北太平洋部 的英文怎麼說

中文拼音 [běitàipíngyángbù]
北太平洋部 英文
boreal pacific province
  • 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...
  • 部 : Ⅰ名詞1 （部分; 部位） part; section; division; region 2 （部門; 機關或組織單位的名稱） unit; mini...
  1. The atmospheric circulation of the wet year deviate from enso year to no - enso year. in enso year, the subtropical high is strong with the deepening of trough over south of baikal lake while in no - enso year, the subtropical high is weak with the high incidence of typhoons over northwest of pacific and south china sea

    多雨年發生在enso年和no - enso年大氣環流形式的不同主要表現在： enso年副熱帶高壓較強，貝加爾湖地區南部低壓槽容易加深；在no - enso年副熱帶高壓強度減弱，在西北太平洋和南海地區多熱帶系統活動。
  2. Boreal pacific province

    北太平洋部
  3. Sailling against the current is the very important period of spawning and feeded in the whole life time. the best fishing season is from december to the next febuary and april to june

    分佈於北太平洋西部近海我國的黃海和渤海產量多，東海較少漁期分春秋兩季， 4 - 5月份為春汛。
  4. The connection is also analyzed between the index of horse latitudes and index of east asian monsoon and index of north pacific oscillation, and the summer extreme precipitation over eastern china

    分析了西太平洋副高指數、東亞季風指數、北太平洋濤動指數的與我國東部夏季極端降水量的關系。
  5. Was a hurricane which formed over the central north pacific. it moved northwestwards across the international date line and entered the western north pacific on 30 august

    是在北太平洋中部形成的颶風，它向西北移動越過國際換日線，於八月三十日進入西北太平洋。
  6. Two of them, namely ele ( 0217 ) and huko ( 0224 ), formed over the central north pacific and moved across the international date line into the western north pacific

    包括艾利（ 0217 ）和胡高（ 0224 ）這兩個在北太平洋中部形成后橫過國際換日線進入北太平洋西部的熱帶氣旋。
  7. Was originally a hurricane which formed over the central north pacific. it moved west - northwestwards across the international date line and entered the western north pacific on 3 november

    是早前在北太平洋中部形成的颶風，但它於十一月三日越過國際換日線后進入西北太平洋。
  8. Morgan and his ally, james j. hill, controlled the two northern transcontinental railroads, the northern pacific and the great northern, in 1901.

    1901年，摩根和他的同夥詹姆斯J希爾控制了兩條北部橫貫大陸的鐵路，即北太平洋鐵路和大北鐵路。
  9. ( 4 ) the anomaly of the ssmcs has better durative when the ah encourter niter - annual variation, and in the inter - decadal scale, when the ah occurs the inter - annual variation, the anomaly of the cef between 100 and 160 e on 925hpa, the strength and area of sh has better durative, the durative of the cef ' s anomaly on 200hpa

    （ 3 ）當澳高發生年際變化時，亞澳地區降水異常主要表現在兩個區域： 1 ） 30 n附近從我國東部地區至日本半島以及西北太平洋一帶。 2 ） 10 n附近的熱帶洋麵上。當澳高偏強時，這兩個地區的降水異常偏多。
  10. Names of tropical cyclones in the western north pacific

    北太平洋西部熱帶氣旋名稱
  11. In the global warming period of 1968 - 2002, the locations of landfalling typhoons in china mostly situated in the middle of the east coastal area of china and the position whereat northwestern pacific typhoons reached their maximum strength had a trend to move northwards during its life

    在1968 - 2002年全球明顯增暖時段，我國臺風登陸位置偏向我國中部，西北太平洋臺風在生命史中強度達最強時的位置有向北移動的趨勢。
  12. Further, correlation analysis is used to the summer rainfall and four seasonal north pacific ssta, the results suggest north pacific ssta which notability cause the summer rainfall anomaly over eastern china are prophase winter ssta of kuroshio region of northwestern pacific, prophase spring ssta of middle and eastern equatorial pacific and summer ssta of west wind drift region

    進一步對上述東部夏季降水異常區夏季降水與春夏秋冬太平洋海溫異常作相關分析，表明對中國東部夏季降水有顯著影響是：西北太平洋黑潮海區前期冬季海溫異常、赤道中東太平洋前期春季海溫異常、中高緯太平洋西風漂流區同期夏季海溫異常。
  13. From april to june, but because of the special habit of sail against the current to the south in the autumn, the catch after september is depanded on the warm weather

    分佈於北太平洋西部我國產于東海黃海和渤海。主要漁場有舟山連雲港外海及山東南部沿海每年的46月份為春汛， 710月份為秋汛， 56月份為旺季。
  14. The observatory contributes to the global maritime distress and safety system of the international maritime organization by preparing weather bulletins and severe weather warnings for the china seas and the western north pacific regions. these messages are broadcast via inmarsat communication satellites four times a day to ships on the high seas

    天文臺負責為國際海事組織的全球海上遇險和安全系統提供中國沿海和北太平洋西部地區的天氣預測，以及發出惡劣天氣警告，這些信息會透過國際海事衛星每日四次向船隻廣播。
  15. 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。
  16. This was due largely to the development of an el nino in the year, which was characterized by above normal sea surface temperatures in the equatorial eastern and central pacific. the associated change in atmospheric steering flow caused tropical cyclones over the western north pacific to turn towards the north before entering the south china sea

    厄爾尼諾是指在赤道太平洋東部及中部出現海面溫度異常變暖的現象，它導致大氣環流的改變，將北太平洋西部的熱帶氣旋引導向北移動，相對減少了它們向西移入南海的機會。
  17. Data used in this work are north pacific ssta, 160 stations precipitation of china, and ncep reanalysis data. main results are as follow : ( 1 ) it is found that a apparent transition of north pacific ssta in later 1970 ' s : eastern and middle - equatorial pacific ssta turns from cold to warm with area extending, and mid - latitude pacific ( west wind drift zone ) turns from warm to cold. during this transition of ssta, different characters also appear in el nino and la nina : before 1976, la nina happens more frequently, and its duration is longer, el nino zone develops from negative ssta in the early stage ; after 1976, el nino happens a little bit frequent and longer with more intensity than before, el nino zone develops from positive ssta in the early stage ; the course of ssta variation has an enso cycle of 2 - 6 years, annual oscillation of 8 - 9 years, and decadal variation of about 22 years

    本文採用1950 - 1999年北太平洋海表溫度（ sst ） 、中國160站夏季降水和ncep再分析的歐亞500hpa高度場等資料，利用eof 、 svd 、小波分析、合成分析和相關分析等方法，在分析北太平洋海溫時空分佈特徵的基礎上，著重探討了海溫異常及其年代際變化對我國東部降水的影響，並對降水、高度場和海溫三者之間的關系進行了分析，以試圖尋找三者異常之間可能的聯系，主要結論如下： （ 1 ） 1976年前後，北太平洋海溫經歷了一次明顯的轉變，赤道中、東太平洋厄爾尼諾海區由冷轉暖，暖水范圍增大，中緯度西風漂流區海溫由暖轉冷；在這樣的年代際背景下，厄爾尼諾、拉尼娜事件在不同的時期也有不同的特徵：在76年前，拉尼娜事件發生頻率高，持續時間長，事件起始於負海溫距平；而76年後，則是厄爾尼諾事件發生頻率略高，持續時間長，強度增大，事件起始於正海溫距平。
  18. 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。
  19. 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。
  20. ( 4 ) in summer, tropic west pacific ssta decadal change infect precipitation decadal change in south and north of changjiang river maybe by : positive ssta in tropic west pacific weaken the summer monsoon circulation, lead more precipitation in south of changjiang river and less precipitation in north of it, vice versa ; middle north pacific ssta decadal change infect precipitation decadal change in mid - down valley of changjiang river maybe by : when ssta is negative in middle north pacific, the height field in tropic rises obviously, the subtropical high strengthens and extends westward, the northern limit retreats southward, leads upper trough retreats northward and move eastward, meiyu front moves northward, then leads more precipitation in mid - down valley of changjiang river, vice versa ; middle northwest pacific - low latitude mid - east pacific infects precipitation in north china possibly by change the activity of northeast china cyclone

    （ 4 ）熱帶西太平洋ssta年代際變化影響夏季中國長江南北降水年代際變化的可能機制是熱帶西太平洋海表溫度正（負）異常減弱（加強）東亞夏季風環流，從而使江南降水增加（減少） ，江北降水減少（增加） ；夏季中部北太平洋ssta年代際變化影響中國長江中下游地區夏季降水年代際變化的可能機制是中部北太平洋海表溫度負異常，將導致熱帶地區高度場普遍增高，副高加強西伸，副高北界南退，致使高空槽北縮東移，梅雨鋒西移北進，中國長江游中游、中卜游降水增多，反之亦反；夏季中高緯西北太平洋一低緯中東太平洋反向距平分佈結構影響中國東北降水的可能機制是低緯中東太平洋海表溫為負異常。
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