逆温 Inversion (meteorology)

（重定向自Air inversion）

逆温（英语：temperature inversion）现象是一种气象学的现象，指地面上的温度随着高度越高而增加，与高度越高温度下降的正常现象相反。因为较高的暖空气覆盖着较低的冷空气，可能会导致空气污染物无法散出，影响当地居民或其他生物的健康，1952年伦敦烟雾事件即为一著名案例。

单词	Air inversion
释义	Air inversion 中文百科逆温 Inversion (meteorology) （重定向自Air inversion）逆温（英语：temperature inversion）现象是一种气象学的现象，指地面上的温度随着高度越高而增加，与高度越高温度下降的正常现象相反。因为较高的暖空气覆盖着较低的冷空气，可能会导致空气污染物无法散出，影响当地居民或其他生物的健康，1952年伦敦烟雾事件即为一著名案例。英语百科 Inversion (meteorology) 逆温（重定向自Air inversion） In meteorology, an inversion is a deviation from the normal change of an atmospheric property with altitude. It almost always refers to a "temperature inversion", i.e. an increase in temperature with height, or to the layer ("inversion layer") within which such an increase occurs.
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Air inversion