How many of these five real-life condensation examples have you experienced?
Morning Dew on the Grass
Have you ever wondered why there are visible water droplets on grass early in the morning even if it didn’t rain during the night? The answer is condensation. During the overnight hours, the air near the ground cools to or below the dew point. As a result, water vapor in the atmosphere becomes saturated and condenses to form dew on the grass.
Clouds in the Sky
To see another example of condensation, all you have to do is look up at the sky. Clouds are formed as a result of water vapor cooling in the atmosphere. As the temperature of the water vapor falls to the dew point or below, it condenses to become tiny water droplets. These droplets cling to tiny particles of dust in the atmosphere and become clouds.
Rain Falling Down
Rain occurs when too much water condenses around atmospheric dust particles for the water to remain in the sky in the form of clouds. Instead, the condensed droplets get bigger, heavier, and eventually fall to the ground in the form of rain. Other forms of precipitation, such as snow and sleet, are also related to condensation. Snow and sleet are frozen droplets of water.
Fog in the Air
Fog forms the same way as clouds, though it stays closer to the ground rather than being in the sky. When water vapor condenses to liquid in the form of droplets that stay suspended in the air, the result is fog. It only occurs when conditions are extremely humid. Fog can vary in thickness, ranging from light to dense.
Visible Breath in Cold Conditions
When conditions are just right, it’s possible to see your own breath in the form of condensation. When the warm and moist vapor that makes up your breath hits air that is cold and humid, it becomes tiny water droplets. These droplets take on a cloud-like appearance that you can see.
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Answer:
Five Common Condensation Examples
How many of these five real-life condensation examples have you experienced?
Morning Dew on the Grass
Have you ever wondered why there are visible water droplets on grass early in the morning even if it didn’t rain during the night? The answer is condensation. During the overnight hours, the air near the ground cools to or below the dew point. As a result, water vapor in the atmosphere becomes saturated and condenses to form dew on the grass.
Clouds in the Sky
To see another example of condensation, all you have to do is look up at the sky. Clouds are formed as a result of water vapor cooling in the atmosphere. As the temperature of the water vapor falls to the dew point or below, it condenses to become tiny water droplets. These droplets cling to tiny particles of dust in the atmosphere and become clouds.
Rain Falling Down
Rain occurs when too much water condenses around atmospheric dust particles for the water to remain in the sky in the form of clouds. Instead, the condensed droplets get bigger, heavier, and eventually fall to the ground in the form of rain. Other forms of precipitation, such as snow and sleet, are also related to condensation. Snow and sleet are frozen droplets of water.
Fog in the Air
Fog forms the same way as clouds, though it stays closer to the ground rather than being in the sky. When water vapor condenses to liquid in the form of droplets that stay suspended in the air, the result is fog. It only occurs when conditions are extremely humid. Fog can vary in thickness, ranging from light to dense.
Visible Breath in Cold Conditions
When conditions are just right, it’s possible to see your own breath in the form of condensation. When the warm and moist vapor that makes up your breath hits air that is cold and humid, it becomes tiny water droplets. These droplets take on a cloud-like appearance that you can see.