upper air circulation 中文意思是什麼

upper air circulation 解釋
高空環流
  • upper : adj 1 (更)上面的,上方的,上部的;較高的;上級的;(議會)上院的;(衣服)穿在外面的。2 上流的...
  • air : n 1 空氣,大氣。2 天空,空中。3 微風,和風。4 態度,樣子,風度,氣派;〈pl 〉高傲的架子。5 傳播,...
  • circulation : n. 1. 循環;運行。2. 傳播;環流(量),流通(量)。3. (雜志等的)發行(額),銷數,銷路。4. 通貨,貨幣;流通證券。5. 【航空】環量,環流。
  1. The basic requirements include good cyclonic inflow i. e. for the northern hemisphere, inward spiralling in an anti - clockwise sense at the lower levels for the initial spin - up process, and good outflow channels at the upper levels for effective ventilation. the convergence of air at the lower levels and divergence aloft imply a vertical circulation which is schematically shown in the following cross - sectional diagram

    熱帶氣旋的誕生及發展的基本條件是:在大氣低層必須有充份的氣旋式氣流輻合(在北半球,沿反時針方向螺旋形地流入) ,在大氣高層要提供足夠的氣流外溢通道,這樣才可以建立有效的通風機制。
  2. The basic requirements include good cyclonic inflow ( i. e. for the northern hemisphere, inward spiralling in an anti - clockwise sense ) at the lower levels for the initial spin - up process, and good outflow channels at the upper levels for effective ventilation. the convergence of air at the lower levels and divergence aloft imply a vertical circulation which is schematically shown in the following cross - sectional diagram

    熱帶氣旋的誕生及發展的基本條件是:在大氣低層必須有充份的氣旋式氣流輻合(在北半球,沿反時針方向螺旋形地流入) ,在大氣高層要提供足夠的氣流外溢通道,這樣才可以建立有效的通風機制。
  3. A transverse secondary circulation is produced by the coupling of high and low jets, while the sinking branch of the secondary circulation providing the dynamic conditions for the dry intrusion air. during the period of the heavy rain process, dry intrusion descends southward along the intense constant potential temperature lines, which promotes the lower cyclone. in addition, the pouring of upper - level dry air not only decreases ground temperature behind the front but also increases surface pressure and velocity

    由於高、低空急流耦合,在高空急流中心左側產生的下沉運動和高空急流中心右側、低空急流左側產生的上升運動在鋒面上形成一次級環流,次級環流的下沉支運動為對流層高層干空氣和高位渦的下傳提供了動力條件;進一步研究發現,干侵入沿相當位溫密集帶向南向下伸展,引起對流層低層氣旋性渦度的發展;此外,高層乾冷空氣向下注入,導致地面溫度降低、氣壓升高、風速加大、低層輻合增強、上升速度加大,從而促進了新的對流運動,引起降水增強。
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