air-sea interaction 中文意思是什麼

air-sea interaction 解釋
大氣海洋相互作用；海
  • air : n 1 空氣，大氣。2 天空，空中。3 微風，和風。4 態度，樣子，風度，氣派；〈pl 〉高傲的架子。5 傳播，...
  • sea : SEA ＝ Southeast Asia 東南亞。n 1 海；海洋；內海；大（淡水）湖。2 〈pl 或與不定冠詞連用〉海面（狀...
  • interaction : n. 1. 相互作用，相互影響，互動。2. 【航空】干擾。
  1. Interaction of air - sea in the middle latitudes and decadal climatic oscillations

    海氣相互作用與年代際氣候振蕩可能機制初探
  2. Firstly, a representative wind and wave model, which could both simulate the main characteristics of wig over sea waves and be suitable for numerical calculation, is presented. the model completely considers the fully nonlinear effect of wave surface on the wavy air flow, separates the disturbance of wave surface from the wing - air wave interaction flow, and overcomes the numerical calculation difficulties due to the large difference of dimensions between wing and water waves

    首先針對機翼在風浪中的非定常非線性氣動力問題，提出了一個既能夠反映風浪場主要特徵又適合於數值計算的風浪場模型，該模型完整地考慮了波浪表面對氣流場的全非線性影響，使波面對流場的擾動分離出來，消除了機翼和波浪幾何尺度上的巨大差異帶來的數值計算上的困難。
  3. Key areas of air - sea interaction in global oceans and their climatic features

    全球海氣相互作用關鍵區及區內氣候特徵分析
  4. Air - sea interaction

    大氣海洋相互作用
  5. 3 ) the upper ocean participates the process of air - sea interaction both in winter and summer in the tropical pacific but only in winter in the north pacific

    3 ）淺層海洋參與海氣相互作用在熱帶太平洋區域冬、夏均存在，而在北太平洋區域僅限於冬季。
  6. Results of recent observation and numerical experiments show that prominent difference exists between air - sea interaction in tropical and in mid - latitude, and work is not enough related to the impact of persistent ssta on the circulation considering different district in pacific

    觀測分析和數值模擬結果表明中緯度與熱帶地區的海氣相互作用存在差異，但深入討論不同關鍵海區的持續性ssta對大氣環流影響的工作還不充分。
  7. On the surface of msta, there exists true dipole mode in the indian ocean, that ' s to say that if the temperature anomaly in the western indian ocean is positive, it is much likely that there is negative anomaly in the eastern indian ocean. dipole mode also exists in the pacific as that in the indian ocean. by virtue of the walker circulation and the similar circulation above the indian ocean, it is showed that the air - sea interaction events in the tropical pacific and the indian ocean develop with each other at the same time

    由於在次表層海溫距平極值面上，熱帶西、東印度洋的海溫距平呈真正意義的偶極子模態，即當西印度洋海溫距平為正（負）時，東印度洋海溫距平為負（正） ，偶極子模態的海溫距平分佈在熱帶太平洋同樣存在，兩大洋海溫距平的偶極子模態間有密切的聯系，結合walker環流和印度洋上空的類似walker環流，進而指出熱帶印度洋和太平洋海氣相互作用事件是協調發展的。
  8. The relationship between sea surface temperature anomaly in pacific and the circulation of northern hemisphere is the focus of air - sea interaction research in recent years. the ssta in pacific contributes to remote response in mid - latitude atmosphere, and is connected with climate changes in global. the cycling of enso is typical phenomena of large scale in pacific air - sea interaction system

    太平洋海溫異常對北半球大氣環流異常有重要影響，而enso循環是太平洋海氣耦合系統中典型的異常演變過程，不僅描述了熱帶地區大氣和海洋異常現象，而且與中高緯度的氣候異常變化相聯系。
  9. 4 ) air - sea interaction retain its character throughtout the seasonal cycle in the tropical pacific, but it is not the same in the north pacific ; and there are also relationships in the two areas : 1 ) for the interdecadal time scale, there is the same abrupt change both in the north pacific and in the tropical pacific, especially in winter

    4 ）熱帶太平洋區域海氣相互作用有較好的季節一致性；而北太平洋區域海氣相互作用季節差異較大。區域間主要聯系為： 1 ）兩個區域主要的年代際躍變點出現時間接近，這在冬季反映最明顯。
  10. It also explain that the correlation between ssta of kuroshio and the change of wind field in equaroral mid - pacific is results of air - sea interaction ; however, when time comes into summer, the instance status of ocean is different from the last winter to next early springtime, the sea surface temperature turn into the definitive factor, so the increase of heat flux in may to jun month which is realized by absorbing more heat from the sun radiation results in the decrease of sst in kuroshio in the season of jun - jul. finally, during the aug to dec season of next year, the sst of kuroshio is increasing again

    最後分析了黑潮海溫與夏季東亞大氣環流及我國降水的時滯關系，發現：當前冬黑潮區域海溫異常偏高時，後期夏季亞洲低壓的強度減弱，西北太平洋副熱帶高壓強度加強，而且位置西伸、偏北，梅雨鋒位置偏南，長江中下游地區降水偏多，北太平洋冬季海域的海溫分佈呈+ 、 - 、 +趨勢（順序為赤道中東太平洋、西北太平洋、我國近海） ；反之亦然。
  11. Diagnostic analysis and contrast are performed in air - sea data and their interaction between the north pacific and the tropical pacific by means of harmonic analysis and svd

    使用諧波分析及奇異值分解（ svd ）方法分析比較了北太平洋、熱帶太平洋區域的海氣資料及海氣相互作用。
  12. Eawm - related air - sea - land interaction and the asian summer monsoon circulation

    相關的海陸氣相互作用及亞洲夏季風
  13. It has long been recognized that sea breeze, an air - sea - land interaction induced by differential heating on land and sea surface, can produce windshear

    眾所皆知，海風是引起風切變的其中一個原因。當陸地與海面存有溫差，氣流由海面吹到陸地，便會形成海風。
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