An air parcel warms while its water-vapor content stays the same. What happens to its relative humidity?
2 Atmospheric Moisture and Cloud Formation Online Quiz Questions
Use this free practice quiz with 20 questions to review 2 Atmospheric Moisture and Cloud Formation, test your knowledge, and prepare for your next test or exam.
When water vapor condenses into liquid water, energy is released to the surrounding air.
- A
True
- B
False
The change from liquid water at a surface into water vapor is called .
Which statement best describes the dew point of an air parcel?
- A
The temperature at which air has no water vapor.
- B
The temperature at which water vapor begins evaporating from the ground.
- C
The temperature to which air must cool at constant pressure and water-vapor content to become saturated.
- D
The temperature at which air always produces precipitation.
Which air-mass type is generally warm and humid?
Cloud droplets shrink or disappear when exceeds condensation.
Which situations describe ways air can be lifted and contribute to cloud formation? Select all that apply.
- A
Sun-warmed air near the ground rises.
- B
Air is forced upward over a mountain.
- C
Liquid water at the surface changes into water vapor.
- D
Air flowing together near the surface is pushed upward.
What are the tiny particles, such as dust or sea salt, onto which water vapor condenses called?
The formation of a visible cloud guarantees that precipitation will fall from it.
- A
True
- B
False
Which statements about air masses and their effects are supported? Select all that apply.
- A
Air that remains over an ocean tends to become moist.
- B
Air that forms over land tends to be drier.
- C
Continental polar air is generally warm and humid.
- D
Maritime tropical air is generally warm and humid, and fronts can help force air upward.
Why can rising moist air cool as it moves higher in the atmosphere?
- A
Rising air encounters higher pressure, contracts, and warms.
- B
Rising air retains its volume and temperature until it reaches the ground again.
- C
Rising air encounters lower pressure, expands, and cools.
- D
Rising air loses water vapor immediately because pressure is lower.
Near-ground air cools overnight to its dew point. What may happen?
- A
The air must become completely dry.
- B
Water may condense near the ground as dew or fog.
- C
The air must warm until it is saturated.
- D
All clouds in the area must produce rain.
Explain how rising moist air can produce a visible cloud. Include what happens to the air as it rises and how cloud particles form.
An air sample warms while its water-vapor content stays constant. What happens to its relative humidity, and why?
- A
Relative humidity increases because the air can hold more water vapor.
- B
Relative humidity decreases because the air's saturation amount increases while its water-vapor content stays the same.
- C
Relative humidity stays the same because water-vapor content is unchanged.
- D
The air becomes saturated as soon as its temperature rises.
When water vapor condenses into liquid water, it absorbs energy from the surrounding air.
- A
True
- B
False
An air mass forms and remains over a warm tropical ocean. Which characteristics should it generally have?
- A
It is generally cold and dry because ocean air loses moisture.
- B
It is generally cold and humid because tropical regions cool the air.
- C
It is generally warm and humid because it forms over a warm ocean.
- D
It is generally warm and dry because oceans prevent evaporation.
A plant releases water vapor into the atmosphere. What is this process called?
Wind carries moist air toward a mountain, where the terrain forces the air upward. Which lifting mechanism is occurring?
- A
Orographic lifting
- B
Convergence
- C
Convection
- D
Frontal lifting
At constant pressure and with no change in water-vapor content, what is the name for the temperature an air sample must reach to become saturated?
Near the ground, winds from several directions flow toward the same area, and air begins to rise. Which process best explains this upward motion?
- A
Orographic lifting, because air is crossing high terrain
- B
Convection, because the air is warmed by the Sun
- C
Frontal lifting, because two air masses are meeting
- D
Convergence, because near-surface air flows together and is pushed upward
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