Kantmist

Kantmist refers to a phenomenon where visibility is significantly reduced due to a combination of fog and mist. It is often experienced in coastal regions or areas with high humidity. The term itself is a portmanteau of "kant," a dialectal term for fog, and "mist." While fog and mist are often used interchangeably, mist is generally considered to be less dense than fog, with visibility typically ranging from 1 kilometer to 10 kilometers. Kantmist, therefore, describes a condition that falls within this range, characterized by a damp, obscuring atmosphere.

The formation of kantmist is similar to that of fog and mist, involving the condensation of water vapor in the air. This typically occurs when warm, moist air comes into contact with cooler surfaces, or when air cools to its dew point. Factors such as temperature, humidity, and wind speed play a role in the development and persistence of kantmist. Its presence can impact transportation, particularly road and air travel, by necessitating slower speeds and increased caution. In some areas, kantmist is a recurring seasonal event. The exact origin of the term "kantmist" is not widely documented, but its usage appears to be localized.