[A-OS18] 海洋物理学一般

[AOS18-17] Upper ocean salinity variability and impact in the Southeast Indian Subantarctic Mode Water formation region during the Argo era

*WANDI JING¹、RONGHUA ZHANG¹、YIYONG LUO² (1.NUIST、2.OUC)

キーワード：Mixed layer salinity, Interannual variability, Mixed layer depth, horizontal advection

Salinity is a state variable that determines the fundamental physical properties of the ocean, and understanding its changes and effects has important implications for the regional and global climate system. Based on Argo observations, changes in upper ocean salinity and their impacts in the Southeast Indian Subantarctic Mode Water (SEISAMW) formation region are investigated from 2004 to 2022. The upper ocean salinity in this region shows significant interannual variability, being relatively salty during 2010–2016 and fresh during 2005–2008 and 2019–2022, respectively. A diagnostic analysis indicates that the interannual variability of winter mixed layer depth and stratification are mainly affected by upper ocean salinity rather than temperature. In the SEISAMW formation region, higher upper ocean salinity acts to weaken the stratification and deepen the mixed layer. Conversely, lower upper ocean salinity acts to strengthen the stratification and shallow the mixed layer. A mixed layer salinity (MLS) budget analysis reveals that horizontal advection, predominantly influenced by meridional Ekman advection, governs the interannual variability of MLS. Furthermore, the interannual variability of meridional Ekman advection is mainly affected by zonal wind stress.