黑潮區 的英文怎麼說

中文拼音 [hēicháoqū]
黑潮區 英文
kuroshio region
  • 潮 : Ⅰ名詞1 （潮汐; 潮水） tide 2 （比喻大規模的社會變動或運動發展的起伏形勢） （social） upsurge; cur...
  • 區 : 區名詞（姓氏） a surname
  • 黑潮 : [地理學] kuroshio; japan current
  1. An anticlockwise gyre near the kuroshio north of japan inland is simulated using a high - resolution topography

    在高分辨的地形條件下，日本西海岸外側的黑潮北部存在一逆時針漩渦，這可能與該區域的漏斗型地形誘導有關。
  2. The results show that the strong winter monsoon will decrease the gradient of ssh, and change the characteristics of sst, which has influence on the sea current, especially in a shallow and closed sea area such as the south china sea

    結果表明：強冬季風會減弱海面高度梯度，普遍降低黑潮區海表溫度，對流場有一定的影響，尤其在南海這樣的封閉海區。
  3. ( 3 ) the previously winter kuroshio ssta relates greatly to the east asian summer monsoon ( easm )

    （ 3 ）前期冬季黑潮區域海溫異常與東亞夏季風存在顯著的聯系。
  4. Conclusions are drawn as follows : ( 1 ) there is a closely relationship between the autumn kuroshio ssta and the east asian winter monsoon ( eawm )

    （ 1 ）秋季黑潮區域海溫異常與東亞冬季風有明顯的正相關關系。
  5. 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。
  6. As a result, we find that in winter when the kuroshio is cooler than the normal, at following summer, the continental cyclone deepen and the east asia monsoon strengthen, that the mid - latitude blocking high weaken and zonal circulation develop, the east asia teleconnection of " - + - " is stired up, so that subtropical high weaken and diminish, and tend to east north, tropical monsoon trough strengthen and mei - yu front weaken, and tend to north, meanwhile south asia high weaken and diminish, and tend to eastvnorth, is easy to form eastern region type

    結果發現當黑潮海溫冷異常時，後期夏季大陸熱低壓加深，東亞夏季風偏強。中緯度阻塞高壓減弱，東亞地區緯向環流發展，在東亞-西太平洋地區激發「 - + - 」的東亞遙相關型，從而西太平洋副高強度偏弱，面積偏小，位置偏東、偏北，東亞梅雨鋒也偏弱，季風槽則變強，位置偏北。同時南亞高壓偏弱，位置偏北、偏東，易形成東部型。
  7. 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。
  8. The well correlation times persist for about six months and the incidence level is reach or pass 0. 01. the meridional wind field which persistly impacting on sst in kuroshio region is near the west tropical pacafic. the result also behave as distinctly positive correlativity. afterwards we investigate the relationship between sst in kuroshio region and ninoc, 4 region and integrate the front conclusion. as a resultjt display that the sst in kuroshio region persists for positive relevance during the course of el - nino and inversely during the course of la - nina. subsequentl y the synthetic fields of kuroshio region ' s ssta in el - nino and la - nina years have proved the front outcome

    對與黑潮海溫異常變化關系密切的風場關鍵區及兩者的相互關系研究表明：黑潮本身的風場和其源地北赤道流海域的風場異常對黑潮海溫的影響僅限於同期及海溫滯后1到2個月，而能持續影響黑潮海溫異常的經向風場的關鍵區出現在赤道西太平洋（ 140 - 160e ， 5s - 5n ） ，緯向的關鍵區則在赤道中太平洋（ 160e - 150w ， 5s - 5n ） ，且緯向關鍵區的強度和范圍均大於經向，兩者對黑潮海溫的影響均能持續六個月左右。
  9. 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。
  10. The condition of profiles in outer station did n ' t change much in spring cruise, but showed more variable in near - shore stations when observed in different time. fluorescent characteristic per cell can be obtained by flowcytometric analysis. based on fluorescence data of synechococcus of all stations, two distinctly pigment - containing cell types coexisting can be found in some stations of east china sea, which located in all depth of p3, mixlayer of e7, 40 - meter depth of e6 of autumn cruise and in mixlayer of p2 of spring cruise

    通過對流式細胞計測量的細胞熒光結果來看，在秋季的p3 、 e7整個混合層、 e6站40米層，春季的p2站均發現有兩群不同色素含量的聚球藻（ high一pe和low一pe ）共存現象，極有可能分別屬于不同品系，春季共存站位位置比秋季時更靠外，表明在秋季p3 、 e7等站位的共存是季節性現象，可能與此季節黑潮次表層水沿陸架坡涌升入侵到中陸架有關，水團的運動及混合使從外海遷移而來的high一pe與近岸的low一pe得以共存，在春季，由於長江沖淡水的日漸強盛，在中陸架區的共存區域有所外移。
  11. During the kuroshio survey, jointly conducted by china and japan from 1986 to 1992, more than 100 field operations were carried out, and meetings of over 200 scientists were arranged, which helped to accumulate a rich store of information for understanding the movement of kuroshio, its regular pattern of changes and its origin, as well as the resources variations in the fishing grounds of the western pacific

    僅中國和日本於1986年至1992年合作進行的黑潮調查，就進行了100多個航次的外業調查，交流科學家200多人次，為認識黑潮運動、變化規律和成因，以及西太平洋漁區資源變動等問題積累了大量資料。
  12. 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。
  13. 2 ) the spring sst of the black current area and nino area with summer precipitation is obviously negative connection

    2 ）黑潮海域及nino3海區春季sst與我國東部夏季極端降水量呈明顯的負相關型。
  14. Then by using of statistics and numerical simulation analysis, research abnormality of the main circulation system at following summer in east asia, and the influence of the abnormality on the rainfall and temperature in summer in china, when sst over the kuroshio area during winter show cold or warm anomaly

    再分別通過統計和數值模擬的方法，系統的分析了冬季黑潮海溫冷暖異常時，後期夏季東亞地區高低空的主要環流系統的異常，以及這些異常又如何進一步影響了我國夏季的降水和氣溫。
  15. ( 2 ) the anomalous eawm predominantly relates to the winter kuroshio ssta. the winter kuroshio ssta becomes positive ( negative ) when there is a strong ( weak ) eawm. the possible links might be the winter latent and sensible heat release in the west - northern pacific ocean

    （ 2 ）東亞冬季風異常對冬季黑潮區域海溫異常有密切的聯系，當東亞冬季風偏強時，冬季黑潮區域海溫偏低；反之，冬季黑潮區域海溫偏高。
  16. A 3d baroclinc ocean model is used to model the ocean current around the kuroshio area on the condition of successively anomalous east asia winter monsoon, some significant results are obtained, and the influence of strong ( weak ) winter monsoon on sea surface height ( ssh ), sea surface temperature ( sst ) and sea current around the kuroshio area is analyzed preliminarily

    摘要運用一個三維斜壓海洋模式對冬季風風場持續異常時期的黑潮區海洋進行了模擬，初步分析了冬季風風場持續異常對黑潮區海面高度、海流和海溫的影響。
  17. By using of eof analysis, distribution of sst over the kuroshio area during winter are identified, which show cold or warm anomaly

    本文首先通過eof分析確定了冬季黑潮區sst的主要分佈形勢，發現冬季黑潮區海溫主要表現為冷異常或暖異常。
  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. ( 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。
  20. When the autumn kuroshio ssta is positive, the sea - land sea level pressure differences in the east asian region become large in winter, the east asian trough at 500hpa shifts eastward and is deep in its south and shallow in the northern, along with strong north winds in the above area and weak westerly circulation in the asian region

    當秋季黑潮區域海溫異常偏高，東亞地區的海陸氣壓差異進一步加大，東亞大槽北部減弱、南部加深、位置東移，東亞地區的偏北風加強，亞洲地區西風環流減弱，即東亞冬季風加強；反之亦然。
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