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Mists and haze Версия для печати
The Mists are formed as a result of concourses of the products to condensations (transition from gaseous condition in fluid or hard) or sublimations (transition from solid state material in gaseous) water pair.

On power mists are divided on:
strong - range to visibility less 50 m
moderate - 50-500 m
low - 500 - 1000 m
moderate haze - 1-2 km
low haze - 2-10 km

Also mists are divided on:
water (to -20°C)
icy

On height distinguish mists: shallow - above 2 m, low - 2-10 m, average - 10-100 m high - more than 100 m

The haze - an utter clouding of atmosphere, caused by ensemble residing midair small hard particles (dust, smoke).

 
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