Journal of Tropical Oceanography ›› 2023, Vol. 42 ›› Issue (2): 1-8.doi: 10.11978/2022055CSTR: 32234.14.2022055

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The role of alongshore wind and ocean wave in generating the northward Somali Current

CHU Xiaoqing1,2(), PENG Qihua3   

  1. 1. State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
    2. Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou 511458, China
    3. Scripps Institution of Oceanography (University of California, San Diego), La Jolla 92093, USA
  • Received:2022-03-23 Revised:2022-05-19 Online:2023-03-10 Published:2022-06-07
  • Contact: CHU Xiaoqing. email: chuxq@scsio.ac.cn
  • Supported by:
    National Natural Science Foundation of China(42076021); National Natural Science Foundation of China(42005035); Guangdong Basic and Applied Basic Research Foundation(2021A1515011534)

Abstract:

By analyzing reanalysis data and conducting ocean modes experiments, this study investigates the seasonal variation and dynamics of the norward Somali current (NSC) in the tropical Indian Ocean. The results show that the NSC starts from May, gradually strengthens and extends norward to 15°N during August-September, and forms a strong anti-cyclonic circulation — the Great Whirl. The NSC weakens significantly in late October, and disappears in November. The NSC results from local alongshore wind forcing and westward propagational Rossby waves. During May-July, alongshore wind forcing induces the East African Coast Current (EACC) to cross the equator to form the NSC. From August to October, even without alongshore wind forcing, the Rossby waves together with EACC can still form the NSC. Further analysis suggests that, although alongshore wind forcing incudes near-shore current, the Great Whirl is caused primarily by the Rossby waves. This research reveals dynamics of the NSC, and provides substantial evidences for ocean waves modulating ocean currents.

Key words: northward Somali Current, ocean waves, local wind forcing, seasonal variation, the tropical Indian Ocean