| Wu Dexing. 1994. Preliminary study on the dynamic mechanism of the deep equatorial jets. Acta Oceanologica Sinica, (4):465－474 |
| Preliminary study on the dynamic mechanism of the deep equatorial jets |
| Preliminary study on the dynamic mechanism of the deep equatorial jets |
| Received:December 15, 1993 Revised:March 07, 1994 |
| DOI： |
| Key words:Deep equatorial jets buoyancy oscillation focus of waves energy boundary effects |
| 中文关键词: Deep equatorial jets buoyancy oscillation focus of waves energy boundary effects |
| 基金项目: |
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| Abstract: |
Observations show that the deep equatorial circulation is surprisingly energetic,with alteroating eastward and westward soml currents (these flows are commonly referred to as the deep equatorial jetis) betwew 1 000 and 3 000 m.This paper shows that the waves generated by an off-equatorial deep buoyancy oscillation,and their energy radiation as well as the equatorial focus of waves energy are the viable dynamic mechanisms of forming the deep equatorial jets.
The results of testing the effects of vertical mixing coefficients on the jets show that as the coefficients increase,the jets become waster and their tonal coherent scales become longer.
The solatbns for different periada of forcing indicate that lengthening the period of forcing results in the position of the core of the deep jets to moving westward and also enhances the tonal coherent scales of the jets. |
| 中文摘要: |
Observations show that the deep equatorial circulation is surprisingly energetic,with alteroating eastward and westward soml currents (these flows are commonly referred to as the deep equatorial jetis) betwew 1 000 and 3 000 m.This paper shows that the waves generated by an off-equatorial deep buoyancy oscillation,and their energy radiation as well as the equatorial focus of waves energy are the viable dynamic mechanisms of forming the deep equatorial jets.
The results of testing the effects of vertical mixing coefficients on the jets show that as the coefficients increase,the jets become waster and their tonal coherent scales become longer.
The solatbns for different periada of forcing indicate that lengthening the period of forcing results in the position of the core of the deep jets to moving westward and also enhances the tonal coherent scales of the jets. |
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