Energy Transfer in the Atmosphere (51) Energy is reflected back into space by clouds, particles, and Earth's surface. Some is absorbed by the atmosphere.

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Presentation transcript:

Energy Transfer in the Atmosphere (51) Energy is reflected back into space by clouds, particles, and Earth's surface. Some is absorbed by the atmosphere or by land and water on Earth's surface.

Heat Energy from the Sun reaches Earth's surface and heats it. Heat then is transferred through the atmosphere in three ways—radiation, conduction, and convection.

Radiation Energy from the Sun reaches Earth in the form of radiant energy, or radiation. Radiation is energy that is transferred in the form of rays or waves. Earth radiates some of the energy it absorbs from the Sun back toward space.

Conduction Conduction is the transfer of energy that occurs when molecules bump into one another. When objects are in contact, energy is transferred from warmer objects to cooler objects.

Convection Convection is the transfer of heat by the flow of material. Convection circulates heat throughout the atmosphere. When air is warmed, the molecules in it move apart and the air becomes less dense The air becomes more dense and air pressure increases. Cooler, denser air sinks while warmer, less dense air rises, forming a convection current.

The Water Cycle Hydrosphere is a term that describes all the water on Earth’s surface. The constant cycling of water between the atmosphere and the hydrosphere plays an important role in determining weather patterns and climate types.

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Energy that is transferred in the form of waves or rays is __________. A. electricity B. condensation C. radiation D. thermal power

Explain the difference between conduction, radiation, and convection?

Describe the process of the water cycle?