Model spread in tropical low cloud feedback tied to overturning circulation response to warming
The magnitude of the tropical low cloud feedback, which contributes considerably to uncertainty in estimates of climate sensitivity, is closely linked to tropical deep convection and its effects on the tropical atmospheric overturning circulation.
Main Authors: | , , , , , , , , , |
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Format: | Article |
Language: | English |
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Nature Portfolio
2022-11-01
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Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/s41467-022-34787-4 |
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author | Kathleen A. Schiro Hui Su Fiaz Ahmed Ni Dai Clare E. Singer Pierre Gentine Gregory S. Elsaesser Jonathan H. Jiang Yong-Sang Choi J. David Neelin |
author_facet | Kathleen A. Schiro Hui Su Fiaz Ahmed Ni Dai Clare E. Singer Pierre Gentine Gregory S. Elsaesser Jonathan H. Jiang Yong-Sang Choi J. David Neelin |
author_sort | Kathleen A. Schiro |
collection | DOAJ |
description | The magnitude of the tropical low cloud feedback, which contributes considerably to uncertainty in estimates of climate sensitivity, is closely linked to tropical deep convection and its effects on the tropical atmospheric overturning circulation. |
first_indexed | 2024-04-13T12:39:31Z |
format | Article |
id | doaj.art-edef5faa3af8477b92a091dd7ae7eac0 |
institution | Directory Open Access Journal |
issn | 2041-1723 |
language | English |
last_indexed | 2024-04-13T12:39:31Z |
publishDate | 2022-11-01 |
publisher | Nature Portfolio |
record_format | Article |
series | Nature Communications |
spelling | doaj.art-edef5faa3af8477b92a091dd7ae7eac02022-12-22T02:46:33ZengNature PortfolioNature Communications2041-17232022-11-0113111210.1038/s41467-022-34787-4Model spread in tropical low cloud feedback tied to overturning circulation response to warmingKathleen A. Schiro0Hui Su1Fiaz Ahmed2Ni Dai3Clare E. Singer4Pierre Gentine5Gregory S. Elsaesser6Jonathan H. Jiang7Yong-Sang Choi8J. David Neelin9Department of Environmental Science, University of VirginiaJoint Institute for Research in Earth Systems Science and Engineering, University of California, Los AngelesJoint Institute for Research in Earth Systems Science and Engineering, University of California, Los AngelesJoint Institute for Research in Earth Systems Science and Engineering, University of California, Los AngelesDepartment of Environmental Science and Engineering, California Institute of TechnologyEarth and Environmental Engineering, Columbia UniversityDepartment of Applied Physics and Applied Mathematics, Columbia UniversityJet Propulsion Laboratory, California Institute of TechnologyDepartment of Climate and Energy Systems Engineering, Ewha Womans UniversityJoint Institute for Research in Earth Systems Science and Engineering, University of California, Los AngelesThe magnitude of the tropical low cloud feedback, which contributes considerably to uncertainty in estimates of climate sensitivity, is closely linked to tropical deep convection and its effects on the tropical atmospheric overturning circulation.https://doi.org/10.1038/s41467-022-34787-4 |
spellingShingle | Kathleen A. Schiro Hui Su Fiaz Ahmed Ni Dai Clare E. Singer Pierre Gentine Gregory S. Elsaesser Jonathan H. Jiang Yong-Sang Choi J. David Neelin Model spread in tropical low cloud feedback tied to overturning circulation response to warming Nature Communications |
title | Model spread in tropical low cloud feedback tied to overturning circulation response to warming |
title_full | Model spread in tropical low cloud feedback tied to overturning circulation response to warming |
title_fullStr | Model spread in tropical low cloud feedback tied to overturning circulation response to warming |
title_full_unstemmed | Model spread in tropical low cloud feedback tied to overturning circulation response to warming |
title_short | Model spread in tropical low cloud feedback tied to overturning circulation response to warming |
title_sort | model spread in tropical low cloud feedback tied to overturning circulation response to warming |
url | https://doi.org/10.1038/s41467-022-34787-4 |
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