Where is heat transferred during the water cycle?

Where is heat transferred during the water cycle?

Latent heating The process of evaporation absorbs tremendous amounts of incoming solar energy. Through the process of latent heating, energy is transferred into the atmosphere when the water vapor condenses during the formation of clouds.

How is heat added and lost in the water cycle?

If heat is added to water, it evaporates. Evaporation turns liquid water into a gas called water vapor. If heat is taken away from water vapor, it condenses. Condensation turns water vapor into a liquid.

Under which process heat is supplied in the water cycle?

When water at the ocean’s surface is heated by the Sun it gains energy. With enough energy, the molecules of liquid water change into water vapor and move into the air. This process is called evaporation.

How does water transfer heat around the world?

Winds and water currents move warm air and water to cooler locations, thus distributing heat energy around the globe. Water evaporates from the surface of the earth, rises and cools, condenses into rain or snow, and falls again to the surface.

Where does evaporation take place in the water cycle?

Evaporation from the oceans is the primary mechanism supporting the surface-to-atmosphere portion of the water cycle. After all, the large surface area of the oceans (over 70 percent of the Earth’s surface is covered by the oceans) provides the opportunity for large-scale evaporation to occur.

How does convection transfer heat from one place to another?

Convection is very important in moving heat through the atmosphere and the oceans. It transfers heat from one place to another. All winds result from uneven heating of the atmosphere. An island, is surrounded by cool water. During the day, the island heats faster than the water and so the air above the island becomes warmer.

Where does water go after it enters the atmosphere?

After the water enters the lower atmosphere, rising air currents carry it upward, often high into the atmosphere, where the air is cooler. In the cool air, water vapor is more likely to condense from a gas to a liquid to form cloud droplets.