The Role of the Southern Hemisphere Polar Cell on Antarctic Sea Ice Variability  

作　　者：Praveen Rao Teleti Alvarinho J. Luis Praveen Rao Teleti;Alvarinho J. Luis(Earth System Science Organization, National Centre for Antarctic and Ocean Research, Ministry of EarthSciences, Govt. of India, Headland Sada, Goa, India)

机构地区：[1]Earth System Science Organization, National Centre for Antarctic and Ocean Research, Ministry of EarthSciences, Govt. of India, Headland Sada, Goa, India

出　　处：《International Journal of Geosciences》2016年第2期120-134,共15页地球科学国际期刊（英文）

摘　　要：The study explores modes of variability in the Southern Polar Cell and their relationship with known global climate modes and Antarctic sea ice. It is found that Polar Cell is barotropic in nature and 500 hPa geo-potential height (Z₅₀₀) field can satisfactorily represent variability in the Polar Cell. First, three leading Empirical Orthogonal Function (EOF) modes of Z₅₀₀ account for nearly 80% of observed variability in the Polar Cell. Dominant mode (PC1₅₀₀) comprises of high pressure divergence zone over Antarctica. Second leading mode (PC2₅₀₀) is low pressure zone covering Amundsen-Bellingshausen Sea (ABS) similar to ABS low feature. A new climate mode called Polar Coastal Index (PCI) is defined, which describes more than 15% and close to 30% variability of circumpolar trough and ABS low, respectively. Out of four modes defined in this study, only PCI and PC2₅₀₀ show linear trends and clear seasonality. Interestingly, both modes are affected by modulation of ABS low due to tropical ENSO forcing. SAM signature is present in Polar Cell as PC1₅₀₀ shares large variance with it. The largest impact on sea ice comes from PC2₅₀₀ followed by PC1₅₀₀ in the Antarctic Dipole regions. However, this study suggests contemporary sea ice trends cannot be sustained, and can reverse given that trends in PCI and PC2₅₀₀ favour a reversal. These results indicate that ENSO-driven Polar Cell variability plays a crucial role influencing Antarctic sea ice as it interacts with other climate modes and leads the combined impact at the interannual time scale.The study explores modes of variability in the Southern Polar Cell and their relationship with known global climate modes and Antarctic sea ice. It is found that Polar Cell is barotropic in nature and 500 hPa geo-potential height (Z₅₀₀) field can satisfactorily represent variability in the Polar Cell. First, three leading Empirical Orthogonal Function (EOF) modes of Z₅₀₀ account for nearly 80% of observed variability in the Polar Cell. Dominant mode (PC1₅₀₀) comprises of high pressure divergence zone over Antarctica. Second leading mode (PC2₅₀₀) is low pressure zone covering Amundsen-Bellingshausen Sea (ABS) similar to ABS low feature. A new climate mode called Polar Coastal Index (PCI) is defined, which describes more than 15% and close to 30% variability of circumpolar trough and ABS low, respectively. Out of four modes defined in this study, only PCI and PC2₅₀₀ show linear trends and clear seasonality. Interestingly, both modes are affected by modulation of ABS low due to tropical ENSO forcing. SAM signature is present in Polar Cell as PC1₅₀₀ shares large variance with it. The largest impact on sea ice comes from PC2₅₀₀ followed by PC1₅₀₀ in the Antarctic Dipole regions. However, this study suggests contemporary sea ice trends cannot be sustained, and can reverse given that trends in PCI and PC2₅₀₀ favour a reversal. These results indicate that ENSO-driven Polar Cell variability plays a crucial role influencing Antarctic sea ice as it interacts with other climate modes and leads the combined impact at the interannual time scale.

关 键 词：ANTARCTICA Sea Ice Polar Cell PCI ENSO TELECONNECTION 

分 类 号：P73[天文地球—海洋科学]