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Stratospheric Ozone Depletion

Authored by Lisa Thompson

Science

12th Grade

NGSS covered

Stratospheric Ozone Depletion
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15 questions

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1.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Ozone in the stratosphere is formed in two steps. The first involves breaking down oxygen (O2) by

particulates

carbon dioxide

ozone

sunlight

Tags

NGSS.HS-PS4-3

NGSS.HS-PS1-5

2.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

The ozone hole is over which place?

Antartica

South America

Aftrica

Arctic

3.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

What important international agreement limited/banned CFCs in many countries?

Clean Water Act

Clean Air Act

Montreal protocol

International Act of Ozone

4.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Media Image

Layer of reactive gas at 20-30km above the Earth (15-20km at the poles) absorbing UV radiation

Greenhouse Gases

Troposphere

Stratosphere

Ozone Layer

Tags

NGSS.HS-PS4-3

5.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Media Image

The breakdown of stratospheric ozone;

I. Can originate from the emission of chlorofluorocarbons (CFCs).

II. Is catalyzed through a free chlorine (Cl) atom.

III. Prevents all UV rays from reaching the earth’s surface.

I only

III only

I,&II

I,II,& III

6.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Media Image

How do CFCs affect ozone production?

UV radiation frees a chlorine atom, which breaks down ozone.

Infrared radiation frees a chlorine atom, which breaks down ozone.

UV radiation frees a fluorine atom, which breaks down ozone.

Infrared radiation frees a chlorine atom, which breaks down ozone.

Tags

NGSS.HS-PS1-5

7.

MULTIPLE CHOICE QUESTION

1 min • 1 pt

Media Image

Though CFC production has been curtailed, the threat to upper atmosphericozone continues because CFCs

become harmless quickly.

destroy ozone for only a short time.

persist but stop destroying ozone.

persist and continue to destroy ozone for decades.

Tags

NGSS.HS-ESS3-6

NGSS.HS-ESS2-2

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