海洋上層的 的英文怎麼說

中文拼音 [hǎiyángshàngcéngde]
海洋上層的 英文
epipelagic
  • : 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...
  • : 上名詞[語言學] (指上聲) falling-rising tone
  • : 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...
  • : 4次方是 The fourth power of 2 is direction
  • 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,夜裡霧靄在高地只留下一轉化為露水白霜,那霧靄還像乳白色一般彌漫于谷地之中。
  2. The somali jet and the south china sea ( scs ) cef in the lower level play an important role in the onset of the south china sea summer monsoon ( scssm ). the somali jet is rapidly enhanced two pentads prior to the onset of scssm, thus accelerating the eastward extension of the westerly over the bay of bengal and leading to the eastward retreat of the western pacific subtropical high ( wpsh )

    索馬里和南越赤道氣流對南夏季風爆發有至關重要作用,在南夏季風爆發前2候,索馬里急流有一次迅速增強,這一增強有利於加速孟加拉灣地區西風向東擴展,並使控制在南西太平副高東撤;同時,南越赤道氣流迅速增強也加速副高,共同促使南夏季風全面爆發。
  3. In this paper, features of decadal variability and the possible mechanism of sea - air system in the pacific are investigated by using upper - ocean temperature, heat storage and wind stress data, the main results are as follows : the most pronounce decadal sign exists at about 160 meter in depth in the western pacific. there are significant decadal abrupt changes in temperature from surface to deep in the subsurface at about 1980. with different depth in the subsurface, there exist 4 types of abrupt change modes, their generation is closely related to the decadal sign which originates from the east of north pacific and propagates along the south - west subduct ion route

    研究表明,太平次表溫最強年代際信號在熱帶西太平約160m深處,此信號在1980年前後從至下,先後經歷了一次顯著年代際突變過程,而且隨深度不同存在著四種不同空間突變模態,這四種模態形成與北太平溫異常西南潛沉路徑有著密切聯系。
  4. 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

    由於在次表溫距平極值面,熱帶西、東印度溫距平呈真正意義偶極子模態,即當西印度溫距平為正(負)時,東印度溫距平為負(正) ,偶極子模態溫距平分佈在熱帶太平同樣存在,兩大溫距平偶極子模態間有密切聯系,結合walker環流和印度類似walker環流,進而指出熱帶印度和太平氣相互作用事件是協調發展
  5. The sea surface high ( ssh ) images in winter show almost a reverse pattern of that in summer

    模擬得到流函數表明盆尺度氣候平均意義下動力是sverdrup平衡。
  6. 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坐標轉換公式將水平渦度向垂直渦度轉化所有項分離出來,這些項具有明顯斜壓特徵,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對流中、高,此轉化項是大尺度斜壓渦度發展重要項。通過對1998年48月game再分析資料進行實際計算也發現,轉化項在東亞夏季風升支600hpa及以次對垂直渦度局地變化貢獻很大,不能忽略。同時發現水平渦度向垂直渦度轉化在南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,在南季風爆發以後,在中國東南部地區,轉化項大小與夏季風活躍和中斷等活動有著幾乎一致變化規律,這從側面也指出了,此轉化項變化是夏季風演變所具有本質特徵,並且它反映出了西太平副高在中國大陸活動情況。
  7. 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:大規模資料處理方法、質量控制;溫躍計算機識別、溫躍統計分類方法;南溫躍三項示性特徵圖繪制;南溫度躍影響因素、南溫度躍分佈狀況;南森資料與bt資料計算南溫躍結果比較;溫度結構模式及計算等。
  8. 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,如俄勒岡州岸,當風把低鹽度水向方向吹時,涌升現象就會出現。這時,下面寒冷、涌升水就暴露了出來。
  9. 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平臺結構動力分析研究現狀基礎,針對淺導管架式平臺型式與結構特點,研究了導管架式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新型阻尼隔振方案。
  10. Thus, as the ocean becomes more and more acidic, the upper, shell - friendly portion will become thinner

    因此,隨著越來越酸,利於有殼生物存活部份會變薄。
  11. ( 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,由於陸分佈差異使得溫在溫要暖于現代,在(約200 ? 1500米)現代溫則要暖於14mab
  12. 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 )模擬溫要暖,形成淺暖池。但單是述通道關閉,暖池只形成在150米以下,中心在300 ? 600米深,而( 150米以)仍為現代冷。依數值模擬來看,只有述通道開啟,並不能形成如現代淺暖池。
  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

    以現有理論研究為基礎,通過分析混合中考慮波浪運動能量平衡方程,探討了混合中波?湍相互作用物理機制,並對波浪破碎導致混合內湍流混合加強和耗散增加現象進行了分析。
  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,本文所得波浪破碎對混合影響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.大氣對物質輸入,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

    混合在大氣和之間水汽、熱量和動量交換過程中有著重要作用。
  17. In some, a destructive fishing practice called bottom trawling, which scours life from the ocean floor, is permitted

    有些地區對生物掠奪性捕撈破壞性底拖網式捕撈事實是允許
  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

    200公尺水域是一片長滿微生物隱形森林,它對地球影響力與陸森林不相下。
  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

    混合動力學和熱力學結構特徵主要受到表風應力、凈熱通量和浮力通量影響,而混合形成與維持依賴于混合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

    木衛二典型冰封表面被認為是躺在100千米冰, 「新視野」小組將分析這些圖片尋找冰蓋特性線索以及使其變形力量。
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