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Why Do Different Places Have Different Climates

Why Do Different Places Have Different Climates

Assessment

Passage

Science

6th Grade

Practice Problem

Hard

Created by

Benjamin Gundlach

FREE Resource

10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the primary direction of prevailing winds in the United States?

North to South

East to West

West to East

South to North

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How do ocean currents affect climate?

They create storms over land.

They carry warm water toward the poles and cool water toward the equator.

They prevent air masses from forming.

They increase the amount of sunlight reaching the Earth.

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Why do cities near warm ocean currents receive heavy rainfall?

Warm ocean currents create strong winds.

Warm ocean currents increase evaporation, making air masses humid.

Warm ocean currents block cold air masses.

Warm ocean currents reduce the amount of sunlight.

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens to air masses as they rise over mountains?

They become warmer and drier.

They cool off and release precipitation.

They move faster and create storms.

They lose all their water vapor.

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the effect of latitude on climate?

It determines the amount of sunlight an area receives.

It controls the direction of prevailing winds.

It affects the elevation of a region.

It decides the type of ocean currents nearby.

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Why is the leeward side of a mountain dry?

Air masses lose moisture as they descend and warm up.

Air masses gain moisture from the ocean.

Air masses are blocked by the mountain.

Air masses become cooler and hold more water vapor.

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the rain shadow effect?

The process of air masses gaining moisture over warm oceans.

The dry conditions on the leeward side of a mountain.

The formation of storms due to colliding air masses.

The cooling of air masses as they rise over mountains.

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