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  5. Seasons, Wind, And The Coriolis Effect
Seasons, wind, and the Coriolis Effect

Seasons, wind, and the Coriolis Effect

Assessment

Interactive Video

Science

10th Grade

Practice Problem

Medium

NGSS
MS-ESS2-6, MS-ESS1-1, MS-LS1-5

+4

Standards-aligned

Created by

Summer King

Used 2+ times

FREE Resource

15 questions

Show all answers

1.

SLIDE QUESTION

30 sec • Ungraded

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary purpose of global circulation?

To create ocean currents.

To redistribute heat across the Earth.

To cause the Earth to rotate.

To form landmasses and oceans.

Tags

NGSS.MS-ESS2-6

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How long does it take for Earth to complete one full orbit around the Sun?

A day

A month

A year

A decade

Tags

NGSS.MS-ESS1-1

NGSS.MS-ESS1-2

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary reason for Earth experiencing different seasons?

Earth's distance from the Sun changes significantly

Earth's rotation speed varies throughout the year

Earth's axis is tilted relative to its orbit

The Moon's gravitational pull affects Earth's orientation

Tags

NGSS.MS-ESS1-1

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

During winter in the Northern Hemisphere, what is true about the sunlight and day length?

Sunlight strikes directly, and days are long

Sunlight strikes at a shallow angle, and days are short

Sunlight strikes directly, and days are short

Sunlight strikes at a shallow angle, and days are long

Tags

NGSS.MS-ESS1-1

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the Coriolis Effect?

A force that makes water drain clockwise in the Northern Hemisphere.

The apparent curving of objects moving in a straight line when observed from a rotating frame of reference.

A phenomenon that only affects large-scale weather systems like hurricanes.

The actual physical force that causes objects to deviate from a straight path on Earth.

Tags

NGSS.MS-ESS2-5

NGSS.MS-ESS2-6

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Describe the movement of air within a Hadley cell.

Cold air rises at the poles and flows towards the equator.

Warm air rises at the equator, spreads towards the poles, cools, sinks, and returns to the equator.

Air flows randomly without a defined pattern.

Air sinks at the equator and rises at the poles.

Tags

NGSS.MS-ESS2-5

NGSS.MS-ESS2-6

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