| Double Kelvin waves along the Okinawa Trough in the East China Sea——Ⅰ. Analytic solutions and observations |
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| 引用本文： | Wang Ji,Yuan Yeli. Double Kelvin waves along the Okinawa Trough in the East China Sea——Ⅰ. Analytic solutions and observations[J]. 海洋学报(英文版), 1994, 13(1): 1-21 |
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| 作者姓名： | Wang Ji Yuan Yeli |
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| 作者单位： | Department of Applied Ocean Physics and Engineering, Woods Hole Oceanographic Institution, Woods Hole, MA 02543 USA;Laboratory of Geophysical Fluid Dynamics, First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China |
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| 摘 要： | ＤｏｕｂｌｅＫｅｌｖｉｎｗａｖｅｓａｌｏｎｇｔｈｅＯｋｉｎａｗａＴｒｏｕｇｈｉｎｔｈｅＥａｓｔＣｈｉｎａＳｅａ－ⅠＡｎａｌｙｔｉｃｓｏｌｕｔｉｏｎｓａｎｄｏｂｓｅｒｖａｔｉｏｎｓ￥ＷａｎｇＪｉａａｎｄＹｕａｎＹｅｌｉ（ＲｅｃｅｉｖｅｄＯｃｔｏｂｅｒ２...
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| 收稿时间： | 1991-10-25 |
| 修稿时间： | 1993-06-05 |
Double Kelvin waves along the Okinawa Trough in the East China Sea——Ⅰ. Analytic solutions and observations |
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| Wang Jia and Yuan Yeli. Double Kelvin waves along the Okinawa Trough in the East China Sea——Ⅰ. Analytic solutions and observations[J]. Acta Oceanologica Sinica, 1994, 13(1): 1-21 |
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| Authors: | Wang Jia and Yuan Yeli |
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| Affiliation: | 1.Department of Applied Ocean Physics and Engineering, Woods Hole Oceanographic Institution, Woods Hole, MA 02543 USA2.Laboratory of Geophysical Fluid Dynamics, First Institute of Oceanography, State Oceanic Administration, Qingdao 266003, China |
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| Abstract: | This study analytically examines the possible presence of double Kelvin waves along the Okinawa Trough in the East China Sea. Not only was the response of sea level to transient and time-periodic wind forcing from the north confirmed following Mysak (1969),but also to steady-state and moving wind forcings was examined according to the realistic wind fields in the East China Sea. Double Kelvin waves generated by these forcings, due to the discontinuous depth trapping, propagate southward and disperse. Finally, these dispersive waves shift to free ones. The moored current meter observations in summer and winter of 1987 along the Okinawa Trough supported the analytic solutions. There was a southward propagating current fluctuation with a speed of 0.32 m/s along the escarpment which was documented by Lin and Guo (1990). |
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