warm pool 中文意思是什麼

warm pool 解釋
暖池
  • warm : adj 1 暖和的，溫暖的；保暖的。2 熱情的，熱心的，熱烈的；多情的。3 易怒的；興奮的；激烈的，激昂的...
  • pool : n 1 （天然）水坑，水塘；水池子，沉澱池；游泳池；龍潭。2 〈美國〉油田地帶；石油層；瓦斯層；煤坑。3...
  1. It could play an important role in the evolution of " warm pool " area. more than 300 pure psychrophilic and psychro - tolerant bacteria were isolated from environmental samples

    對深海沉積物和極地環境樣品進行了低溫微生物的分離和培養，得到了300多株嗜（耐）冷細菌，並對其進行了生長特性的分析。
  2. 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。
  3. 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。
  4. 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。
  5. In a beauty treatment imported from turkey, bathers at " dr fish ", a new spa in the hot spring resort of hakone, dip their feet into a warm pool teeming with fish that nibble away at dead skin and bacteria

    在一個名為「魚醫生」的新溫泉區里，浴療者把他們的腳伸進一個暖水池中，池中的一條條小魚就會慢慢啃掉他們腳上的死皮和細菌。
  6. It is more than 3, 000 miles long. the water in it is 9 degrees warmer than in surrounding areas - a substantial number to oceanographers. and the warm pool is growing

    這條溫水帶長達3000多英里，水溫比周圍海域高9度，這個數字對海洋學家有重要意義。而且，這個溫水域正不斷擴大。
  7. The text takes three slope towns, warm pool towns and west imperial tomb towns as examples, has carried on case study

    本文以三坡鎮、溫塘鎮以及西陵鎮為例，進行了個案研究。
  8. 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。
  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. Workshop on the network system for monitoring and predicting enso event and sea temperature structure of the warm pool in west pacific ocean. 5 - 7 february, 2001, macao

    2002熱帶海洋環境與氣候變化研討會，三亞， 2月26日3月1日。王東曉（南海環流模式比較初步結果、太平洋年代際變化的強迫因子、南海環流的多渦結構） 。
  12. The tropical warm pool international cloud experiment involves scientists from australia, europe, the united states and japan and aims to find out how the high - altitude cirrus clouds are formed and break up

    據路透社1月19日報道，參與該項實驗的科學家們分別來自於澳大利亞美國日本及歐洲等國。科學家們希望通過此舉能弄清高緯度捲雲是如何形成和消散的。
  13. 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。
  14. Eastern pacific warm pool

    東太平洋暖池
  15. 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
  16. 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。
  17. 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。
  18. 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。
  19. 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。
  20. 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。
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