From the Surface to the Stratosphere: Large‐Scale Atmospheric Response to Antarctic Meltwater

Abstract The ocean response to Antarctic Ice Sheet (AIS) mass loss has been extensively studied using numerical models, but less attention has been given to the atmosphere. We examine the global atmospheric response to AIS meltwater in an ensemble of experiments performed using two fully coupled climate models under a pre‐industrial climate. In response to AIS meltwater, the experiments yield cooling from the surface to the tropopause over the subpolar Southern Ocean, warming in the Southern Hemisphere polar stratosphere, and cooling in the upper tropical troposphere. Positive feedbacks, initiated by disrupted ocean‐atmosphere heat exchange, result in a change in the top‐of‐atmosphere radiative balance caused primarily through surface and near‐surface albedo changes. Changes in the atmospheric thermal structure alter the jet streams aloft. The results highlight the global influence of AIS melting on the climate system and the potential for impacts on mid‐latitude climate patterns and delayed regional warming signals.

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Publication Details

Journal
Geophysical Research Letters
Published
2024-11-07
DOI
https://doi.org/10.1029/2024gl110157
Citations
5
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
1.88

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article

From the Surface to the Stratosphere: Large‐Scale Atmospheric Response to Antarctic Meltwater

W. Ellinger, María J. Molina, John P. Krasting, Katherine Turner et al.
5 citations
Geophysical Research Letters
Cryospheric studies and observations
1.88
article

From the Surface to the Stratosphere: Large‐Scale Atmospheric Response to Antarctic Meltwater

W. Ellinger, María J. Molina, John P. Krasting, Katherine Turner, Rebecca L. Beadling, Torge Martin, Pu Lin, Xiaoqi Xu, Anna Coomans, James Milward
article en
5 citations

Abstract

Abstract The ocean response to Antarctic Ice Sheet (AIS) mass loss has been extensively studied using numerical models, but less attention has been given to the atmosphere. We examine the global atmospheric response to AIS meltwater in an ensemble of experiments performed using two fully coupled climate models under a pre‐industrial climate. In response to AIS meltwater, the experiments yield cooling from the surface to the tropopause over the subpolar Southern Ocean, warming in the Southern Hemisphere polar stratosphere, and cooling in the upper tropical troposphere. Positive feedbacks, initiated by disrupted ocean‐atmosphere heat exchange, result in a change in the top‐of‐atmosphere radiative balance caused primarily through surface and near‐surface albedo changes. Changes in the atmospheric thermal structure alter the jet streams aloft. The results highlight the global influence of AIS melting on the climate system and the potential for impacts on mid‐latitude climate patterns and delayed regional warming signals.

Geophysical Research LettersVol. 51(21)
NSF National Center for Atmospheric Research (US), U.S. National Science Foundation (US), University of Arizona (US), NOAA Geophysical Fluid Dynamics Laboratory (US), Chinese Academy of Sciences (CN), Princeton University (US), GEOMAR Helmholtz Centre for Ocean Research Kiel (DE), Institute of Atmospheric Physics (CN), University of Chinese Academy of Sciences (CN), University of Maryland, College Park (US), Temple University (US)
National Science Foundation, U.S. Department of Energy, U.S. Department of Commerce, National Oceanic and Atmospheric Administration, Office of Science, Office of Polar Programs, Division of Polar Programs
Openalex Percentile: Top 15%
Cryospheric studies and observations
1.88
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