

Earth's Climate and Solar Radiation
Interactive Video
•
Physics
•
9th - 10th Grade
•
Practice Problem
•
Hard
Patricia Brown
FREE Resource
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10 questions
Show all answers
1.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is the approximate amount of solar radiation that reaches the top of Earth's atmosphere?
2000 watts per square meter
1500 watts per square meter
1360 watts per square meter
1000 watts per square meter
2.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How does the angle of incoming solar radiation affect the amount received at the poles?
It has no effect on the amount of radiation received.
It increases the amount of radiation received.
It doubles the amount of radiation received.
It decreases the amount of radiation received.
3.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
Where is the peak of incoming solar radiation found?
At mid-latitudes
Evenly distributed across the globe
At the poles
At the equator
4.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What must happen for Earth to maintain thermal equilibrium?
Incoming radiation must exceed outgoing radiation.
Outgoing radiation must exceed incoming radiation.
Incoming and outgoing radiation must be balanced.
There should be no radiation exchange.
5.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is the relationship between incoming and outgoing radiation at the equator?
More outgoing than incoming
No incoming or outgoing radiation
More incoming than outgoing
Equal amounts of incoming and outgoing
6.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What happens to the temperature in regions with a net heat gain?
Temperature decreases
Temperature remains constant
Temperature increases
Temperature fluctuates randomly
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
Why haven't the equatorial regions continuously increased in temperature?
Heat is transported away from these regions.
They are in thermal equilibrium.
They have a natural cooling mechanism.
They receive less solar radiation over time.
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