What is the order of steps through which a particle of gaseous water water vapor world travel as it made one complete trip through the water cycle?

What is the order of steps through which a particle of gaseous water water vapor world travel as it made one complete trip through the water cycle?

And the order is same as written above that is first evaporation then condensation, precipitation and then collection.

What are the 9 parts of the water cycle?

It can be studied by starting at any of the following processes: evaporation, condensation, precipitation, interception, infiltration, percolation, transpiration, runoff, and storage. Evaporation occurs when the physical state of water is changed from a liquid state to a gaseous state.

Where is water stored naturally?

The ocean holds about 97 percent of the Earth’s water; the remaining three percent is found in glaciers and ice, below the ground, in rivers and lakes. Of the world’s total water supply of about 332 million cubic miles of water, about 97 percent is found in the ocean.

Which is a process in the water cycle?

water cycle. the continuous movement of water between the atmosphere, land and the oceans. evaporation. the process by which water is converted from its liquid state to the gaseous state, also known as water vapor. condensation. the process by which water vapor is changed back into liquid water.

How is water converted from a liquid to a gaseous state?

the process by which water is converted from its liquid state to the gaseous state, also known as water vapor. condensation. the process by which water vapor is changed back into liquid water.

Can you follow a drop of water through the water cycle?

You may be familiar with how water is always cycling around, through, and above the Earth, continually changing from liquid water to water vapor to ice. One way to envision the water cycle is to follow a drop of water around as it moves on its way. Read on to learn more about the journey.

Where does water vapor go in the water cycle?

It rose (as tiny “dropettes”) into the air and continued rising until strong winds aloft grabbed it and took it hundreds of miles until it was over land. There, warm updrafts coming from the heated land surface took the dropettes (now water vapor) up even higher, where the air is quite cold.