Clouds and Precipitation
Air Masses and Fronts
Storms
Weather and Climate
Climate Factors
100

Which type of cloud produces thunderstorms?

Cumulonimbus

100

Cold, dry air from Canada creates this mass

Continental Polar

100

A funnel-shaped cloud that touches the ground.

Tornado

100

Scientists who study weather.

Meteroologists

100

Two main factors used to classify climate.

Temperature and Precipitation

200

Any type of water that falls from the clouds

Precipitation

200

When a cold air mass overtakes a warm air mass.

Cold Front

200

These storms form over warm ocean water.

Hurricanes

200

Day-to-day atmospheric conditions.

Weather

200

The uneven heating of Earth’s surface causes this movement of air.

Wind

300

These clouds are thin, wispy, and high in the sky.

Cirrus Clouds

300

When neither air mass moves.

Stationary Front

300

A violent disturbance in the atmosphere.

Storm

300

Long-term average conditions.

Climate

300

This effect causes moving air to curve due to Earth’s rotation.

Coriolis Effect

400

These clouds form a grey layer and often bring steady rain.

Stratus Clouds

400

When a warm air mass is trapped between two cold air masses.

Occluded Front

400

This causes a hurricane’s storm surge.

High Winds and low pressure

400

The difference between weather and climate.

Weather is short-term; climate is long-term

400

These winds are caused by land heating and cooling faster than water during the day and night.

Land and Sea Breezes

500

This process turns water vapor into liquid droplets.

Condensation 

500

These winds move weather across the U.S. from west to east.

Prevailing Westerlies

500

A forecast says a warm front is approaching—what weather conditions should you expect and why?

Warmer temperatures, gradual clouds, and steady precipitation because warm air rises over cold air.

500

The trapping of heat by Earth’s atmosphere.

Greenhouse Effect

500

Explain how uneven heating of Earth leads to global wind patterns.

Warm air rises at the equator, cool air sinks at the poles, creating convection currents and global winds.