Mountain Weather and Humidity Concepts

Mountain Weather and Humidity Concepts

Assessment

Interactive Video

Science

9th - 10th Grade

Hard

Created by

Patricia Brown

FREE Resource

Professor Courter discusses a math problem involving temperature and humidity at different altitudes on a mountain. The video explains how relative humidity and dew point temperature are determined by the presence of clouds. It also covers the effects of air movement on the leeward side of a mountain, using the Big Island of Hawaii as a practical example.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the temperature at the top of the mountain?

72 degrees

66.5 degrees

39 degrees

22.5 degrees

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

At what altitude on the windward side is the relative humidity 100%?

8000 feet

11000 feet

3000 feet

6000 feet

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Why is the relative humidity 100% at 8221 feet on the windward side?

Because it is below the condensation level

Because there is no cloud

Because it is above the condensation level

Because it is at sea level

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the dew point temperature at 6000 feet on the windward side?

72 degrees

22.5 degrees

39 degrees

66.5 degrees

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How does the dew point temperature relate to air saturation?

It is always lower than the air temperature

It is always higher than the air temperature

It is the same as the air temperature when saturated

It is unrelated to air saturation

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Where is the relative humidity higher on the leeward side?

At 6000 feet

At sea level

At 8000 feet

At 3000 feet

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens to the air temperature as it descends on the leeward side?

It fluctuates

It cools down

It remains constant

It warms up

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