baroclinic atmosphere

基本解释

In this paper, the equations of motion of vortices in baroclinic atmosphere are derived in the light of classical hydrodynamics.
本文根据流体力学的基本理论，得出了斜压大气中的涡旋运动方程。
Based on an invariant of semi-potential vorticity, the scale criterion of geostrophic adaptation in tropical baroclinic atmosphere is discussed.
文中利用一个半位势涡度时间不变式对热带斜压大气地转适应过程中的尺度准则进行了研究。
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.
利用一个由表面摩擦和辐射张弛强迫驱动的斜压准地转两层模式作数值试验，来研究斜压大气中的亚临界不稳定现象。