`fog` Related Article Results

Fog is a meteorological phenomenon that occurs when water vapor in the air near the Earth’s surface condenses into suspended tiny water droplets or ice crystals due to the air layer reaching its dew point temperature or gaining additional moisture through evaporation. Lakra and Avishek define fog as an atmospheric boundary layer phenomenon. Fog forms when water vapor near the Earth’s surface condenses into suspended water droplets or ice crystals. This phenomenon, which reduces horizontal visibi