海面風 的英文怎麼說

中文拼音 [hǎimiànfēng]
海面風 英文
sea surface wind
  • 面 : Ⅰ名詞1 （頭的前部; 臉） face 2 （物體的表面） surface; top 3 （外露的一層或正面） outside; the ri...
  • 風 : Ⅰ名詞1 （空氣流動） wind 2 （風氣; 風俗） practice; atmosphere; custom 3 （景象） scene; view 4 ...
  • 海面 : sea level; sea surface; sea海面標志 [工業] sea marker
  1. Zhoushan is sea area which fertility is tiptop in our country. sea surface wind is important factor of influencing contrail of excursion oil and culturist so investigating sea surface wind of zhoushan and setting up numerical forecast model which fits this sea area can offer tool for study sea wind in this area and let us has a mensurable acquaintance ship of effect degree of physics factors which effect sea surface wind in zhoushan sea area and acquaint oneself with physic process

    而海面風是影響溢油油團漂移軌跡和養殖業的重要因素，因此，對舟山海域的海面風進行研究，建立適合此區域的數值預報模式，可為研究該區域海面風作用過程提供數值預報工具，使我們對近海區域海面風場作用中物理因子的影響程度有更定量的認識，並對物理過程和影響機制有更深刻地了解。
  2. From the numerical modeling results, it can be found that there is a clockwise gyre in the middle part of bohai sea, whether in wintertime or in summertime. in summer, the clockwise gyre corresponding to the high - temperature and low - density center in the middle bohai sea is mainly dominated by the density circulation. and in winter, it is mainly dominated by the wind stress curl

    通過數值模擬結果發現，在渤海中部，無論冬季還是夏季，都存在一個順時針的渦旋運動，夏季，對應于渤海中部的高溫低密中心，其流場主體部分呈順時渤海冬夏季環流特徵及變異的初步研究針向旋轉，這主要是密度環流占優的結果，而冬季的順時針向的旋轉，主要是海面風應力旋度影響的結果。
  3. The fifth chapter sum up the article and view the work. the simulation results indicate : ( 1 ) exchanging of sea - air and force of dynamical and thermodynamic processes is very important to bring and maintain sea surface wind. shf is mostly energy sources and lhf is negative effect in some area

    模擬結果充分表明： （ 1 ）感熱和潛熱的海氣交換和動量交換（摩擦作用）對于海面風的發展和維持起著重要作用，潛熱加熱是海面風中最主要的能源，感熱通量在一武漢理工大學碩士學位論文定區域對海面風風場有負面影響。
  4. The methods reported by g. s. young in 2000, are applied on sea surface sar images featured by three dimensional convective cells. then the following parameters are retrieved from sar images : the characteristic wave length of three dimensional convective cell, the mabl depth, the vertical convective scale velocity, the surface buoyancy flux, obukhov length and the stability correction factor for sar derived sea surface wind speed

    針對海洋大氣邊界層中三維對流渦旋sar圖像，用g . s . young在2000年發表的方法，反演三維對流渦旋的特徵長度、海洋大氣邊界層高度、以及海洋大氣邊界層垂直對流尺度速度、表面浮力通量、海面風速穩定性校正因子和obukhov長度。
  5. Hf radar can measure the sea surface parameters. on oceanography, hf radar can be used in researching the property of ocean wave, supervising the sea status timely, getting offshore wind field picture as well

    它在海洋學上可用於研究海浪性質，能實時監測海況而服務于航海業、海洋工程、海洋警戒、海洋漁業和海洋平臺作業等，還能獲取氣象預報中所需要的海面風場圖。
  6. Research on ocean surface wind ambiguity removal algorithm for seawinds scatterometer

    Seawinds散射計海面風場模糊去除方法研究
  7. It is demonstrated very successfully that the simulated or real scatterometer data with the modified model estimation has been retrieved in this paper

    從結果可以看到，所採用的改進的場方式反演方法對模擬數據或真實散射計探測海面風場的反演是成功的。
  8. I stood still a few moments to recover breath, and till the water went from me, and then took to my heels, and run with what strength i had farther towards the shore

    午後不久，海面風平浪靜，潮水也已遠遠退去。我只要走下海岸，泅上幾十米，即可到達大船。這時，我心裏不禁又難過起來。
  9. The sea is quite lively today.

    今天海面風浪很大。
  10. I travell d first along the sea shore, directly to the place where i first brought my boat to an anchor, to get up upon the rocks ; and having no boat now to take care of, i went over the land a nearer way to the same height that i was upon before, when looking forward to the point of the rocks which lay out, and which i was oblig d to double with my boat, as is said above : i was surpriz d to see the sea all smooth and quiet, no ripling, no motion, no current, any more there than in other places

    我先沿海岸走到我上次泊船登上小山的地方。這次我用不著照管小船，就抄近路走上前次登過的那座小山崗。當我遠眺伸入海中的岬角時，前面我曾提到前次到達這兒時我不得不駕船繞道而行，但現在只見海面風平浪靜，那兒既沒有波瀾，也大出乎我的意料。
  11. Remote sensing of sea surface wind of hurricane

    颶風海面風場研究
  12. The terrain effect force wind ' s speed reducing and wind ' s direction turning to left with contrasting the experiments of numerical simulation the text analyses the structure and microcosmic character of sea wind in zhoushan maritime space and consanguineous connection between sea wind and action of dynamical and thermodynamic. the task gets the result of case a by using t213 datum of weather center and contrasts it with the actual sea wind. the task establish a foundation in order to use this mode in the environmental forecasting

    通過數值模擬對比試驗，分析了舟山海域海面風的結構和微觀特徵，以及海面風與動力作用（復雜地形）和熱力作用（海陸熱力差異）之間的密切關系。進一步利用國家氣象中心提供的t213高解析度預報場檢驗海面風風場的數值預報效果，最後將其結果與實際觀測作比較，為將該模式投入環境（海流，海浪，風暴潮等）動力預報奠定基礎。
  13. The main coupled mode of ssw and sst in the tropical pacific - south china sea - tropical indian ocean on interannual time scale

    印度洋海面風與海面溫度年際變化整體耦合的主模態
  14. Influence of initializing on the sea surface wind field numerical forecasting model in limited areas

    初始化方案對有限區域海面風場數值預報模式的影響
  15. By contrasting these simulative results, the experiments check up the forcing of heat flux and complex terrain to sea surface wind

    通過模擬試驗對比，以檢驗地形，感熱，潛熱對海面風風速、風向的強迫作用。
  16. The third chapter introduces the physical mechanism of sea surface wind firstly, then simulate five cases and contrast all results. based on the third chapter, the fourth chapter forecast case a with t213 datum and kzsy test and analyses the result in detail

    為分析方便第三章首先分析了海面風的物理機制，然後針對幾個海面風個例進行了5組模擬試驗，並對其結果進行了對比分析。
  17. The first chapter introduces the signification of working over zhoushan sea area sea surface wind and state - in - art and technical route. the second chapter explains the mesoscale atmosphere model - mm5v3, remark the mode system and controlling equations and emphases introduce the upswing of every module in order to fit zhoushan sea area

    因此第二章針對本論文的主要研究手段：中尺度大氣數值模式mm5v3進行了評述，對本文所採用的模式系統，控制方程組進行了介紹，並重點穿插介紹為適合舟山海域海面風的研究，各模塊所作的改進，為今後的具體應用提供研究基礎。
  18. Combine with the project " hf ground wave radar supervise sea status " of state 863 project, retrieving wind direction from hf radar doppler spectrum and the showing of wind field, current field, wave field are researched in this paper. the problem of how to represent the sea surface parameters by computer is concerned, too

    本文結合863 - 818 - 01 - 02課題「高頻地波雷達海洋環境監測技術」 ，研究了由高頻雷達海面回波提取風向信息和海面風場、浪場、流場信息的計算機表徵方法及其數據傳輸反演和表徵的若干問題。
  19. Upper level winds and surface winds then come together forming a circular pattern of clouds known as a tropical depression

    隨后，高層風和海面風結合，形成圓形雲層，也就是熱帶低氣壓。
  20. A three - dimension baroclinic prognostic model on the o - coordinate is established based on pom to simulate the wintertime circulation and the eddies in the east china seas, considering the topography, inflow and outflow on the open boundary, yangtse runoff, heat flux and wind stress on the sea surface

    本文在pom模式基礎上，建立一個坐標系下的三維斜壓預報模式，考慮了海底地形、外來流、長江徑流、海面風應力、海面熱通量等多方面因素的影響，模擬結果較好地體現了冬季東中國海環流及渦旋的特徵。
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