west pacific 中文意思是什麼

west pacific 解釋
西太平洋
  • west : n 韋斯特〈姓氏〉。n 1 〈常作 the west〉 西，西方，西部（地方）。2 〈the W 〉 西洋；西歐；〈有時作...
  • pacific : adj. 1. 和平的，太平的；平時的。2. 愛好和平的，（性質）溫和的。3. 〈P-〉太平洋的。adv. -ically
  1. Distant effect of jurassic collisions of qiangtang terrane, lasa terrane and paleo - pacific land onto the eurasian land made east qinling - dabie mountains in a compressional circumstance for a long time, and suppressed its orogenic extension ; whereas, cretaceous late - collisional extension and appearance of west pacific trench - arc - basin system relieved east qinling - dabie mountains of external compression, instantly result in violent orogenic lithosphere delamination - extension and depressurized - calefactive melting, and consequently, led to the formation of large scale early cretaceous granitoids and intermediate - acidic volcanic rocks

    羌塘地體拉薩地體和西太平洋古陸在侏羅紀與歐亞大陸拼貼碰撞的遠距離效應使東秦嶺大別造山帶長期處于擠壓環境，伸展作用被抑制白堊紀的碰撞晚期伸展和西太平洋溝弧盆體系的遠距離效應使東秦嶺大別地區的外部擠壓消失，導致造山帶巖石圈迅速強烈拆沉伸展和減壓增溫熔融，從而形成大規模早白堊世花崗巖類和中酸性火山巖。
  2. During flood years, the center of negative anomaly is around ural mountains, the center of positive anomaly is around high - latitude of east asia and another negative and positive center are over okhotsk sea and the north - west pacific, respectively

    通過對夏季旱澇等級指數的morlet型和mexicanhat型小波變換分析，發現山東夏季旱澇指數主要存在著2 5年和7年左右的周期振蕩。
  3. When the intensity of meiyu increasing, the continental low in the northwest of meiyu rainband is getting stronger and the west pacific subtropical high is getting weaker

    當梅雨強度增大時，梅雨西北部的大陸低壓加強而西太平洋副熱帶高壓減弱。
  4. Red sea, india ocean, west pacific ocean

    紅海、印度洋、西太平洋沿海。
  5. The southerly water vapor can progress to 50 n near north - east in china -, the southeasterly water vapor from south side of the west pacific subtropical high and north side of the monsoon trough can march westward to 100 e near south - east part of gansu in summer

    東亞夏季偏南風水汽輸送所能到達的北界為50 n附近的東北北部。西太平洋副高南側、亞洲季風槽北側的東南風水汽輸送在夏季可向西擴展到甘肅東南部地區（ 100 e附近） 。
  6. The summer rainfall anomaly of north china is closely related to indian low, west pacific subtropical high, westerly troughs and ridges in mid - latitude, south asia high, subtropical monsoon circulation and cold air activity on the corresponding period, and similar circulation pattern also appears in the preceding spring

    結果表明： （ 1 ）華北夏季降水異常與同期印度低壓、西太平洋副高、中緯度西風槽脊、南亞高壓、副熱帶季風環流和冷空氣活動的異常都密切相關。華北夏季降水異常年春季的環流特徵與夏季類似。
  7. When the wpi - soi correlation is weak and the west pacific sst warmer ( colder ), a anomalous anticyclonic ( cyclonic ) circulation is found in the lower troposphere over northern equatorial western pacific. this anomalous circulation is not in favor of maintaining a significant correlation between the west pacific sst and enso

    Wpi - soi相關關系微弱時，在西太平洋赤道北側的對流層低層存在高（低）海溫?反氣旋（氣旋）異常環流系統，不利於維持enso與西太平洋海溫變化間的緊密聯系。
  8. During the years of strong monsoon, the convective activities happening in tropical india ocean and tropical west pacific and walker circulation are much stronger than that during the years of weak index, but the convective activities happening in tropical east pacific are weaker than those during the years of weak monsoon

    春季熱帶對流活動對山東夏季降水異常的貢獻比夏季更顯著。強季風年與山東夏澇年相聯系，熱帶印度洋一菲律賓群島、南海一熱帶西太平洋對流活動偏強，熱帶東太平洋地區對流活動偏弱， walker環流加強。
  9. ( 4 ) the fundamental situation of the west - pacific subtropical high takes place variation in the three periods during summerial and monthly in summer

    當年nino3區夏季海溫與低層風場的回歸分析及與500hpa高度場相關分析表明三個階段的環流形勢不同，存在明顯差異。
  10. It was found that the " key regions " from which moisture transports influenced shandong summer rainfall lies in tropical india ocean, south china sea to tropical west pacific, china mainland to japan sea and the upstream area in westerly belt by analysis of svd method on water vapor transport

    夏旱年則相反。通過對旱澇年水汽輸送與山東夏季降水的相關分析，山東夏季降水和水汽輸送svd分析，發現：影響山東夏季降水的水汽輸送「關鍵區」主要位於熱帶印度洋、南海-西太平洋、中國大陸-日本海以及山東上游西風帶地區。
  11. Climatological characteristics of tropical cyclone activities in the west pacific

    1995年西太平洋熱帶氣旋活動的氣候學特徵
  12. Analysis shows that when summer precipitation in north china is richer ( less ), tropical east pacific ssta is colder ( warmer ) phase, and slp and 500hpa geo - potential height are negative ( positive ) anomaly over the asia, west pacific sub - high is northerner ( southerner ), and block high in mid - highs latitude happens less ( more ) than normal, east monsoon is stronger ( weaker )

    分析表明華北夏季多（少）雨期，赤道中東太平洋ssta處于冷（暖）位相，在非洲大陸上slp利500hpa位勢高度均為負（正）異常，西北太平洋副高位置偏北（南） ，中緯度阻塞高壓發生頻率較低（高） ，東亞夏季風偏強（弱） 。
  13. Using ncep / ncar daily reanalysis data and scsmex data, an investigation is carried out of the relationship between the position variation of the west pacific subtropical high ( wpsh ) and the apparent heating in june 1998 based on the complete vertical vorticity equation

    摘要採用ncep / ncar再分析逐日資料和scsmex等資料，根據全型垂直渦度傾向方程，研究了1998年6月西太平洋副高位置變動與大氣熱源的關系。
  14. ( 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。
  15. The double eye - wall structure in tropical cyclones was not rare in the west pacific. it had been observed recently in typhoon kujira 2003, in typhoon kirogi and typhoon kai - tak 2000

    在西太平洋，雙重眼壁結構的熱帶氣旋並不少見， 2003年的臺風鯨魚2000年的臺風鴻雁及臺風啟德都曾出現此現象。
  16. Remarkable areas are the equatorial west pacific, north china, equatorial central america, north of bengal gulf and nepal, eastern australia, west india and south pakistan, east of lena river and west europe and wilkes in antarctic

    顯著的地區是：赤道西太平洋區、中國的華北、赤道中美洲區、孟加拉灣北部及尼泊爾、東澳大利亞區、印度西部及巴基斯坦南部、勒拿河以東地區，西歐及南極的威爾克斯等區域。
  17. The yanshan - liaoning area lies in the crossover zone of the ne - directed west pacific ocenic structural system and near sw - directed paleoz - asian structural system

    燕遼地區位於中國東部北東向展布的西太平洋構造域與近東西向分佈的古亞洲構造域交叉復合部位。
  18. This system plays an important role in the relative movement between the west pacific plate and eurasian continental plate. thus, the paleozoic structures had been modified

    此斷層系列對于西太平洋板塊與歐亞板塊之間的相對運動起重要作用，於是古生代構造帶被改造。
  19. The precipitation in middle and lower reaches of yangtze river response to the positive abnormal in eurasian continent and it also has the relationship with the interannual variability of the middle and high latitude of north atlantic sst and the west pacific warm pool

    長江中下游降水對應于歐亞大陸的位勢高度正異常，長江中下游降水與北大西洋中高緯度和西太平洋暖池sst的年代際變率有關。
  20. ( 4 ) flood season precipitation anomalies has a good correlations with southwest and southeast summer monsoon, polar vortex, west wind trough and west pacific high ( 5 ) the ssta anomalies of west pacific key regions combine with south atlantic key regions has a good predict to the flood season precipitation anomalies in liaoning areas

    遼寧夏季多雨水汽來源於西南夏季風和我國東部海域，汛期降水異常與西南、東南夏季風，極渦，西風槽以及西太平洋副高活動關系密切。西太平洋和南大西洋海溫關鍵區冷暖水年結合對遼寧汛期多少雨年有很好的指示作用。
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