大气辐射平衡，地气系统辐射平衡（Rs）与地面辐射平衡（Rg）之差，称为大气辐射平衡或大气辐射差额（Ra）。
科学家们很早之前就发现，诸如煤烟、灰尘和其他细小的微粒，能改变云体的密度及大气的辐射平衡。
Scientists have known for a long time that aerosols such as soot, dust and other small particulate matter, alter cloud density and the radiative balance of the atmosphere.
介绍了不同类型模式，如能量平衡模式、辐射对流模式、大气环流模式和随机模式等的主要特征。
The basic feature of several types of model, such as energy-equilibrium model, radiative-convective model, general circulation model (GCM). Random model and so on, are described.
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