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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. Fraser
  • Elise 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
    • CNRS Centre National de la Recherche Scientifique
    • ETH Zurich
    • Institute for Marine and Antarctic Studies
    • University of Colorado Boulder
    • Univ. Paris-Diderot
    • University of Wollongong
    • University of Johannesburg
    • EPFL CDM MTEI RAO
    • Universidad de Valparaiso
    • Center for Climate and Resilience Research (CR)2
    • British Antarctic Survey
    • KOPRI
    • Victoria University of Wellington
    • University of Chile
    • University of Tasmania
    • University of Toulouse
    • University of Wisconsin-Madison
    • University of Otago
    • University of Minnesota Twin Cities
    • University of Bergen
    • Université de Bourgogne
    • University of Innsbruck
    • National Center for Atmospheric Research
    • Pennsylvania State University

    Research output: Contribution to journalArticlepeer-review

    69 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 languageBritish English
    Pages (from-to)757-778
    Number of pages22
    JournalJournal of Climate
    Volume37
    Issue number3
    DOIs
    StatePublished - 10 Feb 2024

    Keywords

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

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