Atmospheric Science Concepts Assessment

Atmospheric Science Concepts Assessment

Assessment

Interactive Video

Physics, Science, Chemistry

9th - 12th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video tutorial explains how the Earth's atmosphere reacts to sunlight, focusing on the concept of heat capacity. It discusses how temperature changes throughout the day, the mass and moles of air in a column, and the calculation of internal energy and heat required for temperature changes. The tutorial aims to understand why temperatures rise in the morning and cool down in the evening, emphasizing the role of heat capacity.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary factor that causes the temperature to rise in the morning?

The incoming sunlight

The movement of tectonic plates

The rotation of the Earth

The gravitational pull of the moon

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What does the heat capacity of the Earth's atmosphere determine?

The speed of wind

The amount of sunlight received

The temperature change with added heat

The color of the sky

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the atmospheric pressure at sea level in Pascals?

1013 Pascals

1300 Pascals

101300 Pascals

13000 Pascals

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How is the mass of a column of air calculated?

By multiplying the weight by the acceleration due to gravity

By subtracting the weight from the acceleration due to gravity

By dividing the weight by the acceleration due to gravity

By adding the weight and the acceleration due to gravity

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the average molar mass of air?

8 grams per mole

32 grams per mole

29 grams per mole

18 grams per mole

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How many moles of air are in a column with a cross-sectional area of one square meter?

1,000,000 moles

100,000 moles

356,000 moles

500,000 moles

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the heat capacity at constant volume for diatomic molecules in the atmosphere?

3/2 times the universal gas constant

5/2 times the universal gas constant

7/2 times the universal gas constant

9/2 times the universal gas constant

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