The Extraordinary March 2022 East Antarctica “Heat” Wave. Part I: Observations and Meteorological Drivers

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 30°–40°C temperature anomalies across the ice sheet. This record-shattering event saw numerous monthly temperature records being broken including a new all-time temperature record of -9.4°C on 18 March at Concordia Station despite March typically being a transition month to the Antarctic coreless winter. The driver for these temperature extremes was an intense atmospheric river advecting subtropical/midlatitude heat and moisture deep into the Antarctic interior. The scope of the temperature records spurred a large, diverse collaborative effort to study the heat wave’s meteorological drivers, impacts, and historical climate context. Here we focus on describing those temperature records along with the intricate meteorological drivers that led to the most intense atmospheric river observed over East Antarctica. These efforts describe the Rossby wave activity forced from intense tropical convection over the Indian Ocean. This led to an atmospheric river and warm conveyor belt intensification near the coastline, which reinforced atmospheric blocking deep into East Antarctica. The resulting moisture flux and upper-level warm-air advection eroded the typical surface temperature inversions over the ice sheet. At the peak of the heat wave, an area of 3.3 million km2 in East Antarctica exceeded previous March monthly temperature records. Despite a temperature anomaly return time of about 100 years, a closer recurrence of such an event is possible under future climate projections. In Part II we describe the various impacts this extreme event had on the East Antarctic cryosphere.

Open Access Status

This publication may be available as open access

Volume

37

Issue

3

First Page

757

Last Page

778

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-23-0175.1