Clouds Usually Form When. Clouds form when the air cools below the dewpoint, and the air can not hold as much water vapor. These water droplets form on tiny particles, like dust, that are floating in the air.
Altocumulus clouds Center for Science Education
Web as air rises it cools and decreases pressure, spreading out. Clouds are created when water vapor, an invisible gas, turns into liquid water droplets. Clouds form when the air cools below the dewpoint, and the air can not hold as much water vapor. Fog is a shallow layer of cloud at or near ground. Clouds are made of water droplets or ice crystals that. Web clouds form when air becomes saturated, or filled, with water vapor. These water droplets form on tiny particles, like dust, that are floating in the air. Web cloud, any visible mass of water droplets, ice crystals, or a mixture of both that is suspended in the air, usually at a considerable height (see video). Web the short answer: Warm air can hold more water vapor than cold air, so lowering the temperature of an air mass is like squeezing a sponge.
Web cloud, any visible mass of water droplets, ice crystals, or a mixture of both that is suspended in the air, usually at a considerable height (see video). Fog is a shallow layer of cloud at or near ground. These water droplets form on tiny particles, like dust, that are floating in the air. Web cloud, any visible mass of water droplets, ice crystals, or a mixture of both that is suspended in the air, usually at a considerable height (see video). Clouds form when the air cools below the dewpoint, and the air can not hold as much water vapor. Web clouds form when air becomes saturated, or filled, with water vapor. Web the short answer: Clouds are created when water vapor, an invisible gas, turns into liquid water droplets. Web as air rises it cools and decreases pressure, spreading out. Clouds are made of water droplets or ice crystals that. Warm air can hold more water vapor than cold air, so lowering the temperature of an air mass is like squeezing a sponge.
