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The Extraordinary March 2022 East Antarctica "Heat" Wave. Part Ii: Impacts On The Antarctic Ice Sheet
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
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
WoS ID
WOS:001191392000001
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.
OCDE Subjects
Quartile (Date Issued)
Q1
License
acceso abierto