A regional and seasonal approach to explain the observed trends in the Antarctic sea ice in recent decades

• Published in: International Journal of Climatology
• Main Authors: Yu, Lejiang, Zhong, Shiyuan, Sui, Cuijuan, Sun, Bo
• Other Authors: National Natural Science Foundation of China, Norges Forskningsråd
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2023
• Subjects: Antarctic; Arctic; Indian; Pacific; Southern Ocean; The Antarctic; Antarc*; Sea ice
• Online Access: http://dx.doi.org/10.1002/joc.8010; https://onlinelibrary.wiley.com/doi/pdf/10.1002/joc.8010; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/joc.8010; https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.8010

Abstract In contrast to the declining sea ice extent across most of the Arctic in the past several decades, sea ice extent in the Antarctic has experienced opposite regional trends with regions of sea ice expansion exceeding those of contraction. Various mechanisms have been put forward to explain the Antarctic sea ice trends, but few have been successful at explaining a large portion of the observed trends. Dividing the Southern Ocean into the Pacific, Atlantic, and Indian Ocean sectors and examining the trends over 1979–2018 separately for each sector and for each season of the year, we are able to identify modes of variability that statistically explain more than 42% of the trends in all three sectors and all four seasons. In certain sector and season, up to 94% of the trends can be explained. The leading modes of variability that explain a substantial portion of the trends appear to be related to several known climate variability modes including the Southern Annular Mode (SAM), the Pacific South American (PSA) 1 and 2, and the Zonal Wavenumber 2–6 patterns. In the Atlantic and Indian Ocean sectors, the changes in the occurrences of the main contributing modes to sea ice trends are dominated by local sea‐surface temperature (SST) variations, while in the Pacific sector, they are related to changes in global SST.