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Frontal fog is a type of fog that forms near weather fronts. It occurs when raindrops falling from warmer air above a frontal surface evaporate into cooler air near the Earth's surface. This process increases the moisture content of the cooler air, leading to saturation and the formation of fog. Fog, in general, is a cloud of small water droplets near ground level that reduces horizontal visibility to less than 1,000 meters (3,281 feet). It forms when air becomes saturated with moisture, typically through cooling or the mixing of air masses.12

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