Air stability - condensation and precipitation

Air stability - condensation and precipitation

11th - 12th Grade

15 Qs

quiz-placeholder

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Air stability - condensation and precipitation

Air stability - condensation and precipitation

Assessment

Quiz

Geography

11th - 12th Grade

Medium

Created by

Rhys Williams

Used 6+ times

FREE Resource

15 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens to temperature with increasing altitude through the troposphere?

It increases

It decreases

It remains constant

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Why is Earth's surface warmer than the atmosphere?

Molecules are more tightly packed in the solids and liquids near and on the surface

Molecules are more tightly packed in the gases of the atmosphere

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens to atmospheric pressure as altitude increases?

It increases

It decreases

It remains constant

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens to parcels of air as they rise through the troposphere?

Increase in volume and decrease in temperature

Increase in volume and increase in temperature

Decrease in volume and increase in temperature

Decrease in volume and decrease in temperature

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the dry adiabatic lapse rate (DALR)?

Rate at which a parcel of dry air (less than 100% humidity) warms as it rises

Rate at which a parcel of dry air (less than 100% humidity) cools as it rises

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the value of the DALR?

10C increase for every 1000m above sea level

10C decrease for every 1000m above sea level

7C increase for every 1000m above sea level

7C decrease for every 1000m above sea level

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the saturated adiabatic lapse rate (SALR)?

Rate at which a parcel of dry air (less than 100% humidity) warms as it rises

Rate at which a parcel of dry air (less than 100% humidity) cools as it rises

Rate at which a parcel of saturated (wet) air (100% humidity) cools as it rises

Rate at which a parcel of saturated (wet) air (100% humidity) warms as it rises

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