Global Atmospheric Circulation Concepts

Global Atmospheric Circulation Concepts

Assessment

Interactive Video

Geography, Science

9th - 10th Grade

Hard

Created by

Emma Peterson

FREE Resource

The video provides an in-depth look at global atmospheric circulation, explaining how it affects climate zones and weather patterns. It covers the three main cells: Hadley, Ferrel, and Polar, and discusses the impact of latitudes on climate. The video also explains wind patterns and the Coriolis effect, offering a comprehensive understanding of how these elements interact to shape global climates.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary focus of the video tutorial?

Climate change

Global warming

Global atmospheric circulation

Ocean currents

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What does global atmospheric circulation help explain?

The development of human civilizations

The distribution of world climate zones and weather hazards

The formation of mountains

The creation of ocean currents

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which latitudes are considered major boundaries in global atmospheric circulation?

0, 30, 60, and 90 degrees

10, 20, 50, and 80 degrees

15, 45, 75, and 105 degrees

5, 25, 55, and 85 degrees

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which cell is located around the equator and is associated with tropical climates?

Ferrel cell

Hadley cell

Polar cell

Equatorial cell

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What type of weather is typically found in the Ferrel cell?

Hot and humid

Unstable and changeable

Stable and dry

Cold and icy

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens to air at 30 degrees latitude in the Hadley cell?

It moves towards the poles

It rises and cools

It sinks and warms

It remains stationary

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the Coriolis effect responsible for?

The sinking of air at the poles

The distortion of wind patterns due to Earth's rotation

The formation of deserts

The rising of air at the equator

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