Chapter 12

Chapter 12

Assessment

Quiz

Created by

S Marts

Mathematics

2nd Grade

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15 questions

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1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

_____ is the process by which liquid water changes into water vapor.

condensation

sublimation

melting

evaporation

freezing

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Mixing ratio, relative humidity, and dew-point temperature are all ways of measuring the amount of ________ in the air.

water vapor

condensation level

vapor pressure

convergence

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

The ________ is the temperature to which a parcel of air would need to be cooled in order to reach saturation.

water vapor

dew point

parcel

condensation level

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which of the following statements about relative humidity is true?  (Select all that apply.)

Increasing water vapor content increases relative humidity and increasing temperature decreases relative humidity.

Increasing wind speed increases relative humidity.

Increasing altitude will decrease humidity

Increasing pressure increases relative humidity.

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

The cooling or warming of air that occurs because air is allowed to expand or is compressed, not because heat is added or subtracted is called ________.

sensible heat

wet adiabatic rate

adiabatic temperature changes

dry adiabatic rate

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What condition is required for cloud formation in the atmosphere?

A rising parcel of air attains a relative humidity of 50 percent.

A descending parcel of air reaches its dew-point temperature.

A rising parcel of air reaches its dew-point temperature.

A rising parcel of air reaches the edge of Earth’s atmosphere.

A descending parcel of air reaches Earth’s surface.

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How does frontal lifting cause air to rise?

When warm and cold air masses separate, the warmer, less dense air rises over the cooler, denser air.

When warm and cold air masses collide, the warmer, less-dense air acts a barrier over which the cooler, denser air rises.

When warm and cold air masses collide, the cooler, denser air acts a barrier over which the warmer, less-dense air rises.

When warm and cold air masses collide, the warmer, denser air acts a barrier over which the cooler, less-dense air rises.

When warm and cold air masses separate, the cooler, denser air rises over the warmer, less dense air.

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