poloprchozí

Poloprchozí is a Czech term that describes a type of precipitation. It literally translates to "half-rain." This meteorological phenomenon refers to a mixture of rain and snow that occurs when temperatures are near freezing. The precipitation can appear as a slushy mix, large wet snowflakes that melt before reaching the ground, or a combination of both.

The conditions necessary for poloprchozí typically involve atmospheric temperatures hovering around 0 degrees Celsius (32 degrees Fahrenheit). The exact composition of poloprchozí can vary depending on subtle shifts in temperature and atmospheric moisture. It is often associated with transitional weather patterns, such as the onset of winter or the thaw of spring. While it is not a distinct weather event in the same way as a thunderstorm or blizzard, it is a commonly recognized and experienced form of winter weather in regions with a temperate climate. The term is primarily used in the Czech Republic and Slovakia.