ascending air 中文意思是什麼
ascending air
解釋
上升空氣流-
Impact of windshear on ascending or descending air crafts
風切變對升降中航機造成的影響 -
The discussion is cast in the context of an ascending parcel of air.
討論限定在上升氣塊的情況。 -
During the halt tess s eyes fell upon a three - pint blue mug, which was ascending and descending through the air to and from the feminine section of a household, sitting on the summit of a load that had also drawn up at a little distance from the same inn
休息的時候，苔絲的眼睛看見有一輛馬車的頂上坐著一群婦女，她們正在從車上到車下地互相傳遞著一個裝三品特酒的大酒杯喝酒那輛馬車和苔絲的馬車停在同一個旅館里，不過距離稍為遠一點。 -
( 5 ) the spring greenland sea - ice extent is larger ( smaller ) : then during the following summer the high of the japanese sea is stronger ( weaker ), and the low of the asian land is stronger ( weaker ), which make the pattern of low west and high east easily ( uneasily ) form ; the ascending movement over north china is strengthened ( weakened ) ; the summer monsoon of east asia is stronger ( weaker ), then the southeastern, warm and damp airflow towards the north china is stronger ( weaker ), and the cold airflow of the high level over the north china is also stronger ( weaker ), which make the convergence of the cold and warm air over north china easily ( uneasily ) form ; the sst of the east pacific ocean is lower ( higher ), while the sst of west wind drift is higher ( lower )
（ 5 ）春季格陵蘭海冰面積偏大（小） ：後期夏季日本海高壓偏強（弱） ，而大陸上低壓也偏強（弱） ，易（不易）形成西低東阻的形勢；華北地區的上升運動增強（減弱） ；東亞夏季風偏強（弱） ，向華北地區輸送的西南暖濕氣流偏強（弱） ，而對應高空華北地區上空冷空氣活動偏強（弱） ，利於（不利於）華北上空冷暖空氣的交匯；夏季赤道東太平洋海溫偏低（高） ，西風漂流區海溫偏高（低） 。在以上的環流背景下，華北夏季降水偏多（少） ，易澇（旱） 。 -
The above analysis showed that this heavy rainfall event took on obvious meso - scale characters and was the combination of the three flows, so we can deduce : ( 1 ) surface southeasterly wind and topography may play the main role in this event ; ( 2 ) the easterly cold air rushing into the southern shaanxi province in the lower troposphere was strongly relative to the form of surface cold - front type of occlusion ; ( 3 ) there were two reasons for the secondary circulation ' s strengthen in the evening, one was the effect of a mountain - valley wind and the other may be latent heat leading to ascending motion ; ( 4 ) the shape of potential instability stratification corresponded well with the development of the warm - moisture advection ; and ( 5 ) the vapor providing essential thermodynamics was transported by a southwesterly low - level jet from the bay of bengal and the south china sea. furthermore, with the effect of terrain, the southern shaanxi province became the center of this extremely heavy rain process
中尺度結構分析表明，本次暴雨具有明顯的中尺度特徵，是由三支氣流共同作用的結果，分析發現（ 1 ）地面東南風和地形在這次大暴雨過程起主要作用； （ 2 ）東路冷空氣主要是通過中低層侵入陜南地區的，並與地面冷式錮囚鋒的形成密不可分； （ 3 ）夜博士論文:中尺度地形對陜南暴雨的影響研究間垂直次級環流發展加強可能有兩個原因，一個是由於地形山谷風的作用，另一個是降水的潛熱釋放激發了上升運動: （ 4 ）位勢不穩定層結的形成與低層暖濕平流的發展有很好的對應關系; （ 5 ）本次暴雨的水汽主要靠偏南風急流將孟加拉灣和中國南海的水汽輸送至西北地區東部，為暴雨的發生提供了必要熱力條件。 -
Injury to the soft tissue lining of these air spaces in the body is an inherent problem in scuba diving because of the changing volumes of gas while descending and ascending
由於下潛和浮升過程中空氣體積的變化，這些體內空間軟組織的傷害是水肺潛水固有的問題。 -
In 1999, the dipole existed in between the okhotsk high and the depression in the north of northeast china, thus the okhotsk high became active and maintained, the subh was located to an area quite further south than usual. the high persisted in the east region of nw china, the cold air flowed to the mid - lower reaches of the yangtze river along the high. in the east region of nw china, air steam under troposphere was strong sinking motion, and formatted the negative vorticity region, the vapour flux divergence was divgence. lt was apparently that the rain could n ' t occur in the eastern portin of nw china. in 2000 year, okhotsk high was very weak or did n ' t exist in, there was high in the east asia - japan, the subh is located to an area further north than usual. in the east region of nw china, the trough maintained, air stream under troposphere was strong ascending motion, the cycolonic circulation was prevailing, the vapour flux divergence was intensive convergences the rain easy happened in the east areas of northwest china
4多梅雨1999年鄂霍茨克海阻塞高壓與我國東北北部低壓形成偶極子，使得阻塞高壓穩定少動，西太副高位置偏南，西北地區東部持續受高壓控制，冷空氣沿此高壓流經長江中下游地區上空；在西北地區東部對流層中下層氣流下沉運動較強，呈反氣旋渦度，水汽通量散度輻散，不利於西北地區東部降水。空梅雨2000年相反，鄂霍茨克海高壓減弱甚至不存在，東亞-日本為高壓，西太副高位置偏西偏北，西北地區東部處于西風槽中，對流層中下層氣流上升運動增強，盛行低壓環流，水汽通量散度強烈輻合，有利於降水生成。 -
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。 -
The third part is the analysis to uprightness instability condition. it is made that there was the ascending air current about shenyang, the hailstone forming height is between 700hpa and 400hpa, die water vapor coagulating height is between 950hpa and 900hpa from the simulated tlogp evolvement chart. cape is in favor of severe convection development
干濕空氣間強的風垂直切變是此次冰雹強對流爆發的又一個重要觸發機制，強冷空氣到達地面強迫暖濕空氣抬升，致使對流層中低層出現強風垂直切變，強風垂直切變對強對流的發生和發展起到了非常重要的作用。 -
Ascending to the south gate to heaven, one sees the eighteen bends merely as a vertical stairway hanging in the air, upon which the climbers are moving up like little ants
登上南天門，十八盤如天梯高掛，遊人似蟻往上爬。它是中國山嶽建築借景生輝的典範。 -
A tropical cyclone is akin to a travelling heat engine. it feeds on an incessant supply of latent heat released from condensation in ascending moist air
熱帶氣旋類似一臺會走動的熱能機器，它的能量來自濕空氣上升時水汽凝結而釋放的潛熱。
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