躍層 的英文怎麼說

中文拼音 [yuècéng]
躍層 英文
main thermocline
  • 躍 : 動詞（跳） leap; jump
  • 層 : i 量詞1 （用於重疊、積累的東西 如樓層、階層、地層） storey; tier; stratum 2 （用於可以分項分步的...
  1. The subduct ion sign propagates toward the western tropical pacif ic ; and the decadal sign from the western tropical pacific propagates toward north - east. they meet at about 160 meter in depth in subtropical pacific

    從北太平洋窗口區潛沉的海溫年代際信號沿西南路徑傳播到副熱帶地區，在溫躍層160m上下與熱帶西太平洋向東北傳播的海溫異常信號會合。
  2. The thermocline area gets the largest in june, but its intensity gets the biggest in july

    南海溫躍層面積在6月就達到最大，強度在7月普遍達到最大。
  3. The model is divided into three boxes according to the depths of thermocline and eupthotic layer

    模型採用箱式模型，將模型根據溫躍層與真光層位置從上至下分為三個箱子。
  4. Among them the analysis of thermocline distributional pattern and the influence factor of scs are the core contents

    其中以探討分析南海溫躍層分佈狀況、分佈規律及影響因素為核心內容。
  5. The stratification is very obvious in the vertical profiles of chlorophyll and dissolved oxygen, with high content in the subsurface layer when thermocline exists

    在溫躍層存在季節，黃海冷水團水域的葉綠素和溶解氧含量出現次表層最大值現象。
  6. This study has done a large amount of work on the thermocline statistical method, the result verification and plotting, and has brought forth some new ideas

    南海溫躍層的統計分類方法是在各種溫躍層類型劃分理論的基礎上，結合南海溫度剖面結構特點確定的。
  7. Compared with the time of the thermocline in huanghai, east china sea, the thermocline of scs takes shape a month early, and no thermocline period takes place a month later

    與黃、東海溫躍層相比，南中文摘要海溫躍層形成規模的時間早一個月，晚1個月進入無躍層期。
  8. Research results indicate that, with the thermocline intensity of standard 0. 05 / m as a measure, there are shallow thermocline and deep thermocline all the year round in scs

    研究結果表明：以0 . 05 / m強度標準衡量，南海四季都存在上界小於50米的淺躍層和大於50米的深躍層。
  9. Therefore, in the development process of domestic and international ocean science, thermocline, particularly the seasonal thermocline, is always one of the main subjects

    因此，在國內外海洋科學的發展過程中，海洋溫度躍層，尤其是季節性溫度躍層的調查和研究一直是海洋調查研究的主要內容之一。
  10. In the open ocean above the deep sea bed, the vertical structure of the water mass is characterized by the presence of one of more thermoclines.

    處于深海床之上的外洋中，水體的垂直結構的特點是存在一個或一個以上的溫躍層。
  11. If a decadal positive temperature anomaly occurs in the eastern tropical pacific, the atmospheric response excites a anticyclonic wind stress anomaly in the east of australia, which will lead to generate a negative temperature anomaly in the western tropical south pacific

    當熱帶東太平洋的海溫為暖異常，它將激發澳大利亞的東部沿岸的大氣產生反氣旋性風應力異常，在這種風場的作用，下方海水向四周輻散，導致熱帶西南太平洋的溫躍層變淺，產生負的溫度異常。
  12. In the summer stratified water column, the deeper the maximum depth of food distribution is, the stronger the dvm is performed ; the increase of the gradient of temperature in the thermocline layer can decrease the magnitude of the dvm and form the thermal barricade to the copepod ; the effects of the predation pressure on dvm is complex. on the one hand, the variations in the distribution depth of the predation pressure vs. the thermocline layer or the depth of the maximum food can modify the dvm patterns of the copepod. on the other hand, different predation pressure induces different dvm patterns

    在夏季分層水體中，食物的最大分佈深度越大，動物向下遷移的幅度也越大；溫躍層的溫度梯度增大可以減小動物遷移的幅度，成為橈足類垂直遷移的溫度屏障；捕食壓力對垂直遷移的影響較復雜，一方面，捕食壓力的分佈深度與溫躍層或食物峰值的相對位置的變化能夠改變橈足類垂直遷移的模式，另一方面，捕食壓力強度不同，橈足類垂直遷移的幅度也不同，捕食壓力越大，遷移的幅度越大，當捕食壓力增加到一定程度，橈足類停止向上的遷移，大部分時間呆在水體深層，可能進入捕食壓力引起的「滯育」狀態。
  13. The thermocline reflects the ocean temperature field ' s important physics characteristics. it has important influence on underwater communication, submarine activity as well as fishery farming and fishing. it has close relations with branch subjects such as ocean current, water mass, inside wave, sea and air exchange

    溫度躍層是反映海洋溫度場的重要物理特性指標，對水下通訊、潛艇活動及漁業養殖、捕撈等有重要影響，並與海洋環流、水團、內波、海氣交換等分支學科關系密切。
  14. The shallow thermocline distributes in the areas of guangdong, guangxi, fujian and vietnam continental shelf, with obviously seasonal variabilily, and at the same time, in the south and middle areas of nanhai, even in winter when there is no thermocline in the coastal area, there also exists the shallow thermocline

    後者廣東、廣西、福建沿海陸架區則與黃、東海相同，表現為季節性溫躍層，有成長、強盛、消衰、無躍層的年周期變化過程。南海深溫度躍層基本屬於水團疊置型，躍層分佈范圍及躍層強度、上界深度、厚度與氣候關系不大。
  15. In term of soil water coefficient of variation, the soil water profile in 0 - 100cm can be divided into 3 layers, i. e., hypoactive layer, hypoactive layer and correspondingly stable layer. these soil water layers varied along with soil water consumption seasons alternating

    就綠地類型而言，活躍與次活躍層總深度：本特草坪高羊茅草坪泡桐綠地；就季節變化而言，弱耗水期活躍與次活躍層淺，強耗水期深，微耗水期較深。
  16. For a strong pycnocline, the horizontal resistance is small when the cylinder is in the pycnodine and it is large when the cylinder is outside the pycnocline

    對于強躍層的密度分佈，當樁柱處在躍層中時，受到的水平波阻較小，而在躍層之外則受到較大的水平波阻。
  17. In this text, according to south china sea ( scs ) hydrology investigation data, including the nansen data, bt and ctd data, thermocline distribution of scs and its characteristics have been studied. at same time, with the data of sun " s thermal radiation, air temperature, and other weather data the ocean thermocline has been calculated. the research involves the following aspects : large - scale data processing method ; data quality control ; thermocline identification and statistics method ; thermocline map ; thermocline influence factors of scs ; thermocline results comparison using nansen data and bt data ; thermocline forecast

    研究涉及到以下幾個方面：大規模資料的處理方法、質量控制；溫躍層的計算機識別、溫躍層的統計分類方法；南海溫躍層三項示性特徵圖的繪制；南海溫度躍層的影響因素、南海溫度躍層的分佈狀況；南森資料與bt資料計算南海溫躍層的結果比較；海洋上層溫度結構模式及計算等。
  18. Compared to bare land, soil water cycling on grassland with intensive transpiration was deeper in depth and greater in intensity

    與裸地相比，荒草地由於植被強烈的蒸騰作用，其土壤水分循環強度加劇，表現為活躍層、次活躍層以及蒸發蒸騰作用層深度增大。
  19. The correlation analysi s between sst and sea surface height, heat content and depth of thermocline also shows the important role of ocean dynamic processes in some regions, besides the influence of heat exchange between air and sea

    Sst與海表面高度、熱含量、溫躍層深度等的相關分析也表明，在某些區域，除受海洋-大氣之間熱交換的影響外，海洋動力過程對sst的影響也占重要地位。
  20. The surface of the maximum sea temperature anomaly ( msta ) was constructed from the subsurface sea temperature anomaly data in the tropical pacific from 1955 to 2002. it is quite similar to the depth distribution of the 20 ? c isotherm, which is usually used to represent the center of the thermocline layer

    利用1955 - 2002年48年熱帶、副熱帶太平洋地區次表層溫度距平資料，構造了溫度距平極值深度分佈的曲面圖（ msta ） ，它很接近20溫度面的深度分佈，因此有理由認為這一深度曲面很接近熱帶溫躍層的深度面。
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