Unprecedented mass gain over the Antarctic ice sheet between 2021 and 2022 caused by large precipitation anomalies

• Published in: Environmental Research Letters
• Main Authors: Wei Wang, Yunzhong Shen, Qiujie Chen, Fengwei Wang
• Format: Article in Journal/Newspaper
• Language: English
• Published: IOP Publishing 2023
• Subjects: Antarctic ice sheet; mass balance; GRACE/GRACE-FO; sea level change; climate change; Environmental technology. Sanitary engineering; TD1-1066; Environmental sciences; GE1-350; Science; Q; Physics; QC1-999; Antarctic; Antarctic Peninsula; Queen Mary Land; Southern Ocean; The Antarctic; Wilhelm II Land; Wilkes Land; Antarc*; Ice Sheet; Queen Mary land
• Online Access: https://doi.org/10.1088/1748-9326/ad0863; https://doaj.org/article/22e313ca8b174596a39935392170e449

The Antarctic ice sheet (AIS) is susceptible to global climate change, and its mass loss has been 92 ± 18 Gt yr ^−1 between 1992 and 2020. Given the current intensive global warming, we investigate the AIS mass changes from January 2003 to December 2022, using the newly released satellite gravimetry and atmospheric datasets. The results show that the continuous mass loss in the AIS between 2003 and 2020 was 141.8 ± 55.6 Gt yr ^−1 . However, the AIS showed a record-breaking mass gain of 129.7 ± 69.6 Gt yr ^−1 between 2021 and 2022. During this period, the mass gain over the East AIS and Antarctic Peninsula was unprecedented within the past two decades, and it outpaced the mass loss in the Amundsen sector of the West AIS from 2003 to 2022. Basin-scale analysis shows that the mass gain mainly occurred over Wilhelm II Land, Queen Mary Land, Wilkes Land, and the Antarctic Peninsula due to anomalously enhanced precipitation. Further investigation reveals that during 2021–2022, a pair of symmetrically distributed high-low pressure systems, located at approximately 120°W and 60°E in the Southern Ocean, drove the observed abnormal precipitation and mass accumulation.