Quantifying Cloud Feedbacks for Climate Sensitivity
A new study,[8] however, has succeeded at quantifying these cloud feedbacks at 0.43 ± 0.35 W/m^2/K. This means that for every 1 C warming, we can expect an additional 0.43 W/m^2, amplifying warming. Given these results, there is just a 2.5% chance that the net cloud feedback has a negative sign. These findings also help constrain values for ECS. “Considering changes in just these two factors, we are able to constrain global cloud feedback to 0.43 ± 0.35 W⋅m−2⋅K−1 (90% confidence), implying a robustly amplifying effect of clouds on global warming and only a 0.5% chance of ECS below 2 K.” The paper is currently behind a paywall, but you can read a summary of it on CarbonBrief.[9]
The observational constraints also reduces the uncertainty for ECS with respect to AR5's assessment, and assesses ECS to be 3.2, though the 1σ and 2σ confidence intervals are larger above the mean than below it. "The observational constraint translates into a probability distribution for ECS... with central value 3.2 K and CIs 2.6 to 4.2 K (17 to 83%; Fig. 4B, blue bar) and 2.3 to 5.2 K (5 to 95%). The former is considerably (49%) narrower than the IPCC AR5 likely (17 to 83%) range of 1.5 to 4.5 K and agrees well with the slightly narrower 66% ECS range proposed by the WCRP assessment (2.6 to 3.9 K), which accounts for multiple lines of evidence and expert judgment, rather than being based solely on cloud radiative observations."
References:
[1] Dessler, A. E. (2010), A determination of the cloud feedback from climate variations over the past decade, Science, 330, 1523– 1527, doi:10.1126/science.1192546.
[2] Dessler, A. E., and Loeb, N. G. (2013), Impact of dataset choice on calculations of the short‐term cloud feedback, J. Geophys. Res. Atmos., 118, 2821– 2826, doi:10.1002/jgrd.50199.
[3] Zhou, C., M. D. Zelinka, A. E. Dessler, and P. Yang, 2013: An Analysis of the Short-Term Cloud Feedback Using MODIS Data. J. Climate, 26, 4803–4815, https://doi.org/10.1175/JCLI-D-12-00547.1.
[4] Zelinka, M. D., Myers, T. A., McCoy, D. T., Po-Chedley, S., Caldwell, P. M., Ceppi, P., et al. (2020). Causes of higher climate sensitivity in CMIP6 models. Geophysical Research Letters, 47, e2019GL085782. https://doi.org/10.1029/2019GL085782
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2019GL085782
[5] Myers, T.A., Scott, R.C., Zelinka, M.D. et al. Observational constraints on low cloud feedback reduce uncertainty of climate sensitivity. Nat. Clim. Chang. 11, 501–507 (2021). https://doi.org/10.1038/s41558-021-01039-0
[6] MĂ¼lmenstädt, J., Salzmann, M., Kay, J.E. et al. An underestimated negative cloud feedback from cloud lifetime changes. Nat. Clim. Chang. 11, 508–513 (2021). https://doi.org/10.1038/s41558-021-01038-1
[7] Stephens, G.L. The cooling of light rains in a warming world. Nat. Clim. Chang. 11, 468–470 (2021). https://doi.org/10.1038/s41558-021-01056-z
[8] Paulo Ceppi, Peer Nowack. Observational evidence that cloud feedback amplifies global warming. Proceedings of the National Academy of Sciences Jul 2021, 118 (30) e2026290118; DOI: 10.1073/pnas.2026290118 https://www.pnas.org/content/118/30/e2026290118
[9] Ayesha Tandon.Clouds study finds that low climate sensitivity is ‘extremely unlikely.’ CarbonBrief. July 21 2021. https://www.carbonbrief.org/clouds-study-finds-that-low-climate-sensitivity-is-extremely-unlikely?fbclid=IwAR225L6aKkDv4IVx-U6-t1qQeHJ01yEkF5NwAMULkJM_N51qugi9clbplSc
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