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Fog can be considered a type of low-lying cloud, and is heavily influenced by nearby bodies of water, topography, wind conditions, and even human activities.
Infra-red cooling of a cloud-free, humid air mass at night can lead to fog formation – this is called “radiation fog”. Radiation fog is most common in Autumn, when nights get longer, air masses begin to cool, and land and water surfaces that have warmed up during the summer are still evaporating a lot of water into the atmosphere.