Atmospheric River Brings Warmth and Rainfall to the Northern Antarctic Peninsula During the Mid‐Austral Winter of 2023

Author:

Bozkurt D.123ORCID,Carrasco J. F.4,Cordero R. R.5ORCID,Fernandoy F.6ORCID,Gómez‐Contreras A.7ORCID,Carrillo B.4ORCID,Guan B.8ORCID

Affiliation:

1. Departamento de Meteorología Universidad de Valparaíso Valparaíso Chile

2. Center for Climate and Resilience Research (CR)2 Santiago Chile

3. Center for Oceanographic Research COPAS COASTAL Universidad de Concepción Concepción Chile

4. Centro de Investigación Gaia Antártica Universidad de Magallanes Punta Arenas Chile

5. Departamento de Física Universidad de Santiago de Chile Santiago Chile

6. Facultad de Ingeniería Universidad Nacional Andrés Bello Viña del Mar Chile

7. Departamento de Geofísica Universidad de Chile Santiago Chile

8. Joint Institute for Regional Earth System Science and Engineering University of California Los Angeles Los Angeles CA USA

Abstract

AbstractContrasting the extensive research on summer atmospheric rivers (ARs) in the Antarctic Peninsula (AP), winter AR impacts are less understood. This study examines a unique warming event from 1 to 3 July 2023, using in situ winter observations and ERA5 reanalysis. On 2 July, Frei station experienced an extreme warm event with a temperature of 2.7°C and a significant rise in the freezing level, coinciding with winter rainfall. A pressure dipole pattern over the AP, with contrasting circulations over Bellingshausen and Weddell Seas, facilitated an AR, carrying warm, humid air initially from South America/Atlantic and then the southeast Pacific. This shift resulted in anomalous water stable isotope composition in precipitation. Trends suggest a strengthening winter pressure dipole, associated with increased AR frequency and higher temperatures in northern AP. These findings highlight the importance of winter observations in exploring AR impacts, bridging knowledge gaps about winter AR behaviors.

Publisher

American Geophysical Union (AGU)

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