碩士 / 國立臺灣大學 / 海洋研究所 / 86 / Analysising the bouy data of WOCE/KSVP, the RyuKyu arc showsits effect to
the path of Kuroshio. A branch of Kuroshio turns toeastward and moves as wav
es. Developing a barotropic numerical model to examine the influence of the r
idge across the Western boundary current. According to model results, the rid
ge leads toTaylor column effect, blocks the northward flow and forces it totur
n to eastward. Analysising the balance of vorticity, in the southern region o
f the ridge, some non-linear performance likerecirculation or Rossby wave can
be found, and it has almost thesame dynamic structure of the Northwestern regi
on of the generalwind-driven ocean circulation. The length of the ridge, its
location and the width of the channel between boundary and ridgedetermine the
pattern of this region.
| Identifer | oai:union.ndltd.org:TW/086NTU00274012 |
| Date | January 1998 |
| Creators | Kao, YingHsun, 高英勛 |
| Contributors | CHING-SHENG CHERN, JOE WANG, 陳慶生, 王冑, --- |
| Source Sets | National Digital Library of Theses and Dissertations in Taiwan |
| Language | zh-TW |
| Detected Language | English |
| Type | 學位論文 ; thesis |
| Format | 40 |
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