赤道海域 的英文怎麼說

中文拼音 [chìdàohǎiyù]
赤道海域 英文
equatorial sea region
  • 赤 : Ⅰ形容詞1. （紅色） red 2. （忠誠） loyal; sincere; single-hearted 3. （光著; 裸露） bare Ⅱ名詞（姓氏） a surname
  • 道 : Ⅰ名詞（道路） road; way; route; path 2 （水流通過的途徑） channel; course 3 （方向; 方法; 道理） ...
  • 域 : 名詞（在一定疆界內的地方; 疆域） land within certain boundaries; territory; region
  • 赤道 : 1. [地] （地球赤道） the equator 2. [天文學] （天球赤道） the celestial equator
  • 海域 : sea area; maritime space
  1. Gnomonic charts are published covering the atlantic, pacific and indian oceans, except for an equatorial belt in each ocean

    出版大圓海圖覆蓋大西洋，太平洋和印度洋（各大洋近赤道帶水域除外） 。
  2. The mld of the ocean near the equator from 10 ? s to 10 ? n are less than 50 m and have no evident seasonal variability

    而在10 s 10 n之間的赤道附近海域，因風應力和凈熱通量的季節變化不大，且該區降水量較大，浮力通量增加， mld較淺，低於50米，且沒有明顯的季節變化。
  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. Castle peak is located quite a distance from clk. since the affected airflow was confined to the waters downstream of castle peak, only marginally reaching the approach and departure areas of the north runway, it is believed that the disrupted airflow might have only minimal effect on arriving and departing aircraft

    由於赤角與青山相隔一段較遠的距離，氣流改變的區域集中在青山下游的海域，僅僅觸及北跑道的升降區，相信並不會對飛機升降構成太大影響。
  5. This paper reported the general situations of tuna fishery in indian ocean in recent ten years, and studied die fishing efforts, catch, cpue, and fishing grounds of two long - line crafts from zhonglu oceanic fishery co. ltd in equatorial waters of indian ocean in 2002, in order to gave the new fishery information to the producer, and to improve the technique of our tuna long - line fishery

    為提高我國遠洋金槍魚延繩釣漁業的技術水平，並為我國相關生產企業提供產業發展的最新信息，本文報道了印度洋海域金槍魚漁業近十年的生產概況，並以中魯遠洋漁業股份有限公司兩條大型金槍魚延繩釣漁船2002年的生產數據為基礎，對印度洋赤道附近海域金槍魚延繩釣漁業的捕撈努力量、漁獲量、單位捕撈努力量漁獲量及作業漁場等進行了初步研究。
  6. ( 4 ) the correlations are significant between the sth position index and the general circulation. in the westerly ( easterly ) year, equatorial westerly is weaker ( stronger ), cross - equatorial flow is weaker ( stronger ), south china sea summer monsoon is weaker ( stronger ), the yangtze river valley westerly is stronger ( weaker ), which has the positive ( negative ) effect on the maintenance of rain band over the yangtze river valley, so the rainfall is more ( less ) in this area and it is hit by floods ( droughts ), vice versa

    （ 4 ）本文運用定義的副高指數研究了六月份副高偏東偏西年份的大型環流特徵及其對我國東部天氣的影響，風矢量場和相關場分析結果表明：副高偏西（東）年，赤道西風減弱（增強） ，越赤道氣流偏弱（增強） ，南海夏季風偏弱（強） ，而長江流域西風增強（減弱） ，有（不）利於雨帶在江淮流域維持，該地區降水偏多（少）易澇（旱） 。
  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. In continuous radio contact with the vtc, the hps launches patrol the main harbour area, all port approaches and the restricted areas around the hong kong international airport at chek lap kok

    海港巡邏組轄下的船隊負責巡邏主要港區、所有進港航道和赤蒼角香港國際機場四周的限制區域，利用無線電通訊與船隻航行監察中心不斷聯絡。
  10. With a party of 31 scientists, technicians and students onboard our research vessel, we spent almost two months sampling the physical and chemical properties of the western south atlantic, from top to bottom, starting near antarctica and ending near the equator

    研究船上共有31位科學家、技師和學生，我們花了將近兩個月，在南大西洋西側進行海水物理與化學性質的取樣剖面，涵蓋區域從南極附近開始，到赤道附近結束。
  11. El ninos can push temperatures higher than they might ordinarily be. this happened in 1998 when a so - called % 22super el nino % 22 helped heat the earth to a record high

    論文中提到，重要的一點是， 2005年的全球溫度范圍和1998年相同，可能是近百萬年來地球溫度最高的一年，但常發生% 22厄爾尼諾% 22現象的東赤道太平洋海域的海表水溫並沒有變暖的跡象。
  12. 3 ) the teleconnection between winter sst of north pacific and summer precipitation is the areas of equator east pacific and black current with the areas of middle and lower reaches of yangtze river and hetao

    3 ）冬季太平洋sst與我國東部夏季極端降水量的遙相關型主要表現在，赤道東太平洋及黑潮海域的冬季海溫與長江中下游地區和河套地區的遙相關型。
  13. What ' s important is that 2005 was in the same temperature range * as 1998, and probably was the warmest year ever, but with no sign of the warm surface water in the eastern equatorial * pacific typical of el nino

    論文中提到，重要的一點是， 2005年的全球溫度范圍和1998年相同，可能是近百萬年來地球溫度最高的一年，但常發生「厄爾尼諾」現象的東赤道太平洋海域的海表水溫並沒有變暖的跡象。
  14. What is significant, the scientists wrote, is that 2005 was in the same temperature range as 1998, and probably was the warmest year ever, with no sign of the warm surface water in the eastern equatorial pacific typical of an el nino

    論文中提到，重要的一點是， 2005年的全球溫度范圍和1998年相同，可能是近百萬年來地球溫度最高的一年，但常發生"厄爾尼諾"現象的東赤道太平洋海域的海表水溫並沒有變暖的跡象。
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