latent heat release 中文意思是什麼

latent heat release 解釋
潛熱釋放
  • latent : adj. 存在但看不見的;潛伏的;潛在的。n. 隱約的指印,潛指印。adv. -ly
  • heat : n 1 熱;熱力;熱度;熱量。2 體溫;發燒。3 (氣候的)高溫,暑氣。4 【冶金】熔煉的爐次;裝爐量;一...
  • release : vt 1 放(箭等),投(炸彈);解放,釋放(囚犯、俘虜等);使免除;救出;解除(痛苦、債務等) (fro...
  1. In a word, convective instability strong baxoclinicity barotropic advection of potential vorticity and latent heat release are factors which activize this explosive development of cyclone

    總之,對流不穩定、強斜壓性和正壓位渦平流、潛熱釋放是本次氣旋發展的啟動因子。
  2. The results show that vorticity advection, thermal advection and latent heat release made great contribution to the development of the depression

    中低層的溫度平流、降水凝結釋放潛熱維持上升運動,是低壓進一步發展的有利條件。
  3. 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。
  4. At the same time, the effects of dragging force from fall of hydrometeors and latent - heat release from phase transfer are tested. from the analyses we conclude that the distributing of the cloud particles relates with temperature closely. huanan heavy rainfall and mei - yu front heavy rainfall have mixed - phase process with vapor phase, liquid phase and ice phase

    詳細分析了形成降水的雲物理過程,探討了源匯項對水凝物的貢獻,並通過敏感性試驗,考察了雲物理過程對降水熱力動力過程的反饋作用,研究結果表明:華南暖區暴雨和長江梅雨鋒暴雨的雲物理過程具有汽、水、冰三相混合雲特徵。
  5. It is found that the climatological mean of wind speed and air - sea humidity difference are both large, the variation of wind speed are almost in phase with air - sea humidity difference, yielding much larger or smaller latent heat flux. so the ocean release the most latent heat in its own winter of the two hemispheres when both wind speed and air - sea humidity difference are large

    發現在南北兩信風區,風速和海氣濕度差的變化幾乎是同位相的,平均背景風速和海氣濕度差都較大,他們互相加強彼此對潛熱通量變化的貢獻,所以海洋潛熱損失最大是發生信風南北兩區的各自風速和海氣濕度差都較大的冬季。
  6. It is shown that the parameters of the flow field are disturbed and a condensation shock is generated due to the sudden release of the latent heat of condensation

    結果表明由於水蒸氣的凝結釋放熱量對流場局部進行加熱,使流場參數發生擾動而產生凝結激波。
  7. It is necessary to include as a heat source in the thermodynamic energy equation at erm which represems the timerate of release of the latent heat of condensation of water vapor

    譯為:有必要把代表水汽凝結潛熱釋放的隨時間變化率的一項作為熱源項包括在熱力學能量方程中。
  8. The effect of dragging force weakens the convection and the effect of latent - heat release strengthens the instability. both of them are evidently feedback actions to the environment

    雲中水凝物下落的拖曳作用削弱了對流,相變潛熱釋放加劇了層結不穩定,均對熱力動力過程有明顯反饋作用。
  9. In equatorial region, the mean air - sea humidity difference is much smaller, so the variations of air - sea humidity difference under large mean wind speed dominate the variations of latent heat flux. the ocean release the most heat during the period from march to may, when sst is highest in the whole year because sst dominates the variation of air - sea humidity difference

    在赤道冷舌區,平均的背景海氣濕度差比較小,所以平均風速背景下的海氣濕度差的熱帶大西洋海表潛熱和感熱通量的季節和年際變化研究變化主導該區的潛熱通量的變化。
  10. ( 2 ) the anomalous eawm predominantly relates to the winter kuroshio ssta. the winter kuroshio ssta becomes positive ( negative ) when there is a strong ( weak ) eawm. the possible links might be the winter latent and sensible heat release in the west - northern pacific ocean

    ( 2 )東亞冬季風異常對冬季黑潮區域海溫異常有密切的聯系,當東亞冬季風偏強時,冬季黑潮區域海溫偏低;反之,冬季黑潮區域海溫偏高。
  11. And the feedback actions of the dragging force and the latent - heat release are not evident

    水凝物的下落拖曳作用和相變潛熱作用對環境場的熱力動力反饋不明顯。
  12. The effect of dragging force also weakens the convection and the effect of latent - heat release strengthens the instability

    水凝物的下落拖曳作用和相變潛熱作用對環境場的熱力動力過程有一定的反饋。
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