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Convection and Radiation Consolidation

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Convection and Radiation Consolidation

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Review of concepts in chapters 8.5, 8.6 and 8.7

Created by

Ms. Hellewell
Ms. Hellewell
Canada

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Convection and Radiation Consolidation
 

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Convection and Radiation ConsolidationOnline version

Review of concepts in chapters 8.5, 8.6 and 8.7

by Ms. Hellewell
1

is the transfer of energy from one area of a to another by a circulating curren t

2

energy is energy that travels in the form of waves through empty spac e

3

is the transfer of by means of electromagnetic wave s

4

Convection does not occur in because the particles of a only

5

Uneven of liquid on a stove can produce

6

The air above the land is less ( ) than the air over the wate r

7

The air that rises high into the atmosphere over the land eventually moves over the , , , and then moves toward the agai n

8

Thunderstorms often form on , day s

9

Large amounts of energy are released as the water

10

Over millions of years , mantle rock sinks as mantle rock rises closer to

11

The amount of that reaches Earth's surface depends on a number of factors , such as the level of in the atmosphere , the time of day , the , and the

12

Energy that is the objec t

 
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