Temperate climates are most likely to experience snow during the winter months due to their seasonal temperature variations.

Temperate climates experience distinct seasons, including cold winters where snow is common. These regions are characterized by moderate temperatures, with winter temperatures often falling below freezing, allowing for snow to form. Areas in temperate zones, such as parts of the U.S. Northeast or Europe, regularly see snowfall in winter. The snowfall in temperate climates is typically a result of cold air masses and moisture from the atmosphere. While snow is more common in higher latitudes and mountainous regions, temperate zones can still experience significant snowfall, especially during colder winter months, adding to their seasonal climate variation.