klasklimaat

Klasklimaat is a term used to describe a specific type of climate characterized by distinct, pronounced seasonal variations. The name itself, derived from Dutch, suggests a "clasping" or "gripping" climate, highlighting the strong influence of different seasons. This typically means experiencing clearly defined summers that are noticeably warmer and winters that are distinctly colder. Transitions between these seasons, spring and autumn, are also usually evident, bringing their own set of weather patterns.

The defining feature of a klasklimaat is the significant difference in temperature and precipitation between the summer and winter months. This contrast is more pronounced than in regions with more moderate or maritime climates. While not a formal climatological classification like Köppen or Trewartha, the term is often used in informal discussions and descriptive contexts to convey the experience of living in a place with such stark seasonal changes.

Geographically, areas often described as having a klasklimaat are typically found in continental interiors, away from the moderating influence of large bodies of water. These locations tend to experience more extreme temperature swings due to factors like landmass heating and cooling. The precise characteristics of a klasklimaat can vary, but the core concept remains the strong, often dramatic, shift between hot and cold periods of the year.