tropopause 中文意思是什麼
tropopause
解釋
n. 名詞 【氣象學】對流層頂。-
The balance must be made up by heat transport through the tropopause.
必須通過對流層頂的熱輸送來建立平衡。 -
Statistical features of tropopause over qinghai province
青海省對流層頂若干統計特徵 -
Statistics of the global tropopause temperature change
全球對流層頂溫度場演變的氣候學特徵分析 -
The variation of spatial - temporal distribution of the global tropopause ozone
大氣對流層頂的臭氧時空分佈變化 -
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。 -
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。 -
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
輻射力的定義是由於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。 -
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
輻射力的定義是由於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。 -
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。 -
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徵是：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。
分享友人