海洋上層 的英文怎麼說

中文拼音 [hǎiyángshàngcéng]
海洋上層 英文
u er layer of the ocea
  • 洋 : Ⅰ名詞1 （海洋） ocean 2 （洋錢） silver coin 3 （姓氏） a surname Ⅱ形容詞1 （盛大; 豐富） vast; m...
  • 上 : 上名詞[語言學] （指上聲） falling-rising tone
  • 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...
  • 海洋 : seas and oceans; ocean; [詩歌用語] blue海洋霸權 maritime hegemony; 海洋保護區 marine preserve; 海...
  1. Towards morning nothing was left of the fog on the heights but a hoar frost passing into dew, but in the valleys the fog still lay in a milky - white sea

    黎明前，夜裡的霧靄在高地上只留下一層轉化為露水的白霜，那霧靄還像乳白色的海洋一般彌漫于谷地之中。
  2. On the surface of msta, there exists true dipole mode in the indian ocean, that ' s to say that if the temperature anomaly in the western indian ocean is positive, it is much likely that there is negative anomaly in the eastern indian ocean. dipole mode also exists in the pacific as that in the indian ocean. by virtue of the walker circulation and the similar circulation above the indian ocean, it is showed that the air - sea interaction events in the tropical pacific and the indian ocean develop with each other at the same time

    由於在次表層海溫距平極值面上，熱帶西、東印度洋的海溫距平呈真正意義的偶極子模態，即當西印度洋海溫距平為正（負）時，東印度洋海溫距平為負（正） ，偶極子模態的海溫距平分佈在熱帶太平洋同樣存在，兩大洋海溫距平的偶極子模態間有密切的聯系，結合walker環流和印度洋上空的類似walker環流，進而指出熱帶印度洋和太平洋海氣相互作用事件是協調發展的。
  3. The sea surface high ( ssh ) images in winter show almost a reverse pattern of that in summer

    模擬得到的流函數表明海盆尺度氣候平均意義下的南海上層海洋動力是sverdrup平衡。
  4. To the large - scale atmosphere, we separate the terms of the horizontal vorticity converting into the vertical vorticity, which considered as the baroclinic terms, from the terms that not including horizontal vorticity by the rules of the p coordinate transforming to the z coordinate in the traditional vorticity equation, and carry out the scale analysis, and then conclude that the baroclinic terms are able to reach the same magnitude grade as the partial derivative of the vertical vorticity to time when it takes place the large scale precipitation in the summer monsoon period in china. by analyzing the game reanalysis data from april to august in 1998 in the region of chinese continent, we found that the baroclinic terms is important to the large - scale cyclone developing above the 600hpa, and the magnitude changing of the baroclinic terms is nearly in - phase as the monsoon movement, so which imply exactly that the magnitude changing of the baroclinic terms is the one of the natural characters of the summer monsoon evolution and equivalent to the movement rule of the subtropical high of the western pacific

    在p坐標垂直渦度方程中，利用p坐標向z坐標轉換的公式將水平渦度向垂直渦度轉化的所有項分離出來，這些項具有明顯的斜壓特徵，對其進行尺度分析后，得出在可以忽略潛熱釋放對渦度影響的對流層中、高層，此轉化項是大尺度斜壓渦度發展的重要項。通過對1998年48月的game再分析資料進行實際計算也發現，轉化項在東亞夏季風上升支的600hpa及以上層次對垂直渦度的局地變化貢獻很大，不能忽略。同時發現水平渦度向垂直渦度的轉化在南海季風爆發時和江淮梅雨入梅及發展過程中均有指示性意義，在南海季風爆發以後，在中國東南部地區，轉化項的大小與夏季風的活躍和中斷等活動有著幾乎一致的變化規律，這從側面也指出了，此轉化項的變化是夏季風演變所具有的本質特徵，並且它反映出了西太平洋副高在中國大陸的活動情況。
  5. 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。
  6. Near small river, as along the oregon coast, upwelling can occur when winds move the low - salinity surface layer seaward and the cold, upwelled waters underneath are exposed

    靠近小河口地區，如俄勒岡州海岸，當風把低鹽度的表層水向海洋方向吹時，涌升現象就會出現。這時，下面寒冷的、涌升上來的海水就暴露了出來。
  7. Jacket is the most widely used offshore platform structural style. first of all, the paper summarizes the present achievements of dynamic analysis for offshore platform, and studies both the vibration isolation system for jacket and vibration - suppressed effectiveness. considering the style and character of jacket, and in order to make best use of dampers to reduce vibration, a damping isolation scheme, in which the damping layer is laid between the jacket cap and deck is put forward

    本文在總結國內外對海洋平臺結構動力分析研究現狀的基礎上，針對淺海導管架式海洋平臺的型式與結構特點，研究了導管架式海洋平臺結構阻尼隔振體系及其減振效果，為了充分發揮阻尼器的耗能減振作用，提出了在平臺結構導管架端帽和甲板之間設置柔性阻尼層的新型阻尼隔振方案。
  8. Thus, as the ocean becomes more and more acidic, the upper, shell - friendly portion will become thinner

    因此，隨著海洋越來越酸，海洋上層利於有殼生物存活的部份會變薄。
  9. ( 2 ) ln winter of the northern hemisphere, because of the difference in the land - ocean distribution, the temperature nowadays is lower than that of 14mab. p. simulated in the upper layer but higher in the middle layer ( about 200 - 1500m ). in deep ocean the discrepancy of temperature seems hardly to be obvious

    （ 2 ）北半球冬季，由於海陸分佈的差異使得海溫在海洋上層古海溫要暖于現代，在海洋中上層（約200 ? 1500米）現代的海溫則要暖於14mab
  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. In each of the three major topics involved in the dynamics of the upper ocean this process can be followed.

    上面談到了涉及上層海洋動力學的三個主要方面，我們可以就這三個方面來回顧一下本學科的發展過程。
  12. The interannual and decadal variability of precipitation for yunnan province in rainy season and its relationship with tropical upper layer heat content

    雲南省雨季降水的年際年代際變化特徵及其與熱帶上層海洋熱含量分佈的關系
  13. We analyze the energy balance equations for mean flow, turbulence and wave motion in the ocean surface mixed layer, and discuss the wave - turbulence interaction involved. the observed phenomena, in which vertical turbulence mixing and turbulence dissipation are enhanced by the action of breaking wave, are explained

    以現有的理論研究為基礎，通過分析海洋上混合層中考慮波浪運動的能量平衡方程，探討了混合層中波?湍相互作用的物理機制，並對波浪破碎導致混合層內湍流混合加強和耗散增加的現象進行了分析。
  14. Furthermore, because of the scarcity of measurements and data, our work has to be limited to investigating the effect of wave breaking on the ocean surface mixed layer by the numerical models

    同時，由於無法獲得觀測資料，本文所得的波浪破碎對海洋上混合層影響的數值研究結果沒能與現場觀測結果比較。
  15. Gao huiwang, aerosol pollution from dust storms in qingdao ， sino - us workshop on dust storm and its effect on human health ， nov. 25 - 26 ， 2002, raleigh, north carolina, usa

    高會旺.大氣對海洋的物質輸入，上層海洋低層大氣相互作用及其氣候效應學術研討會， 2002年11月，青島。
  16. The ocean surface mixed layer plays an important role in the processes of the exchange of heat and momentum between the upper ocean and the atmosphere

    海洋上混合層在大氣和海洋之間的水汽、熱量和動量的交換過程中有著重要的作用。
  17. In some, a destructive fishing practice called bottom trawling, which scours life from the ocean floor, is permitted

    有些地區對海洋底層生物掠奪性捕撈的破壞性底層拖網式捕撈事實上是允許的。
  18. An unseen “ forest ” of microscopic beings fills the upper 200 meters of ocean, exerting an influence on this planet every bit as profound as the forests on land

    海洋表層200公尺水域是一片長滿微生物的隱形森林，它對地球的影響力與陸上森林不相上下。
  19. The understanding of the effects of atmospheric forcings, including mainly the surface wind stress, net heat flux and buoyant flux, on the dynamical and thermal structure of the ocean surface mixed layer necessitates a proper knowledge of the mechanisms and influences of the different turbulent mixing processes involved in the upper ocean

    海洋上混合層的動力學和熱力學結構特徵主要受到海表風應力、凈熱通量和浮力通量的影響，而混合層的形成與維持依賴于混合層內的湍流生成和湍流垂向混合。
  20. Europa ' s fractured icy surface is thought to overlie an ocean about 100 kilometers ( 60 miles ) below the surface, and the new horizons team will be analyzing these images for clues about the nature of the icy crust and the forces that have deformed it

    木衛二的典型冰封表面被認為是躺在100千米冰層下的海洋上， 「新視野」的小組將分析這些圖片尋找冰蓋特性的線索以及使其變形的力量。
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