baroclinic atmosphere

基本解釋

In this paper, the equations of motion of vortices in baroclinic atmosphere are derived in the light of classical hydrodynamics.
本文根據流體力學的基本理論，得出了斜壓大氣中的渦旋運動方程。
Based on an invariant of semi-potential vorticity, the scale criterion of geostrophic adaptation in tropical baroclinic atmosphere is discussed.
文中利用一個半位勢渦度時間不變式對熱帶斜壓大氣地轉適應過程中的尺度準則進行了研究。
A two layer quasi geostrophic model forced by surface friction and radiative relaxation is used to study numerically the phenomenon of subcritical instability in baroclinic atmosphere.
利用一個由表面摩擦和輻射張弛強迫驅動的斜壓準地轉兩層模式作數值試驗，來研究斜壓大氣中的亞臨界不穩(wěn)定現象。