The role of atmospheric and oceanic factors on the record low Antarctic sea ice extent of 2023

IF 4 1区 地球科学 Q1 GEOGRAPHY, PHYSICAL
M. Swathi , Avinash Kumar , Juhi Yadav , Rahul Mohan
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Abstract

In February 2023, the Antarctic Sea ice extent (SIE) reached a historic low of 1.7 million km2, which was 43 % lower than the monthly average extent recorded since 1979. This marked the second consecutive year of record lows, surpassing the minimum SIE from the previous year. Our study aims to understand the atmospheric and oceanic factors from September 2022 to August 2023 that contributed to these new lows. Throughout the study period, the monthly SIE consistently indicated lower extents compared to the long-term average. The Weddell Sea and Amundsen-Bellingshausen Sea (ABS) experienced the most decline in austral spring and summer, respectively, while the Ross Sea showed the minimum sea ice loss. The lower stratospheric cooling patterns observed during summer resulted in a reinforcement of the Southern Annular Mode (SAM), which caused intensification of the surface temperature inversion. This disturbance led to the Antarctic Polar Vortex shifting towards the Equator. The transition from the distinct triple La Niña event to the onset of a warm phase in 2023 resulted in the Amundsen Sea Low (ASL) deepening, which advected warm air into the region and push sea ice back towards the coast, reducing its extent particularly in the west of the Antarctic Peninsula region. Additionally, anomalies in the upper ocean (0–300 m) indicate subsurface ocean warming in most sectors.
大气和海洋因素对2023年南极海冰面积创历史新低的作用
2023年2月,南极海冰面积(SIE)达到170万平方公里的历史最低水平,比1979年以来记录的月平均面积低43%。这是该指数连续第二年创历史新低,超过了前一年的最低SIE。我们的研究旨在了解2022年9月至2023年8月期间造成这些新低点的大气和海洋因素。在整个研究期间,与长期平均值相比,月度SIE始终显示较低的程度。威德尔海(Weddell Sea)和阿蒙森-别令斯豪森海(Amundsen-Bellingshausen Sea, ABS)分别在春季和夏季海冰减少最多,罗斯海(Ross Sea)海冰减少最少。夏季观测到的平流层低层降温模式导致了南环模(SAM)的增强,这导致了地表温度逆温的增强。这种扰动导致南极极地涡旋向赤道移动。从明显的三重La Niña事件过渡到2023年暖期的开始,导致阿蒙森海低压(ASL)加深,将暖空气平流到该地区,并将海冰推向海岸,减少了其范围,特别是在南极半岛西部地区。此外,上层海洋(0-300米)的异常表明大部分扇区的次表层海洋变暖。
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来源期刊
Global and Planetary Change
Global and Planetary Change 地学天文-地球科学综合
CiteScore
7.40
自引率
10.30%
发文量
226
审稿时长
63 days
期刊介绍: The objective of the journal Global and Planetary Change is to provide a multi-disciplinary overview of the processes taking place in the Earth System and involved in planetary change over time. The journal focuses on records of the past and current state of the earth system, and future scenarios , and their link to global environmental change. Regional or process-oriented studies are welcome if they discuss global implications. Topics include, but are not limited to, changes in the dynamics and composition of the atmosphere, oceans and cryosphere, as well as climate change, sea level variation, observations/modelling of Earth processes from deep to (near-)surface and their coupling, global ecology, biogeography and the resilience/thresholds in ecosystems. Key criteria for the consideration of manuscripts are (a) the relevance for the global scientific community and/or (b) the wider implications for global scale problems, preferably combined with (c) having a significance beyond a single discipline. A clear focus on key processes associated with planetary scale change is strongly encouraged. Manuscripts can be submitted as either research contributions or as a review article. Every effort should be made towards the presentation of research outcomes in an understandable way for a broad readership.
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