and children if nothing is done and the worst 
happens?


Kind regards,

John

---

On 18/03/2012 15:29, John Latham wrote:

Hello John Nissen and All,

John N says:-

Just before the hearing, the committee had received an email [6] from 
some
geoengineering experts recommending research but suggesting that development
and deployment of geoengineering techniques was premature, thus undermining
the AMEG position.

I was one of the signatories that John alluded to. I believe that each one of 
us feel
it shameful and dangerous that that  research into promising SRM ideas has not
been significantly financially supported. The major stages of the required 
research
involve modelling, resolution of all technological questions, examination of - 
and
international agreement on - possible adverse consequences of deployment, and
the execution of (in the case of MCB, for example), of a limited area 
field-testing
experiment. If the required funding was available now I think I think all the 
above
goals could be achieved in 5 years, perhaps even 3.

At the moment these goals are far from being achieved. An attempt to 
successfully
deploy now any likely SRM  technique would be doomed to failure. The 
technological
questions have not been fully resolved - so it would not work - and there would 
be
- in my opinion - an international outcry against deployment.

We would be shooting ourselves in the foot, I think, if we tried to deploy now. 
If
there was a major failure - which is likely - the response could be such as to 
prohibit
further SRM work for a long time.We need to engage in crash programmes of 
research
now, which means that we need immediately to obtain the required funding. [How, 
I
dont know, I'm afraid].

All Best,  John (Latham)

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 John Nissen [johnnissen2...@gmail.com]
Sent: Sunday, March 18, 2012 12:40 PM
To: joshuahorton...@gmail.com
Cc: geoengineering; John Nissen; P. Wadhams; Stephen Salter; JON HUGHES; Albert 
Kallio
Subject: Re: [geo] Re: We are top story on BBC environmental news

Hi Josh,

Before commenting on your question, I need to explain the recent activities of AMEG, a 
group whose position Professor Salter supports.  Professor Peter Wadhams and I gave 
evidence, on behalf of AMEG, to the first of two hearings of the Environment Audit 
Committee (AEC) inquiry Protecting the Arctic on 21st February.  We were 
given an opportunity to make a further presentation of the AMEG case to the All-Party 
Parliamentary Climate Change Group (APPCCG) on 13th March, i.e. last Tuesday, where we 
were joined by Professor Salter and journalist, Jon Hughes.  Richard Black, of the BBC, 
reported on the APPCCG meeting [1].  The second hearing of EAC was on 14th March, at 
which the Met Office gave oral evidence, reported by the Guardian [2] [3].

I am a great supporter of Stephen's cloud brightening approach, and we both 
want it deployed as soon 

RE: [geo] Re: We are top story on BBC environmental news

2012-03-18 Thread David Keith
John

Do you have a physically based model that backs up these about collapse and 
quadrupling of warming rate?

If so, please let us see it.

If not, please consider either retracting these claims or finding a way to make 
clear the level of uncertainty involved.

We have a climate problem and a public relations problem.

The first email I have from you in my archives is dated 2008 and suggests the 
complete disappearance of summer Arctic sea ice at the by 2013. This now seems 
highly unlikely.

If the current claims about immanent collapse are also proved false (as I 
expect they will be) you will provide ammunition to those who argue against 
action.

Reality is bad enough.

David

-Original Message-
From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of John Nissen
Sent: Sunday, March 18, 2012 11:24 AM
To: John Latham
Cc: johnnissen2...@gmail.com; joshuahorton...@gmail.com; geoengineering; P. 
Wadhams; Stephen Salter; JON HUGHES; Albert Kallio
Subject: Re: [geo] Re: We are top story on BBC environmental news


Dear John,

How I wish we had the time.  We should have been doing what you suggest 
immediately after the crash in sea ice extent of September 2007 - a
wake-up call.   We have just left it far too late, and have no option
but to try anything that might reduce the chance of a collapse in sea ice 
extent this year.  If you just look at the PIOMAS graph of sea ice volume which 
is down 75% in three decades and compare it with the sea ice extent which is 
down 40%, it is obvious that the sea ice extent cannot hold out much longer 
while the ice continues thinning.  There must be a great deal of heat going 
into melting the ice - and much of this heat is from the heating of open water 
by the sun when the sea ice
retreats - i.e. from the albedo flip effect.   After a collapse such
that there's little sea ice left in September, there will be a spurt in Arctic 
warming, perhaps to double the current rate of warming.  And after we have a 
nearly sea ice free Arctic ocean for six months, the warming could increase to 
triple or quadruple the current rate.
Meanwhile there is the methane to contend with.  There are already signs of an 
escalation of methane emissions from shallow seas of the continental shelf.  
That by itself would be cause for concern, since the sea ice retreat is 
allowing the seabed to warm well above the thaw point for methane hydrates.

So I have three questions for you:

1.  Do you seriously recommend that nobody does anything for at least three 
years while there is more research into geoengineering?

2.  How can you say that geoengineering is doomed to failure?  Do you really 
lack confidence in your own modelling?

3.  What do I tell my wife and children if nothing is done and the worst 
happens?

Kind regards,

John

---

On 18/03/2012 15:29, John Latham wrote:
 Hello John Nissen and All,

 John N says:-

 Just before the hearing, the committee had received an email
 [6] from some geoengineering experts recommending research but
 suggesting that development and deployment of geoengineering
 techniques was premature, thus undermining the AMEG position.

 I was one of the signatories that John alluded to. I believe that each
 one of us feel it shameful and dangerous that that  research into
 promising SRM ideas has not been significantly financially supported.
 The major stages of the required research involve modelling,
 resolution of all technological questions, examination of - and
 international agreement on - possible adverse consequences of
 deployment, and the execution of (in the case of MCB, for example), of
 a limited area field-testing experiment. If the required funding was 
 available now I think I think all the above goals could be achieved in 5 
 years, perhaps even 3.

 At the moment these goals are far from being achieved. An attempt to
 successfully deploy now any likely SRM  technique would be doomed to
 failure. The technological questions have not been fully resolved - so
 it would not work - and there would be
 - in my opinion - an international outcry against deployment.

 We would be shooting ourselves in the foot, I think, if we tried to
 deploy now. If there was a major failure - which is likely - the
 response could be such as to prohibit further SRM work for a long
 time.We need to engage in crash programmes of research now, which
 means that we need immediately to obtain the required funding. [How, I dont 
 know, I'm afraid].

 All Best,  John (Latham)

 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 John Nissen
 [johnnissen2...@gmail.com]
 

RE: [geo] Source on SRM causing warming

2012-03-18 Thread David Keith
Steven

I am in favor of serious research on both strat aerosols and sea salt CCN.

Your comments suggest that you already know the outcome of that research. You 
may of course be correct, and in many ways I hope you are. I, however, see less 
basis for certainty. 

A few facts that seem relevant: 

1. All simulations of stratospheric aerosols of which I am aware do show an 
arctic cooling tendency and increase in sea ice extent. 

2. There is little reason to doubt that 1 Wm^2 radiative global forcing could 
be produce by sulfate aerosols using well understood technologies. (That is not 
a claim about risks and side effects, just about basic capability.) 

3. There are large uncertainties about the efficacy of sea salt CCN in 
producing radiative forcing. It will certainly work sometimes under some 
conditions, but we don't yet have a good quantitative understanding of extent 
of conditions in which it might work and therefore of the aggregate 
effectiveness. 

4. There are advantages and disadvantages to the fact that the sea salt CCN is 
more patchy.

Given this is seems to me hard to conclude that we know the answer yet.

Yours,
David






-Original Message-
From: geoengineering@googlegroups.com [mailto:geoengineering@googlegroups.com] 
On Behalf Of Stephen Salter
Sent: Sunday, March 18, 2012 10:52 AM
To: mmacc...@comcast.net
Cc: Ken Caldeira; Andrew Lockley; Geoengineering; j.e.kristjans...@geo.uio.no
Subject: Re: [geo] Source on SRM causing warming

Mike

I had thought that the plan was stratospheric aerosol to be released at low 
latitudes and would slowly migrate to the poles where is would gracefully 
descend.  If you can be sure that it will all have gone in 10 days then my 
concerns vanish.  But if the air cannot get through the water surface how can 
the aerosol it carries get there?  It will form a blanket even if it is a very 
low one.

A short life would mean  that we do not have to worry about methane release.  
But can we do enough to cool the rest of the planet?  Perhaps Jon Egil can tell 
us about blanket lifetime.

Stephen

Mike MacCracken wrote:
 The Robock et al simulations of an Arctic injection found that the 
 lifetime of particles in the lower Arctic stratosphere was only two 
 months. In that one would only need particles up during the sunlit 
 season (say three months, for only really helps after the sea ice 
 surface has melted and the sun is high in the sky). During the 
 relatively calm weather of Arctic summer, the lifetime of tropospheric 
 sulfate, for example‹and quite possibly sea salt CCN--emitted above 
 the inversion is likely 10 days or so. It is not at all clear to me 
 that the 6 to 1 or so lifetime advantage of the lower stratosphere is really 
 worth the effort to loft the aerosols.

 And on the temperature rise in the polar stratosphere, I would hope 
 any calculation of the effects of the sulfate/dust injection only put 
 it in during the sunlit season‹obviously, there would be no effect on 
 solar radiation during the polar night, so, with a two month lifetime 
 of aerosols there, it makes absolutely no sense to be lofting anything 
 for about two thirds of the year. And so likely no effect on winter 
 temperatures (although warming the coldest part of the polar winter 
 stratosphere might well help to prevent an ozone hole from forming).

 So, I think a tropospheric brightening approach is likely the better option.
 Whether it can be done with just CCN or might also need sulfate seems 
 to me worth investigating (what one needs may well be not just cloud 
 brightening, but also clear sky aerosol loading).

 Best, Mike

 *

 On 3/17/12 8:41 PM, Ken Caldeira kcalde...@carnegie.stanford.edu wrote:

   
 That is just misleading.  The third attachment is a top-of-atmosphere 
 radiation balance on the email I am responding to shows shortwave radiation.

 The attached figure shows the corresponding temperature field from 
 the same simulation for the same time period.  Note Arctic cooling.

 Also, we should not focus on individual regional blobs of color in an 
 average of a single decade from a single simulation.

 The paper these figures came from is here: 
 http://www.atmos-chem-phys.net/10/5999/2010/acp-10-5999-2010.pdf

 ___
 Ken Caldeira

 Carnegie Institution Dept of Global Ecology
 260 Panama Street, Stanford, CA 94305 USA
 +1 650 704 7212 kcalde...@carnegie.stanford.edu
 http://dge.stanford.edu/labs/caldeiralab  @kencaldeira

 YouTube:
  http://www.youtube.com/watch?v=a9LaYCbYCxo Climate change and the 
 transition from coal to low-carbon electricity 
 http://www.youtube.com/watch?v=a9LaYCbYCxo
 Crop yields in a geoengineered climate 
 http://www.youtube.com/watch?v=-0LCXNoIu-c




 On Sat, Mar 17, 2012 at 1:31 PM, Andrew Lockley 
 and...@andrewlockley.com
 wrote:
 
 Hi

 Here are some model outputs which Stephen sent me. These appear to 
 show localized arctic warming in geoengineering simulations. This 
 could be due to 

Re: [geo] Re: We are top story on BBC environmental news

2012-03-18 Thread Alan Robock
I have to agree with David and Ken. Stick to refereed literature if you have 
something to say, so the idea can be peer reviewed.  And don't pretend to talk 
for all of us to the press, like Salter and Nissen are doing. 

Alan

[On sabbatical for current academic year.  The best way to contact me is by 
email, rob...@envsci.rutgers.edu, or at 732-881-1610 (cell).]

Alan Robock, Professor II (Distinguished Professor)
Editor, Reviews of Geophysics
Director, Meteorology Undergraduate Program
Associate Director, Center for Environmental Prediction
Department of Environmental SciencesPhone: +1-732-932-9800 x6222
Rutgers University  Fax: +1-732-932-8644
14 College Farm Road   E-mail: rob...@envsci.rutgers.edu
New Brunswick, NJ 08901-8551  USA  http://envsci.rutgers.edu/~robock

On Mar 18, 2012, at 11:01 AM, David Keith david_ke...@harvard.edu wrote:

 John
 
 Do you have a physically based model that backs up these about collapse and 
 quadrupling of warming rate?
 
 If so, please let us see it.
 
 If not, please consider either retracting these claims or finding a way to 
 make clear the level of uncertainty involved.
 
 We have a climate problem and a public relations problem.
 
 The first email I have from you in my archives is dated 2008 and suggests the 
 complete disappearance of summer Arctic sea ice at the by 2013. This now 
 seems highly unlikely.
 
 If the current claims about immanent collapse are also proved false (as I 
 expect they will be) you will provide ammunition to those who argue against 
 action.
 
 Reality is bad enough.
 
 David
 
 -Original Message-
 From: geoengineering@googlegroups.com 
 [mailto:geoengineering@googlegroups.com] On Behalf Of John Nissen
 Sent: Sunday, March 18, 2012 11:24 AM
 To: John Latham
 Cc: johnnissen2...@gmail.com; joshuahorton...@gmail.com; geoengineering; P. 
 Wadhams; Stephen Salter; JON HUGHES; Albert Kallio
 Subject: Re: [geo] Re: We are top story on BBC environmental news
 
 
 Dear John,
 
 How I wish we had the time.  We should have been doing what you suggest 
 immediately after the crash in sea ice extent of September 2007 - a
 wake-up call.   We have just left it far too late, and have no option
 but to try anything that might reduce the chance of a collapse in sea ice 
 extent this year.  If you just look at the PIOMAS graph of sea ice volume 
 which is down 75% in three decades and compare it with the sea ice extent 
 which is down 40%, it is obvious that the sea ice extent cannot hold out much 
 longer while the ice continues thinning.  There must be a great deal of heat 
 going into melting the ice - and much of this heat is from the heating of 
 open water by the sun when the sea ice
 retreats - i.e. from the albedo flip effect.   After a collapse such
 that there's little sea ice left in September, there will be a spurt in 
 Arctic warming, perhaps to double the current rate of warming.  And after we 
 have a nearly sea ice free Arctic ocean for six months, the warming could 
 increase to triple or quadruple the current rate.
 Meanwhile there is the methane to contend with.  There are already signs of 
 an escalation of methane emissions from shallow seas of the continental 
 shelf.  That by itself would be cause for concern, since the sea ice retreat 
 is allowing the seabed to warm well above the thaw point for methane hydrates.
 
 So I have three questions for you:
 
 1.  Do you seriously recommend that nobody does anything for at least three 
 years while there is more research into geoengineering?
 
 2.  How can you say that geoengineering is doomed to failure?  Do you really 
 lack confidence in your own modelling?
 
 3.  What do I tell my wife and children if nothing is done and the worst 
 happens?
 
 Kind regards,
 
 John
 
 ---
 
 On 18/03/2012 15:29, John Latham wrote:
 Hello John Nissen and All,
 
 John N says:-
 
Just before the hearing, the committee had received an email
 [6] from some geoengineering experts recommending research but
 suggesting that development and deployment of geoengineering
 techniques was premature, thus undermining the AMEG position.
 
 I was one of the signatories that John alluded to. I believe that each
 one of us feel it shameful and dangerous that that  research into
 promising SRM ideas has not been significantly financially supported.
 The major stages of the required research involve modelling,
 resolution of all technological questions, examination of - and
 international agreement on - possible adverse consequences of
 deployment, and the execution of (in the case of MCB, for example), of
 a limited area field-testing experiment. If the required funding was 
 available now I think I think all the above goals could be achieved in 5 
 years, perhaps even 3.
 
 At the moment these goals are far from being achieved. An attempt to
 successfully deploy now any likely SRM  technique would be doomed to
 failure. The technological 

RE: [geo] Re: We are top story on BBC environmental news

2012-03-18 Thread John Latham
John (N)

Taking  yr 3 questions:-

1.  Do you seriously recommend that nobody does anything for at least
three years while there is more research into geoengineering?

Performing research is not doing nothing. It is a vital component of the 
total effort (as is fund-raising, unfortunately) and must precede
deployment. This includes assessments of adverse consequences, 
seeking international agreement and field-testing the idea. Not to follow 
this route could SLOW DOWN geo-eng drastically, as argued earlier.


2.  How can you say that geoengineering is doomed to failure?  Do you
really lack confidence in your own modelling?

I did not say that, John. I said that I am not aware of any SRM scheme 
that has been optimally and exhaustively studied in the way defined above,
and is therefore ready for deployment. In the case of MCB, we do not yet
have a fully functioning spray production system. Our work on adverse
consequences is far from completion.etc. Our modelling work provides us
with encouragement to continue.


3.  What do I tell my wife and children if nothing is done and the worst
happens?

I suppose you could say that you issued warnings which were not listened 
to sufficiently. I could not.

All of us are trying to help avoid the scenario you pose. It is healthy for us 
to 
fight, try to persuade, allow oneself to be persuaded.

I may be completely wrong, John, but I think that the people who agree with
you have - in some instances -  a different interpretation of the scientific 
facts, 
or the completeness or general validity of them than people who do not.. If so, 
with time and tolerance, it should be possible to reach concerted agreement.


You might like to know that we have initiated computational studies of the 
possible role of MCB in inhibiting coral bleaching. Should the work turn out
to be potentially valuable, the required field-testing of the idea need only be 
on a small spatial scale.

All Best,   John (L).



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: John Nissen [j...@cloudworld.co.uk]
Sent: Sunday, March 18, 2012 5:23 PM
To: John Latham
Cc: johnnissen2...@gmail.com; joshuahorton...@gmail.com; geoengineering; P. 
Wadhams; Stephen Salter; JON HUGHES; Albert Kallio
Subject: Re: [geo] Re: We are top story on BBC environmental news

Dear John,

How I wish we had the time.  We should have been doing what you suggest
immediately after the crash in sea ice extent of September 2007 - a
wake-up call.   We have just left it far too late, and have no option
but to try anything that might reduce the chance of a collapse in sea
ice extent this year.  If you just look at the PIOMAS graph of sea ice
volume which is down 75% in three decades and compare it with the sea
ice extent which is down 40%, it is obvious that the sea ice extent
cannot hold out much longer while the ice continues thinning.  There
must be a great deal of heat going into melting the ice - and much of
this heat is from the heating of open water by the sun when the sea ice
retreats - i.e. from the albedo flip effect.   After a collapse such
that there's little sea ice left in September, there will be a spurt in
Arctic warming, perhaps to double the current rate of warming.  And
after we have a nearly sea ice free Arctic ocean for six months, the
warming could increase to triple or quadruple the current rate.
Meanwhile there is the methane to contend with.  There are already signs
of an escalation of methane emissions from shallow seas of the
continental shelf.  That by itself would be cause for concern, since the
sea ice retreat is allowing the seabed to warm well above the thaw point
for methane hydrates.

So I have three questions for you:

1.  Do you seriously recommend that nobody does anything for at least
three years while there is more research into geoengineering?

2.  How can you say that geoengineering is doomed to failure?  Do you
really lack confidence in your own modelling?

3.  What do I tell my wife and children if nothing is done and the worst
happens?

Kind regards,

John

---

On 18/03/2012 15:29, John Latham wrote:
 Hello John Nissen and All,

 John N says:-

 Just before the hearing, the committee had received an email [6] 
 from some
 geoengineering experts recommending research but suggesting that development
 and deployment of geoengineering techniques was premature, thus undermining
 the AMEG position.

 I was one of the signatories that John alluded to. I believe that each one of 
 us feel
 it shameful and dangerous that that  research into promising SRM ideas has not
 been significantly financially supported. The major stages of the required 
 research
 involve modelling, resolution of all technological questions, examination 

[geo] Re: Stoat strongly criticises AMEG

2012-03-18 Thread Andrew Revkin
I'm with Stoat, Ken Caldeira, David Keith, Alan Robock and others who see 
this emergency effort to rush cloud intervention in the Arctic on behalf 
of sea ice (and indirectly seabed methane) as undermining the case for a 
serious push on geo-engineering options, impacts and policy issues. You're 
getting headlines and the attention of factions in Parliament now, but just 
wait until the variability kicks the other way.


Yelling fire on a hot 
planethttp://www.nytimes.com/2006/04/23/weekinreview/23revkin.html?_r=2can 
have unanticipated consequences.

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[geo] Geoengineering company news

2012-03-18 Thread Andrew Lockley
http://motherboard.vice.com/2012/3/18/what-if-we-could-just-suck-all-those-greenhouse-gases-out-of-the-atmosphere--2

In the year 2012, with the two biggest greenhouse gas creators in the world
(the U.S. and China, of course) unwilling to do much of anything to cut
emissions, we’re basically light years and an autocratic world government
away from staving off catostrophic climate change through reductions. So,
that leaves us with the ignoble options of just dealing with the rising sea
levels and extreme weather and famines etc. as they come or, maybe just
maybe, digging our way out with some new technology. Civilization at large
deals with — or ignores — problems via this latter mindset more than it
would like to admit. Meet Kilamanjaro Air, a tech startup in the would-be
business of capturing and selling carbon dioxide, e.g. closing the carbon
cycle.

The science is essentially the same as that used on submarines and
spaceships to scrub CO2 from the air, albeit writ very large. Writer Mark
Gunther, a contributing editor at Fortune, details the history Kilimanjaro
in a new e-book called Suck It Up, excerpted at the “Ecomagination” blog.
(Ecomagination is a blog apparently run by GE, of nuclear weapons
engineering, railway locomotive, and 30 Rock fame, so let’s help ourselves
to some grains of salt.) Anyhow:

The company stumbled at first. As Lackner explained it to me, air capture
is a multi-step process —a chemical absorbent first has to bind with CO2,
after which the CO2 needs to be separated from the absorbent and compressed
into a liquid to be sold or stored. “The hard part is getting the CO2 back
off,” he said. GRT’s first absorbent was sodium hydroxide, which
effectively captured CO2. But the bond between them was so strong that
separating the CO2 required a great deal of energy. In 2007, after testing
other absorbents, GRT had devised a new air-extraction technology that uses
a plastic resin that bonds with CO2 when dry and gives it back when wet.
This was hailed as a breakthrough in a company press release quoting, among
others, Jeffrey Sachs, the director of the Earth Institute at Columbia.
“This significant achievement holds incredible promise in the fight against
climate change,” Sachs said. “Thanks to the ingenuity of GRT and Klaus
Lackner, the world may, sooner rather than later, have an important tool in
this fight.” It would be later rather than sooner. In 2008, Wright was
replaced as CEO by William “Billy” Gridley, an investor in the firm and a
former managing director at Goldman Sachs.

Kilimanjaro has a staff of 12 working on prototype machines that “catch”
C02 via large flat filters via an absorbent and then, once captured,
release the C02 and concentrate it into liquid form, where it can be used
as fuel (more dirty fuel and then only after being converted to carbon
monoxide). I can’t find anything on Kilimanjaro’s website about the
machine’s efficiency, which would seem to be a primary limiting factor of
the technology. (If it costs more energy to produce a lesser amount of
energy, that’s kind of a slim victory.) It’s addressed a very little bit
below:

Because greenhouse gases are dispersed around the globe, they can be
extracted from the air anywhere. Carbon dioxide spewing from a tailpipe in
Sao Paulo or a coal plant in China can be captured by a machine in Iceland
or the Middle East because the atmosphere functions as a conveyor belt,
moving CO2 from its sources to any sink. That’s important because while we
can envision a world where most or all of the electricity we use comes from
nuclear, solar or wind energy, or from fossil fuels where the CO2 is
captured at the power plant, it’s harder to see how emissions from cars,
trucks, trains, ships and planes can be eliminated. The beauty of air
capture, Lackner and his colleagues explained, is that “one could collect
CO2 after the fact and from any source….One would not have to wait for the
phasing out of existing infrastructure before addressing the greenhouse gas
problem.” Air capture plants, they wrote, could be located atop the best
underground reservoirs for storing CO2, which may be in isolated locations.
This fact is key to the business plans of all the air-capture startups. In
only one regard was Lackner’s paper clearly mistaken —he estimated that the
cost of air capture would be “on the order of $10 to $15 per ton,” a target
that now looks wildly optimistic.

Actually, what’s even more wildly optimistic is the widespread, worldwide
deployment of a new industry based upon the harvesting and sale of enriched
carbon dioxide any time before we’re living on a pseudo-Venus. While I’m
sure Gunther and anyone involved in Kilamanjaro would argue that this
technology isn’t meant as a stand-alone solution — though the title Suck It
Up kinda suggests otherwise —and there needs to be reductions as well, one
can’t help but think diversions like this are just that — less about
addressing the problem than addressing our anxiety about the 

Re: [geo] Source on SRM causing warming

2012-03-18 Thread Mike MacCracken
Hi Stephen--My wording must have been confusing.

For stratospheric injections at low latitudes, the lifetime is 1-2 years.
The aerosols do move poleward and are carried into the troposphere in mid
and high latitudes. This is one approach to trying to limit global climate
change, and, as David Keith says, studies indicate that these cool the polar
regions, though perhaps not in the stratosphere.

Your cloud brightening approach is also to limit global warming. I'd also
suggest that we could offset some of the global warming by sulfate aerosols
out over vast ocean areas instead of sulfate's present dominance over, now,
southeastern Asia, China, etc.--so keeping or modestly enhancing the present
cooling offset. [And reducing cirrus may also be a viable approach.]
 
A third approach is to cool the poles (and this might be good for regional
purposes alone), but cooling also pulls heat out of lower latitudes and
helps to cool them somewhat. The Caldeira-Wood shows it works conceptually
(they reduced solar constant) and Robock et al. injected SO2 into
stratosphere to do (but the full year injection of SO2/SO4 likely spread
some to lower latitudes and the monsoons were affected). One thing Robock et
al. found was that the lifetime of sulfate in the polar stratosphere is
about two months, and so that means that the potential 100 to 1 advantage of
stratospheric sulfate is not valid, and we're down to 6 to 1 compared to
surface-based approaches such as CCN or microbubbles to cool incoming
waters, sulfate or something similar over Arctic area, surface brightening
by microbubbles, etc.--noting that such approaches are only needed (and
effective) for the  few months per year when the Sun is well up in the sky.

As David Keith also says, there is a lot of research to be done to determine
which approaches or alone or in different variants might work, or be
effective or ineffective and have unintended consequences, much less how
such an approach or set of approaches might be integrated with mitigation,
adaptation, suffering, etc.

Best, Mike MacCracken






On 3/18/12 12:52 PM, Stephen Salter s.sal...@ed.ac.uk wrote:

 Mike
 
 I had thought that the plan was stratospheric aerosol to be released at
 low latitudes and would slowly migrate to the poles where is would
 gracefully descend.  If you can be sure that it will all have gone in 10
 days then my concerns vanish.  But if the air cannot get through the
 water surface how can the aerosol it carries get there?  It will form a
 blanket even if it is a very low one.
 
 A short life would mean  that we do not have to worry about methane
 release.  But can we do enough to cool the rest of the planet?  Perhaps
 Jon Egil can tell us about blanket lifetime.
 
 Stephen
 
 Mike MacCracken wrote:
 The Robock et al simulations of an Arctic injection found that the lifetime
 of particles in the lower Arctic stratosphere was only two months. In that
 one would only need particles up during the sunlit season (say three months,
 for only really helps after the sea ice surface has melted and the sun is
 high in the sky). During the relatively calm weather of Arctic summer, the
 lifetime of tropospheric sulfate, for example‹and quite possibly sea salt
 CCN--emitted above the inversion is likely 10 days or so. It is not at all
 clear to me that the 6 to 1 or so lifetime advantage of the lower
 stratosphere is really worth the effort to loft the aerosols.
 
 And on the temperature rise in the polar stratosphere, I would hope any
 calculation of the effects of the sulfate/dust injection only put it in
 during the sunlit season‹obviously, there would be no effect on solar
 radiation during the polar night, so, with a two month lifetime of aerosols
 there, it makes absolutely no sense to be lofting anything for about two
 thirds of the year. And so likely no effect on winter temperatures (although
 warming the coldest part of the polar winter stratosphere might well help to
 prevent an ozone hole from forming).
 
 So, I think a tropospheric brightening approach is likely the better option.
 Whether it can be done with just CCN or might also need sulfate seems to me
 worth investigating (what one needs may well be not just cloud brightening,
 but also clear sky aerosol loading).
 
 Best, Mike
 
 *
 
 On 3/17/12 8:41 PM, Ken Caldeira kcalde...@carnegie.stanford.edu wrote:
 
   
 That is just misleading.  The third attachment is a top-of-atmosphere
 radiation balance on the email I am responding to shows shortwave radiation.
 
 The attached figure shows the corresponding temperature field from the same
 simulation for the same time period.  Note Arctic cooling.
 
 Also, we should not focus on individual regional blobs of color in an
 average
 of a single decade from a single simulation.
 
 The paper these figures came from is here:
 http://www.atmos-chem-phys.net/10/5999/2010/acp-10-5999-2010.pdf
 
 ___
 Ken Caldeira
 
 Carnegie Institution Dept of Global Ecology
 260 Panama 

Re: [geo] Re: Stoat strongly criticises AMEG

2012-03-18 Thread Mike MacCracken
Just to note, however, that we really do not have a good sense of how big or
small variability can be at this melting trend continues‹variability is very
unlikely, in my view to be much of a saving influence on the decadal scale
unless some strong cooling influence results‹whether from a major volcanic
eruption, lots more sulfate pollution on the global scale, or climate
engineering. With world warming, it is hard to have the Arctic go very far
or very long in the opposite direction.

Mike MacCracken




On 3/18/12 3:43 PM, Andy Revkin rev...@gmail.com wrote:

 I'm with Stoat, Ken Caldeira, David Keith, Alan Robock and others who see this
 emergency effort to rush cloud intervention in the Arctic on behalf of sea
 ice (and indirectly seabed methane) as undermining the case for a serious push
 on geo-engineering options, impacts and policy issues. You're getting
 headlines and the attention of factions in Parliament now, but just wait until
 the variability kicks the other way.
 
 Yelling fire on a hot planet
 http://www.nytimes.com/2006/04/23/weekinreview/23revkin.html?_r=2  can have
 unanticipated consequences.

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[geo] Re: Stoat strongly criticises AMEG

2012-03-18 Thread Nathan Currier
May I make the reminder that their group is not called the Arctic Sea
Ice Emergency Group,
but the Arctic Methane Emergency Group?

The primary issue in all this is: what is happening with arctic
methane
emissions right now. That's what matters here. Criticizing PIOMAS or
whatever is what Al Gore
made into effectively exploding fish in the newest version of his
slideshow - red herrings.
Connelley's blog hardly addresses methane, and nor do these various
posts either, to a degree
that is, frankly, a little odd.

For the record, if I were in the group and asked my opinion of them,
I'd recommend against the
sea ice loss statements in question, in part because even if the ice
losses evolved as predicted, it could end up being more as
a consequence and not as a driver. That is, methane increases and sea
ice losses are looped, but
in complex ways, and the group makes it sound as though it's a one-way
street, sea ice loss leading to more methane releases.
It should hardly be controversial to say that if there ARE really
major methane releases there that the paper Ken attached will no
longer be relevant.
And thus far the news on the ground makes AMEG seem like quite a
rational enterprise, since from what we know it looks
relatively probable (much more than so than anyone should be
complacent about) that there are rapidly increasing methane
excursions going on there.

The thing that really matters here for AMEG in terms of expertise and
credibility is what Shakhova
and Semiletov have been finding in the ESAS region. They are there
again right now, and what they see
is what will be important. Those wishing to critique the legitimacy of
their group should really have things to add
to the discussion about those methane releases.

Best,

Nathan



On Mar 18, 3:43 pm, Andrew Revkin rev...@gmail.com wrote:
 I'm with Stoat, Ken Caldeira, David Keith, Alan Robock and others who see
 this emergency effort to rush cloud intervention in the Arctic on behalf
 of sea ice (and indirectly seabed methane) as undermining the case for a
 serious push on geo-engineering options, impacts and policy issues. You're
 getting headlines and the attention of factions in Parliament now, but just
 wait until the variability kicks the other way.



 Yelling fire on a hot 
 planethttp://www.nytimes.com/2006/04/23/weekinreview/23revkin.html?_r=2can 
 have unanticipated consequences.

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To post to this group, send email to geoengineering@googlegroups.com.
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