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Global Atmospheric Circulation and Climate Patterns
Presentation
•
Science
•
9th - 12th Grade
•
Practice Problem
•
Easy
Standards-aligned
Anthony Dilemme
Used 6+ times
FREE Resource
8 Slides • 11 Questions
1
2
3
Multiple Choice
Why is insolation (incoming solar radiation) stronger at the equator than at the poles?
Because the equator receives more direct sunlight due to the angle of the sun's rays
Because the equator is closer to the sun
Because the poles have more clouds
Because the equator has less atmosphere
4
5
Multiple Choice
Which of the following best describes the Hadley Cell?
Hot air rises at the equator, rains, and sinks dry at 30°
Cold, dense air sinks at the poles, weak easterlies
Weaker, pushed by Hadley & Polar cells
Air circulates only at the poles
6
7
8
Fill in the Blanks
The major deserts of the world are typically found at
9
10
Multiple Choice
Which wind belt is primarily associated with the Hadley Cell?
Trade Winds
Westerlies
Polar Easterlies
Monsoon Winds
11
Open Ended
Explain how the three major atmospheric cells (Hadley, Ferrell, and Polar) interact to influence global wind patterns and the distribution of deserts and rainforests.
12
13
Multiple Choice
What is a common misconception about why deserts form at the equator?
People think deserts form at the equator because it is hot, but the equator is actually a wet rainforest.
People think deserts form at the equator because of sinking cold air.
People think deserts form at the equator due to high albedo.
People think deserts form at the equator because of the Coriolis effect.
14
Labeling
Label the following global winds.
polar easterlies
horse latitudes
trade winds
westerlies
doldrums
15
Multiple Select
Which of the following are true about the Ferrell Cell?
It is weaker than the Hadley Cell
It is influenced by neighboring cells
It is responsible for the Trade Winds
It is found between 30° and 60° latitude
16
17
Fill in the Blanks
Insolation is strongest at the
18
Match
Trade Winds
Prevailing Westerlies
Polar Easterlies
0-30 degrees North and South
30-60 degrees North and South
60-90 degrees North and South
0-30 degrees North and South
30-60 degrees North and South
60-90 degrees North and South
19
Open Ended
How does the distribution of insolation (incoming solar radiation) across the Earth's surface influence global atmospheric circulation and climate patterns?
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