水氣訂正 的英文怎麼說

中文拼音 [shuǐqìdìngzhēng]
水氣訂正 英文
water vapor correction
  • 水 : 名詞1 （由兩個氫原子和一個氧原子結合而成的液體） water 2 （河流） river 3 （指江、河、湖、海、洋...
  • 氣 : Ⅰ名詞1 （氣體） gas 2 （空氣） air 3 （氣息） breath 4 （自然界冷熱陰晴等現象） weather 5 （氣味...
  • 訂 : 動詞1 （經過研究或商議后立下） conclude; draw up; agree on 2 （預先約定） subscribe to （a newspa...
  • 正 : 正名詞（正月） the first month of the lunar year; the first moon
  • 水氣 : brume; steam
  • 訂正 : make corrections; correct; revise; emend; correction; reduction
  1. As a result, in the paper, considering the altitudinal effect ( topography factor ) and the influence on the temperature lapse rate by topography and latitude and longitude and moisture transfer, the study on the daily surface air mean, max and min temperature in the reaches of yangtze rive is attempted by five models, which include the gaussian weighted model, the gaussian weighted model associated with the error - modification, the gradient plus inverse distance squared model and the modified gaussian weighted model a and b that take topography - factor into account

    本文考慮海拔高度和溫度直減率受地形和經、緯度及水汽等因素的影響，通過利用高斯權重法、結合逐步訂正的高斯權重法、梯度距離權重反比法和加入地形影響項（地形因子）的兩種改進高斯權重法的方案a 、 b ，對長江流域的地面日平均、最高和最低氣溫場進行了空間化插值研究。
  2. Main conclusions drawn from the analyses of calculating results are as follows : ( 1 ) the microwave absorption of atmosphere gas have obvious attenuation at the wavelengths for cloud detection, thereinto, the water attenuation effect changes greatly, so the 94ghz cloud detecting radar should have water vapor attenuation correction scheme. ( 2 ) when 37ghz and 94ghz radars detect clouds, the difference between the atmosphere and cloud attenuation and the large variety of radar reflectivity conduce the intension of the radar backscatter signals change. ( 3 ) for the thin cloud layer and low water content of cloud, 37 - ghz radar backscatter signals are not as good as 94 - ghz radar, that is to say that the 94ghz radar has better capability in thin clouds detection

    本工作得出如下結論： （ 1 ）大氣氣體的微波吸收在測雲波段產生明顯的衰減，其中水汽衰減效應變化很大；即將上天的空間94ghz測雲雷達必須有水汽衰減訂正方案； （ 2 ） 37ghz和94ghz雷達測雲，由於大氣和雲衰減不同和雷達反射率的很大差異，導致雷達回波信號強弱不同； （ 3 ）對雲層較薄、含水量較少的雲，在不計雷達參數的情況下， 37ghz雷達回波信號不如94ghz測雲雷達，也就是說94ghz對薄雲有更強的探測能力；對雲層較厚、含水量大的雲，由於強衰減的作用， 94ghz雷達回波信號小於37ghz雷達； （ 4 ）從大氣衰減的不利因素方面考慮，空間94ghz雷達測高層薄雲的效果最好；測低層薄雲時需要考慮氣體衰減訂正；因濃厚雲的強衰減作用，探測其中下部的能力大大減弱，不僅要進行衰減訂正，而且要藉助其他信息來反演整個雲層的含水量垂直分佈； （ 5 ）為了獲得從極薄到極濃厚雲的垂直分佈探測能力，未來測雲雷達系統最好採用雙波長甚至三波長（如94 、 37和13ghz ） 。
  3. The result of the two experiments implied that the correcting scheme of combined eof reached the level of operation. it is valuable greatly for climate prediction

    訂正試驗、預測試驗的結果說明聯合自然正交展開訂正方案已經達到實際業務應用的水平，這對于氣候的跨年度預測，尤其是對enso預測有十分重要的應用價值。
  4. Refining measured water content values of wet snow - correcting errors arising from air temperature in t

    秋田穀式含水率計測量值的氣溫訂正
  5. Whether the pollutant emission level of cruise ships within hong kong territory is subject to regulation by the " international convention for the prevention of pollution from ships, 1973, as modified by the protocol of 1978 relating thereto " and the merchant shipping prevention of air pollution regulation which is being drafted ; if so, of the details, and whether the situation is regularly monitored by the environmental protection department ; if there is monitoring, of the results ; if the emission level is not subject to regulation, the reasons for that ; and

    三郵輪在香港境內的污染物排放水平是否受經1978年議定書修訂的1973年國際防止船舶造成污染公約及正在草擬中的商船防止空氣污染規例規管若然，詳情為何，以及環境保護署有否定期監察有關情況若有監察，結果為何若有關水平不受規管，原因為何及
  6. ( 2 ) model correction and comparison in the process of conversion from zenith day delay to gps water vapor and precision evaluation. saastamoinen ( sa ) model and hopfield ( h ) for dry delay and bevis model for atmospheric weighted temperature are adopted

    （ 2 ）模型訂正與比較在gps水汽反演過程中，一般干延遲和大氣加權平均溫度的計算是採用「普適性」模型，目前應用較多的有saastamoinen （ sa ）模型、 hopfield （ h ）模型和bevis模型。
  7. Acceding to the theory of crop water requirement, maximum potential evapotranspirations are calculated by applying fao penman - monteith method, and then we obtain the water requirement, water balance and water correction factors ect. of main crops ( spring maize, summer maize, spring wheat, winter wheat, cotton ) and different type grasslands, and the space - time distribution regularities of water requirement of cropland and natural grassland are analysed, the result show : the water requirements of same kind crop in different areas are different, water satified degrees are different to different crops in the same area, and water requirement of same crop are different between years for climatic variation ; the water requirements of main crops are increasing from east to west and from south to north, water satified degrees are decreasing from east to west and from south to north. in growing season, there are deficits in crops water supply in most area, so the irrigation is needed to meet the requirement for crop growing normally

    根據作物需水的理論和方法，採用計算精度較高的faopenman - monteith方法（ 1998 ）計算了半乾旱區最大可能蒸散，並基於此計算五種主要旱地作物（春玉米、夏玉米、春小麥、冬小麥、棉花）和不同類型的天然草地的需水量、水分盈虧、水分訂正系數等，分析了農田和天然草地水分供需的時空分佈規律，結果表明：不同地區同一種作物的需水量是不同的，同一地區對不同作物的水分滿足程度是不同的，而且同一種作物在同一地區隨著氣候的變化需水量也會有一個年際變化；主要作物需水量由東向西，由南向北遞增，正常生長發育的水分保證程度由東向西，由南向北遞減。
  8. The paper have built the local correction models for dry delay and atmospheric weighted temperature and have made a comparison between two models for calculating actual water vapor on the basis of actual upper - air detecting data. ah results show that the conclusion is satisfied

    本研究利用實際探空資料建立了大氣干延遲和大氣加權平均溫度的局地訂正模型，並對實際水汽計算模型進行了比較，得到了滿意的結果。
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