暖池 的英文怎麼說

中文拼音 [nuǎnchí]
暖池 英文
warm drop
  • 暖 : Ⅰ形容詞（暖和） warm; genial Ⅱ動詞（使東西變熱或使身體變溫暖） warm up
  • 池 : 名詞1 （池塘） pool; pond 2 （旁邊高中間窪的地方） an enclosed space with raised sides 3 （舊指劇...
  1. The topography and the physiognomy of the south china sea are very complex such as continental slop, continental shelves, seamounts, sea basin, etc. the south china sea lies between qingzang plateau, which is as the main driver of the variety of climate, and the western part of the pacific, which is called warm pool, and is influenced by some current systems, such as coastal current, kuroshi, etc. the south sea has considerable species

    南海具有陸坡、陸架、海溝、海盆等復雜的地形、地貌；南海位於作為地球氣候變化的主要驅動力的青藏高原和西太平洋暖池之間；南海受到沿岸流、南海暖流水、黑潮入侵水等流系的影響；南海具有豐富的物種分佈；上述因素共同影響南海生源要素的分佈、輸送和遷移。
  2. Members of the cfb ( cytophaga - flexibacter - bacteroides ) were found to be rich in upper sediment of " warm pool " while they were not detected in sediment from " manganese nodule " area, which indicated that there were more organic substances in the " warm pool " area

    除了紫細菌之外， cfb類群在「暖池」區沉積物中也是一類較重要的細菌，主要集中在表層沉積物；而在「結核」區沒有檢測到屬于cfb類群的細菌，表明「暖池」區表層存在較多的有機物。
  3. The results of archaeal diversity analysis showed that most of the members belonged to crenarchaeota, and included many unidentified archaea species. abundant bacteria related to the metabolism of sulfur and methane were found in sediment collected from " warm pool " area, which indicated that the metabolism of sulfur and methane played an important role in the substance and energy conversion of this area

    在「暖池」區沉積物中發現了豐富的與硫及甲烷代謝相關的細菌，對這些細菌的種類組成及其在各層次沉積物中的分佈、數量進行了分析，發現該海區沉積物中存在一條完整的硫和甲烷代謝循環途徑，它們的代謝在物質能量代謝中占據重要的地位。
  4. Based on the epwp and wpwp in conjunction with abnormal north and west wind, a new possible iii mechanism is provided for the evolution of the 1997 / 1998 el nino. to be specific, the warm kelvin wave propagating to east excited by the abnormal west wind can suppress the cold upwelling flow in the eastern pacific, which, in turn, is favorable to the eastern pacific sst increase ; abnormal west wind can make the warm water of the wpwp east edge extend to east, which is conductive directly to eastern pacific sst increase ; the abnormal west wind propagating to east can make the sea surface warm water near two equatorial laterals converge to the equator by ekman drifting, which, in rum, strengthens the downwelling flow near the equator, leading to eastern pacific sst increase

    將東、西太平洋暖池及異常北風、西風一併結合起來考慮，提出1997 1998elnino事件發生、發展的一種新的可能機制：異常西風激發東傳的暖kelvin波對東太平洋的冷上翻流有抑制作用，從而有利於東太平洋海表溫度增加；異常西風驅動西太平洋暖池東端暖水向東伸展直接有利於東太平洋海表溫度增加；東傳的異常西風可以通過埃克曼漂流效應將赤道兩側的海表暖水向赤道輻合從而加強了赤道附近的下沉流，也有利於東太平洋赤道附近海表溫度增加。
  5. Scientists from 10 countries will release 1, 000 weather balloons in australia ' s northern city of darwin over the next month as part an international experiment to try to find out the nature of tropical clouds

    來自10個國家的科學家們將于下個月在澳大利亞北方城市達爾文放飛1000個氣象氣球。作為一項名為熱帶暖池國際雲層實驗計劃的組成部分，此舉旨在進一步弄清熱帶雲層的「真面目」 。
  6. 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。
  7. 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。
  8. Almost meanwhile, the north wind anomaly brings epwp warm water to equatorial vicinity by producing north ocean flow, which causes directly nino3 sst increase

    幾乎與此同時，北風距平通過產生北風吹流將東太平洋暖池暖水由北向南輸送至赤道附近直接導致nino3區海表溫度增加。
  9. ( 3 ) during the 1997 / 1998 el nino we find western pacific warm pool ( wpwp ) sst variation, abnormal west wind, eastern pacific warm pool ( epwp ) sst variation and abnormal north wind are associated with the nino3 index change

    （ 3 ）在1997 1998elnino事件期間，西太平洋暖池海表溫度變化及異常西風和東太平洋暖池海表溫度變化及異常北風兩者都與nino3指數變化密切相關。
  10. But only for the closure of indonesia passage, warm pool can be formed under 150m with the center between 300m and 600m or so while in upper layer the modern sea temperature is still colder, so seen from the simulation, only the open of indonesia passage can not form the warm pool like the present

    P ）模擬的海溫要暖，形成淺層暖池。但單是上述通道關閉，暖池只形成在150米以下，中心在300 ? 600米深海洋層，而海洋上層（ 150米以上）仍為現代冷。依數值模擬來看，只有上述通道的開啟，並不能形成如現代淺層海洋暖池。
  11. Especially, t - test shows that significance of the asia polar vortex, zonal circulation index, the most northern extension edge of subtropical high of northern west pacific and the warm pool of pacific ocean, are at 95 % （ 90 % ）

    特別地，亞洲極渦、緯向環流指數、西太平洋副熱帶高壓北界位置及太平洋暖池的海表面溫度等因子均通過了95 % （ 90 % ）信度水平檢驗。
  12. Eastern pacific warm pool

    東太平洋暖池
  13. Interannual variation of the indo - pacific warm pool and the atmospheric response to the variations

    太平洋暖池年代際變化及其大氣響應
  14. Based on the sst data, the temporal and spatial variations of ssta in western pacific warm pool region have been analyzed in this paper by means of eof

    本文通過對夏季熱帶西太平洋暖池區ssta的eof分析，發現夏季暖池區海溫存在兩種主要空間分佈型，即ssta的一致性分佈和南北半球反對稱分佈。
  15. The west pacific ocean " warm pool " plays an important role in global climate change, which makes it become one of the most important focuses of geoscience research

    西太平洋「暖池」在全球氣候變遷過程中起著舉足輕重的作用，是目前氣候變遷機制研究的熱點，同時也是地球科學研究的焦點之一。
  16. ( 4 ) the epwp climatologic sst has a clear intraseasonal variability, which is very similar to el nino growth process, i. e., occurring in spring, developing in summer, maturing in autumn and decaying in winter

    進一步分析表明，東太平洋暖池及異常經向風僅對日nino （ lanina ）事件發生、發展起促進（抑制）作用而不起決定作用。
  17. When the spatial pattern is of the north - south asymmetry, in the warm north - cold south years, there is a anticyclone circulation existing over the warm pool at 850hpa, easterly at 15 n and westerly in the tropical region have been greatly strengthened, while the center of anticyclone circulation moves to the east asia at 200hpa, and the hadley circulation has been affected evidently, so the summer rainfall may be above normal in the middle and lower reaches of the yangtze river, vice versa. there are different relations to east asia atmospheric circulation and summer rainfall in china

    當ssta為南北半球反對稱分佈時，與ssta北暖南冷分佈相對應， 850hpa暖池區上空為一反氣旋偏差環流， 15 n附近東風氣流和赤道附近西風氣流增強，長江中下游地區盛行偏南風氣流； 200hpa反氣旋偏差環流中心移到東亞大陸上空；副熱帶高壓強度、西伸脊點都明顯變強、西伸； hadley環流得到發展，長江中下游（華北）地區為上升（下沉）氣流，降水明顯增多（減少） ，北冷南暖年則相反。
  18. The difference of microbial group between different sea areas was the 8 - and e - subdivision of proteobacteria, which was abundant at upper sediment of " warm pool " area while they were not detected at the sediments of " manganese nodule " area. at the core sediment of " warm pool " area, members of - proteobacteria reduced from upper to lower sediments

    在「結核」區沉積物中沒有檢測到屬于這兩個亞群的細菌，而在「暖池」區沉積物中屬于這兩個亞群的細菌數量較多（最高可達29 ） ，並且-亞群的細菌呈現隨沉積物深度增加而減少的趨勢。
  19. Based on the analyses, it was found that if the subsurface warm pool is regarded as the beginning point, the warm or cold signal propagates initially eastward and upward along the equatorial surface of msta to the eastern pacific and stays there several months and then turns north, usually moves westward near 10 to western pacific and finally propagates southward to return to warm pool to form an off - equator closed circuit. it takes about 2 to 4 years for the temperat ure anomaly to move around the cycle. if the smta of warm ( cold ) water is strong enough, there will be two successive el nino ( la nina ) events during the period of 2 to 4 years

    ） a事件下/負海溫距平信號的分佈和傳播「軌跡」 ，發現如果以暖池次表層為起點，則一般來說，暖水或冷水先是沿赤道的極值深度面向東、向上「傳播」或運動，到達赤道東太平海盆邊界附近后，分別轉向向北和向南運動，然後在南、北緯10左右再折向西運動，並在暖池的經度范圍內再作經向運動傳到暖地，即在南、北半球以赤道為一邊， 「傳播」或運動路徑形成扁的閉合環路，溫度距平運動一圈需時2 - 4年。
  20. When the spatial pattern is uniform in the whole area, there is a better relations between the wp ssta and walker circulation, hadley circulation, enso and the summer rainfall of the upper and middle reaches of the yangtze river, while the spatial pattern is of the north - south asymmetry, there is a better relation between the wp ssta and hadley circulation and the summer rainfall of the middle and lower reaches of the yangtze river

    暖池區ssta不同分佈型與東亞大氣環流和中國夏季降水關系不同， ssta的一致性分佈與hadley 、 walker環流、 enso循環及長江中上游地區降水關系較好，而ssta南北反對稱分佈與hadley環流和長江中下游地區降水關系較好。
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