Check “sunny greenland” + Richard  S Scorer.

> On 6 Dec 2020, at 07:43, SALTER Stephen <[email protected]> wrote:
> 
> 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] 
> <mailto:[email protected]> <[email protected] 
> <mailto:[email protected]>> On Behalf Of Andrew Lockley
> Sent: 06 December 2020 13:28
> To: geoengineering <[email protected] 
> <mailto:[email protected]>>
> Subject: [geo] Reduction of the future Greenland ice sheet surface melt with 
> the help of solar geoengineering
>  
> This email was sent to you by someone outside the University.
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> 
> https://tc.copernicus.org/preprints/tc-2020-347/ 
> <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 <https://doi.org/10.5194/tc-2020-347>, in 
> review, 2020 
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