Vapor into liquid is condensation.
Changing water vapor into tiny drops of water is known as condensation. This process occurs when the temperature of the air cools, causing the water vapor to lose energy and form liquid water droplets. Condensation is a key step in the water cycle.
These particles are molecules of gaseous water.
Condensation
When water vapor changes into tiny drops of water, it is called condensation. This process occurs when the air cools down and cannot hold as much moisture, leading the water vapor to transform into liquid water droplets.
Tiny drops of water can come from condensation, which occurs when warm and moist air cools down and can no longer hold all the water vapor it contains. This excess water vapor then forms into tiny droplets that we see as water droplets. They can also come from processes like misting, spraying, or atomizing liquids.
When cooled enough, water vapor condenses into tiny water droplets. This process occurs as the temperature drops, causing the water vapor molecules to lose energy and come together to form liquid droplets. This phenomenon is commonly observed in the formation of clouds or dew.
This physical process is called liquefaction and occur under the boiling point. Thie depends on the pressure.
Condensed water vapor is water vapor that has cooled and changed back into a liquid state. This can happen when the temperature drops and the water vapor loses energy, causing it to condense into tiny droplets or ice crystals. This process is what forms clouds, fog, and dew.
When warm air rises, it cools as it ascends in the atmosphere. This cooling causes water vapor to condense into tiny droplets, forming clouds. The process is part of the water cycle, where warm, moist air leads to cloud formation and, eventually, precipitation.
The tiny drops of water are cool and it condenses.
Fog forms when water vapor condenses into tiny water droplets close to the ground. It usually occurs when the air near the surface becomes saturated and the temperature drops, causing the vapor to condense into fog. Clouds, on the other hand, form at higher altitudes and are made up of tiny water droplets or ice crystals suspended in the air.
One way to show that water vapor is present in the air is to cool the air. If the air temperature drops below its dew point, water vapor in the air will condense into tiny droplets, forming visible fog or mist. This process demonstrates that water vapor is a component of the air.