北太平洋海域 的英文怎麼說

中文拼音 [běitàipíngyánghǎiyù]
北太平洋海域 英文
north pacific region
  • 太 : Ⅰ形容詞1 （極高; 極大） highest; greatest; remotest 2 （極; 最） extreme; most 3 （身分最高或輩分...
  • 平 : Ⅰ形容詞1 （沒有高低凹凸 不頃斜） flat; level; even; smooth 2 （高度相同; 不相上下） on the same l...
  • 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...
  • 域 : 名詞（在一定疆界內的地方; 疆域） land within certain boundaries; territory; region
  • 海域 : sea area; maritime space
  1. The archipelago is a hazardous traffic median in the great circle route, the shortest path between ports on either side of the north pacific

    多島海域是大圓航線上極具危險的運輸中樞，也是連接北太平洋各端港口的最短通道。
  2. 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。
  3. 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。
  4. 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。
  5. On the other hand, the methods of reof analysis was also used to north pacific ssta on spring and summer. the middle and eastern equatorial pacific and the kuroshio region of northwestern pacific are two mostly anomaly regions

    另一個方面，對太平洋春季、夏季海表溫度進行reof分析，表明太平洋海表溫度分佈具有明顯的區域特徵，其中最強的異常分佈區是赤道中東太平洋和西北太平洋黑潮海區。
  6. They contain warnings of winds of gale force or above, a synopsis of significant meteorological features and 24 - hour forecasts of weather and sea state for ten marine areas in the south china sea and the western north pacific

    預報內容包括烈風或以上風力的警告、重要氣象特徵的概述及在南海與北太平洋西部上十個海洋區域的天氣與海面狀況之24小時預報。
  7. The temporal and spatial variations of summer precipitation anomaly in northeast china ( nespa ) are studied, and its relations with contemporary circulation anomalies over north pacific ( np ) and sst departure of pacific on the interdecadal and interannual scale are discussed by means of harmonic analysis, reof and svd

    採用諧波分析、 reof 、 svd等方法分析了東北夏季降水異常的時空特徵，並按年代際、年際尺度分析了它與同期北太平洋區域對應尺度環流、相關海表溫度異常的聯系。
  8. Genetic analysis shows that it may be caused by the difference of the response of each area to winter monsoon ' s abnormal, the kuroshio and our offshore is influenced mostly by heat flux between the sea and atmosphere, but in the other areas, the abnormal current incited by abnormal wind has decisive effect on the change of the sea temperature, at the same time, air pressure also has some impact on the sea temperature

    其區域性形成的原因主要可能是因為各海區對冬季風異常的響應方式不同，強冬季風使得黑潮與我國近海海洋過多散熱，海溫降低；在西北太平洋暖池北部，強冬季風引起西風異常，從而引發異常氣旋性環流，海水輻合下沉加熱其表層以下海水，同時異常環流使得更多東側異常暖水向西加熱其表層水；在黑潮與親潮交匯處的升溫也主要是由於強冬季風導致的流場異常，海水輻合下沉升溫。
  9. 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。
  10. 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。
  11. 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。
  12. 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。
  13. 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。
  14. 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。
  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 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。
  16. 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。
  17. 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。
  18. 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。
  19. Based on the analysis of the features of asia winter monsoon and north - west pacific temperature ' s temporal and spatial variation, using simulation and statistic analysis methods such as correlation analysis, synthesis, svd and so on, this paper study priority the regional characters of asian winter monsoon ' s influence on north - west pacific temperature. statistic analysis and simulation all indicate that winter monsoon ' s impact on north - west pacific temperature contains regional characters positively, abnormal strong winter monsoon will causes the temperature ' s reducing of kuroshio and our offshore and increasing of the north of pacific warm pool synchronous, and the temperature of the adjacent area between the north of kuroshio and the oyashio will rise in later season

    在分析東亞冬季風與西北太平洋海溫時空變化特徵的基礎上，通過相關、合成以及svd等統計分析方法和數值模式模擬，本文重點研究了東亞異常冬季風對西北太平洋海溫影響的區域性特徵，統計分析與模式模擬結果都表明：東亞冬季風對西北太平洋海溫影響存在明顯的區域性特徵，主要分為三個區域，黑潮與我國近海、西太平洋暖池北部、日本東部的親潮與黑潮交界處。
  20. Study on water temperature distributions and fishing grounds of squid in the north pacific during may - july in

    7月北太平洋海域水溫分佈及柔魚漁場研究
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