cloud chamber
Particles of salt and dust in the air can serve as nuclei around which water vapor can condense, leading to the formation of cloud droplets. These particles provide a surface for water vapor to condense onto, promoting the growth of cloud droplets and ultimately the formation of clouds.
The presence of dust in the air can expedite cloud formation by providing a surface for water droplets to condense and form cloud droplets around. Dust particles act as cloud condensation nuclei, which help water vapor in the air to condense into clouds.
The term for droplets of water that condense on aerosols in the sky is called "cloud condensation nuclei." These particles serve as the nuclei around which water vapor in the atmosphere condenses to form clouds.
Clouds are formed when warm, moist air rises and cools, causing water vapor to condense into tiny droplets or ice crystals around dust particles in the atmosphere. The droplets then come together to form clouds.
Clouds form when water vapor in the air condenses around tiny particles like dust, salt, or pollution in the atmosphere. These particles serve as nuclei for the water vapor to condense onto, eventually forming droplets and leading to cloud formation.
cloud chamber
Water vapor needs to cool down in order to turn into droplets. This cooling process can happen by either coming into contact with a colder surface or by the surrounding air temperature dropping. Once the water vapor cools sufficiently, it will condense into droplets.
The device you are referring to is called a cloud chamber. It is used to observe the paths of charged particles, such as those emitted from radioactive decay, as they ionize the alcohol vapor in the chamber, producing visible tracks.
Clouds form when water vapor in the atmosphere condenses into liquid droplets around tiny particles like dust, pollen, or pollution. These particles act as nuclei around which the water vapor can condense and form visible clouds.
Particles of salt and dust in the air can serve as nuclei around which water vapor can condense, leading to the formation of cloud droplets. These particles provide a surface for water vapor to condense onto, promoting the growth of cloud droplets and ultimately the formation of clouds.
The presence of dust in the air can expedite cloud formation by providing a surface for water droplets to condense and form cloud droplets around. Dust particles act as cloud condensation nuclei, which help water vapor in the air to condense into clouds.
Aerosols, such as dust, smoke, or pollution particles, act as nuclei for cloud droplets to form around in the atmosphere. These solid particles provide a surface for water vapor to condense onto, leading to the formation of cloud droplets.
The term for droplets of water that condense on aerosols in the sky is called "cloud condensation nuclei." These particles serve as the nuclei around which water vapor in the atmosphere condenses to form clouds.
Clouds are formed when warm, moist air rises and cools, causing water vapor to condense into tiny droplets or ice crystals around dust particles in the atmosphere. The droplets then come together to form clouds.
A large concentration of tiny water droplets is called a cloud. Clouds are formed from water vapor that condense into clouds.
Dew is formed by condensation - the water from the air around the ground becomes heavy enough to form into droplets on any areas which are colder than the air.Rain is formed when water droplets condense above the ground and fall.
Clouds form when warm, moist air rises and cools, causing the water vapor in the air to condense into water droplets or ice crystals around particles like dust or salt. These tiny droplets then collect together to form clouds.