higher troposphere 中文意思是什麼

higher troposphere 解釋
上對流層
  • higher : adj 〈high 的比較級〉較高的；高等的。 higher command 【軍事】＝ high command higher criticism 聖...
  • troposphere : n. 【氣象學】對流層。
  1. Nitrous oxide ( n2o ), a naturally occurring greenhouse gas, was one of the trace gases of nitrogen cycle. its lifetime was about 120 years in the troposphere. it has caused considerable concern since n2o not only contributed to the destruction of stratospheric ozone, but also its greenhouse effect strength was about 200 times higher than carbon dioxide ( co2 )

    溫室效應氣體n _ 2o是氮素循環中的痕量氣體之一，其溫室效應強度是co _ 2的200倍左右，它在大氣中的停留時間長達120年，而且，其消耗或轉化是以破壞o _ 3為代價的。
  2. The analysis of dry pv shows that the high pv dominate the area of typhoon, the higher is the center value of pv, the stronger is the typhoon. lt is also shown that the most important reason resulting in rainstorm is the cold air ( high pv ) which spreads to south from the upper troposphere or lower stratosphere and transports into the warm air. the joining situation of upper and lower pv area make vortex develop. pv transpotation reduces static stability, which increases the releasing of instability energy and makes rainstorm amplify

    對干位渦的分析表明：臺風或臺風環流區為高值位渦區，臺風越強，位渦中心值越大；對流層上部或平流層下部冷空氣（高位渦）的擴散南下與暖濕氣流的交匯是造成特大暴雨的重要原因，因為上游斜壓性的發展使對流層頂發生折疊，平流層與對流層相互作用增強，上下位渦區相接的形勢使低層渦旋發展，上升運動加強，位渦的下傳有效地降低了靜力穩定度，有利於位勢不穩定能量的釋放，使得暴雨增幅。
  3. The results show that mesoscale low level jet, the perturbation in the high level troposphere can enhance and accelarate occurrence and development of mesoscale system ; convergence of low level and divergence of higher level are dynamical condition of storm rainfall system

    本文的研究結果表明，中尺度低空急流、高空擾動對中尺度低渦系統的發生發展有加強和促進作用；低層輻合和高層輻散是降水系統的發展的動力條件。
  4. The main difference of the three sites ozone vertical distributions is as follows : both the maximum ozone partial pressure and its altitude are different ; the ozone concentration at 1016km height of lin an is much higher than that of kunming and hong kong ; there exists one high ozone concentration layer over the hong kong and kunming, but hong kong is more obvious ; in the upper troposphere there is no lower ozone distribution over lin an

    其主要不同點有，最大臭氧分壓和所處高度不同臨安1016km高度的臭氧濃度遠遠大於昆明與香港在對流層低層，香港有一特別突出的高臭氧濃度層，昆明次之臨安對流層的中上層沒有像昆明和香港出現的臭氧低值區現象。
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