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

Jonathan D. Wille, Simon P. Alexander, Charles Amory, Rebecca Baiman, Léonard Barthélemy, Dana M. Bergstrom, Alexis Berne, Hanin Binder, Juliette Blanchet, Deniz Bozkurt, Thomas J. Bracegirdle, Mathieu Casado, Taejin Choi, Kyle R. Clem, Francis Codron, Rajashree Datta, Stefano Di Battista, Vincent Favier, Diana Francis, Alexander D. FraserElise Fourré, René D. Garreaud, Christophe Genthon, Irina V. Gorodetskaya, Sergi González-Herrero, Victoria J. Heinrich, Guillaume Hubert, Hanna Joos, Seong Joong Kim, John C. King, Christoph Kittel, Amaelle Landais, Matthew Lazzara, Gregory H. Leonard, Jan L. Lieser, Michelle Maclennan, David Mikolajczyk, Peter Neff, Inès Ollivier, Ghislain Picard, Benjamin Pohl, F. Martin Ralph, Penny Rowe, Elisabeth Schlosser, Christine A. Shields, Inga J. Smith, Michael Sprenger, Luke Trusel, Danielle Udy, Tessa Vance, Étienne Vignon, Catherine Walker, Nander Wever, Xun Zou

Research output: Contribution to journalArticlepeer-review

2 Scopus citations

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.

Original languageEnglish (US)
Pages (from-to)757-778
Number of pages22
JournalJournal of Climate
Volume37
Issue number3
DOIs
StatePublished - Feb 10 2024

Bibliographical note

Publisher Copyright:
© 2024 American Meteorological Society.

Keywords

  • Antarctica
  • Atmospheric river
  • Automatic weather stations
  • Climate records
  • Extreme events

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