FogDisc

FogDisc is a type of fog that forms in a disc shape, typically above a body of water. It is often observed in coastal regions and is a result of the interaction between the warm, moist air from the water and the cooler air above it. The fog forms when the warm air rises and cools, causing the water vapor to condense into tiny droplets, which then form the fog disc. This phenomenon is often seen in the early morning or late evening, when the temperature difference between the water and the air is greatest. FogDiscs can vary in size and density, and they can sometimes be quite thick, reducing visibility to near zero. They are a common sight in many coastal cities around the world, including San Francisco, California, and London, England. The formation of FogDiscs is a fascinating example of how weather patterns can create unique and visually striking phenomena.