Humidity and Dew Point Concepts

Humidity and Dew Point Concepts

Assessment

Interactive Video

Science

9th - 10th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video tutorial explains humidity, its dependence on temperature, and the concept of relative humidity. It compares warm and cold air's capacity to hold water vapor and describes how relative humidity changes throughout the day. Methods to alter relative humidity by adding water vapor or changing temperature are discussed. The video also covers measuring humidity using devices like the sling psychrometer and explains the dew point's significance in weather reports.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary factor that determines the capacity of air to hold water vapor?

Altitude

Wind speed

Air temperature

Air pressure

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How is relative humidity expressed in weather reports?

In degrees Celsius

As a percentage

As a fraction

In millimeters

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens to relative humidity as air temperature increases during the day?

It fluctuates randomly

It remains constant

It decreases

It increases

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which of the following can increase relative humidity without changing the temperature?

Increasing air pressure

Increasing wind speed

Decreasing altitude

Adding more water vapor

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary function of a sling psychrometer?

To measure temperature

To measure wind speed

To measure air pressure

To measure humidity

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What does a small difference between wet and dry bulb temperatures indicate?

High humidity

High wind speed

Low humidity

Low air pressure

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the dew point?

The temperature at which air pressure is highest

The temperature at which air pressure is lowest

The temperature at which wind speed is highest

The temperature at which air becomes saturated

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