water-ice cloud 中文意思是什麼

water-ice cloud 解釋
冰水混合雲
  • water : n 1 水；雨水；露；〈常作 pl 〉 礦泉，溫泉；藥水。2 〈常 pl 〉水體；水域；水道；海；湖；河；海域；...
  • ice : n 1 冰，冰塊。2 〈英國〉冰淇淋，冰淇淋 （＝ ice cream）; 〈美國〉冰涼飲料[點心]。3 冰狀物，糖衣。...
  • cloud : n 1 雲。2 雲狀塵埃、煙（等）；（鳥、蟲、飛機等的）大群，大隊。3 （水晶等的）霧斑，（鏡子等上的）...
  1. Condensation trails ( contrails ) are formed high in the sky where water vapour from aircraft exhaust condenses in the surrounding cold air, producing water droplets andor ice crystals. they appear as narrow, sometimes rather straight, streaks on satellite cloud images

    飛機在高空航行時排出水氣，水氣被周圍的冷空氣冷凝下來，結成水點或冰晶，在高空留下了一條痕跡，稱為凝結尾跡。
  2. Based on the dynamic frame of mm5 and reisner 2 explicit cloud scheme, a new double - moment microphysical scheme was developed, in which both the mixing ratios and number concentrations of cloud water, rain water, cloud ice, snow and graupel were predicted

    從本質上說，該方案預報的僅僅是粒子的比含水量。在mm5動力框架內，在其中的reisner2方案基礎上採用雙變參數方案，增加了雲水、雨水、雪和霰的數濃度預報方程。
  3. The simulative cloud image, made from the mixing ratios of cloud liquid water, rain water, ice crystal, snow, graupel which were outputted by the mesoscale model mm5, resemble the gms satellite infrared image very well and also show the cloud evolution of typhoon winnie from tropical cyclone to extratropical cyclone after landing

    利用高解析度中尺度數值模式輸出的大氣中雲水冰水雨水雪水成功地模擬出1997年登陸臺風winnie的雲系結構。模擬雲圖與氣象衛星實際觀測的臺風雲圖非常相似。由於模擬雲圖可以給出大氣中不同形態水物質的三維空間分佈，彌補了衛星只能觀測雲頂表面的不足。
  4. The influence of the cloud droplet spectrum character and the spectrum growth and change is considered, which does not use a cut - off value for conversion from cloud water into rain water process. in the continuous coalescence equation, the particles fall velocity difference is not moved out from the integral, but is integrated in the equation as the function of diameter d to avoid the error of using particles average fall velocity. in the new scheme, generation rate of graupel due to the collection of snow by graupel and the collection of cloud ice by graupel are included

    雲中凝結核ccn的數濃度採用超幾何函數表示；雲水向雨水的自動轉換過程採用grabowski （ 1999 ）的公式，考慮了雲滴譜的特徵和發展變化對該過程的影響，而不是採用原方案給定閾值的方法描述該過程；對連續碰並方程不再將粒子落速差作為常量提出積分號外，而是直接作為粒子直徑函數在積分號內求解，這樣處理可以迴避使用粒子群的平均落速帶來的誤差；增加了霰和雪、霰和冰晶的碰並微物理過程。
  5. A complex mixed - phase explicit microphysical parameterization scheme, which also be known as reisner 2 explicit scheme was developed for use in the ncar / penn state mesoscale model versions ( mm5 ). the single - moment schemes has additional variables for graupel and ice number concentration, in which the mixing ratio of cloud water, rain water, cloud ice, snow and graupel are predicted and number concentration specified

    Mm5中的reisner2方案是一種含霰的復雜混合相顯式雲物理方案，該方案包含了雲水、雨水、冰晶、雪和霰的混合比預報方程，同時對冰晶的數濃度作了預報。
  6. Release of silver iodide ( agi ) into an existing supercooled cloud ( i. e., air temperature between - 39 and - 5 celsius ) can convert water vapor to ice crystals, which is called sublimation

    將碘化銀播灑至已形成的過冷卻雲中（既空氣溫度在- 39攝氏度? - 5攝氏度）能將水汽轉化為冰晶，這個轉化過程被稱為凝華。
  7. The hydrometeors distribution in mcc illustrat that the precipitable ice is dominant which fills in the cloud cluster in almost entire troposphere with maximum cores at the mid - levels. rain water and cloud liquid water are in the middle and lower troposphere, and cloud ice water only scatters at the 8 - 18km upper levels

    水凝物垂直分佈顯示， mcc中可降水冰含量最大，分佈在幾乎整個對流層，雨水和雲水主要分佈在的對流層中、低層，而雲冰則分佈於高層大氣中。
  8. The heaviest hourly rainfall orients to the density ice cloud portion where ice cloud become turn to be water cloud

    降水強度最大的區域位於多層雲附近，密實的冰雲向水雲過渡的冰雲一側。
  9. The cloud top properties and cloud phase show that mcc develops in a broad water cloud area with multi - layer cloud, density ice cloud, and cirrus cloud consisted

    雲頂相態顯示mcc由多層雲、捲雲和密實冰雲構成，在廣闊的水雲區里發展起來。
  10. In an unstable and moist atmosphere, water droplets and ice pellets in the cloud will become electrically charged in convective motion

    在不穩定及潮濕的大氣中，雲層內的水滴及冰粒在對流活動中產生電荷。
  11. It was well known that the main process of precipitation formation was collecting cloud water in the warm area and ice phase particles melting in the cold area. positive vertical velocity existed between 700hpa and 500hpa in the warm area and near surface in the cold area. wind convergence existed at the height of 700hpa, and divergence existed above and below the height of 700hpa

    通過對降水雲系的綜合研究，建立了河南省春季層狀雲降水概念模型：暖區降水主要通過雲水碰並形成，冷區降水機制以冰粒子融化等冷雲過程為主;暖區700一50ohpa通常有上升氣流，冷區上升氣流分佈在近地面附近: 700沖a存在風場的輻合，其上下則主要是輻散區;水汽主要集中在7o0hpa高度上，暖區水汽來自南、東南方向，冷區水汽以西南輸送為主;暖區位勢不穩定分佈在o 。
  12. Rainfall is started mainly in cold portions. microphysics for ground rainfall consists of low - level warm portions in which precipitating particles are produced, growing through collision with cloud water and when descending into the warm portions below, ice - phase particles melt and continue to grow by collecting cloud water there. 4 )

    降水主要以冷雨過程發動，地面降水形成的微物理過程分別為低層暖雲過程產生並通過碰並雲水增長、降落到暖區的冰相粒子融化和融化的冰相粒子在雲的暖區收集雲水繼續長大等三部分組成。
  13. Li bai remarked : " bright moon over the tianshan, out of moisty cloud " as the bright moon shines, urumqi people are bathed in silvery radiance, here cloud inter - depend with water, white moon is as clean as ice crystal, whose spirits accompany each other, this place is just a land of wonder in the earth

    舉天池為鏡，襟烏魯木河而舞，肩塔準兩大盆地，懷鹹淡兩大湖泊，一帶青翠，風光旖旎，不是江南，勝是江南。
  14. The paper works out the ice crystal spectrum distributing in the different macroscopic and micro - backgroud of the cloud ( ie, the thickness, the temperature and the supersaturation with respect to ice of the nucleation layer ). this paper also works out the amount of catalyst which is allowed in the cloud nucleation layer according to the different quantity of the supercooled water, the density of the supersaturation of the vapor with respect to ice. simultaneously, the paper discusses the i nfluence of remaining time when seeding artificial ice nucleus in the different ascending - velocity and altitude, and elicits the proper seeding altitude of the catalyst

    以此解為依據，得出了不同均流時，人工引入冰核在核化層存留時間，再以此時間作為人工冰核凝華增長時間，求出不同的雲宏微觀背景（如核化層厚度、溫度、冰面過飽和度等）下的冰晶譜分佈，經和實際資料比對符合相當好。進而求出核化層中不同過冷水量、冰面過飽和水汽密度下雲核化層可允許的催化用量。同時討論了不同升速，不同高度引入人工冰核時對其存留時間的影響。
  15. Since there is not much water vapour at that altitude, the growth of ice crystals in the cloud is limited and the crystals can remain suspended atop some ascending air

    卷積雲所在的高空，水汽含量極少，雲內的冰晶不會長到很大，所以能夠藉助上升氣流的支撐而懸浮在空中。
  16. There is an active growth layer and super cooled water exists with ice crystals that may be an important feature layer to occur rain in stratiform cloud

    過冷水滴和冰晶共存層存在，且冰晶活躍增長，此層的存在可能是發生降水的關鍵。
  17. Through the analysis of 11 typical mesoscale convective systems occurring at china continent and adjacent ocean on june, july and august, 1998, it is found that 10. 65ghz v channel and 19. 35ghz v channel can well response to the absorbability and emission of liquid water in cloud and precipitation, and that 85. 5ghz v channel and 37. 00ghz v channel can response to the ice scatting in cloud well

    通過對1998年68三個月內發生在我國大陸和鄰近洋麵上的11個中尺度對流系統的分析，發現10 . 65和19 . 35ghz垂直通道能較好的反應雲中液態水和降水的吸收和發射85 . 5和37 . 0ghz垂直通道能較好的反應雲中冰晶冰粒的散射。
  18. The cloud water in the concerned clouds was consumed quickly after seeding. ice - phase particles appear earlier, and their concentrations and contents increased. microphysical processes turn more active

    在雲體內部，雲水迅速被消耗，冰相粒子出現時間提前，濃度和含量明顯增加，各種冰相過程反應強烈。
  19. Finally, it briefly discusses the feasibility, the applying foreground and the approach with regard to the calculating method about the amount of catalyst provided in this paper by integrating the ascending - velocity field and cloud water field in the possible working section abstracted from the mm5 mesoscale model with the thickness of the ice crystal particles in nucleation layer and supercooled water quantity which is surveyed by the plane

    得出適合的催化劑引入高度等。最後，簡要討論了用mm5中尺度區域模式提取可能作業區的升速場和雲水量場，並結合飛機實測核化層冰晶粒子濃度、過冷水量等，探討了本文提出的催化劑用量計算方法的可行性，應用前景和途徑。
  20. Because it is very turbulent inside a cumulonimbus cloud, the water droplets and ice crystals in it will break up and become electrically charged

    由於積雨雲內有急劇的氣流擾動，雲中的水珠和冰粒便會分裂而產生電荷。
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