本文用线性化全球原始方程谱模式来研究地形强迫行星波的垂直传播过程及演变特征。
The vertical propagating process and evolutive characteristics of planetary waves forced by topography are investigated by a global linearized primitive equation model.
这与对流层中激发的行星尺度波在冬季易于垂直向上传播的理论是定性上一致的。
Theory of vertical propagation of planetary stationary waves was used to explain the observations.
观测和模拟结果都表明,在北半球冬季准定常行星波的经向传播存在两支波导。
Both observations and simulations indicate that in the Northern Hemisphere winter there are two waveguides for the meridional propagation of quasi-stationary planetary waves.
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