tropopause n.【氣象學】對流層頂。
n. 【氣象學】對流層頂。 “arctic tropopause“ 中文翻譯： 極地對流層頂“artic tropopause“ 中文翻譯： 北極對流層頂“extratropical tropopause“ 中文翻譯： 溫帶對流層頂“foliated tropopause“ 中文翻譯： 復對流層頂“multiple tropopause“ 中文翻譯： 復對流層頂“tropical tropopause“ 中文翻譯： 熱帶對流層頂“tropopause break“ 中文翻譯： 對流層頂斷裂“tropopause chart“ 中文翻譯： 對流層頂圖“tropopause discontinuity“ 中文翻譯： 對流層頂不連續“tropopause folding“ 中文翻譯： 對流層頂折疊“tropopause funnel“ 中文翻譯： 漏斗狀對流層頂“tropopause inversion“ 中文翻譯： 對流層頂逆溫“tropopause leaf“ 中文翻譯： 葉狀對流層頂“tropopause break-line“ 中文翻譯： 對流層頂斷裂線“tropoparasite“ 中文翻譯： 轉主寄生“tropopanse“ 中文翻譯： 對流層頂“troponrurosis of romberg“ 中文翻譯： 羅姆伯格營養神經病,單側面萎縮“troponoid“ 中文翻譯： 環庚三烯酮型化合物; 卓酮類; 卓酮型
tropophilous |
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3 in the years of cold spring , the inner mongolia high and the aliushen low are strengthened with the low index of the east asia trough and the negative anomaly center of temperature over northeast china from surface to tropopause while the contrary conditions occur in the years of warm spring 3 、東北地區出現春季低溫的主要環流特征是：內蒙古高壓，阿留申低壓的強度加強；阿流申低壓指數以及東亞大槽強度指數減弱，東北地區從地面到對流層頂處在溫度負距平中心內，東北地區春季高溫時則出現與上面相反的變化形式。 |
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Wet and dry numerical simulation tests for explosive cyclone over western pacific were performed . by contrast the results show that : tropopause and constant temperature surface were raised by latent heat release in upper level and disturbance trough was produced because air flow ascended and became cold . owing to this process adaption , inertial instability emergenced 對氣旋強烈爆發的過程進行干濕對比數值模擬試驗，得出：潛熱釋放使對流層項和等溫面抬高，氣流在高層的上升冷卻形成擾動槽，其適應過程使高層出現慣性不穩定。 |
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Radiative forcing is defined as a change in average net radiation at the top of the troposphere ( tropopause ) due to a change in either solar or infrared radiation 輻射力的定義是由于太陽或紅外線輻射份量的轉變而引致對流層頂部的平均輻射改變。 |
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Radiative forcing is defined as a change in average net radiation at the top of the troposphere tropopause due to a change in either solar or infrared radiation 輻射力的定義是由于太陽或紅外線輻射份量的轉變而引致對流層頂部的平均輻射改變。 |
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3 . synoptic meteorology : the general circulation ; air masses ; fronts ; tropopause ; jet stream ; fog ; local winds ; severe local storms 3 .天氣學：大氣環流氣團鋒對流層頂急流霧地方性風強烈地方性風暴。 |
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As soon as the tropopause is reached , temperature stops decreasing with height 一達到對流層，溫度就停止隨高度上升。 |
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The variation of spatial - temporal distribution of the global tropopause ozone 大氣對流層頂的臭氧時空分布變化 |
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Statistics of the global tropopause temperature change 全球對流層頂溫度場演變的氣候學特征分析 |
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Statistical features of tropopause over qinghai province 青海省對流層頂若干統計特征 |