The Extraordinary March 2022 East Antarctica “Heat” Wave. Part II: Impacts on the Antarctic Ice Sheet

Authors

Jonathan D. Wille, CNRS Centre National de la Recherche Scientifique
Simon P. Alexander, Australian Antarctic Division
Charles Amory, CNRS Centre National de la Recherche Scientifique
Rebecca Baiman, University of Colorado Boulder
Léonard Barthélemy, Sorbonne Université
Dana M. Bergstrom, Australian Antarctic Division
Alexis Berne, École Polytechnique Fédérale de Lausanne
Hanin Binder, Institut für Atmosphäre und Klima
Juliette Blanchet, CNRS Centre National de la Recherche Scientifique
Deniz Bozkurt, Universidad de Valparaiso
Thomas J. Bracegirdle, British Antarctic Survey
Mathieu Casado, CNRS Centre National de la Recherche Scientifique
Taejin Choi, Korea Polar Research Institute
Kyle R. Clem, Victoria University of Wellington
Francis Codron, Sorbonne Université
Rajashree Datta, Australian Antarctic Division
Stefano Di Battista, Meteogiornale
Vincent Favier, CNRS Centre National de la Recherche Scientifique
Diana Francis, Khalifa University of Science and Technology
Alexander D. Fraser, Institute for Marine and Antarctic Studies
Elise Fourré, CNRS Centre National de la Recherche Scientifique
René D. Garreaud, Centro de Ciencia del Clima y la Resiliencia (CR)2
Christophe Genthon, Sorbonne Université
Irina V. Gorodetskaya, CIIMAR - Interdisciplinary Centre of Marine and Environmental Research
Sergi González-Herrero, WSL - Institut für Schnee- und Lawinenforschung SLF - Davos
Victoria J. Heinrich, University of Tasmania
Guillaume Hubert, Université Fédérale Toulouse Midi-Pyrénées
Hanna Joos, Institut für Atmosphäre und Klima
Seong Joong Kim, Korea Polar Research Institute

Publication Name

Journal of Climate

Abstract

Between 15 and 19 March 2022, East Antarctica experienced an exceptional heat wave with widespread 308–408C temperature anomalies across the ice sheet. In Part I, we assessed the meteorological drivers that generated an intense atmospheric river (AR) that caused these record-shattering temperature anomalies. Here, we continue our large collaborative study by analyzing the widespread and diverse impacts driven by the AR landfall. These impacts included widespread rain and surface melt that was recorded along coastal areas, but this was outweighed by widespread high snowfall accumulations resulting in a largely positive surface mass balance contribution to the East Antarctic region. An analysis of the surface energy budget indicated that widespread downward longwave radiation anomalies caused by large cloud-liquid water contents along with some scattered solar radiation produced intense surface warming. Isotope measurements of the moisture were highly elevated, likely imprinting a strong signal for past climate reconstructions. The AR event attenuated cosmic ray measurements at Concordia, something previously never observed. Last, an extratropical cyclone west of the AR landfall likely triggered the final collapse of the critically unstable Conger Ice Shelf while further reducing an already record low sea ice extent.

Open Access Status

This publication may be available as open access

Volume

37

Issue

3

First Page

779

Last Page

799

Funding Number

ASCI000002

Funding Sponsor

National Science Foundation

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Link to publisher version (DOI)

http://dx.doi.org/10.1175/JCLI-D-23-0176.1