kondensatsioonil

Kondensatsioonil is a type of cloud that forms when warm, moist air rises and cools, causing the water vapor to condense into tiny water droplets or ice crystals. These clouds are typically associated with precipitation and are often found at lower altitudes. Kondensatsioonil clouds can vary in appearance, ranging from thin, wispy cirrus clouds to thick, puffy cumulus clouds. They play a crucial role in the Earth's water cycle, as they help to distribute water vapor throughout the atmosphere and contribute to the formation of precipitation. Kondensatsioonil clouds are also important for weather forecasting, as they can indicate the presence of storms or other weather phenomena.