| NUMERICAL SIMULATION OF THE MINDANAO EDDY AND TROPICAL CURRENTS OF PACIFIC OCEAN |
| |
| 作者姓名： | 李荣凤 曾庆存 季仲贞 |
| |
| 作者单位： | LASG，Institute of Atmospheric Physics，Academia Sinica，Beijing，100080，LASG，Institute of Atmospheric Physics，Academia Sinica，Beijing，100080，LASG，Institute of Atmospheric Physics，Academia Sinica，Beijing，100080 |
| |
| 摘 要： | Results of numerical simulation of currents in the western North Tropical Pacific Ocean by using a barotropic primitive equation model with fine horizontal resolution agreed well with observations and showed that the Mindanao Cyclonic Eddy located north of the equator and east of Mindanao Island exists during most of the year with monthly (and large seasonal) variations in scope . strength and central location . In June , an anticyclonic eddy occurs northeast of Halmahera Island, strengthens to maximum in August , exists until October and then disappears . The observed large-scale circulation systems such as the North Equatorial Current . the Mindanao Current and the North Equatorial Countercurrent are all very well reproduced in the simulations.
|
| 收稿时间： | 12 April 1991 |
Numerical simulation of the Mindanao Eddy and Tropical Currents of Pacific Ocean |
| |
| Li Rongfeng,Zeng Qingcun,Ji Zhongzhen.NUMERICAL SIMULATION OF THE MINDANAO EDDY AND TROPICAL CURRENTS OF PACIFIC OCEAN[J].Chinese Journal of Oceanology and Limnology,1992,10(3):258-267. |
| |
| Authors: | Li Rongfeng Zeng Qingcun Ji Zhongzhen |
| |
| Institution: | (1) LASG, Institute of Atmospheric Physics, Academia Sinica, 100080 Beijing |
| |
| Abstract: | Results of numerical simulation of currents in the western North Tropical Pacific Ocean by using a barotropic primitive equation model with fine horizontal resolution agreed well with observations and showed that the Mindanao Cyclonic Eddy located north of the equator and east of Mindanao Island exists during most of the year with monthly (and large seasonal) variations in scope . strength and central location . In June , an anticyclonic eddy occurs northeast of Halmahera Island, strengthens to maximum in August , exists until October and then disappears . The observed large-scale circulation systems such as the North Equatorial Current . the Mindanao Current and the North Equatorial Countercurrent are all very well reproduced in the simulations. |
| |
| Keywords: | numerical simulation North Equatorial Current Mindanao Current North Equatorial Countercurrent Mindanao Eddy Halmahera Eddy |
| 本文献已被 CNKI SpringerLink 等数据库收录！ |
