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Freezing rain begins its journey to the surface as snow. As the snow descends, it encounters a layer of warm air and melts. Then, just above the ground, it travels through a shallow layer of subfreezing air. The raindrops don’t have time to refreeze but remain in the liquid state at temperatures below freezing. In other words, they become supercooled. Most precipitation originates in clouds as ice crystals. As an ice crystal descends through a cloud, it grows by collecting water vapor and droplets of supercooled water, which remains in the liquid state below the freezing point. In the process, the ice crystal takes on the shape of a snowflake, a lump of snow or ice, or in severe thunderstorms, hail. What happens next depends on the air temperature at various heights throughout Trending vintage book lovers reading jane austen book stack all over printed tote bag the ice crystal’s descent. There are other winter hazards not associated with falling precipitation. Black ice can develop on paved surfaces when temperatures drop below freezing and there is standing water. The ice can be clear and difficult to see and the sheer ice surface is especially slick. Frost, which tends to form on clear and calm nights, can occasionally affect runway traction. Fog is always problematic at airports. The reduction in visibility can often lead to flight delays. Besides your common fog,
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