Particles can interact with water vapor in the air by absorbing or adsorbing moisture. This interaction can lead to the particle's size increasing due to water condensation on its surface. In some cases, particles can also serve as nuclei around which water droplets form, leading to the creation of clouds or fog.
Water vapor attaches to tiny particles in the air, such as dust or pollutants, to form cloud droplets. These particles serve as nuclei for the water vapor to condense onto, starting the process of cloud formation.
When water vapor cools and condenses into water droplets, it forms clouds in the atmosphere. This process is crucial for cloud formation, as the water droplets accumulate and interact with other particles in the air to create visible cloud structures.
Clouds are visible masses of condensed water droplets or ice crystals floating in the atmosphere, while water vapor is the invisible gaseous form of water that is present in the air. Clouds form when water vapor in the air condenses around particles like dust or salt nuclei.
Water vapor, which is the gaseous form of water. This moisture in the air makes it feel damp and sticky. Additionally, humid air can also contain other particles such as dust, pollutants, and microscopic organisms.
Clouds form from water vapor in the air that condenses into water droplets or ice crystals. This condensation occurs when the air reaches its dew point, causing the water vapor to change into visible cloud particles.
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Dust particles can serve as nuclei for water vapor to condense onto, forming cloud droplets. This interaction can lead to the formation of clouds, precipitation, and affects the processes of rain and snow formation. Dust in the air can also influence the properties of clouds, such as their brightness and lifespan.
Water vapor attaches to tiny particles in the air, such as dust or pollutants, to form cloud droplets. These particles serve as nuclei for the water vapor to condense onto, starting the process of cloud formation.
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condensation (the water vapor condenses onto the small dust particles in the air creating clouds)
When water vapor molecules in the atmosphere stick to particles in the air and become a liquid, it is called condensation. This process occurs when the air cools down, causing the water vapor to lose energy and turn into liquid droplets.
When water vapor cools and condenses into water droplets, it forms clouds in the atmosphere. This process is crucial for cloud formation, as the water droplets accumulate and interact with other particles in the air to create visible cloud structures.
When water vapor condenses around dust particles a cloud is formed
Condensation Nuclei
Clouds are made up of tiny water droplets and ice crystals. Water droplets form when water vapor in the air condenses onto particles such as dust or salt. Ice crystals form when the temperature is below freezing and the water vapor in the air freezes onto particles.
saturation of the air with water vapor. When the air cools to its dew point and becomes saturated with water vapor, the excess vapor condenses onto tiny particles in the air to form water droplets, resulting in cloud formation.
When it contains smoke, dust, volcanic ash, particles of water vapor, and/or soot