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Chapter 2 Weather Factors Section 2 Heat Transfer.

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Chapter 2 Weather Factors Section 2 Heat Transfer
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Page 1: Chapter 2 Weather Factors Section 2 Heat Transfer.

Chapter 2

Weather Factors

Section 2

Heat Transfer

Page 2: Chapter 2 Weather Factors Section 2 Heat Transfer.

How Heat is Transferred

• Heat is transferred in 3 ways: radiation, conduction, and convection.

Page 3: Chapter 2 Weather Factors Section 2 Heat Transfer.

How Heat is Transferred

• Heat is the energy transferred from a hotter object to a cooler one.

Page 4: Chapter 2 Weather Factors Section 2 Heat Transfer.

Radiation

• Radiation is the direct transfer of energy by electromagnetic waves.

Page 5: Chapter 2 Weather Factors Section 2 Heat Transfer.

Radiation

• You can’t see it, but you can feel it.

Page 6: Chapter 2 Weather Factors Section 2 Heat Transfer.

Radiation

• Examples: sun’s rays, campfire.

Page 7: Chapter 2 Weather Factors Section 2 Heat Transfer.

Conduction

• Conduction is the direct transfer of heat from one substance to another substance that it is touching.

Page 8: Chapter 2 Weather Factors Section 2 Heat Transfer.

Conduction

• Solids conduct heat better than liquids or gases (molecules are closer together).

Page 9: Chapter 2 Weather Factors Section 2 Heat Transfer.

Conduction

• Examples: walking on hot sand, touching a hot pot.

Page 10: Chapter 2 Weather Factors Section 2 Heat Transfer.

Convection

• Convection is the transfer of heat by the movement of a fluid.

Page 11: Chapter 2 Weather Factors Section 2 Heat Transfer.

Convection

• Examples: steam furnace, boiling water.

Page 12: Chapter 2 Weather Factors Section 2 Heat Transfer.
Page 13: Chapter 2 Weather Factors Section 2 Heat Transfer.

Heat Transfer in the Troposphere

• Radiation, conduction, and convection work together to heat the troposphere.

Page 14: Chapter 2 Weather Factors Section 2 Heat Transfer.

Heat Transfer in the Troposphere

1. Earth’s surface absorbs solar energy and is heated by radiation.

Page 15: Chapter 2 Weather Factors Section 2 Heat Transfer.

Heat Transfer in the Troposphere

2. Earth’s surface reradiates heat and warms the lower troposphere by conduction.

Page 16: Chapter 2 Weather Factors Section 2 Heat Transfer.

Heat Transfer in the Troposphere

3. The heated air molecules move faster making the warm air rise and the cold air sink.This creates convection currents which move heat throughout the troposphere.

Page 17: Chapter 2 Weather Factors Section 2 Heat Transfer.

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Earth’s surface is heated by radiation.

Earth’s surface reradiates heat.

Lower atmosphere is heated by

conduction.

Warm gases rise, cool gases sink = convection.

HEATING THE TROPOSPHERE

Page 18: Chapter 2 Weather Factors Section 2 Heat Transfer.

The Greenhouse Effect

•When Earth’s surface is heated, it radiates some of the energy back into the atmosphere.

Page 19: Chapter 2 Weather Factors Section 2 Heat Transfer.

The Greenhouse Effect

•Most of this energy can’t travel back into space so is absorbed by gases in the atmosphere.

Page 20: Chapter 2 Weather Factors Section 2 Heat Transfer.

The Greenhouse Effect

• These heated gases form a “blanket” around Earth that holds heat in the atmosphere.

Page 21: Chapter 2 Weather Factors Section 2 Heat Transfer.

The Greenhouse Effect

• Greenhouse effect is the process by which gases hold heat in the air.

Page 22: Chapter 2 Weather Factors Section 2 Heat Transfer.

The Greenhouse Effect

• The greenhouse effect is a natural process that keeps Earth’s atmosphere at a comfortable temperature for most living things.

Page 23: Chapter 2 Weather Factors Section 2 Heat Transfer.

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