Volume 41 Issue 2
Feb.  2022
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Yang Zhang, Fei Chai, Joseph Zhang, Yang Ding, Min Bao, Yunwei Yan, Hong Li, Wei Yu, Liang Chang. Numerical investigation of the control factors driving Zhe-Min Coastal Current[J]. Acta Oceanologica Sinica, 2022, 41(2): 127-138. doi: 10.1007/s13131-021-1849-4
Citation: Yang Zhang, Fei Chai, Joseph Zhang, Yang Ding, Min Bao, Yunwei Yan, Hong Li, Wei Yu, Liang Chang. Numerical investigation of the control factors driving Zhe-Min Coastal Current[J]. Acta Oceanologica Sinica, 2022, 41(2): 127-138. doi: 10.1007/s13131-021-1849-4

Numerical investigation of the control factors driving Zhe-Min Coastal Current

doi: 10.1007/s13131-021-1849-4
Funds:  The Scientific Research Fund of the Second Institute of Oceanography, MNR under contract Nos JG2104 and 14283; the National Natural Science Foundation of China under contract Nos 41730536, 42076010 and 42130403; the Shanghai Pujiang Program under contract No. 19PJ1404300; the Shandong Natural Science Foundation under contract No. ZR2021MD007; the Project of State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, MNR under contract No. SOEDZZ2103; the Zhejiang Provincial Natural Science Foundation of China under contract No. LY21D060003.
More Information
  • Corresponding author: fchai@sio.org.cn
  • Received Date: 2020-10-16
  • Accepted Date: 2021-05-20
  • Available Online: 2021-12-01
  • Publish Date: 2022-02-01
  • During the northeast monsoon season, Zhe-Min Coastal Current (ZMCC) travels along the Chinese mainland coast and carries fresh, cold, and eutrophic water. ZMCC is significantly important for the hydrodynamic processes and marine ecosystems along its path. Thus, this bottom-trapped plume deserves to be further discussed in terms of the major driving factor, for which different opinions exist. For this purpose, in this study, a high resolution Semi-implicit Cross-scale Hydroscience Integrated System Model (SCHISM) is established and validated. High correlation coefficients exist between along-shelf wind speeds and seasonal variations of both ZMCC volume transport and the freshwater signal. These coefficients imply that the wind is important in regulating ZMCC. However, for similar annual mean ZMCC volume transports, the extreme south boundaries of Zhe-Min Coastal Water (ZMCW) are different among different years. This difference is attracting attention and is explored in this study. According to the low wind/discharge experiment, it was found that although the volume transport of ZMCC is more sensitive to the variation of local wind speeds, the carried freshwater is limited by the Changjiang River discharge, which ultimately determines the south boundary of ZMCW. The momentum analysis at transects I and II shows that, for driving ZMCC, the along-shore wind forcing is as important as the buoyancy forcing. Note that this conclusion is supported by a zero-discharge experiment. It was also found that the buoyancy forcing varies with respect to time and space, which is due to variations of the discharge of Changjiang River. In addition, a particle tracking experiment shows that the substance carried by the Changjiang River diluted water would distribute along the Zhe-Min coastal region during the northeast monsoon season and it may escape due to the wind relaxation.
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