Hi All

The highest estimate for Greenland ice sheet loss is 325 billion tonnes a year.

If I multiply this by the latent heat of fusion of ice and divide by the area 
of Greenland 2.166 million square kilometres I get 1.59 watts per square metre. 
 I think that this could be done by marine cloud brightening in just a month 
either side of midsummer provided that we can cool other places at the same 
time to reduce problems of controlling direction.

How do we square this with 40?

Please do not use this to reduce the need for CO2 removal.

Stephen

From: [email protected] <[email protected]> On 
Behalf Of Andrew Lockley
Sent: 06 December 2020 13:28
To: geoengineering <[email protected]>
Subject: [geo] Reduction of the future Greenland ice sheet surface melt with 
the help of solar geoengineering

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https://tc.copernicus.org/preprints/tc-2020-347/

Brief Communication: Reduction of the future Greenland ice sheet surface melt 
with the help of solar geoengineering
Xavier Fettweis et al.
Received: 25 Nov 2020 – Accepted for review: 03 Dec 2020 – Discussion started: 
04 Dec 2020
Abstract. The Greenland Ice Sheet (GrIS) will be losing mass at an accelerating 
pace throughout the 21st century, with a direct link between anthropogenic 
greenhouse gas emissions and the magnitude of Greenland mass loss. Currently, 
approximately 60 % of the mass loss contribution comes from surface melt and 
subsequent meltwater runoff, while 40 % are due to ice calving. Where most of 
the surface melt occurs (in the ablation zone), most of the energy for the 
surface melt is provided by absorbed shortwave fluxes, which could be reduced 
by solar geoengineering measures. However, so far very little is known about 
the potential impacts of an artificial reduction of the incoming solar 
radiation on the GrIS surface energy budget and the subsequent change in 
meltwater production. By forcing the regional climate model MAR with the latest 
CMIP6 future scenarios ssp245, ssp585 and associated G6solar experiment from 
the Earth System Model CNRM-ESM2-1, we evaluate the local changes due to the 
reduction of the solar constant on the projected GrIS surface mass balance 
(SMB) decrease. Overall, our results show that even in case of low mitigation 
greenhouse gas emissions scenario (ssp585), the Greenland surface mass loss can 
be brought in line with the medium mitigation emissions scenario (ssp245) by 
reducing the solar downward flux at the top of the atmosphere by ~40 W/m2 or 
~1.5 % (using the G6solar experiment). In addition to reduce Global Warming in 
line with ssp245, G6solar also decreases the efficiency of surface meltwater 
production over the Greenland ice sheet by damping the well-known positive 
melt-albedo feedback which mitigates the projected Greenland ice sheet surface 
melt increase by 6 %. However, only more constraining geoengineering 
experiments than G6solar allows to maintain positive SMB till the end of this 
century without any reduction in our greenhouse gas emissions.

How to cite: Fettweis, X., Hofer, S., Séférian, R., Amory, C., Delhasse, A., 
Doutreloup, S., Kittel, C., Lang, C., Van Bever, J., Veillon, F., and Irvine, 
P.: Brief Communication: Reduction of the future Greenland ice sheet surface 
melt with the help of solar geoengineering, The Cryosphere Discuss., 
https://doi.org/10.5194/tc-2020-347, in review, 2020
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