Frost
Frost is a meteorological phenomenon that occurs when condensation of moisture happens at temperatures below freezing points (0°C), resulting in minute ice crystals forming on surfaces. In the atmospheric context, frost typically forms under specific conditions, much like dew, but it distinctly requires cooler temperatures where the dew point aligns with or drops below freezing. This section delves into the characteristics of frost formation, elucidating the necessary atmospheric conditions such as clear skies, calm air, and increased relative humidity. These elements converge to ensure that moisture deposits as solid ice instead of liquid water. Furthermore, this discussion ties into broader meteorological concepts such as humidity, condensation, and the impacts of temperature on atmospheric processes, firmly situating frost within the framework of water's cycle through the atmosphere.