熱帶海洋區域 的英文怎麼說

中文拼音 [rèdàihǎiyángqūyù]
熱帶海洋區域 英文
tropical ocean region
  • 洋 : Ⅰ名詞1 （海洋） ocean 2 （洋錢） silver coin 3 （姓氏） a surname Ⅱ形容詞1 （盛大; 豐富） vast; m...
  • 區 : 區名詞（姓氏） a surname
  • 域 : 名詞（在一定疆界內的地方; 疆域） land within certain boundaries; territory; region
  • 熱帶 : tropics; burning zone; [氣象學] torrid zone熱帶草原 campos; llanos savanna; [巴西] matto grosso; ...
  • 海洋 : seas and oceans; ocean; [詩歌用語] blue海洋霸權 maritime hegemony; 海洋保護區 marine preserve; 海...
  1. 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。
  2. 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。
  3. 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。
  4. Based on ncep / ncar reanalysis sst and wind data set and fsu wind stress data, the dynamical roles of atmosphere over the tropical pacific on ocean are diagnostically analyzed. by using a dynamical ocean model over tropical pacific, the importance of dynamical roles of different areas atmosphere on ocean is studied. in the part iii of this work, a intermediate coupled model ( icm ) is employed to study ssta forecast experiment

    本文用ncep / ncar再分析海表溫度、風應力和風場資料就熱帶太平洋地區大氣對海洋的強迫進行診斷分析，並用一個熱帶太平洋動力海洋模式研究不同區域大氣對海洋強迫作用的重要性，在此基礎上用一個中等復雜程度的耦合模式對enso事件進行預報試驗。
  5. China lies east to pacific ocean and includes tropical zone, subtropical zone and mid - latitude zone. continent coastal dimate is variable

    我國瀕臨太平洋，跨越熱帶、亞熱帶和溫帶三個氣候帶，大陸沿海及近海區域天氣和海洋現象復雜多變。
  6. The swic website provides tropical cyclone information and warnings for all ocean basins affected by tropical cyclones as well as charts showing the global distribution of severe weather information such as heavy rainsnow

    惡劣天氣信息中心網站則提供各受熱帶氣旋影向的海洋區域的熱帶氣旋信息及警告，另外亦顯示全球惡劣天氣信息諸如大雨大雪的分布圖。
  7. The frequency analysis of area - averaged ssta time series in key regions indicates that the power spectrum peaks is centered at 2 - 4yr annual oscillation, and there is also long temporal scale oscillation such as quasi decadal oscillation revealed by wavelet analysis

    時頻分析表明，這兩個海區區域平均的ssta時間序列存在顯著的2 - 4年年際振蕩以及準年代際變化。自相關分析表明西風漂流區與熱帶中東太平洋ssta在冬季的持續性較好。
  8. A monthly overview of tropical cyclones is given in this section

    這一節逐月介紹二零零五年北太平洋西部及南海區域的熱帶氣旋概況。
  9. Besides, japan meteorological agency has been delegated since 1981 with the responsibility of assigning to each tropical cyclone in the western north pacific and the south china sea of tropical storm strength a numerical code of four digits

    另外，日本氣象廳在一九八一年起已獲委託為每個在北太平洋西部及南海區域出現而達到熱帶風暴強度的熱帶氣旋編配一個四位數字編號。
  10. Apart from being used in forecasts and warnings issued to the international aviation and shipping communities, the names will also be used officially in information on tropical cyclones issued to the international press. besides, japan meteorological agency has been delegated since 1981 with the responsibility of assigning to each tropical cyclone in the western north pacific and the south china sea of tropical storm strength a numerical code of four digits

    這些名字除了用於為國際航空及航海界發放的預測和警報外，亦是向國際傳媒介發放熱帶氣旋消息時採用的規范名稱。另外，日本氣象廳在一九八一年起已獲委託為每個在北太平洋西部及南海區域出現而達到熱帶風暴強度的熱帶氣旋編配一個四位數字編號。
  11. The first half of the year was very unusual in that not a single tropical cyclone was found over the entire western north pacific and the south china sea. this broke all records since 1946

    一九九八年首六個月並沒有熱帶氣旋在北太平洋西部及南海形成，這是自一九四六年以來最遲有熱帶氣旋在這些區域形成的一年。
  12. 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。
  13. 2 ) the leading svd modes of interdecadal variability are indicative of stronger statistical significiance in the north pacific than in the tropical pacific, while the conclusion is contrary as for interannual variability

    2 ）年代際變化海氣相互作用北太平洋區域較熱帶太平洋區域顯著，年際變化海氣相互作用熱帶太平洋區域較北太平洋區域顯著。
  14. Over the western north pacific and the south china sea between 1947 and 1999, tropical cyclone names were assigned by the u. s. armed forcess joint typhoon warning center according to a pre - determined but unofficial list

    從一九四七年至一九九九年，北太平洋西部及南海區域的熱帶氣旋非正式地採用美國軍方聯合臺風警報中心所編訂的名單上的名字。
  15. Over the western north pacific and the south china sea between 1947 and 1999, tropical cyclone names were assigned by the u. s. armed forces joint typhoon warning center according to a pre - determined but unofficial list

    從一九四七年至一九九九年，北太平洋西部及南海區域的熱帶氣旋非正式地採用美國軍方聯合臺風警報中心所編訂的名單上的名字。
  16. Results show that the interdecadal anomalies are more significant in the variance of the system anomaly in the north pacific ( np ), and the interannual and interdecadal anomalies are about equivaleut in the tropical pacific ( tp ) ; the interdecadal change characters of the surface ( shallow ) layer of the ocean and the atmosphere aloft are unanimous in the same season and region, and their transition from a low mode to a high mode both occurred from the end of 1970s to the beginning of 1980s, with an exception for july in the np, which is related to the stability of the stratification of sea temperature within the sub - surface layer ; the interannual scale air - sea anomalies are associated with enso, is most typical for january, then july in the tp, followed by january in the np, and there is no visible relationship for july in the np

    在海氣系統異常的方差構成中，北太平洋區域以年代際異常為主，熱帶太平洋區域年際和年代際異常相當；表（淺）層海洋與大氣的年代際變化特徵對同一季節、區域是一致的，且20世紀70年代後期到80年代初均發生由低模態向高模態的轉變；北太平洋區域的7月與此不同，這與該季節近表層海溫層結穩定有關；年際尺度的海、氣異常與enso有關，且以熱帶太平洋區域1月最典型， 7月次之，北太平洋區域1月再次之， 7月無明顯關系。
  17. When the winter kuroshio ssta is high, there is high ( low ) pressure ( compared with mean ) in the asia and weak ( strong ) easterly jet at high level in summer. at the same time, the west - northern pacific high becomes strong ( weak ) and shifts westward ( eastward ) and northward ( southward )

    當冬季黑潮區域海溫異常偏高時，亞洲熱低壓強度減弱，西北太平洋副熱帶高壓位置西伸且偏北，強度明顯偏強，梅雨鋒位置偏南，長江中下游地區降水偏多。
  18. In drought or flood years over the yangtze river basin, the features of the establishment, progression and decrease of moisture transport is significantly different, meanwhile the differences of the moisture transport by the monsoon circulation between mid and low latitudes in the northern hemisphere, and by the subtropical high are obvious, so are their convergence, especially over south china sea, the tropical west pacific, the yangtze river basin, north china and north - east in china

    （ 4 ）長江流域旱澇年亞澳季風區夏季風水汽輸送的建立、推進、減弱的階段性特徵顯著不同，對應的中低緯季風環流、副高環流等季風系統水汽輸送、匯合也有顯著差別，尤其是在南海、熱帶西太平洋、長江流域、華北和東北等地區。
  19. Tropical cyclones over the western north pacific including the south china sea

    2 . 1 . 1北太平洋西部包括南海區域的熱帶氣旋
  20. ( 4 ) based on the ncar ccm3 simulations, the influence of the previously winter kuroshio ssta on the easm is investigated. results from the simulations are highly coincidence with the observations, namely, the winter kuroshio ssta may impacts the subsequent year east china summer rainfall by making influencing on the strength and location of the west - northern pacific high and the easm systems

    （ 4 ）利用ncarccm3模式模擬冬季黑潮區域海溫異常對東亞夏季風的影響，模式模擬的結果與統計分析結果是一致的，即前期冬季黑潮區域海溫異常可以通過影響次年夏季的西太平洋副熱帶高壓的強度和位置變化以及東亞夏季風環流的強弱，從而進一步影響我國東部地區的降水，尤其是長江中下游地區。
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