wind stress的例句大全

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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the monthly mean fsu ( florida state university) wind stress data for the period 1960-1991 are decomposed into a vortical and a divergent component with each of which to force the model ocean in the context of a 2 layer tropical pacific model.

将1960～1991年的月平均FSU风应力资料分解为旋转部分和辐散辐合部分，分别用以强迫模式海洋。所用的模式为一个2层热带太平洋区域海洋模式。

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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。

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synchronous response of tropical ocean to meridional and zonal wind stress

热带大洋对纬向和经向风应力的联合响应

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variability of tropical pacific subsurface physical quantity fields and their correlations with zonal wind stress

赤道太平洋次表层要素变化特征及其与表面风应力关系

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air-sea gas transfer: its dependence on wind stress, small-scale roughness, and surface films

海-气的气体转换：它随风应力，小尺度粗糙度和陆面轻烟雾的变化

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wind stress anomaly on enso time scales in complex models

大气环流模式对ENSO时间尺度风应力距平的模拟

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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。

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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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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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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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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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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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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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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 problems on the wind stress in large-scale bin

大型筒仓风应力问题

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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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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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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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