The June 2022 extreme warm event in central West Antarctica

• Published in: Antarctic Science
• Main Authors: Evangelista, Heitor, Prado, Luciana F., Gorodetskaya, Irina V., Reis Passos, Heber, Nadal Villela, Franco, Sampaio, Marcelo, Alves dos Santos, Elaine, de Brito, Carla M.C.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press (CUP) 2023
• Subjects: Geology; Ecology, Evolution, Behavior and Systematics; Oceanography; Antarctic; Southern Ocean; The Antarctic; Antarctic Peninsula; West Antarctica; Pacific; Antarc*; Antarctic Science; Antarctica
• Online Access: http://dx.doi.org/10.1017/s0954102023000238; https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102023000238

Abstract The Antarctic surface mass balance has been shown to be sensitive to the impacts of atmospheric rivers (ARs), which bring anomalous amounts of both moisture and heat from lower latitudes poleward. Therefore, describing the characteristics of ARs and their intensity and frequency in the Antarctic regions by applying detection algorithms became a key method to evaluating their impacts on the surface mass balance and melting events. Several intense AR events have influenced Antarctica during the year 2022, and here we report an event with a peak on 10 June 2022 that was detected at 84°S, having a potential impact on West Antarctica. The extreme warm event originated in the Southern Pacific subtropical region and evolved towards the Southern Ocean, crossing the northern Antarctic Peninsula, before reaching as far as most inland regions in Antarctica, different from other typical ARs that are mostly restricted to the continental coast.