由于地面辐射冷却而形成的逆温。
本文分析了北京市郊一类典型辐射逆温。
In this paper, a typical radiation inversion in the north suburbs of Peking is analysed.
而地表的辐射冷却，对近地层逆温的影响，表现为较强的回波强度峰值，对应气温变化的谷值。
That the surface's radiation cooling affects on the ground layer temperature inversion is presented as the relatively strong echo peak value corresponding to the temperature variety's valley value.
但白天，随着太阳短波辐射的加强，逆温结构很快被破坏，城市热岛强度也迅速减弱。
In daytime, with the strong solar radiation, the inversion structure is destroyed soon, and the UHI intensity decreases rapidly.
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