wet vapor 中文意思是什麼

wet vapor 解釋
濕蒸氣
  • wet : adj (opp dry )1 濕,潮濕的,有濕氣的。2 雨的,下雨的,多雨的。3 〈美俚〉允許賣[制]酒的,不禁酒...
  • vapor : n. 〈美國〉= vapour.
  1. We can use the mm5 model in definite time, definite area weather forecasting. we conclude that : : the moving route of this necw in its developing progress was direct - south along latitude, the cold air is rough, and just this made the rough vertical velocity ; the necw southern moving and conflicting with the west pacification sub - tropical high makes rough jet steam. the plenty south - west warm and wet air made by the jet stream gave the rainstorm demanded vapor ;. the rough vertical velocity by jet stream is a main reason in this rainstorm ; the mm5 model uses four - direction analysis data as its input, this avoids some errors occurred in observe and transfer, thus made the result more useful

    綜合分析認為: ( 1 ) 、這次冷渦在其發生發展過程中,其移動路徑是沿經圈直線南壓,攜帶的冷空氣勢力較強,形成槽后較強的垂直運動; ( 2 ) 、西太平洋副熱帶高壓偏北位置與東北冷渦南壓形成的急流軸,把源源不斷的西南暖濕氣流輸送到遼西地區,也就是急流軸的左前方位置,為這次暴雨的產生提供了充足的水汽來源; ( 3 ) 、低空急流不但為暴雨輸送水汽,其造成的較強的垂直環流也是產生強降水的一個主要原因; ( 4 ) 、 mm5模式以四維同化資料作為初始場,最大限度地避免了觀測誤差可能造成的積分不穩定,提高了模擬結果的參考價值。
  2. ( 3 ) the polar eddy, the west circumfluence on 500hpa medium latitudinal region ands subtropic circumfluence are the key systems of tpnes floods precipitation and, the wet years have abundant vapor, moreover, the omga is positive in all atmosphere

    ( 3 )極渦、中高緯西風環流系統和副熱帶系統是影響青藏高原東北側區汛期降水的大尺度環流背景關鍵系統。同時,多雨年的主要流場特點是有利於水汽輸送,且整層大氣始終表現為上升運動。
  3. The dried material is put into the middle of shell, mixing by the rake teeth and the material shaft works back and forth. the indirect heating, equal agitation of rake teeth and grinding of breaking stick makes water in material evaporation. under the effect of vacuum system, the water in the dried material and apparent water are discharged and the vapor water is discharged from outlet of vacuum pump passing dry dust collector, wet dust collector and condenser

    被乾燥物料從殼體上方正中間加入,在不斷正反轉動的耙的攪拌下,物料軸向來回走動,與殼體內壁接觸的表面不斷更新,受到蒸汽的間接加熱,耙的均勻攪拌,粉碎棒的粉碎,使物料內的水份氣化,在真空系統的作用下,使被乾燥物料內部水份和表面水份更有利的排出,氣化的水份經乾式除塵器濕式除塵器冷凝器,從真空泵出口處放空。
  4. For improving the flow manner on the plate, the downcomer apron was modified from straight shape to trapezoidal shape. the hydrodynamics performance of the modified ctst tray, for example, the pressure - drop of dry tray and wet tray, liquid weeping and vapor entrainment etc were measured

    對優化后的塔板流體力學性能進行了測試,分別測量了不同氣液流量下的干板及濕板壓降、霧沫夾帶量和漏液量等數據,並與改造前的塔板流體力學性能進行了對比。
  5. The dynamical structure of the convective system at cl imax is studied and the air flow field is dep i cted. the ana i yses further show that north j i angsu and north annul is water vapor source of the rainstorm, and the inclining flow of wet air mass in pbl is the main water pass of convective systems

    淮北、蘇北是魯南暴雨區對流層中下層氣流的源地,其充沛的水汽是此次過程前期水汽條件改善的重要原因,除水汽平流造成比濕增加外,對流層70ohpa及850hpa較強的上升運動也是該層次濕度增加的重要因素。
  6. From the conditions of fluoride salt by wet process, the paper introduces the method of how to use rigid pvc instead of q235 steel lining rubber to improve the vapor - liquid separator and its using results

    摘要從濕法氟化鹽工藝條件出發,介紹了用硬聚氯乙烯材料替代q235鋼襯膠材料改進氣液分離器的方法及使用效果。
  7. Lastly, the precipitable water ( pv ) and vapor transport flux during the great drought affair in the east of nwc in 1990s " have been analyzed and compared with what during wet years. the reason that resulted to that drought affair was studied from the point of water vapor in the atmosphere

    再次,對上世紀90年代西北地區重大幹旱事件期間大氣可降水量、水汽輸送等進行了分析,並與典型濕年進行對比,從大氣水分特徵的角度探討了這次重大幹旱事件的可能形成原因。
  8. Under the cloudless conditions, the precipitable water was calculated by satellite data and ground humidity parameter respectively, and it was also calculated by the combinable satellite data and ground humidity parameter data. research results were showed as follows : the distribution of the precipitable water retrieved from satellite data was of well spatial and temporal resolutions. the configuration of vapor field was quietly fine, whose distribution of " hot centers " and " wet centers " was obvious

    對于晴空大氣的可降水量,分別用衛星資料和地面濕度參量資料以及將兩種資料結合起來進行了估算,其結果如下:用衛星資料(紅外分裂窗數據)反演晴空大氣可降水量,其反演的水汽場分佈時間和空間的解析度都很高,且其結構精細, 「干中心」和「濕中心」分佈明顯。
  9. The assimilation experimentation results indicate that after assimilating radar wind field of small spatial scale, mesoscale and small - scale precipitation prediction can be improved and mesoscale and small - scale information which ca n ' t appear by tradition datum can be gained, which is valuable to analyze the mesoscale and small - scale system structure ; the effect assimilating radar humidity field is n ' t obvious, which is perhaps correlation with precipitation types and assimilating time. the results also show that adding radar humidity field to initial condition at initial time can supply the gap of the regular data in reflecting the mesoscale and small - scale systems, strengthen the humidity in the initial field, and eventually help to improve precipitation. the experiment of assimilating radar wind field and radar humility field at the same time shows that vapor transportation and local vapor divergence play more significant role in causing excessively heavy rain than only high wet center

    同化試驗結果表明:同化空間解析度很高的雷達風場后,能改善中小尺度降水的預報效果,並且能夠得到常規觀測資料所不能得到的中小尺度信息,對分析中小尺度系統結構具有重要意義;同化雷達濕度場效果不明顯,可能與降水類型和同化時刻有關;而直接在初始時刻加入雷達濕度場,補充了常規資料在反映中小尺度系統方面的不足,增強了初始場中的水汽,有利於降水量的增加;同時同化雷達風場和雷達濕度場的試驗表明,水汽的輸送和局地的水汽輻合對于產生特大暴雨的貢獻遠大於僅有高濕中心的貢獻。
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