Upwelling front and two-cell circulation in a two-dimensional model

Takeshi Matsuno, Kensuke Takeuchi, Nobuo Suginohara

研究成果: ジャーナルへの寄稿記事

2 引用 (Scopus)

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
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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Wind stress
Coastal zones
upwelling
cells
geostrophic flow
pycnocline
downwelling
wind stress
oceans
heat
coasts
Hot Temperature
coast
ocean

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

Matsuno, Takeshi ; Takeuchi, Kensuke ; Suginohara, Nobuo. / Upwelling front and two-cell circulation in a two-dimensional model. :: Journal of the Oceanographical Society of Japan. 1978 ; 巻 34, 番号 5. pp. 217-221.
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