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Antarctica and the Southern Ocean

journal contribution
posted on 2025-10-15, 04:31 authored by MN Raphael, KR Clem, Mohamed Adjou, Susheel Adusumilli, Charles Amory, Mahsa Bahrami, Rebecca Baiman, Alison F Banwell, Sandra Barreira, Rebecca L Beadling, Steve Colwell, Lawrence Coy, Rajashree T Datta, Jos De Laat, Marcel du Plessis, Ryan L Fogt, Helen A Fricker, Alyce HancockAlyce Hancock, Bryan Johnson, Simon A Josey, Linda M Keller, Christoph Kittel, Natalya A Kramarova, Leslie R Lait, Matthew A Lazzara, Jan LieserJan Lieser, Michael MacFerrin, Michelle L MacLennan, Robert A Massom, David E Mikolajczyk, James Milward, Thomas L Mote, Paul A Newman, Taylor Norton, Irina Petropavlovskikh, Luciano P Pezzi, Phillip Reid, Thomas J Ryan-Keogh, Michelle L Santee, Theodore Scambos, Cristina Schulz, Jia-Rui Shi, Everaldo Souza, Sharon Stammerjohn, Sandy Thomalla, Luke Trusel, Jonathan D Wille
<div> <div> <div> <p>In 2024, atmospheric conditions over Antarctica exhibited significant anomalies, and were marked by major surface and stratospheric warming and pressure fluctuations. The first half of the year (January–June) featured persistent below-normal surface pressure over the continent, a distinct zonal wavenumber-3 pattern with three deep atmospheric troughs extending over the Weddell Sea, Prydz Bay, and Ross Ice Shelf, and a positive phase of the Southern Annular Mode, with strong circumpolar westerlies. Surface pressure anomalies in February and April were par- ticularly pronounced, with multiple stations recording record-low pressures. [...]</p> </div> </div> </div><p></p>

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    DOI - Is supplement to Antarctica and the Southern Ocean

Sub-type

  • Article

Publication title

Bulletin of the American Meteorological Society

Volume

106

Issue

8

Pagination

s357-s400

eISSN

1520-0477

ISSN

0003-0007

Department/School

Australian Antarctic Program Partnership, Oceans Ice and Climate

Publisher

American Meteorological Society

Publication status

  • Published

Rights statement

© 2025 American Meteorological Society

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