溫躍層 的英文怎麼說

中文拼音 [wēnyuècéng]
溫躍層 英文
thermal layer
  • 溫 : Ⅰ形容詞（不冷不熱） warm; lukewarm; hot; gentle; mild Ⅱ名詞1 （溫度） temperature 2 （瘟） acute ...
  • 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. 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。
  9. 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。
  10. 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。
  11. 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。
  12. 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。
  13. 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。
  14. 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。
  15. But it will affect the airflow organization with the cooled airflow drops. also, it studies the impact of solar radiation on displacement ventilation and cooled ceiling system. horizontal warm areas lowers the height of thermocline and is unfavorable to displacement ventilation system ; vertical hot surfaces will destroy the thermal stratification

    水平熱表面的存在，會使系統的溫躍層高度降低，對置換通風系統會有負面影響，為了減小水平熱表面的影響，對于地板材料應該選擇對長波輻射吸收較低的物質;垂直局部熱表面的存在會破壞置換通風系統溫度分層的特性，使垂直方向溫度變化減小。
  16. Furthermore, analysis on the relation between the local wind stress curl anomalies ( wsca ) and smta shows that wsca plays different roles on smta due to its different variances. there exists strong correlation between them in those regions with large variance of wsca, and the change of wsca precedes that of smta. the analysis also shows that wsca mainly affects smta by changing the depth of the thermocline

    進一步分析了局地風應力旋度異常（ wsca ）與smta的關系，指出由於不同區域的wsca的變率不同，從而對smta的影響也不同，在wsca變率大的區域，兩者具有很強的相關性，而且風應力的變化早於溫度距平的變化；分析還表明， wsca主要是通過影響溫躍層深度對smta產生影響的。
  17. The mean error of ssp inversion by this algorithm is less than that by mfi when the sediment parameters is known a priori. the ssp inversion by this algorithm shows a better match to the measured ssp in the step layer

    Mbi反演ssp對沉積層參數失配具有較高的穩定性，當根據先驗信息確定沉積層參數后， mbi反演ssp均方根誤差小於匹配場反演方法反演得到的結果，並且mbi反演ssp的溫躍層部分更接近實際測量ssp 。
  18. The thermocline classification method has been worked out on the basis of the classification theory for various thermocline types and in the light of temperature profile characteristics of scs. so the result can clearly reflect the distributional pattern of the thermocline in the south china sea

    用該方法分類、統計計算並繪制的南海溫躍層圖件，能夠真實清楚地反映出南海溫躍層的分佈規律，對整個研究工作起到至關重要的核心作用。
  19. Based on this, the numerical model is used in the south china sea. the upper thermocline is the first level, and the rest is the second level. the initial values kv of assimilation is 2. 0xl ( t4 / ? 1s ' ~ l and the time window of assimilation is 1 month

    在此基礎上，我們將該模式應用於南中國海，分層取在溫躍層處，選取2 . 0 10 ~ （ - 4 ） m ~ 2s ~ （ - 1 ）為垂直混合系數的同化初值，同化時間長度為一個月。
  20. The approach adopted in the thesis was proven to be successful, and can be generally applied to study the mixing and stratification process in other shallow seas and shelf oceans

    且完整、全面地反映了整個渤海溫躍層空間分佈特徵，及其隨時間演變的細致過程。這種方法具有適普性，可用於其它陸架海域混合和層化的研究。
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