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- Wind Stress Vector over Ocean Waves. 作用于海洋波的风应力矢量。
- Only forcing in Sverdrup Model is wind stress. 风应力吧，没有风应力，何来流动？
- Much progress has been made in the modeling of the equatorial oceans, which respond primarily to changes in the wind stress. 在对赤道海洋的模拟方面取得了很大的进展。赤道海洋主要对风应力变化作出响应。
- 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。
- When the wind stress curl reaches a maximum negative value in winter, an anticyclonic eddy develops and the flow in the study area is toward the south. 在风速最大的冬天，风应力旋度负值有最大值，会是一反气旋式涡流，呈顺时针方向旋转。
- The area extension of the anticyclonic wind stress curl is beneficial to the formation and development of the anticyclonic circulation to the west of Luzon Island. 反气旋风应力涡度范围的扩展有助于吕宋岛以西反气旋环流系统的形成和发展.
- 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 results show that, for the planetary scale ocean system, wind Stress can produce stable wind-driven ocean currents, and for the synoptic scale ocean system, it can only excite several ocean waves with different periods. 结果表明：对于行星尺度的海洋系统，大气风应力可以激发出比较稳定的风生洋流；而对于天气尺度以下的海洋系统，大气风应力则主要激发出几种不同周期的海洋波动。
- The negative maximum of the wind stress curl may determine the intensity of the Southern Antarctic Circumpolar Current Front(SACCF):The stronger the Ekman Pumping caused by the negative maximum of the wind stress curl is,the more intense the SACCF is. 风应力旋度负最大值很可能决定了南极绕极流锋(SACCF)的强度:负最大值越大,埃克曼抽吸越强,南极绕极深层水(CDW)向海面涌升程度越大,CDW与变性南极绕极深层水(MCDW)之间温盐梯度的深度范围越大,锋强度越强。
- The result shows that the atmosphere response to the ocean is mainly the Gill-type mode and simultaneously, the ocean is affected by Ekman pumping from the wind stress vorticity of the low level atmosphere. 结果显示;大气对海洋热力强迫的响应主要是Gill型;而大气又可以通过风应力旋度造成的Ekman抽吸作用来影响海洋;这种海气相互作用影响着ENSO循环的发展.
- The wind was whispering in the trees. 一阵风穿过树林沙沙作响。
- Stress can be the undoing of so many fine players. 紧张可能是这许多优秀选手失败的原因。
- The wind whirled the dead leaves about. 风吹得枯叶在四处回旋。
- The boat heeled over in a strong wind. 船在强风吹袭下倾侧了。
- The shutters thumped the wall in the wind. 在风中百叶窗砰砰地碰在墙上。
- This paper studies the interaction relationship between the Wind Stress (wind) field over the tropical Pacific and SST by use of the diagnostic analysis and numerical simulation on the basis of SST,850hpa wind data from NCEP/NCAR and FSU wind stress data. 本文根据NCEP/NCAR再分析海温、850hpa风场资料以及FSU风应力资料，利用诊断分析和数值模拟方法研究了热带太平洋风应力(风)场和海温的相互作用的关系。
- Based on the monthly analysis data of wind stress, which provided by FSU, typical wind stress patterns associated with the El Nino/La Nina are determined with the techniques of POP (Principal Oscillation Pattern) analysis. 本文利用FSU风应力逐月资料，运用POP分析方法，分析了热带太平洋地区风应力异常场结构与El Nino/La Nina事件的联系。
- The formation and the southbound movement of the anticyclonic circulation offshore to the middle of Vietnam is related to change of the zonal integral of the wind stress curl and the Sverdrup balance. 对于越南中部外海反气旋环流的形成和南移;看来是与纬向积分风应力涡度的改变和Sverdrup平衡有关.
- Besides, the effect of seasonal variation of wind stress, Ekman pumping and horizontal diffusivity on the ocean current and heat budget are studied, using both ideal model and complex model. 在此基础上，利用理想化的数值试验与数值模拟结果相结合的方式，证实了风应力的季节变化和Ekman抽吸，以及水平热量扩散系数对北印度洋海洋环流和热收支的影响。
- Twenty years of wind stress and SSTA data for the tropical Pacific are studied by the EOF method so that the characteristic modes of spacial distribution and features of temporal variation are revealed. 使用EOF分析方法对20年热带太平洋地区风应力场资料和SSTA资料进行分析，研究它们的空间分布特征模态和时间变化特征，发现风应力场的第一特征向量与海温距平场的第一特征向量的时间系数具有相同的变化特征。
