meridional stress 中文意思是什麼
meridional stress
解釋
經線應力- meridional : adj. 1. 子午圈[線]的；最高的，全盛的。2. 南歐（人）的，法國南部人的；南方的。n. 南歐人，（尤指）法國南部人。
- stress : n 1 壓力，壓迫，緊迫，緊張。2 【語音】重音；重讀；【詩】揚音；語勢，著重點。3 重要（性），重點，...
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( 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 ）風應力距平場具有空間非對稱性，同時又有時間非對稱性： 80年代以後，太平洋中部的西風異常偏強；從赤道兩側向赤道輻合的經向風應力異常偏強。 -
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，風應力場對兩類elnino作用的關鍵區也有所不同，而且緯向風應力對東部型elnino有重要作用，經向風應力對中部型elnino的產生則起著至關重要的作用。 -
All these results confirm the important of wind in meridional circulation and heat transport. based on mom2 model, a rectangular basin model with ideal w ind stress and other ideal conditions is designed to study the main processes and dynamical mechanism in setting the depth of cross - equator flow. the effects of horizontal diffusivity, seasonal variations of
我們還通過全球海洋環流模式，進一步證實了風應力的季節變化在北印度洋熱收支、 sst以及海洋環流變化中的作用:即包含風應力的季節變化將使長期平均的sst降低，海面凈熱通量增加。 -
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
結果顯示：緯向風應力有35 、 47和57個月周期的傳播型振蕩；經向風應力有28和38個月周期的傳播型振蕩。 -
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
影響nino3區ssta的緯向風應力區域的位置隨風應力超前的時間縮短由東太平洋向中太平洋擴展，經向風應力區域的位置由東太平洋和西太平洋向中太平洋移動。 -
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
保留在重建的經向風應力中的大尺度振蕩成分也起到加強了elnino lanina事件的強度的作用，但強度比緯向風應力模擬的弱，與觀測風應力模擬的強度相差不大，在空間范圍上與觀測風應力模擬的基本一致。 -
Diagnostic results show that the westerly wind stress anomaly and convergent meridional wind stress anomaly over the tropical pacific correspond to the every el nino, and the easterly anomaly and divergent meridional wind stress anomaly correspond to the vanishing of el nino
通過研究表明，每次elnino事件在熱帶太平洋都伴隨著西風應力異常以及向赤道輻合的經向風應力異常，東風應力異常及向兩極輻散的經向風應力異常與elnino消亡對應。 -
( 3 ) west wind stress anomaly and meridional wind stress anomaly occur in the east of tropic pacific, which can boost the formation of el nino events. the stronger wind stress anomaly, the stronger the corresponding el nino event. when east wind stress anomaly and meridional wind stress anomaly happen the la nina events occur
（ 3 ）熱帶太平洋東部伴隨著西風應力異常以及向赤道輻合的經向風應力異常，能夠有利於驅動elnino事件的形成，而且當風應力異常強則對應的那次elnino事件也偏強；當東風應力異常偏強及經向風應力異常向赤道南北兩側輻散偏強則與lanina事件對應。 -
( 4 ) latitude and meridional wind stress fields both have the character of quasi - quadrennial and quasi - biennial oscillation, but their phases are different. so their conjunct effect makes enso oscillation have both quasi - quadrennial and quasi - biennial periodicity and erratic, which causes the forecast of enso events uncertainty
（ 4 ）緯向和經向風應力距平場具有準4a和準2a的振蕩性質，但是位相存在差異，因此共同作用下造成enso振蕩既有準4a和準2a的周期性，又有不規則性，對于enso事件的預報帶來不確定性。
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