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輻散氣流英文怎麼說

輻散氣流 的英文翻譯

輻散氣流 英文 divergent flow 輻 : 名詞(車輪中車轂和輪圈的連接物) spoke 散 : 散動詞1. (由聚集而分離) break up; disperse 2. (散布) distribute; disseminate; give out 3. (排除) dispel; let out 氣 : Ⅰ名詞1 (氣體) gas 2 (空氣) air 3 (氣息) breath 4 (自然界冷熱陰晴等現象) weather 5 (氣味... 流 : Ⅰ動1 (液體移動; 流動) flow 2 (移動不定) drift; move; wander 3 (流傳; 傳播) spread 4 (向壞... 氣流 : 1 [氣象學] air current; airflow; wind current; airstream2 [語言學] breath氣流紡紗 open end spinni...

輻散氣流 例句

  1. Air velocity inside solar chimney decreases with the increase of chimney gap and increases with the increase of solar radiation
    氣 流 速度隨著通道寬度的增加而減小,隨著太陽 輻 射強度的增加而增大。
  2. It was well known that the main process of precipitation formation was collecting cloud water in the warm area and ice phase particles melting in the cold area. positive vertical velocity existed between 700hpa and 500hpa in the warm area and near surface in the cold area. wind convergence existed at the height of 700hpa, and divergence existed above and below the height of 700hpa
    通過對降水雲系的綜合研究,建立了河南省春季層狀雲降水概念模型:暖區降水主要通過雲水碰並形成,冷區降水機制以冰粒子融化等冷雲過程為主;暖區700一50ohpa通常有上升 氣 流 ,冷區上升 氣 流 分佈在近地面附近: 700沖a存在風場的 輻 合,其上下則主要是 輻 散 區;水汽主要集中在7o0hpa高度上,暖區水汽來自南、東南方向,冷區水汽以西南輸送為主;暖區位勢不穩定分佈在o 。
  3. Because of the low temperature there, water vapour condenses into small, clear crystals. a layer of glossy cirrus forms which drifts out from the centre of the tropical cyclone because of divergence at that level. so, when the outer edge of a tropical cyclone reaches hong kong, we can see cirrus high in the sky
    熱帶 氣 旋強烈的上升 氣 流 會把潮濕的空 氣 帶到近五六千公尺以上的高空,由於溫度很低,水 氣 結成了透明的小冰粒,形成像絹絲一樣發光的雲彩-捲雲,這些在高層 輻 散 流 場區域的捲雲,會從熱帶 氣 旋中心向外 流 出,所以當香港還是位於熱帶 氣 旋邊緣時,我們便已看到那些在熱帶 氣 旋外圍的捲雲,並稱為臺母。
  4. ( d ) in the weak monsoon year, nwc lies in the northwest airflow region, west and south wind, as well as moisture transportation are remarkably reduced. except part of the first field, there is vapour flux divergenceon in nwc ( e ) in the strong monsoon years, the height field is low on the west and high on the east, west and south wind, and it ' s vapor flux transportation, are evidently boosted up. there is vapour flux conflurnce in the he first and sixth region
    ( d )弱夏季風年,西北區高度場西高東低,處于脊前西北 氣 流 的控制之下,西風和南風明顯減小,水汽通量輸送也大大減少,除一區的甘肅河東大部( 30 35 n , 101 105 e )存在水汽通量 輻 合外,其它地區為水汽通量 輻 散 (弱的 輻 合) 。 ( e )強夏季風年,西北區高度場東高西低,西風和南風明顯增強,水汽通量輸送同樣顯著增強,一、三區存在大范圍的水汽通量 輻 合。
  5. There are two parts in this paper : firstly, a set of single doppler velocity models are presented for typical ambient windfields that include those of being uniform horizontally, macroscale convergence and divergence, which overlap warm and cold advection. which are marked by different signatures in the single doppler velocity field. the models proposed can help users identify useful information from the dopple velocity patterns
    本論文包括兩個部分:第一篇通過對典型風場的單多普勒天 氣 雷達徑向速度圖象進行模擬,典型風場包括水平均勻一致的風場、非均勻水平風場的大尺度運動的 輻 合 輻 散 風場以及大尺度運動的 輻 合 輻 散 風場與冷暖平 流 的迭加等。

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