The primary meteorological categories of fog, often grouped into classic classification lists, include: (1) Radiation fog, formed by nighttime cooling; (2) Advection fog, caused by warm air moving over a cold surface; (3) Upslope fog, created when wind pushes air up a mountain; (4) Steam fog, rising over warm water; (5) Precipitation fog, formed by falling rain; (6) Frontal fog, associated with weather boundaries; and (7) Valley fog, trapped in terrain depressions.
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