| Luo Yiyong,Yu Guangyao,Huang Zuke. 1998. Numerical studies of upwelling in coastalareas of the East China Sea——Ⅰ The tide-induced upwelling. Acta Oceanologica Sinica, (1):15-25 |
| Numerical studies of upwelling in coastalareas of the East China Sea——Ⅰ The tide-induced upwelling |
| Numerical studies of upwelling in coastalareas of the East China Sea——Ⅰ The tide-induced upwelling |
| Received:October 08, 1996 Revised:February 15, 1997 |
| DOI: |
| Key words:East China Sea tide-induced horizontal residual current tide-induced upwelling sea bottom topography with a steep slope |
| 中文关键词: East China Sea tide-induced horizontal residual current tide-induced upwelling sea bottom topography with a steep slope |
| 基金项目:This project was supported by the National Natural Science Foundation of China under contract No. 49136143. |
|
| Hits: 776 |
| Download times: 604 |
| Abstract: |
| The M2 constituent in the coastal areas of the East China Sea is computed based on three-dimensional nonlinear tidal wave equations.The distributions of the tide-induced horizontal residual currents and the tide-induced vertical residual currents indicate that there exists a coastal upwelling stripe off Fujian and Zhejiang with a width of 40 km or so.The computed largest upwelling, 0.5×10-3 cm/s, occurs between 10 and 20 m levels. |
| 中文摘要: |
| The M2 constituent in the coastal areas of the East China Sea is computed based on three-dimensional nonlinear tidal wave equations.The distributions of the tide-induced horizontal residual currents and the tide-induced vertical residual currents indicate that there exists a coastal upwelling stripe off Fujian and Zhejiang with a width of 40 km or so.The computed largest upwelling, 0.5×10-3 cm/s, occurs between 10 and 20 m levels. |
|
HTML
View Full Text
View/Add Comment Download reader |
| Close |