On multiple solutions to a low-spectrum model of oceanic current driven by the boundary force—The bimodality of the Kuroshio south of Japan[J]. 海洋湖沼学报(英文), 1996,14(2):113-120.
Chang-ming, D., Shui-ming, C., Qing-hua, Z. et al. On multiple solutions to a low-spectrum model of oceanic current driven by the boundary force—The bimodality of the Kuroshio south of Japan., Chin. J. Ocean. Limnol. 14, 113–120 (1996). https://doi.org/10.1007/BF02850367
On multiple solutions to a low-spectrum model of oceanic current driven by the boundary force—The bimodality of the Kuroshio south of Japan[J]. 海洋湖沼学报(英文), 1996,14(2):113-120. DOI: 10.1007/BF02850367.
Chang-ming, D., Shui-ming, C., Qing-hua, Z. et al. On multiple solutions to a low-spectrum model of oceanic current driven by the boundary force—The bimodality of the Kuroshio south of Japan., Chin. J. Ocean. Limnol. 14, 113–120 (1996). https://doi.org/10.1007/BF02850367DOI:
On multiple solutions to a low-spectrum model of oceanic current driven by the boundary force—The bimodality of the Kuroshio south of Japan
摘要
Abstract
This low-spectrum model study on the multiple solutions to a nonlinear quasi-geostrophic oceanic current equation shows that they depend on the combination ofRo
Re
λ and ε
that the bimodality of the Kuroshio depends strongly on the nonlinear effect represented byRo and λ
and that its occurrence probability is reduced by the dissipation represented byRe and ε. The stability of solutions is discussed in detail with Hurwitz's theory.
关键词
Keywords
references
Dong Changming, Zhang Qinghua, 1993. On the Bimodal Characteristics of the Kuroshio South of Japan. PACON Symposium. China Ocean Press. Beijing pp. 341–350.
Ji Zhongzheng, Zheng Chaozhou, 1990. The multiple solutions to a low-spectrum model of wind-driven ocean current equation.Scientia Atmos. Sinica 14(4): 395–403. in Chinese)
Masuda, A., 1982. On the interpretation of the bimodal characteristic of the stable Kuroshio path.Deep Sea Res. 29: 471–484.
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Yoon, J., Yasuda, I., 1987. Dynamics of the Kuroshio large meander. two-layer model.J. P. O. 17: 66–81.
Veronis, G., 1963. An analysis of wind-driven ocean circulation with a limited number of Fourier component.J. Atmos. Sci. 20: 577–593.
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