air sea 中文意思是什麼

air sea 解釋
空海兩用的
  • 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...
  1. He said the department is also engaged in an effort to modernize air, sea and land forces for the kinds of operations to come, which will include both conventional and counterinsurgency type campaigns

    同時，國防部也正力圖使海陸空三軍更加現代化，以應付即將到來的各種軍事行動，其中包括傳統的戰斗和反游擊戰。
  2. 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
  3. The u. s. coast guard employs the eads hh - 65 dolphin in an air - sea rescue

    美國海岸防衛隊使用海豚直升機進行海空拯救行動。
  4. Mascot air sea services co. ltd

    馬士高海空貨運有限公司
  5. Flying colt air sea services ltd

    飛駒空運有限公司
  6. Yusen air & sea service co. ltd. ( yas ), as the leading global freight forwarder, has contributing to the multi - national enterprises their global logistics needs for half a century

    郵申國際貨運有限公司是世界知名的貨運代理公司，隸屬世界500強企業之一郵船集團。郵申國際貨運在美洲，歐洲，東亞，南亞世界各個角落都有子公司。
  7. Air - sea stochastic climatic model and its application

    海氣隨機氣候模式及其應用
  8. Air - sea boundary layer

    大氣海洋邊界層
  9. 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
  10. Air - sea interaction

    大氣海洋相互作用
  11. Modes of air - sea interactions in the indian ocean and their relationships with the rainfall over china as revaled by svd analysis

    揭示的印度洋海氣相互作用模態及其與中國降水的聯系
  12. 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。
  13. 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。
  14. 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。
  15. 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。
  16. 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。
  17. 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。
  18. An air, sea and land search and rescue operation was immediately conducted

    海陸空搜索救援行動隨即展開。
  19. In equatorial regions, the air - sea humidity difference is overestimated in whoi relative to pirata, which leads to the biases in latent heat flux

    在赤道區， whoi對海氣濕度差的估計相對于pirata偏高，直接導致其對潛熱通量的估計偏差。
  20. It is found that the climatological mean of wind speed and air - sea humidity difference are both large, the variation of wind speed are almost in phase with air - sea humidity difference, yielding much larger or smaller latent heat flux. so the ocean release the most latent heat in its own winter of the two hemispheres when both wind speed and air - sea humidity difference are large

    發現在南北兩信風區，風速和海氣濕度差的變化幾乎是同位相的，平均背景風速和海氣濕度差都較大，他們互相加強彼此對潛熱通量變化的貢獻，所以海洋潛熱損失最大是發生信風南北兩區的各自風速和海氣濕度差都較大的冬季。
分享友人
分享到 Line

分享到臉書