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"Pea soup fog," also known as a "pea-souper," refers to a very thick and dense fog. This type of fog is not a natural atmospheric formation but rather a result of pollution. It occurs when water vapor condenses onto airborne particulates, creating dark, heavy clouds that significantly reduce visibility.123

Historically, London was particularly known for these fogs, especially during the 19th century and into the 20th century, often exacerbated by the burning of coal for industrial and domestic purposes. The term "smog," a blend of "smoke" and "fog," emerged to describe this polluted haze. The Great Smog of London in 1952 was a severe instance, lasting five days and causing thousands of deaths due to respiratory illnesses, prompting significant environmental legislation.3

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