抄録
The intensification of upwelling front and two-cell circulation is studied numerically in a two dimensional level model. Upwelling front is set initially with longshore geostrophic flow. The uniform wind stress forces the ocean which has an infinite north-south coast line. Two-cell circulation, downwelling just inshore-side of the front and upwelling offshore-side, is induced, and the front is intensified. It is found that the intensification is occurred in the inshore-side of the front, and the intensification is basically due to the deviation from the thermal-wind balance, as is shown by Suginohara (1977). It is found that the inshore-side cell intrudes under the pycnocline. It seems to reproduce the observed two-cell circulation.
| 元の言語 | 英語 |
|---|---|
| ページ（範囲） | 217-221 |
| ページ数 | 5 |
| ジャーナル | Journal of the Oceanographical Society of Japan |
| 巻 | 34 |
| 発行部数 | 5 |
| DOI | |
| 出版物ステータス | 出版済み - 9 1 1978 |
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All Science Journal Classification (ASJC) codes
- Environmental Science(all)
- Soil Science
- Engineering(all)
- Earth-Surface Processes
- Earth and Planetary Sciences(all)
これを引用
Upwelling front and two-cell circulation in a two-dimensional model. / Matsuno, Takeshi; Takeuchi, Kensuke; Suginohara, Nobuo.
：: Journal of the Oceanographical Society of Japan, 巻 34, 番号 5, 01.09.1978, p. 217-221.研究成果: ジャーナルへの寄稿 › 記事
}
TY - JOUR
T1 - Upwelling front and two-cell circulation in a two-dimensional model
AU - Matsuno, Takeshi
AU - Takeuchi, Kensuke
AU - Suginohara, Nobuo
PY - 1978/9/1
Y1 - 1978/9/1
N2 - The intensification of upwelling front and two-cell circulation is studied numerically in a two dimensional level model. Upwelling front is set initially with longshore geostrophic flow. The uniform wind stress forces the ocean which has an infinite north-south coast line. Two-cell circulation, downwelling just inshore-side of the front and upwelling offshore-side, is induced, and the front is intensified. It is found that the intensification is occurred in the inshore-side of the front, and the intensification is basically due to the deviation from the thermal-wind balance, as is shown by Suginohara (1977). It is found that the inshore-side cell intrudes under the pycnocline. It seems to reproduce the observed two-cell circulation.
AB - The intensification of upwelling front and two-cell circulation is studied numerically in a two dimensional level model. Upwelling front is set initially with longshore geostrophic flow. The uniform wind stress forces the ocean which has an infinite north-south coast line. Two-cell circulation, downwelling just inshore-side of the front and upwelling offshore-side, is induced, and the front is intensified. It is found that the intensification is occurred in the inshore-side of the front, and the intensification is basically due to the deviation from the thermal-wind balance, as is shown by Suginohara (1977). It is found that the inshore-side cell intrudes under the pycnocline. It seems to reproduce the observed two-cell circulation.
UR - http://www.scopus.com/inward/record.url?scp=34250277868&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=34250277868&partnerID=8YFLogxK
U2 - 10.1007/BF02108634
DO - 10.1007/BF02108634
M3 - Article
AN - SCOPUS:34250277868
VL - 34
SP - 217
EP - 221
JO - Journal of the Oceanographical Society of Japan
JF - Journal of the Oceanographical Society of Japan
SN - 0029-8131
IS - 5
ER -