energy transfer in the atmosphere chapter 4 - section 2 pgs 99 - 102

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Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

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Page 1: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

Energy Transfer in the Atmosphere

Chapter 4 - Section 2Pgs 99 - 102

Page 2: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

Energy from the SunEnergy from the SunMost of the EarthMost of the Earth’’s s energy comes from the energy comes from the sunsun

35% is reflected back 35% is reflected back into spaceinto space

15% is absorbed by the 15% is absorbed by the atmosphereatmosphere

50 % is absorbed by the 50 % is absorbed by the earthearth’’s surfaces surface

Page 3: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

HeatHeat

energy that flows from an object with a higher temperature to an object with a lower temperature

Page 4: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

HeatHeatHeat always moves from a warmer place to a cooler place.

Hot objects in a cooler room will cool to room temperature.

Cold objects in a warmer room will heat up to room temperature.

Page 5: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

Question?Question?

If a cup of coffee and a red popsicle were left on the table in this room what would happen to them? Why?

Page 6: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

AnswerAnswer

The cup of coffee will cool until it reaches room temperature. The popsicle will melt and then the liquid will warm to room temperature.

Page 7: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

Heat TransferHeat TransferThe Earth is heated by energy from the sun

This heat is then transferred through the atmosphere by radiation, conduction or convection

Page 8: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

RadiationRadiation energy transferred in the form of waves or rays

Page 9: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

ConductionConduction The transfer of heat that occurs when molecules bump into each other

Energy transferred through direct contact

Page 10: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

ConvectionConvection Transfer of heat by the flow of material

Convection circulates heat throughout the atmosphere

Page 11: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

ExampleExample

Page 12: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

The Water CycleThe Water CycleHydrosphere - all the waters on Earth

The constant cycling of water in the atmosphere and hydrosphere that plays an important role in determining weather patterns and climate types

Page 13: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

The Water CycleThe Water Cycle Evaporation - change of matter from a liquid to a gas state

Condensation - change of matter from a gas to a liquid state

Precipitation - rain, snow, sleet or hail that falls to the ground

Transpiration - giving off of moisture through the surface of leaves or other plant parts

Groundwater- water that collects and flows under ground

Runoff- water that runs along the surface of land into a body of water

Page 14: Energy Transfer in the Atmosphere Chapter 4 - Section 2 Pgs 99 - 102

The Water CycleThe Water Cycle

Adding or subtracting heat keeps the cycle Adding or subtracting heat keeps the cycle goinggoing