| 1. | 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。 |
| 2. | One is the change of the basic - state parameters ( e . g . , the zonal wind field ) ; the other is existence , in the real atmosphere , of instabilities not described in our model , like for instance , baroclinic instability
一个是基态参数（例如纬向风场）的变化；另一个在实际大气存在的不稳定（此模式未予涉及） ，例如斜压不稳定。 |
| 3. | The correlation between the transition dates in middle stratosphere and the ozone quantity in stratosphere . the correlation between the zonal wind of 10hpa and 70hpa and the transition dates of these two layers is remarkable
中平流层环流转型异常与赤道平流层纬向风准两年振荡( qbo )及平流层臭氧总量异常存在显著相关联系。 |
| 4. | In addition to the thermal reasons , the advection of arctic sea ice ( pacific section ) , which is the result of dynamic factors , is closely related to the frequency shift that occurred in chukchi sea
楚科奇海海冰范围的年际变化中存在由低频向高频变化的现象，该现象除了在局地气温变化中存在之外，在北冰洋区域风涡度、波弗特海纬向风、东西伯利亚海经向风等动力因素中也有所体现。 |
| 5. | 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。 |
| 6. | Moreover , as for average state , the crucial areas of wind stress acting on the two kinds of el nino exist different sites , and the zonal wind stress play a important role on eastern el nino models , the meridional wind stress , however , play a significant effect on the middle el nino models
此外，平均而言，风应力场对两类elnino作用的关键区也有所不同，而且纬向风应力对东部型elnino有重要作用，经向风应力对中部型elnino的产生则起着至关重要的作用。 |
| 7. | When the zonal wind of 10hpa is apheliotes ( zephyrus ) and that of 70hpa is zephyrus ( apheliotes ) , the transition delays ( advances ) . the correlation between the ozone quantity and the transition dates in middle stratosphere is opposite . when the ozone quantity is excessive ( lack ) , the transition advances ( delays )
分析发现10hpa及70hpa层的热带纬向风与相应层环流转型日期之间的相关显著， 10hpa热带东(西)风位相、 70hpa西(东)风位相时环流转型滞后(提早) 。 |
| 8. | Long scale oscillations in the meridional wind stress rebuild by pop analysis make the intention of el nino / la nina events deeply too . however , the change is slender and the range is adjacent with true position . we also draw a conclusion that the zonal wind stress is more important than the meridional wind stress in creating el nino / la nina evolution
保留在重建的经向风应力中的大尺度振荡成分也起到加强了elnino lanina事件的强度的作用，但强度比纬向风应力模拟的弱，与观测风应力模拟的强度相差不大，在空间范围上与观测风应力模拟的基本一致。 |
| 9. | Numerical studies suggest that long scale and slow - changed oscillations in the zonal wind stress rebuild by pop anal ysis make the intention of el nino / la nina events deeply . it also enlarges their range . but , positive and negative anomaly center is toward west than actual conditions
数值试验的结果表明，由pop重建的纬向风应力中缓慢变化的大尺度振荡成分加深了elnino lanina事件的强度，加大了它们的空间分布范围，但正负距平中心的位置比观测风应力模拟的情况偏西。 |
| 10. | It is showed that the heat transport crossing the equator has the similar magnitude and the same period of one year , compared with that of 10 n in arabian sea . by contrast , the heat transport across 10 n in bay of bengal has a much smaller value with a prominent semiannual period ; there are tight relationship between integrated zonal wind stress in one latitude of the indian ocean north of 7 n and the total heat transport across that latitude , as well as the total net surface heat flux north of that latitude . the maximum correlation coefficient is less than - 0 . 5
结果表明越赤道和越10on阿拉伯海的热输送量大小具有可比性，且有相同的年循环特征，而10on孟加拉湾纬度的经向热输送较小，且具有半年变化周期;俨s以北印度洋任一纬度上的纬向风应力异常与此纬度上的经向热输送异常以及此纬度以北印度洋总的海面净热通量异常有很好的相关关系，相关系数最大可达一0 . 5以上。 |
