The results show that the leading wind stress anomalies field is correlated well with nino3 ssta and the correlation has appeared when the wind stress is prior to nino3 ssta by 8 months 研究结果表明，前期风应力距平场与nino3区ssta有很好的相关关系，这种相关性超前8个月时就有所显现。
In chapter three , we negative the nonliear terms in the system of equations which include surface pressure , wind stress and coriolis force terms . the height of the storm surge and the storm current can be seen as two terms 在第三章里，我们忽略了控制方程中的非线性项，将风暴潮潮高和风暴潮流分成气压效应和风应力效应的叠加。
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elnino lanina事件的联系。
A series of numerical experiments were carried out to reveal the roles of the following effects in driving the circulation : 1 ) topography , 2 ) wind stress curl , 3 ) p effect , 4 ) inertial effect and 5 ) open boundary inflow / outflow 实验中考虑以下动力因子对南海冬夏季环流的影响： 1 )地形， 2 )风应力旋度， 3 )效应， 4 )惯性效应， 5 )开边界流量驱动。
The results are as follows : ( 1 ) the 925hpa necp / ncar reanalysis wind stress anomaly ( hereafter referred to as necp wind stress anomaly ) is more fit to observed ssta than the fsu wind stress anomaly both in 1980s and in 1990s 结果表明： ( 1 ) 80 、 90年代925hpancep ncar再分析风应力距平(以下简称ncep风应力距平)较fsu风应力距平与观测的ssta匹配更为合理。
( 5 ) the decadal variations of quasi - quadrennial and quasi - biennial components of wind stress fields make west wind anomaly of east pacific and meridional wind stress anomaly converging upon the equator stronger since 1980s ( 5 )风应力距平场具有空间非对称性，同时又有时间非对称性： 80年代以后，太平洋中部的西风异常偏强；从赤道两侧向赤道辐合的经向风应力异常偏强。
When the effect of surface wave breaking is considered , mld is 50 cm deeper than that obtained without wave breaking , and with the enhancement of wind stress forcing , the deepening of mld is increased 模拟结果表明，当考虑波浪破碎的影响时，混合层深度比无波浪影响时的结果加深了约50cm ；随着风应力作用的增加，波浪破碎加强了混合层中的湍流混合，促使加深幅度也增加。
With the reduction of the leading time , the location of the zonal wind stress area influencing nino3 ssta expands toward the middle pacific from the eastern pacific , as well as the meridional wind stress in the eastern pacific and the western pacific 影响nino3区ssta的纬向风应力区域的位置随风应力超前的时间缩短由东太平洋向中太平洋扩展，经向风应力区域的位置由东太平洋和西太平洋向中太平洋移动。
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。
Although sea surface temperature anomaly center generally occur in the equatorial eastern pacific , key zone of pre - wind stress anomaly forcing signal related to ssta lies in the central western pacific . both diagnostic and numerical analyses results show this idea 热带太平洋海温异常的关键区虽然在赤道东太平洋，但与海温异常显著相关的前期风应力(风)强迫作用的位置在中西太平洋，这一点从诊断分析和数值模拟的结果中都可以得到。
