Hi David--I have run the MAGICC model of Wigley turning off all emissions
(all GHGs, all aerosols)--so an impossibly aggressive limiting case. The
black carbon and sulfate effects go away virtually immediately, tropospheric
ozone almost as fast, methane over 1-2 decades, and then one is left with
the slowly decreasing forcing of the long-lived species--CO2, N2O and
halocarbons (with no cooling offset). This leads to several decades of
forcing not unlike net forcing today, so one would get continued ocean
warming.

You can also look at the IPCC Fourth Assessment and their case of constant
forcing (that goldish curve). They kept all concentrations and aerosol
loadings the same--which is actually not self-consistent as to keep the CO2
concentration constant, emissions would have to drop by 80% or maybe more,
and so SO2 emissions would be expected to drop equivalently, reducing the
cooling offset by 80% or so. Of course, so would the black carbon warming
influence, which may almost offset the sulfate loss. As the IPCC temperature
result shows, one would get about a half degree of further warming.

One would thus expect the Arctic to warm more and likely mean there would be
virtually no summer sea ice, and this would lead to quite thin winter sea
ice that would melt earlier in the spring, and so more solar absorption,
etc.--so warming in Arctic would be greater than global average (as is now
the case).

Now, I happen to think (see my ERL paper) that the reduction in sulfate
loading in the Arctic (the cleaning up of Arctic haze) as a result of
reduced SO2 emissions from Europe and Russia (at least springtime air into
the Arctic typically passes over these regions) is likely contributing to
the accelerated melting of the Arctic as compared to models (which don't
typically treat this effect, especially as global SO2 emissions are likely
headed back up). Thus, in my view we have an analog for a reverse
geoengineering experiment--I admit this is a hypothesis, but given all the
data that has been taken over the last few decades in cleaning up Arctic
haze, there is likely an observational data base for exploring this
possibility. While I know some attribute the accelerated melting to soot,
Quinn et al in Tellus show, at least for some months, that soot deposition
has been going down along with the sulfate decline. What needs to be looked
at are data for changes in sunlight and downward IR onto the sea ice as a
function of season--and NOAA and others may at least have some data on this.
Less springtime sulfate may well lead to earlier melting of surface snow
cover, lowering the albedo and then increasing the loss.

If all of this is the case, then, indeed, we might want to put the sulfate
back over the Arctic--in the troposphere where during summer lifetime might
be up to 2 weeks or so [Alan Robock's lower Arctic stratosphere injection
had a lifetime of 2 months--far below the global average 2 year versus one
week ratio for stratospheric (volcanic) to tropospheric sulfate.] Injection
could be done from a few mountain locations on days when winds are headed
into the Arctic and need only occur for a the few sunlit months starting
when the snow cover albedo drops, so geoengineering injection would likely
be a small fraction of recent surface emissions and we thus likely could
estimate impacts on sea ice, ecosystems, etc. from past records as well as
from models. And, done cleverly, it is not at all clear that just cooling
the summertime Arctic would lead to summertime cooling of the surrounding
continental areas and suppress the monsoon.

What we need to get at all of this is a solid research program where efforts
are made to refine and develop ideas, seeing if adjustments can overcome the
worst of the side effects (injections on one or the other side of the
Arctic, at various times during the sunlit season, injections at additional
locations, and so on) rather than just assertions like mine and model
simulations that aren't directly representing the proposed intervention.

Best, Mike

On 12/10/09 7:12 PM, "John Nissen" <[email protected]> wrote:

> 
> Curiously, I can't find you any references.  But it's rather obvious if
> you think about the relative timescale - and I've challenged many top
> climate scientists to dispute it, and nobody has managed!  The Arctic
> sea ice is indeed the "Elephant in the room", that nobody chooses to
> notice, because the prospect of having to deploy geoengineering  is so
> uncomfortable for them.
> 
> Perhaps it's cowardice.  But it's potentially tragic because
> geoengineering could be left too late.
> 
> John
> 
> --
> 
> Hawkins, Dave wrote:
>> Hi John,
>> In your note you say,  "The undisputed fact that emissions reduction cannot
>> save the Arctic sea ice, at its current rate of retreat..."
>> Can you provide a reference or two that reaches this conclusion?
>> (I'm not asking to dispute what you say but would like to see what you have
>> in mind as support for the proposition.)
>> Thanks
>> David
>> 
>> ----- Original Message -----
>> From: [email protected] <[email protected]>
>> To: Geoengineering <[email protected]>
>> Sent: Thu Dec 10 16:46:31 2009
>> Subject: [geo] Population control, emission cuts, but geoengineering?
>> 
>> 
>> Hi all,
>> 
>> Two excellent programmes on the environment and mankind's impact:
>> 
>> David Attenborough:
>> http://www.bbc.co.uk/iplayer/episode/b00pdjmk/Horizon_20092010_How_Many_Peopl
>> e_Can_Live_on_Planet_Earth/
>> 
>> 
>> Iain Stewart:
>> http://www.bbc.co.uk/iplayer/episode/b00jf6md/Hot_Planet/
>> 
>> Unfortunately, although Iain had sympathetic mention of Klaus Lackner's
>> artificial trees, solar radiation management was represented by sulphur
>> being fired into the stratosphere by guns - mention of ozone disruption
>> - and the programme ended with punch line "geoengineering is too
>> expensive and too dangerous".  This was an unwarranted dismissal of the
>> technology with probably the best chance of saving the Arctic sea ice.
>> The undisputed fact that emissions reduction cannot save the Arctic sea
>> ice, at its current rate of retreat, was not mentioned.
>> 
>> Cheers,
>> 
>> John
>> 
>> 
>> 
>> --
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>>   
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