
Global Wind Patterns and Effects
Interactive Video
•
Geography
•
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 are the primary convection cells responsible for global wind patterns?
Hadley, Ferrel, and Polar cells
Equatorial, Tropical, and Arctic cells
Doldrums, Horse, and Cyclone cells
Trade, Westerly, and Easterly cells
2.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
Why do deserts commonly form at around 30 degrees latitude?
As a result of the Coriolis Effect
Because of high solar density
Because of descending dry air from Hadley cells
Due to the presence of polar easterlies
3.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How do Ferrel cells contribute to global wind patterns?
By generating trade winds
By creating a strong convection cell at the equator
By acting as a mixing zone between Hadley and Polar cells
By causing air to rise at the poles
4.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What is the Coriolis Effect?
A force that causes objects to move in a straight line
An effect that makes objects appear to curve due to Earth's rotation
A phenomenon that causes hurricanes to form
A process that affects the speed of Earth's rotation
5.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How does the Coriolis Effect influence hurricanes?
It causes hurricanes to form at the equator
It makes hurricanes spin in opposite directions in different hemispheres
It prevents hurricanes from forming in the southern hemisphere
It increases the speed of hurricane winds
6.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What are the doldrums?
Regions with strong trade winds
Regions with constant westerly winds
Areas with little to no wind near the equator
Zones of high pressure and dry air
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
Why are the horse latitudes known for having little wind?
Because of the descending air from Hadley cells
As a result of the mixing of Ferrel and Polar cells
Because of the strong influence of the Coriolis Effect
Due to the presence of high-pressure systems
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