| 1. | A response of iap lasg oceanic general circulation model to the observed wind stress
海洋环流模式对风应力的响应 |
| 2. | Tangential wind stress
切向风应力 |
| 3. | The wind in summer dominates other seasons with annual mean westerly on the equator
夏季的风应力在一年中占有优势，在赤道上出现了西风。 |
| 4. | The authors also indicate that the local oscillation is worthy of consideration too
风应力异常的局地振荡对elnino lanina现象的影响也不应忽视。 |
| 5. | The negative wind stress curl in winter is basic driving mechanism responsible for the scs warm current
冬季南海暖流的一个基本驱动机制是南海北部负的风应力旋度。 |
| 6. | The variations of wind stress curl are dominated by the monsoons in japan sea and south china sea and the value is stronger in winter than in summer
日本海与南海的风应力旋度周期变化由其冬夏季风决定。冬季影响强于夏季。 |
| 7. | And this research also proves that heat flux influence predominantly the sst , but the impact of wind stress can reach the levels behind the isothermal layer
研究还证明了热通量对海温的影响主要出现在表层，而风应力的影响可以达到等温层以下。 |
| 8. | The results show that the oscillations of zonal wind stress have 35 47 57 months , the oscillations of meridional wind stress have 28 38 months
结果显示：纬向风应力有35 、 47和57个月周期的传播型振荡；经向风应力有28和38个月周期的传播型振荡。 |
| 9. | The mld of the ocean near the equator from 10 ? s to 10 ? n are less than 50 m and have no evident seasonal variability
而在10 s 10 n之间的赤道附近海域，因风应力和净热通量的季节变化不大，且该区降水量较大，浮力通量增加， mld较浅，低于50米，且没有明显的季节变化。 |
| 10. | In addition , the wind stress near the equator basically changes from west to east , resulting in southward ekman transport on both sizes of the equator
此外，在赤道附近风应力大致从赤道以南的向西变为赤道以北的向东，这意味着年平均意义上有跨越赤道向南的ekman流。 |
