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Chapter 1.3 The Energy Cycle

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Page 1: Chapter 1.3 The Energy Cycle. The movement of energy into and out of the Earth system. Different than the previous cycles we have learned about. More

Chapter 1.3

The Energy Cycle

Page 2: Chapter 1.3 The Energy Cycle. The movement of energy into and out of the Earth system. Different than the previous cycles we have learned about. More

The Energy Cycle• The movement of energy into and out of

the Earth system.

• Different than the previous cycles we have learned about.

• More like a scale.– When you measure on a scale you want the

two sides to balance.– What is on one side should equal what is on

the other side.

Page 3: Chapter 1.3 The Energy Cycle. The movement of energy into and out of the Earth system. Different than the previous cycles we have learned about. More

The Energy Cycle Continued…

• The amount of energy entering a system should equal the amount of energy leaving a system.– If a system were to take in more energy than it

released, the system would increase in temperature.– If it released more energy than it took in,

temperatures would decrease.

• Because of this balance-scale nature, scientists refer to the energy cycle as the energy budget

• There are 3 main sources of energy in the energy budget: solar energy, geothermal energy, and tidal energy.

Page 4: Chapter 1.3 The Energy Cycle. The movement of energy into and out of the Earth system. Different than the previous cycles we have learned about. More

Solar Energy

• Most of the energy that enters the Earth system(99.985%) system comes from the Sun.

• Solar energy drives the winds, ocean currents, and waves.

• It is also the source of the energy that causes rocks to weather and soil to form.

Page 5: Chapter 1.3 The Energy Cycle. The movement of energy into and out of the Earth system. Different than the previous cycles we have learned about. More

Geothermal Energy

• Heat from within the Earth (0.013%)

• Geothermal energy is responsible for driving the tectonic plates, powering volcanoes, geysers and earthquakes, and also contributes to rock formation.

Page 6: Chapter 1.3 The Energy Cycle. The movement of energy into and out of the Earth system. Different than the previous cycles we have learned about. More

Tidal Energy

• Smallest part of the energy budget (0.002%)

• Resuts from the sun and moon’s pull on the Earth’s oceans.

• Powerful enough to slow Earth’s rotation because of the “tidal bulge”.

Page 7: Chapter 1.3 The Energy Cycle. The movement of energy into and out of the Earth system. Different than the previous cycles we have learned about. More

Maintaining the Balance

• Incoming energy must go somewhere.• About 40% of it is reflected back into

space.• Albedo

– The percentage of energy that is reflected without being changed.

– A forest has a low albedo (5-10% reflected).– A snow field has a high albedo (80-90%

reflected).

Page 8: Chapter 1.3 The Energy Cycle. The movement of energy into and out of the Earth system. Different than the previous cycles we have learned about. More

The Laws of Thermodynamics

• Energy follows predictable rules that explain what it will do.

• Thermodynamics is the branch of physics that deals with how heat energy is converted into other forms of energy.

• The laws of thermodynamics deals with how energy will flow.

Page 9: Chapter 1.3 The Energy Cycle. The movement of energy into and out of the Earth system. Different than the previous cycles we have learned about. More

First Law of Thermodynamics

• Energy can never be created or destroyed, only changed from one form to another.

• Example)– Solar energy is stored in plants which die and

eventually become fossil fuels.– Fossil fuels are burned at electrical power

plants and generate electricity, which can then power a light bulb.

Page 10: Chapter 1.3 The Energy Cycle. The movement of energy into and out of the Earth system. Different than the previous cycles we have learned about. More

Second Law of Thermodynamics

• When energy changes, it is converted from a more useful, more concentrated form to a less useful, less concentrated form.

• Unlike water which can convert from liquid to solid back to liquid without harm, energy cannot be recycled completely.

• Some energy will always be lost, usually in the form of heat.