Hózápor

Hózápor, also known as snowfall, is a meteorological phenomenon characterized by the precipitation of ice crystals in the form of snowflakes. It occurs when the atmospheric temperature is at or below the freezing point of water, typically 0 degrees Celsius (32 degrees Fahrenheit). Snowfall is a common winter weather event and is a significant component of the global water cycle.

The process of hózápor begins when water vapor in the atmosphere condenses into ice crystals, which then grow and aggregate to form snowflakes. These snowflakes fall to the ground when they become too heavy to remain suspended in the air. The size, shape, and density of snowflakes can vary depending on atmospheric conditions, such as temperature and humidity.

Snowfall can have various impacts on the environment and human activities. It provides a significant source of fresh water for ecosystems and can contribute to soil moisture and groundwater recharge. However, heavy snowfall can also lead to disruptions in transportation, power outages, and other infrastructure-related issues.

The measurement of hózápor is typically done using snow gauges, which collect and measure the amount of snowfall over a specific period. Snowfall is often reported in terms of the depth of snow on the ground, which can vary depending on factors such as the density of the snow and the rate of melting.