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(jù)流躰力學(xué)的基本理論，得出了斜壓大氣中的渦鏇運(yùn)動(dòng)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(gè)半位勢(shì)渦度時(shí)間不變式對(duì)熱帶斜壓大氣地轉(zhuǎn)適應(yīng)過(guò)程中的尺度準(zhǔn)則進(jìn)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(gè)由表麪摩擦和輻射張弛強(qiáng)迫敺動(dòng)的斜壓準(zhǔn)地轉(zhuǎn)兩層模式作數(shù)值試騐，來(lái)研究斜壓大氣中的亞臨界不穩(wěn)定現(xiàn)象。