赤道重力陷波在近赤道区海流运动中的作用THE ROLE OF THE EQUATORIAL TRAP WAVE IN EQUATORIAL CURRENT MOVEMENT
侍茂崇
摘要(Abstract):
对小风天气条件下表层海流观测资料进行能谱密度分析,指出:东分量海流具有很明显的0.51d、3.9d和7.7d周期。0.51d是半日潮周期,即12h25min的周期;3.9d周期恰与赤道重力陷波n=2相对应,这是南纬3°~4°范围内一个重要波动;7.7d则是大小潮周期。而在北分量海流能谱中,则只有潮流0.51d和7.7d周期,3.9d周期消失,它进一步说明陷波的特征。此外,还用7m和40m层流资料与表层流进行对比,两者变化规律基本一致。
关键词(KeyWords): 陷波;海流;赤道;周期;能谱
基金项目(Foundation):
作者(Author): 侍茂崇
DOI: 10.16441/j.cnki.hdxb.1993.s2.005
参考文献(References):
- [1] Matsuno. T., Quasi-geostrophic motions in the equatorial area. J. Meteorol. Soc. Jpn. 1966, 44. 25-43
- [2] Moore. D. W., Planetary-gravity waves in an equatorial ocean Ph. D. Thesis. Harvard university, Cambridge. Massachusetts. 1968.
- [3] Dighthill, M. J., Dynamic response up the Indian ocean to on-set of the southwest Mansoon. Philos. Trans. R. Soc. London, Ser. A 1969 .265. 45-92.
- [4] Moore. D. J., and philander, S. G. H., Modeling of the tropical ocean circulation. In "the sea"(E. D. Doldberg. I. N. Mccave. J. J. O Bricn and J. H. Stecle. eds 1977. Vol. 6. pp. 319-362. Wileg. NewYork
- [5] Cane, M.. and Saracnik. E., The response of a liner baroclinic equatorial ocean to periodic forcing. J. Mar. Res. 1981. 39. 651-693
- [6] Knox, R. A., On a long series of measurements of Indian ocean equatorial currents near Addu Afoll. Deep-Sea Res. 1976, 23. 211-221
- [7] Enrson, C.. Evidence for a continuous spectrum of equatorial waves in the Indian Ocean. J. Geophys. Res. 1980. 85. 3285-3303
- [8] A. E.. Atmosonere-Ocean Dynamics 1982. pp. 440-444. Academic Press A subsidiary of Harcourt Brace lovanovicn publishers
文章评论(Comment):
|
||||||||||||||||||
|
||||||||||||||||||