Kurzawka

Kurzawka (Polish pronunciation: [kuˈʐafka]) refers to a meteorological phenomenon and a geological feature. It describes a shallow, temporary body of water or a marsh that forms in depressions or on flat terrain, typically after heavy rainfall or snowmelt. These formations are characterized by their ephemeral nature, disappearing relatively quickly due to evaporation and seepage into the ground.

In meteorological terms, "kurzawka" can also describe a short, intense period of rainfall, often a brief but heavy shower. This usage emphasizes the rapid onset and short duration of the precipitation.

Geologically, kurzawka areas are often associated with poorly draining soils and a high water table. The presence of kurzawki can indicate the potential for waterlogging and may influence land use planning and agricultural practices in affected regions. These temporary wetlands can provide habitat for various plant and animal species, especially amphibians and insects, while they exist.

The term "kurzawka" is most commonly used in Poland and other parts of Central and Eastern Europe, reflecting the geographical areas where this phenomenon is frequently observed.