zonal wind 中文意思是什麼

zonal wind 解釋
緯向風
  • zonal : adj. 1. 成帶的，帶狀的。2. 區域[地區]性的。
  • wind : n 1 風；大風，暴風；氣流；【機械工程】壓縮空氣。2 【航海】上風；風向；〈古語〉〈pl 〉方向。3 氣息...
  1. 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。
  2. Finally the article discusses the physical mechanism of meridional and zonal wind field ' s effect on sst in kuroshio region and think that justly the adjustion of macro - dimension wind field connects the two facts

    考慮到赤道中太平洋風場異常與el - nino及la - nina事件關系密切，進一步的研究證實el - nino及la - nina事件與黑潮海溫異常有著密切的關系。
  3. And the 30 - 60 day low - frequency character is more distinct in flood years than in drought years ; ( 2 ) the relationship of low - frequency olr and zonal wind is greatly different in drought years and flood years

    重點研究的旱、澇各4個年份的分析結果表明，澇年olr場的30 60天振蕩比旱年更為顯著。
  4. 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。
  5. 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

    一個是基態參數（例如緯向風場）的變化；另一個在實際大氣存在的不穩定（此模式未予涉及） ，例如斜壓不穩定。
  6. 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

    中平流層環流轉型異常與赤道平流層緯向風準兩年振蕩（ qbo ）及平流層臭氧總量異常存在顯著相關聯系。
  7. 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。
  8. 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 )

    分析發現10hpa及70hpa層的熱帶緯向風與相應層環流轉型日期之間的相關顯著， 10hpa熱帶東（西）風位相、 70hpa西（東）風位相時環流轉型滯后（提早） 。
  9. 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。
  10. 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

    數值試驗的結果表明，由pop重建的緯向風應力中緩慢變化的大尺度振蕩成分加深了elnino lanina事件的強度，加大了它們的空間分佈范圍，但正負距平中心的位置比觀測風應力模擬的情況偏西。
  11. 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

    結果表明越赤道和越10on阿拉伯海的熱輸送量大小具有可比性，且有相同的年循環特徵，而10on孟加拉灣緯度的經向熱輸送較小，且具有半年變化周期;儼s以北印度洋任一緯度上的緯向風應力異常與此緯度上的經向熱輸送異常以及此緯度以北印度洋總的海面凈熱通量異常有很好的相關關系，相關系數最大可達一0 . 5以上。
  12. With the wind, pressure and sea surface temperature ( sst ) data provided by ncep / ncar reanalysis project and excess length of day ( lod ) data provided by international earth rotation service ( iers ), atmospheric angular momentum ( aam ) and its horizontal and vertical transportation are computed and analyzed, which are in accordance with maintenance of the zonal circulation. and the anomalous aam is highly consistent with el nino events

    應用ncep / ncar40年再分析計劃提供的風場、氣壓場、海溫等資料以及國際地球自轉服務局（ iers ）提供的日長變化資料，計算大氣角動量及其水平、垂直輸送，分析其氣候及異常特徵，發現角動量及其輸送與緯向環流的維持相一致，角動量異常與厄爾尼諾事件緊密相關。
  13. During 1950 ~ 1976 / 1977, the walker circulation over the tropical pacific and the vertical zonal monsoon circulation over the tropical indian ocean coupled at the oceanic continent, the same period when el nino occurs, the anomaly of the west wind over the tropical pacific can correlate with the departure of east wind over the tropical indian ocean through the two coupled vertical zonal circulation. but after 1976 / 1977, the updraft of the walker circulation moved eastward. locating at the north of australia. therefore the two vertical zonal circulation could n ' t coupled, and the anomaly of west wind and the departure of east wind could n ' t geared. in the result. the signal of enso decreased in indian ocean after 1976 / 1977

    1951 1976 1977年，熱帶太平洋的walker環流和熱帶印度洋的緯向季風環流在海洋性大陸附近耦合，當elnino事件發生時，太平洋的西風異常可以通過這兩個緯向的垂直環流與印度洋的東風異常聯系起來，而1976 1977年以後，由於西太平洋walker環流上升支東移到澳大利亞北部，熱帶兩洋的緯向垂直環流無法耦合，熱帶太平洋elnino事件中的西風異常與熱帶印度洋的東風異常聯系減弱，所以1976 1977年以後， enso在熱帶印度洋的信號減弱了。
  14. The probability distributions of climatic elements are discussed. based on the characters of them, a multimode model is introduced and verified through the nonlinear fitting. the climate features of quasi - biennial oscillation of the stratospheric zonal wind over equator, the enso index, the surface pressure at reykjavik 21 90w 64 13n and swedish temperature, and the northern hemisphere tree ring all show that the multimode are universal in the climatic system

    對氣候要素的概率分佈進行了討論，根據這些概率分佈的特點提出了多模態模型，並用非線性擬合的方法進行了驗證。對赤道平流層緯向風enso指數esi序列冰島reykjavik 21 . 90w ， 64 . 13n氣壓和瑞典溫度北半球樹木年輪等數據的分析表明：氣候系統中多模態現象具有普遍性。
  15. The chief content of this article concludes three parts. among it, the research of third chapter involve : use extended svd and correlation analyse between ncep wind stress data in pacafic and sst field of kuroshio nearly 50 years show that there are distinctly positive correlativity between lagging sst of kuroshio and zonal wind field in tropical pacafic region

    本文採用海溫資料和ncep ncar再分析的海平面氣壓場（ slp ） 、高度場、風場等資料，利用eof 、 svd 、相關分析和合成分析方法，重點研究了黑潮海溫異常的機制及其對我國夏季降水的影響。
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