Regarding:
Furthermore, existing observing systems for stratospheric aerosols
are
difficult to use. The SAGE satellites are no longer working. There
is
a spare SAGE III on the shelf at NASA, but there are no plans to
launch
it. Calipso lidar can make episodic measurements along very narrow
As you say, pinatubo etc. prove that stratospheric aeroslols would cool the
world and it is therefore the disadvantages that we have to evaluate.
Many of us see the greatest and most urgent dangers in the Arctic and Antarctic
and think that localised stratospheric aerosols would probably avoid
Although I was initially worried by Denis's point that arctic aerosols will
capture some rays that would otherwise just pass tangentially through the
stratosphere, I have now done some geometry and believe that this will only
apply to about 0.2% of the incident sunlight on the Arctic at
You'd have to calculate this across the whole globe, surely? If the whole
atmos was affected, then this would mean the Earth turned from being a sharp
round disc to a bigger, hazy one? But, the evidence from Pinatubo surely
demonstrates that this doesn't cause a problem, it still cools down.
A couple of points:
1. On the angle issue, this is of course taken into consideration in
calculating how much solar radiation reaches the Arctic at any given
timeā¹and rays just passing tangentially through will not count much at all.
That the actual incident light in high latitudes in summer,
I have to admit I hadnt thought of that aspect of aerosols in the arctic.
To Gregory Benfold -What do you think ?
John Gorman
- Original Message -
From: Bonnelle Denis
To: gorm...@waitrose.com ; andrew.lock...@gmail.com ; John Nissen ;
geoengineering@googlegroups.com
Sent:
Andrew
There is a list of packages at
http://atol.ucsd.edu/scatlib/scatterlib.htm
You can download a wonderful free computing package for liquid drops
written by Philip Laven from
http://www.philiplaven.com/mieplot.htm
See also:
http://www.philiplaven.com/index1.html
All:
Bonnelle Denis is right that a detailed study of aerosol reflections
needs doing. Someone may wish to use research time on it, but without
any funding it's difficult to mount a determined attack on the many
parameters that need varying.
The issue of particle size demands some actual
First, of course, one would be working to do the reflection only during the
sunlit months, so Sun is a bit higher in the sky. During peak summer, there
is as much solar incident on Arctic latitudes over 24 hours as at the
equator. Yes, at a lower sun angle, but still a lot of solar.
And as to
John,
No you may not assume any such thing. Far, far too low on both % and
numbers for a max possible risk.
A
2009/5/11 John Nissen j...@cloudworld.co.uk
Hi all,
In the absense of any figures from you for monsoon failure risk, may I
suggest a maximum probability of 1% of severe failure,
Since nobody knows, estimates are pointless without better data,
simulations etc
Gregory
-Original Message-
From: Andrew Lockley andrew.lock...@gmail.com
To: John Nissen j...@cloudworld.co.uk
Cc: geoengineering geoengineering@googlegroups.com
Sent: Mon, 11 May 2009 3:29 pm
Subject:
John,
This is really flimsy thinking. It springs from a WAG (wild-ass-guess) type
analysis of risk--i.e. If it's not a lot, then it must be a little. For a
humorous take on this, watch Jon Stewart's daily show last week on the LHC
(Large Hadron Collider). I think it's about 19 minutes in.
It is all about risk reduction.
You cannot say how much risk we would be willing to accept from a climate
intervention without first characterizing the risk of not intervening in
climate.
If it is clear that a climate intervention would reduce risk (taking into
account relevant distributional
Debate, analysis, and modeling of the status quo and thought experiments should be continuous. The more the better.
-Original Message- From: Andrew Lockley Sent: May 11, 2009 6:29 PM To: John Nissen Cc: geoengineering
Eugene
good idea
I think Biosphere Carbon Stock Management is a game plan but for reasons
stated previously think it needs to be associated with an ocean surface
cooling programme.**
Any more ideas or modifications needed?
I'm 73 and not very well
Why don't you do it?
Peter
**And a lot of
Comments:
2) Stratospheric sulphur aerosols look fairly promising, and we can
cheaply deploy them with balloons. They might wreck the hydrological
cycle in general, and the monsoon in particular. Other aerosols are
worth a look.
Balloons are not optimal. Airplanes work fine at Arctic needed
Greg,
I don't think the us-them dichotomy is helpful. As in all areas of controversy
there is a spectrum ranging from those who indiscriminately deploy whatever
argument crosses their radar screen if it fits their pre-conceived idea of the
right answer to those who actually would like to see
Dave:
Of course us/them is there--we have plenty of ferocious opponents--and
without funding, we won't get to do the rigorous description of how
to design field experiments that both have trivial risks and are
capable of providing useful information to better characterize the
risks of full
Dear Stephen,
I would not put much faith in this highly idealized model, unless it
could be shown to actually simulate past monsoon variations. It is a
nice intellectual exercise, but ignores many of the important processes
of the climate system.
Alan
Alan Robock, Professor II
Director,
Good discussion. This is what geoengineering is all about.
-Original Message-
From: geoengineering@googlegroups.com
[mailto:geoengineer...@googlegroups.com] On Behalf Of Alvia Gaskill
Sent: Saturday, May 09, 2009 11:50 AM
To: s.sal...@ed.ac.uk; rob...@envsci.rutgers.edu
Cc:
A few comments on that:1) Droplet size shouldn't affect chemistry. Both
surface area and the cross sectional area are proportional to the square of
the radius. Volume affects residence time, and is proportional to the cube
of the radius. Big droplets are shorter-lived, and hence more
Droplet size may affect chemistry because of surface tension. At
sufficiently small scales, a high-curvature surface isn't the same
chemically as a lower-curvature surface.
My impression is that the Brewer Dobson circulation is the net
circulation after east-west wind is canceled out, since the
John:
You strike the nub of it:
Alan claims that the aerosols would not be confined to the polar
region. But doesn't this depend on: the timing range of the release of
precursor, the height range in the stratosphere, and the latitude
range? Suppose that the release is in spring such that
It's essential to consider the 'unmodified case'. Whatever 'damage' geoeng
does has to be weighed against the damage that would occur from unfettered
global warming to the Arctic region. The plight of the Polar bear is the
poster child for global warming, which makes my point in a very clear
Dear Ken,
I agree. We need several models to do the same experiment so we can see
how robust the ModelE results are. That is why we have proposed to the
IPCC modeling groups to all do the same experiments so we can compare
results. Nevertheless, observations after large volcanic eruptions,
Hi all,
I'm restricting this analysis to geoengineering with stratospheric aerosols to
save the Arctic sea ice. I've not received any additions to the list of pros
and cons I posted on 29th April.
Some points have been discussed, mostly on 29th April also:
S11. Cannot stop quickly
William
This scare ,that stratospheric areosols would result in an even more global
warming if stopped, has appeared in many articles. I therefore read the
relevent papers fairly carefully and my reading is that temeratures would
simply rise quickly to where they would have been without
Dear John:
I did not see a principal advantage of SRM listed. That is that it is
reversible, at least for sulfates in the stratosphere and for cloud
whitening.
Cheers,
Bill
On Apr 29, 2009, at 10:34 AM, John Nissen wrote:
Hi all,
Alan Robock has said:
Whether we should use
Hi All
A comment about John's item G2 'that we make such a hash of everything
in the past that we are bound to make a hash of geo-engineering'.
Everyone likes to believe this but the reality is that we magnify the
hashes and ignore the many successes.
I was certainly very bad to introduce
Shame on you. Were they white rabbits?
I was certainly very bad to introduce rabbits to Australia. But horses
to America?
- Original Message -
From: Stephen Salter s.sal...@ed.ac.uk
To: j...@cloudworld.co.uk
Cc: geoengineering geoengineering@googlegroups.com;
The Kasotchi eruption column only went up to 35,000 ft, the Lowermost
Stratosphere, not the Lower Stratosphere, so no global or regional climatic
impact would have been expected. Concept correct, example wrong. What one
means by full scale has yet to be determined. A level that would
Dear Alvia,
You can guess whatever you want, but I know of no examples of such low
stratospheric loading that had a detectable climatic effect. And I have
no idea what you mean by lowermost or lower stratosphere. The
stratosphere begins at the tropopause, which is lower in the Arctic and
You seem to be ignoring the fact that smokestack emissions and tailpipe
emissions of SO2 aerosols had a substantial cooling effect pre 1973 and were
outlawed in the US and Europe thereafter, at which time the cooling
immediately stopped and warming continued. That is documented in a NASA
paper.
I
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