The third EOF indicates sea surface height of ACC in response to the wind stress field variability which is not zonally symmetric .

EOF的第三模态则体现了南极绕极流对南大洋表面 风 场东西方向不均匀变化的响应。

Then the response of the SCS to Typhoon Imbudo is examined using POM model which is driven by the wind stress calculated above by the wave model .

其次，采用上述计算的海面 风 应 力作为POM模式的驱动，研究了南海流场和温度对于台风的响应。

Physically it resembles very much the process of surface wave breakdown and saturation in the presence of a thin vortical surface drift layer induced by wind stress .

物理上，该机制很象存在由 风 应 力所致薄表面涡旋漂流层时表面波的破碎与饱和过程。

The seasonal variability of the wind stress is dominant in the formation of the SSH seasonal variability .

风的季节变化是南海SSH季节变化的主要原因。

Only forcing in Sverdrup Model is wind stress .

风 应力吧，没有 风 应 力，何来流动？

The calculation of limit equilibrium and wind stress of this structure have also been discussed in this paper .

文中还对这种结构的极限平衡计算和 风 应 力计算进行了探讨。

Therefore for the tropical Indian Ocean the results manifest that the IOD mode is mainly response to the asymmetry of wind stress anomaly .

可见，对于热带印度洋而言，IOD模态主要是对 风 应 力异常的响应。

The effects of zonal variation of western wind stress on tropical ocean-atmosphere coupling process

西风 应 力的纬向变化对热带海气耦合过程的影响

We obtain the role of vortex-induced vibration in the wind stress at the time under the hot spot location .

得到了塔架在 风涡激振动作用下热点处的 应 力时程曲线。

In addition we discussed the relationship between the cyclonic eddies and the local wind stress as well as the Kuroshio based on correlation and power spectrum analysis .

本文还利用相关分析、功率谱分析等，研究了局地 风 应 力和黑潮与吕宋西北海域气旋式涡旋的关系。

Wind stress vector over ocean waves .

作用于海洋波的 风 应 力矢量。

Wind stress and freshwater work as two important forcings over the Southern Ocean ( SO ) .

风 应 力和淡水通量是南大洋的两种重要外强迫。

The east boundary flow in Atlantic is more sensitive to sea surface heat flux than wind stress by the same external forcing ( 20 % ) .

此外，热通量异常还对南太平洋东海岸的 洋流和南极大陆的绕极环流有较为明显的影响。

The results show that wind stress anomalies play an important role in ENSO cycle .

结果表明，热带西太平洋地区的 风 应 力异常对ENSO循环有很重要的作用。

The second experiment incorporates wind stress anomalies over western equatorial Pacific .

第二个数值试验，在第一个数值模拟的基础上给定赤道西太平洋一个 风 应 力异常区，数值积分了几个月。

The action of wind stress and Kuroshio system on the circulation in the East China Sea

黑潮和 风 应 力对东中国海环流的作用

The second dynamical mechanism is because of the interaction between the wind stress and relief .

南海环流的动力机制有两个：最重要的动力因子为斜压场与地形相互作用项，其次为 风 应 力与地形相互作用项。

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 .

气压场对海温的升高也有一定的贡献。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。

The combination force of the slop of bottom with the baroclinic effect and wind stress makes the upwelling stronger .

倾斜的底形与斜压效应、 风 应 力的联合作用使吕泗海区的上升流更明显。

The sea surface wind stress and net heat flux affect the seasonal variation of water mass character in the PN section by changing the mixed layer depth every season .

海面 风 场和净热通量场通过改变混合层的深度影响PN断面处黑潮水和陆架水之间的混合，而海面降水对于PN断面上的水团分布特征没有显著影响。

THE WIND STRESS FIELD OVER THE SOUTH CHINA SEA The average follow-up time was 1 year .

南海的季节与年平均 风 应 力平均随访1年。

When east wind stress anomaly and meridional wind stress anomaly happen the La Nina events occur .

当 东风 应 力异常偏强及经向风应力异常向赤道南北两侧辐散偏强则与LaNina事件对应。

Numerical study on the role of vortical and divergent components of wind stress in ENSO cycle

风 应 力的旋转和辐散分量在ENSO循环中作用的数值试验研究

Wind stress curl has a periodic variation of two months .

风 应 力旋度有周期为2个月左右的变化。

The central equatorial Pacific is the area of the most frequent change in both zonal wind stress and current anomaly .

纬 向风 应 力和纬向流异常变化最显著的区域都在赤道中太平洋。

But in winter the effect of the wind stress on the Bohai Sea general circulation is dominant .

在冬季，渤海环流 应 是 风 应 力的作用占主导地位。

Wind stress and tidal dissipation are the primary sources of mechanical energy .

风和潮汐是最主要的机械能源。

^ calculation and analysis of wind stress and wind field in the world ocean

大洋 风 应 力和风场的计算与分析

Using wind stress data from NCEP-NCAR a prediction of the future low-frequency SST variability has been made .

利用NCEP-NCAR的 风 应 力再分析资料，本研究预报了上述海域SST的低频变异。

Sensitivity experiments of the response of tropical Pacific to the wind stress in an Oceanic General Circulation Model

热带太平洋对 风 应 力拖曳系数响应的敏感性试验