Hi All
A paper at https://link.springer.com/content/pdf/10.1007/s00376-022-2036-z.pdf
says that there are significant biases in simulated cloud physical properties over the Southern Ocean.
Section 5 mentions a mean bias of “more than 30 Watts per square metre” lots more than I thought was the problem.
However it is not clear, at least to an engineer, whether it means plus or minus 30 watts per square metre.
This does not increase my admiration for climate modellers. Please help.
Stephen
Professor of Engineering Design
School of Engineering
University of Edinburgh
Mayfield Road
Edinburgh EH9 3DW
Scotland
0131 650 5704 or 662 1180
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Dear Bala
That helps a bit. But even if we do not know the starting point accurately, can we deduce the size of the change we have to make by doing some geoengineering?
I thought from Julia Slingo that the problem was 1.7 watts per square metre out of a mean solar input of 340 so we only had to do 0.5%.
Stephen
From: Govindasamy Bala <bala...@gmail.com>
Sent: 22 September 2022 16:26
To: Stephen Salter <S.Sa...@ed.ac.uk>
Cc: geoengi...@googlegroups.com; noac-m...@googlegroups.com
Subject: Re: [geo] Climate model bias
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Stephen
The article states “Absorbed solar radiation (ASR) is calculated as the downwelling minus upwelling shortwave radiation of all-sky conditions at the top of atmosphere. A previous study by Trenberth and Fasullo (2010) found that too large ASR over the SO was simulated by the CMIP3 models, showing a substantial bias of more than 32 W m–2. The serious overestimation of ASR and underestimation of cloudiness over the SO led to poor model performance in simulating the energy budget in the Southern Hemisphere in climate models (Marchand et al., 2014).”
They say the more recent CMIP6 models reduced this failure to accurately model Southern Ocean albedo to ±10 w/m2, compared to the CMIP3 ASR heating figure that was 30 watts too high due to underestimating cloudiness.
Robert
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