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  4. The Extraordinary March 2022 East Antarctica "Heat" Wave. Part I: Observations And Meteorological Drivers
 
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The Extraordinary March 2022 East Antarctica "Heat" Wave. Part I: Observations And Meteorological Drivers

Journal
Journal of Climate
Date Issued
2024-02-10
Author(s)
Jonathan D. Wille
Simon P. Alexander
Charles Amory
Rebecca Baiman
Léonard Barthélemy
Dana M. Bergstrom
Alexis Berne
Hanin Binder
Juliette Blanchet
Bozkurt, Deniz  
Facultad de Ciencias  
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
Étienne Vignon
Catherine Walker
Nander Wever
Xun Zou
DOI
10.1175/jcli-d-23-0175.1
WoS ID
WOS:001190317700001
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.
Subjects

Atmospheric Science

Meteorology And Atmos...

OCDE Subjects

Natural Sciences::Phy...

Quartile (Date Issued)
Q1
License
acceso abierto

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