湿霾 [
shī mái]
[气象] damp haze
- 降温是达到饱和形成雾滴的最主要、最重要的物理过程,在自然界中的霾滴通过吸湿过程增长成雾滴几乎不可能。
The most important physical process to form fog drop is by falling the temperature to the saturation point. - 霾滴要想通过吸湿增长成为雾滴,必须有足够的过饱和度,能够越过过饱和驼峰才行,这在自然界并不容易。
Only under the enough supersaturation can the haze nuclei grow into fog droplet through moisture absorption, and such process is not easy to happen. - 在非饱和条件下,不但非水溶性的霾不能转化成雾滴,即便是水溶性的霾粒子一般也不可能吸湿转化为雾滴。
Under non-saturation conditions, not only the insoluble haze nuclei are impossible to transform into fog drop, but also the soluble ones are commonly impossible.
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