When the temperature in clouds drops, the water vapor within the clouds can condense into tiny water droplets or ice crystals, depending on the temperature. This process can lead to the formation of precipitation, such as rain, snow, or sleet, as the droplets coalesce and become heavy enough to fall to the ground. Additionally, colder temperatures can enhance the cloud's ability to hold ice crystals, contributing to cloud types like cirrus or cumulonimbus. Overall, the drop in temperature plays a crucial role in cloud dynamics and weather patterns.
What happens when the clouds hang very low is that it becomes foggy. Fog is clouds that are very low to the ground and that are are made up of tiny water drops.
It drops.
rain.
Yes, clouds are affected by temperature.
Fluffy clouds are called cumulus clouds. Cumulus clouds may be formed by three things: supercooled water droplets, ice crystals, or water vapor. What they are made of depends on the temperature. They are formed when warm surface air rises from the earth and the temperature in the atmosphere drops.
Before it snows, the moisture in the air condenses and forms clouds. As the temperature drops, the moisture in the clouds freezes and falls to the ground as snow when the conditions are right. This process is part of the water cycle and can be influenced by factors such as temperature, humidity, and air pressure.
It drops.
What happens when the clouds hang very low is that it becomes foggy. Fog is clouds that are very low to the ground and that are are made up of tiny water drops.
Drops of condensed water in the atmosphere can form clouds, fog, or precipitation such as rain or drizzle, depending on atmospheric conditions like temperature, pressure, and humidity.
It drops.
it drops
The water gets colder.
When air pressure drops temperature also drops. Thus on high mountains low air pressure is accompanied by low temperature. This is true for high atmosphere also.
When the temperature drops the less water vapor in the air
It drops.
you die
Saturation happens when the air cannot hold any more water vapor, leading to condensation and the formation of clouds or precipitation. It can occur when the temperature of the air drops, when moisture is added to the air, or when the air is cooled to its dew point.