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1·Only forcing in Sverdrup Model is wind stress.

风应力吧，没有风应力，何来流动？

2·To set the main wall of building hit by the wind directly as a slant to reduce the wind stress.

将建物的平面配置将主要面临风向的墙面，设定为斜面以减少风压力。

3·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。

4·The results show that the wind stress can always create a direct gyre below it in the sea with the same direction of rotation.

结果表明，风应力的作用总可在其下方的海洋中激发出与风应力旋转方向相同的直接涡旋。

5·The decadal variation of ITF is that the decadal signal lies in the change of latitude-oriented wind stress in the Equator-Pacific region.

ITF的年代际变化是：年代际信号取决于赤道太平洋纬向风应力的变化。

6·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。

7·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。

8·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。

9·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障碍层深度的季节变化，而海面降水对于季节平均的障碍层分布和变化都没有显著的影响。

10·The anomalous lift of the thermoclines was associated closely with the west wind anomaly and intensification of positive wind stress curl on both sides of the equator.

这种温跃层的异常上升是与事件期间此区西风异常的出现和赤道两侧正的风应力旋度增大有着密切关系。