Quick Answer: Is rain a form of condensation?

What are examples of condensation?

Clouds are a large-scale example of condensation, and generally form when water vapor in warm air rises to meet cold air higher in the atmosphere. As the warm air cools and the molecules coalesce and stick together, drops of water or ice crystals form and surround dust particles in the air.

What is a good example of condensation?

Examples of Condensation: 1. Having a cold soda on a hot day, the can “sweats.” Water molecules in the air as a vapor hit the colder surface of the can and turn into liquid water.

How does rain form in the water cycle?

Within a cloud, water droplets condense onto one another, causing the droplets to grow. When these water droplets get too heavy to stay suspended in the cloud, they fall to Earth as rain. … Water vapor turns into clouds when it cools and condenses—that is, turns back into liquid water or ice.

What is the difference between rainfall and precipitation?

Distinguish between Rainfall and Precipitation.


Rainfall Precipitation
(i)Rainfall is a type of precipitation when moisture falls on the earth in the form of drops of water. (i)It is the collective name given to different forms of release of moisture after condensation.
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What is not a form of condensation?

Precipitation consisting of small ice pellets formed by the freezing of raindrops or of melted snowflakes is called sleet. Sleet is liquid water that freezes before it hits the ground. Hence it is not the form of condensation.

What is condensation What are its form?

Condensation is a phenomenon that occurs when air shrinks so much that it is no longer able to capture and hold humidity. Water molecules are pressed (forced) out of the spaces between the air molecules. As a result, we see vapor (e.g. “giving out”, damping, dew, mist, clouds) or water (e.g. rain, hail, snow).

What are the different forms of condensation answer?

Four chief forms of condensation are clouds, fog, mist and dew droplets.

Where do we find condensation?

When warm air hits the cold surface, it reaches its dew point and condenses. This leaves droplets of water on the glass or can. When a pocket of air becomes full of water vapor, clouds form. The point at which condensation starts can be easily viewed in cumulus clouds, which have flat bottoms.