vapor cloud 中文意思是什麼

vapor cloud 解釋
蒸發雲
  • vapor : n. 〈美國〉＝ vapour.
  • 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. 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。
  2. The evaporation of sodium tellurite glass in low gravity is explored and the formation and growth processes of teo2 microspheres are explained. the size of teo2 microspheres from low gravity is much larger than that from ground experiments and it is affected mainly by the temperature of melt in the heating coil and the duration time of vapor cloud during drop experiments

    探索了微重力對亞碲酸鈉玻璃熔體氣化的影響，分析了微重力下由於玻璃熔體氣化而生成teo _ 2玻璃微球的過程，解釋了微重力下形成的微球尺寸遠遠大於摘要地面模擬實驗所得微球的原因。
  3. Usually the magneto - optical trap is used to obtain the cold atoms from the vapor. it is reported that experiments for obtaining the ultra - cold cesium atoms by optical molasses directly from the vapor cell without mot. the lowest temperature achieved for the cesium atomic cloud was 3k. the relationship between the temperature and the detuning of cooling laser was measured

    報告了採用直接從銫蒸汽氣室而不用磁光阱實現了光學粘團的方法。用此辦法得到了3的銫的超冷原子團。這是我國目前用激光冷卻方法得到的最低溫度。
  4. 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 ） 。
  5. At the same time, the effects of dragging force from fall of hydrometeors and latent - heat release from phase transfer are tested. from the analyses we conclude that the distributing of the cloud particles relates with temperature closely. huanan heavy rainfall and mei - yu front heavy rainfall have mixed - phase process with vapor phase, liquid phase and ice phase

    詳細分析了形成降水的雲物理過程，探討了源匯項對水凝物的貢獻，並通過敏感性試驗，考察了雲物理過程對降水熱力動力過程的反饋作用，研究結果表明：華南暖區暴雨和長江梅雨鋒暴雨的雲物理過程具有汽、水、冰三相混合雲特徵。
  6. At first it went up slowly in a cloud of orange exhaust and white vapor.

    它首先在橙黃的排氣雲和白色的霧氣中緩緩上升。
  7. 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。
  8. These works include the cloud system families of the meiyu heavy rainfall and their interactions, the structure, precipitation characteristics and microphysical features of the mesoscale convective complexes ( mcc ), the favorable genesis and evolution settings for mcs, the different environments between mcc and meso - p - scale convective system, the relationship between the tropical water vapor plume ( wvp ) and mcs, and what characteristics of the wvp

    先後分析了梅雨暴雨系統的雲系成員及其相互作用；中尺度對流復合體（ mcc ）的結構、降雨特徵、微物理特徵及其形成和發展的有利環境條件；不同類型中尺度對流系統（ mcs ）形成與發展的環境條件差異；熱帶水汽羽和暴雨雲團的關系，水汽羽的動力和熱力特徵。
  9. The analysis shows that, for any type of medium, the modes of ultimate explosion accidents only include condensed - phase explosion, vapor - cloud explosion, vapor explosion of boiled liquid expanding and vessel explosion with various forms

    結果表明：無論從哪種介質進行分析，最終的爆炸事故模式只有凝聚相爆炸、氣雲爆炸、沸騰液體擴展蒸氣雲爆炸及各類形式的容器爆炸。
  10. As an part of a project " investigation on new protection techniques and principle of dust and vapor cloud industrial explosion hazards " supported by nsfc, the interaction between shock waves and liquid like drops and sprays is studied experimentally and numerically

    本文針對國家自然科學基金重點項目「粉塵和氣雲工業爆炸災害新的防治方法及其原理的研究」的子課題?水霧抑爆機理，進行了激波與液滴、液霧相互作用的實驗和理論研究。
  11. Because a hurricane draws much of its energy from heat released when water vapor over the ocean condenses into clouds and rain, the first researchers to dream of taming these unruly giants focused on trying to alter the condensation process using cloud - seeding techniques ? then the only practical way to try to affect weather

    由於颶風大部份的能量，來自海面上水氣凝結成雲雨時釋放的潛熱，因此希望馴服這個頑強巨人的先驅研究人員，便專注于利用人造雨技術來改變凝結的過程，這也是當時要影響天氣現象唯一可行的方法。
  12. First, under the given boundary condition and reasonable simplified condition, this paper develops radiation transmitting equations in atmosphere applied in infrared waveband and visual light waveband from common equation of radiation transmitting. then, the formula between observation of satellite and net surface radiation is established according to the developed equations, from which it is found that net surface radiation is relative to sun zenith, land surface and cloud albedo, etc. at last, by using data of satellite visual light ( vis ), infrared 1 ( ir1 ), infrared 2 ( ir2 ) and water vapor ( ir3 ) channel, sun zenith and net surface radiation, a regression formula is built

    本文從大氣中太陽輻射傳輸的一般性方程入手，引入邊界條件及簡化條件，推導出紅外波段和可見光波段的大氣輻射傳輸方程，由此建立起衛星觀測輻射與地面凈輻射的關系，文章還就衛星觀測到的輻射與雲量、雲高、雲的光學厚度、雲及地面反照率等之間的關系進行了理論分析，可以幫助更好地理解雲對地面凈輻射的影響。
  13. Three passages of vapor transfer are related to the regional precipitation, especially the one carrying water from the bay of bengal. mixed cold and warm cloud portions are favorable for " catalysis - water supply ". the duration and rainfall - hit area are about half the lifecycle and rainbelt size, respectively

    ；降水天氣的主要水汽輸送路徑有三條，以來自孟加拉灣的西南水汽輸送帶對降水最為有利；雲系以冷暖混合雲體為主，具有發生「播撒-供應」機制有利的宏觀雲體條件；雲系降水的時段和面積一般只有雲系生命期和面積的一半。
  14. Vapor cloud explosion

    汽雲爆炸
  15. In the case of beijing snowfall, the temperature is below 0. there are only vapor, ice and snow in the cloud

    屬于東風迴流的北京小雪雲物理特徵與暴雨不同，其過程溫度在零度以下，液相粒子微弱，只有水汽、冰晶和雪兩相粒子。
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