wind stress

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。

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Tidal force field the air-sea coupling modes of SSTA and wind stress over tropical Pacific

潮汐力场热带太平洋地区SSTA和风应力场的海气耦合模态

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Interaction between the tropical Pacific and the tropical Atlantic through the wind stress bridge was numerically studied with intermediate models of global tropical atmosphere and ocean.

利用中等复杂程度热带大气和海洋模式研究了热带太平洋和大西洋SST通过风应力桥梁的相互作用。

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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。

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Wind stress curl decreases, then sea level rises, and vice versa.

上游区风应力旋度减弱，海平面上升，反之亦然。

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Particularly, we research relation between speed of wind and water and cap stress.

特别地，定性研究了承台应力与下放时的风速和水流速度的关系。

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The energy sources and sinks for the oceanic general circulation include tidal forces, sea surface atmospheric pressure variations, wind stress, heating and cooling at the upper surface, freshwater flux, and geothermal heat flux.

驱动大洋环流的能源和能汇包括潮汐，海表大气压力脉动，风应力，海表加热和冷却，海表淡水通量，以及海底地热。

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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。

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The problems on the wind stress in large-scale bin

大型筒仓风应力问题

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Wind stress, nonlinear effect and the source depth of barotropic tide may change the amplitude of the internal tide;

风应力、非线性效应以及正压潮源地的深度等都可改变内潮的波动振幅；

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The magnitude of seasonally meridional migration in the location of the primary Polar Front ( PF1) is much less than that of the climatic monthly mean zero wind stress curl, but is near the mean position of zero wind stress curl.

第一极锋（PF1）位置的经向季节变化幅度远小于气候月平均零旋度线的经向季节变化幅度，但位于零旋度线的平均位置附近。

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Winter wind stress and continent slope are determinants for WUF to form.

风应力、大陆坡是冬季逆风流产生的决定因素。

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For the simulation of the wave fields of the East China Sea, analyzed wind data of NCEP and QSCAT/ NCEP blended wind data ( July 1999 later, with higher precision than the former) are used respectively in the calculation as input wind stress.

分别以NCEP再分析风场和QSCAT/NCEP的混合风场（1999年7月之后，比前者的空间精度要高）为输入风场，对东中国海海域的海面海浪场进行模拟。

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The reasons are as follows: the evolution of the northern cyclonic circulation system of the SCS mainly attributes to the existence and southbound extension of the cyclonic wind stress curl in the northwest of the SCS.

原因如下：南海北部气旋型环流系统的演变主要归于南海西北部气旋风应力涡度的存在和南扩。

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it indicates the wind stress curl associated with land topography may be an important mechanism to form those eddies that lie near southwest of taiwan island, northwest of luzon island and southwest of luzon island in winter.

结果表明与高山地形相关的风应力旋度场可能是冬季在台湾岛西南、吕宋岛西北及吕宋岛西南中尺度涡形成的动力机制。

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Sheets of newly formed sea ice break into pieces under stress of wind and waves.

大块新形成的海冰在风和海浪的作用下裂成碎片.

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Response of the Subtropical and subpolar gyres to wind stress anomalies in the North Pacific

北太平洋副热带海洋涡旋和副极地海洋涡旋对风应力异常的响应

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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La Nina事件对应。

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On the other hand, the wind stress curl anomaly also strengthens the subpolar gyre so as to cool the Kuroshio/ Oyashio Extension region ( KOE).

另一方面该风应力旋度变化也可增强副极地海洋涡旋，从而引起黑潮及其续流区（KOE）海温降低。

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POP Analysis of Wind Stress Anomalies in the Tropical Pacific Ocean

热带太平洋风应力距平场的主振荡型分析

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The Ekman pumping deduced by the curl of wind stress accounts mainly for the formation of the east branch.

海表风应力的旋度异常产生的Ekman抽吸是东支逆流形成的主要原因。

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The temporal response of calm sea to surface wind stress

海面对风应力的非定常响应

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