bay of bengal 中文意思是什麼

bay of bengal 解釋
孟加拉灣
  • bay : n 1 （比 gulf 小、比 cove 大的）灣，海灣。2 （山中的）凹地。3 【火箭】凹槽；盤，艙。4 【英軍】戰...
  • of : OF ＝Old French 古法語。
  • bengal : n. 1. 孟加拉〈亞洲〉。2. 孟加拉生絲（織品）。
  1. Arakan stretched for some 350 miles along the eastern shore of the bay of bengal.

    阿拉干山脈沿著孟加拉灣東岸延伸約350英里。
  2. The somali jet and the south china sea ( scs ) cef in the lower level play an important role in the onset of the south china sea summer monsoon ( scssm ). the somali jet is rapidly enhanced two pentads prior to the onset of scssm, thus accelerating the eastward extension of the westerly over the bay of bengal and leading to the eastward retreat of the western pacific subtropical high ( wpsh )

    低層的索馬里和南海越赤道氣流對南海夏季風的爆發有至關重要的作用，在南海夏季風爆發前2候，索馬里急流有一次迅速的增強，這一增強有利於加速孟加拉灣地區西風的向東擴展，並使控制在南海的西太平洋副高東撤；同時，南海越赤道氣流的迅速增強也加速副高的北上，共同促使南海夏季風全面爆發。
  3. About 100 bangladeshi fishermen are feared drowned after their boats sank in a storm in the bay of bengal

    大約100個孟加拉國的漁夫被嚇到在他們的船洗物槽之後在孟加拉的海灣的一陣暴風雨中淹死。
  4. The above analysis showed that this heavy rainfall event took on obvious meso - scale characters and was the combination of the three flows, so we can deduce : ( 1 ) surface southeasterly wind and topography may play the main role in this event ; ( 2 ) the easterly cold air rushing into the southern shaanxi province in the lower troposphere was strongly relative to the form of surface cold - front type of occlusion ; ( 3 ) there were two reasons for the secondary circulation ' s strengthen in the evening, one was the effect of a mountain - valley wind and the other may be latent heat leading to ascending motion ; ( 4 ) the shape of potential instability stratification corresponded well with the development of the warm - moisture advection ; and ( 5 ) the vapor providing essential thermodynamics was transported by a southwesterly low - level jet from the bay of bengal and the south china sea. furthermore, with the effect of terrain, the southern shaanxi province became the center of this extremely heavy rain process

    中尺度結構分析表明，本次暴雨具有明顯的中尺度特徵，是由三支氣流共同作用的結果，分析發現（ 1 ）地面東南風和地形在這次大暴雨過程起主要作用； （ 2 ）東路冷空氣主要是通過中低層侵入陜南地區的，並與地面冷式錮囚鋒的形成密不可分； （ 3 ）夜博士論文:中尺度地形對陜南暴雨的影響研究間垂直次級環流發展加強可能有兩個原因，一個是由於地形山谷風的作用，另一個是降水的潛熱釋放激發了上升運動: （ 4 ）位勢不穩定層結的形成與低層暖濕平流的發展有很好的對應關系; （ 5 ）本次暴雨的水汽主要靠偏南風急流將孟加拉灣和中國南海的水汽輸送至西北地區東部，為暴雨的發生提供了必要熱力條件。
  5. One of the first tasks of the recovery team will be to organize surveys of the main non - breeding grounds for this shorebird in the bay of bengal bangladesh, which has previously not been surveyed extensively

    救援小組的首個任務是前往這種濱鳥的主要非繁殖地孟加拉灣，進行比以往詳盡的調查。
  6. ( 3 ) when the heat source over the bay of bengal is abnormally strong ( weak ), the sourthern asian high extends westward ( eastward ), and the western pacific subtropical high extends eastward ( westward ), and the indian summer monsoon is stronger ( weaker ), and the eastern asian tropical summer monsoon is weaker ( stronger )

    （ 3 ）當孟加拉灣熱源異常強（弱）時，南亞高壓偏西（東） ，西太平洋副熱帶高壓位置偏東（西） ；印度夏季風偏強（弱） ，東亞熱帶季風偏弱（強） 。
  7. When the heat source over the bay of bengal was abnormally strong ( weak ), the southern asian high extended westward ( eastward ), and the western pacific subtropical high extended eastward ( westward ), and the indian summer monsoon was stronger ( weaker ), and the eastern asian tropical summer monsoon was weaker ( stronger )

    當孟加拉灣熱源異常強（弱）時，南亞高壓偏西（東） ，西太平洋副熱帶高壓位置偏東（西） ；印度夏季風偏強（弱） ，東亞熱帶季風偏弱（強） 。
  8. ( 4 ) there exists obviously negative correlation between the heat source over the bay of bengal and the precipitation of the sourtn of the yangtze river and the parts of the east of south china in summer, and there exists obviously positive correlation between the heat source over the bay of bengal and the precipitation of the area from the sourth west in china to the west of south china

    孟加拉灣熱源異常對南亞高壓、南亞季風、副熱帶高壓的影響是顯著的，對東亞熱帶季風的影響並不顯著。 （ 4 ）夏季孟加拉灣熱源與同期長江以南、華南東部的部分地區的降水存在明顯的負相關關系，而與西南到華南西部地區呈明顯的正相關關系。
  9. The responses of asian monsoon circulation to the heat source annual anomalies over the bay of bengal and philippines in summer and the annual relationships between the heat sources over the bay of bengal and philippines and the precipitation of china in summer are studied emphatically, with the results as follows : ( 1 ) the coverage and intensity of atmospheric heat source are the largest and strongest in summer and then turn smaller and weaker in autumn and winter, and in turn begin to become larger and stronger in spring again

    著重討論了夏季孟加拉灣和菲律賓熱源年際異常時，亞洲季風環流系統的響應，及其與中國夏季降水的年際關系。結果表明： （ 1 ）夏季大氣熱源的范圍最大，強度最強，以後以秋、冬季依次變小變弱，春季又開始變大變強。夏季亞洲季風區有三個強的大氣熱源中心，其中以孟加拉灣熱源最強，菲律賓熱源和印度半島西部熱源次之。
  10. Using the daily and monthly ncep / ncar reanalysis data from 1951 to 2000 and monthly precipitation of 160 stations in china in summer from 1951 to 2000, the climatic distribution of heat source are computed. the responses of the asian monsoon circulation to the annual anomaly of the heat source over the bay of bengal in summer and the annual relationship between the heat source and the precipitation of china in summer are analyzed

    摘要利用1951 - 2000年ncep / ncar再分析逐日及月平均資料和我國160個測站1951 - 2000年月降水量資料，計算了夏季大氣熱源氣候分佈，分析了夏季孟加拉灣地區熱源年際異常及亞洲季風環流系統的響應，以及夏季孟加拉灣地區熱源與中國夏季降水的年際關系。
  11. It is showed that the heat transport crossing the equator has the similar magnitude and the same period of one year, compared with that of 10 n in arabian sea. by contrast, the heat transport across 10 n in bay of bengal has a much smaller value with a prominent semiannual period ; there are tight relationship between integrated zonal wind stress in one latitude of the indian ocean north of 7 n and the total heat transport across that latitude, as well as the total net surface heat flux north of that latitude. the maximum correlation coefficient is less than - 0. 5

    結果表明越赤道和越10on阿拉伯海的熱輸送量大小具有可比性，且有相同的年循環特徵，而10on孟加拉灣緯度的經向熱輸送較小，且具有半年變化周期;儼s以北印度洋任一緯度上的緯向風應力異常與此緯度上的經向熱輸送異常以及此緯度以北印度洋總的海面凈熱通量異常有很好的相關關系，相關系數最大可達一0 . 5以上。
  12. The results show that the strongest heat source heating center was located over the north - east of the bay of bengal in summer

    結果表明：夏季亞洲季風區最強的熱源中心位於孟加拉灣東北部一帶。
  13. The sundarbans mangrove forest, one of the largest such forests in the world ( 140, 000 ha ), lies on the delta of the ganges, brahmaputra and meghna rivers on the bay of bengal

    孫德爾本斯國家公園是世界上最大的紅樹森林之一，佔地面積140 ， 000公頃，位於孟加拉灣的恆河、布拉馬普特拉河和梅克納河三角洲。
  14. The first few days of the voyage passed prosperously, amid favourable weather and propitious winds, and they soon came in sight of the great andaman, the principal of the islands in the bay of bengal, with its picturesque saddle peak, two thousand four hundred feet high, looming above the waters

    不久，仰光號上的旅客已經看見了安達曼群島的主島大安達曼島。島上美麗的鞍峰山高達兩千四百英尺，老遠地就為航海家們指出了前進的方向。
  15. River transport in the sunderbans site, bay of bengal an appropriate analogy to this ramsar site designation is the recognition of a scholar awarded a nobel prize

    一片濕地能獲得拉姆薩爾公約的認定，可比擬學者獲頒諾貝爾獎的殊榮。
  16. Three passages of vapor transfer are related to the regional precipitation, especially the one carrying water from the bay of bengal. mixed cold and warm cloud portions are favorable for " catalysis - water supply ". the duration and rainfall - hit area are about half the lifecycle and rainbelt size, respectively

    ；降水天氣的主要水汽輸送路徑有三條，以來自孟加拉灣的西南水汽輸送帶對降水最為有利；雲系以冷暖混合雲體為主，具有發生「播撒-供應」機制有利的宏觀雲體條件；雲系降水的時段和面積一般只有雲系生命期和面積的一半。
  17. Are eddies nature ' s trigger to enhance biological productivity in the bay of bengal

    在孟加拉海灣渦旋是增強生物學能力的自然的引發嗎？
  18. It was related with the genesis and development of the sw monsoon surge over the bay of bengal

    它是與孟加拉灣西南季風潮發生發展相聯系的。
  19. ( 2 ) there exist obviously interannual and interdecadal changes in the heat sources over the bay of bengal and philippines

    （ 2 ）夏季孟加拉灣熱源和菲律賓熱源都存在明顯的年際和年代際變化。
  20. Countries in bay of bengal affected by the strongest earthquake in 40 years caused massive tidal waves, killing hundreds of thousand people, over one million people homeless

    印度洋多國遭受四十年來最嚴重地震及海嘯侵襲，死傷無數，上百萬人無家可歸。
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