Numerical study on the tidal front in the Western Yellow Sea
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Numerical study on the tidal front in the Western Yellow Sea
Numerical study on the tidal front in the Western Yellow Sea
海洋湖沼学报(英文)1993年11卷第4期 页码:305-313
Affiliations:
Institute of Oceanology
Author bio:
Funds:
Contribution No. 2224 from the Institute of Oceanology, Academia Sinica.;This work is a part of the M. S. thesis of Bi Yawen and supported by the National Natural Science Foundation of China.
Numerical study on the tidal front in the Western Yellow Sea[J]. 海洋湖沼学报(英文), 1993,11(4):305-313.
Yawen, B., Baoren, Z. Numerical study on the tidal front in the Western Yellow Sea., Chin. J. Ocean. Limnol. 11, 305–313 (1993). https://doi.org/10.1007/BF02850635
Numerical study on the tidal front in the Western Yellow Sea[J]. 海洋湖沼学报(英文), 1993,11(4):305-313. DOI: 10.1007/BF02850635.
Yawen, B., Baoren, Z. Numerical study on the tidal front in the Western Yellow Sea., Chin. J. Ocean. Limnol. 11, 305–313 (1993). https://doi.org/10.1007/BF02850635DOI:
Numerical study on the tidal front in the Western Yellow Sea
摘要
Abstract
The formation and evolution of the tidal front in the western Yellow Sea are studied by means of a two-dimensional model in which wind and tide mixing
sun radiation and wind stress
and realistic topography are incorporated. In this numerical study
the schemes employed are stable for time step Δt=900 s
so the model can be run for 4 months to simulate the front evolution. The authors examined the effects of mixing and atmospheric focing on the tidal front under conditions of: mixing and solar heating without wind stress on the sea surface; mixing
solar heating and 50 hours of wind stress; mixing
solar heating and long time periodical wind stress. Results show that (1) the tidal front forms at the beginning of May
and strengthens with the increasing of heat input
(2) the temperature structure in the shallow well-mixed water is dominated by mixing
while in the front and deeper stratified regions
it is controlled by the joint effects of (mainly) mixing and advection
(3) the currents and front all respond to the variation of wind stress on the sea surface with a time lag of 7 and 30 hours respectively
(4) the front strength and position can be affected by the Ekman transport.
关键词
Keywords
references
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