It turns into ice.
Hail forms when water drops freeze in layers around small nuclei of ice as they are carried up and down in strong updrafts within thunderstorms. The process of repeated freezing and melting of the water droplets contributes to the growth of hailstones.
These are called graupel or soft hail. Graupel forms when supercooled water droplets in a thunderstorm freeze on contact with ice nuclei, creating layered ice pellets. Graupel is typically smaller and softer than hailstones.
Sleet forms when raindrops freeze into ice pellets before reaching the ground. This occurs when rain falls through a layer of cold air near the surface.
Ponds freeze when the air temperature drops below freezing, causing the water in the pond to also freeze. The ice that forms is less dense than liquid water, so it floats on top of the pond. This ice layer acts as an insulator, preventing further freezing of the water underneath.
Colliding drops of water freeze together in the cold upper regions of a thunderstorm to form hailstones. These hailstones grow in size as they continue to collect ice and water until they become too heavy to be supported by the updrafts and fall to the ground as hail.
Water droplets form around condensation nuclei, which are tiny particles in the atmosphere that provide a surface for water vapor to condense onto. This process is essential for the formation of clouds and precipitation. Examples of condensation nuclei are dust, salt particles, and pollutants.
It forms a cloud
Testostrone
Testostrone
sleet
A cell plate forms
It forms a cloud