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ToolsPo-Chedley, Stephen, Zelinka, Mark D., Jeevanjee, Nadir, Thorsen, Tyler J. and Santer, Benjamin D. (2019) Climatology Explains Intermodel Spread in Tropical Upper Tropospheric Cloud and Relative Humidity Response to Greenhouse Warming. Geophysical Research Letters, 46 (22). pp. 13399-13409. ISSN 0094-8276
Full text not available from this repository. (Request a copy)Abstract
The response of upper tropospheric clouds and relative humidity (RH) to warming is important to the overall sensitivity of the Earth to increasing greenhouse gas concentrations. Previous research has shown that changes in hydrologic fields should closely track rising isotherms in a warming climate. Here we show that the distribution of tropical clouds and RH in general circulation models is approximately constant under greenhouse warming when using temperature as a vertical coordinate. By assuming that these fields are an invariant function of atmospheric temperature and that temperature change follows a dilute moist adiabat, we are able to accurately predict cloud fraction and RH changes in the tropical upper troposphere (150–400 hPa) in 27 general circulation models. Our results indicate that intermodel spread in changes of tropical upper tropospheric clouds and RH is closely related to differences in model climatology and could be substantially reduced if model ensembles reliably reproduced observed climatologies.
| Item Type: | Article |
|---|---|
| Additional Information: | Publisher Copyright: ©2019. The Authors. |
| Uncontrolled Keywords: | geophysics,earth and planetary sciences(all) ,/dk/atira/pure/subjectarea/asjc/1900/1908 |
| Faculty \ School: | Faculty of Science > School of Environmental Sciences |
| Related URLs: | |
| Depositing User: | LivePure Connector |
| Date Deposited: | 18 Mar 2026 13:30 |
| Last Modified: | 19 Mar 2026 09:33 |
| URI: | https://ueaeprints.uea.ac.uk/id/eprint/102407 |
| DOI: | 10.1029/2019GL084786 |
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