convectively unstable air 对流不稳空气
convectively mixing 对流混合
convectively stable 对流稳定
convectively unstable 对流不稳定
Generation Mechanisms of Convectively Forced Internal Gravity Waves and Their Propagation to the Stratosphere.
对流强迫重力内波的生成机制和向平流层的传播。
In the convectively heating region latent heat release causes a heating peak in the upper troposphere and a moisture sink in the lower troposphere.
在对流加热区，大量的潜热释放形成深厚的热源和水汽汇，热源峰值出现在上部对流层，水汽汇峰值出现在下部对流层；
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