An Updated Estimate of the Indonesian Throughflow Geostrophic Transport: Interannual Variability and Salinity Effect

被引:5
作者
Guo, Yaru [1 ]
Li, Yuanlong [1 ,2 ]
Cheng, Lijing [3 ]
Chen, Gengxin [4 ]
Liu, Qinyan [4 ]
Tian, Tian [3 ,5 ]
Hu, Shijian [1 ,2 ]
Wang, Jing [1 ,2 ]
Wang, Fan [1 ,2 ]
机构
[1] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China
[2] Laoshan Lab, Qingdao, Peoples R China
[3] Chinese Acad Sci, Inst Atmospher Phys, Beijing, Peoples R China
[4] Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou, Peoples R China
[5] Natl Univ Def Technol, Coll Meteorol & Oceanog, Changsha, Peoples R China
基金
中国博士后科学基金;
关键词
Indonesian Throughflow; geostrophic transport; XBT-IX1; section; salinity component; uncertainty estimation; temperature component; SOUTHEAST INDIAN-OCEAN; SEA-LEVEL; LEEUWIN CURRENT; HEAT-CONTENT; PACIFIC; CIRCULATION; EXCHANGE; DIPOLE; PATHWAYS; IMPACTS;
D O I
10.1029/2023GL103748
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
While the pivotal role of the Indonesian Throughflow (ITF) in the global ocean circulation and climate has been widely recognized, accurate estimation of its volume transport based on observational data remains challenging. This work provides an updated estimate of the monthly ITF geostrophic transport (ITFG) in the upper 700 m at the IX1 section between Indonesia and Australia. The ITFG estimate is better constrained by improved data correction and new salinity data products. The mean ITFG of 1993-2018 is 8.2 & PLUSMN; 0.2 Sv, in which contributions of the temperature and salinity components (ITFT and ITFS) are 5.5 & PLUSMN; 0.2 and 2.8 & PLUSMN; 0.1 Sv, respectively. The interannual variability (& SIM;4.4 Sv in standard deviation) is dominated by ITFT, as the result of wind-driven thermocline dynamics, and slightly attenuated in amplitude by ITFS. The strengthening trend of 1.33 Sv decade(-1) during 1993-2018 primarily arises from ITFS and secondarily from ITFT.
引用
收藏
页数:10
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