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Albern, Nicole, Voigt, Aiko, Thompson, David W. J. 
ORCID: https://orcid.org/0000-0002-5413-4376 and Pinto, Joaquim G.
(2020)
The role of tropical, midlatitude, and polar cloud-radiative changes for the midlatitude circulation response to global warming.
Journal of Climate, 33 (18).
7927–7943.
ISSN 0894-8755
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PDF ([15200442 - Journal of Climate] The Role of Tropical, Midlatitude, and Polar Cloud-Radiative Changes for the Midlatitude Circulation Response to Global Warming)
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Abstract
Previous studies showed that global cloud-radiative changes contribute half or more to the midlatitude atmospheric circulation response to global warming. Here, we investigate the relative importance of tropical, midlatitude, and polar cloud-radiative changes for the annual-mean, wintertime, and summertime circulation response across regions in AMIP-like simulations. To this end, we study global warming simulations from the ICON model run with the cloud-locking method and prescribed sea surface temperatures, which isolate the impact of changes in atmospheric cloud-radiative heating. Tropical cloud changes dominate the global cloud impact on the 850 hPa zonal wind, jet strength, and storm track responses across most seasons and regions. For the jet shift, a more diverse picture is found. In the annual mean and DJF, tropical and midlatitude cloud changes contribute substantially to the poleward jet shift in all regions. The poleward jet shift is further supported by polar cloud changes across the Northern Hemisphere but not in the Southern Hemisphere. In JJA, the impact of regional cloud changes on the jet position is small, consistent with an overall small jet shift during this season. The jet shift can be largely understood via the anomalous atmospheric cloud-radiative heating in the tropical and midlatitude upper troposphere. The circulation changes are broadly consistent with the influence of cloud-radiative changes on upper-tropospheric baroclinicity and thus the mean potential energy available for conversion into eddy kinetic energy. Our results help to explain the jet response to global warming and highlight the importance of tropical and midlatitude cloud-radiative changes for this response.
| Item Type: | Article |
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| Additional Information: | Funding Information: N.A. and A.V. are supported by the German Ministry of Education and Research (BMBF) and FONA: Research for Sustainable Development (www.fona.de) under grant agreement 01LK1509A. D.W.J.T. is supported by the U.S. National Science Foundation Climate and Large Scale Dynamics under Grants 1547003 and 1734251. J.G.P. thanks AXA research fund for support. Acknowledgments: N.A. thanks D.W.J.T. for hosting a three-month visit at Colorado State University. The ICON simulations were carried out by N.A. at the Mistral supercomputer of the German Climate Computing Center (DKRZ) in Hamburg, Germany. This work contributes to the WCRP’s Grand Challenge on Clouds, Circulation, and Climate Sensitivity and the BMBF-funded project "HD(CP)2: High Definition Clouds and Precipitation for Advancing Climate Prediction". |
| Uncontrolled Keywords: | atmospheric science ,/dk/atira/pure/subjectarea/asjc/1900/1902 |
| Faculty \ School: | Faculty of Science > School of Environmental Sciences |
| UEA Research Groups: | Faculty of Science > Research Groups > Centre for Ocean and Atmospheric Sciences Faculty of Science > Research Groups > Climatic Research Unit |
| Related URLs: | |
| Depositing User: | LivePure Connector |
| Date Deposited: | 10 Jun 2022 10:30 |
| Last Modified: | 15 Jun 2023 04:31 |
| URI: | https://ueaeprints.uea.ac.uk/id/eprint/85498 |
| DOI: | 10.1175/JCLI-D-20-0073.1 |
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