| 南海上层流场对Frankic(9606)强热带风暴响应的数值计算 |
| |
| 引用本文： | 李东辉,张铭.南海上层流场对Frankic(9606)强热带风暴响应的数值计算[J].海洋预报,2003,20(4):56-63. |
| |
| 作者姓名： | 李东辉 张铭 |
| |
| 作者单位： | 解放军理工大学气象学院,江苏,南京,211101 |
| |
| 基金项目： | 国家自然科学基金(40076009、4017600);中国科学院知识创新工程项目(KZCX1-SW-01-16和KZCX2-205)资助. |
| |
| 摘 要： | 本文用一个三维、自由表面、斜压海洋模式计算了南海上层流场对Frankic(9606)强热带风暴的响应。结果表明：南海表层流场对Frankic的响应时间在1d之内，其流场结构与气旋型风场的对应十分吻合；表层以下流场对Frankic的响应时间随深度的增加而加大：Frankic经过的海域，海面起伏有不同程度的抬高。
|
| 关 键 词： | 南海 上层流场 数值计算 强热带风暴 热带气旋 |
| 文章编号： | 1003-0239(2003)04-0056-08 |
| 修稿时间： | 2003年3月7日 |
NUMERICAL CALCULATION OF THE RESPONSE OF UPPER CURRENTS FIELD OF SOUTH CHINA SEA TO FRANKIC (9606) SEVERE TROPICAL STORM |
| |
| Li Dong-hui,Zhang Ming.NUMERICAL CALCULATION OF THE RESPONSE OF UPPER CURRENTS FIELD OF SOUTH CHINA SEA TO FRANKIC (9606) SEVERE TROPICAL STORM[J].Marine Forecasts,2003,20(4):56-63. |
| |
| Authors: | Li Dong-hui Zhang Ming |
| |
| Abstract: | A three-dimensional baroclinic model with a free surface has been employed to calculate the response of upper current field to Frankic (9606) severe tropical storm in South China Sea (SCS). The results are that: the response of surface currents field to the wind filed changes of Frankic only need one day, and the deeper of the ocean, the slower of the response rate, the configuration of surface ocean currents are well related with the corresponding cyclonic wind field, sea surface elevations are risen to some extent while Frankic passes. |
| |
| Keywords: | numerical calculation South China Sea upper current field response |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
