Narrow belts of high-speed winds that blow from east to west between 7km and 16km above Earth's surface

Narrow belts of high-speed winds that blow from west to east, between 7km and 16km above Earth's surface

The movement of air over short distances that can blow from any direction, depending on features of the area

The apparent curving of the path of a moving object from an otherwise straight path due to Earth's rotation

The movement of air caused by differences in air pressure

The apparent curving of the path of a moving object from an otherwise straight path due to Earth's rotation

The movement of air over short distances that can blow from any direction, depending on the features of the area

Narrow belts of high-speed winds that blow from west to east, between 7km and 16km above Earth's surface

When wind blows south

When wind blows east

Wind systems that occur far away from Earth's surface

Wind systems that occur at or near the Earth's surface

Wind that spirals in a circular motion

Wind systems that occur at or near the Earth's surface

The movement of air over short distances that can blow from any direction, depending on the features of the area

The movement of air over long distances that can only blow from one direction

True

False

The place in which air, instead of moving in one circle between the equator and the poles, air moves in smaller circular patterns

The place in which water cools down

The place in which water warms up

The place in which there is only high pressure

Polar Easterlies

Westerlies

Trade Winds

Winds on the top and bottom of the Earth and blow between the poles by 60 degrees latitude in both hemispheres ( Also curve to the east )

Winds on the top and bottom of the Earth and blow between the poles by 60 degrees latitude in both hemispheres ( Also curve to the west )

Winds between 30 degrees and 60 degrees latitude in both hemispheres ( Also curve to the east )

Winds that blow between 30 degrees latitude in both hemispheres

True

False

True

False

Fast/Rapid

Curvy

Dull/Sluggish

Where the air starts moving at 30 degrees latitude and rises

Where the air stops moving at 30 degrees latitude and sinks

Where trade winds in both hemispheres meet in a calm area around the equator

Where trade winds in both hemispheres meet in a calm area around the equator

Where trade winds in both hemispheres meet in a rapid area around the equator

Sea Breezes

Tree Breezes

Land Breezes

When during the day, the air above the land becomes warmer than the air above water, so that the colder, denser air over the water flows towards the land and pushes the warm air on the land upward.

When at night, the cooler air on land causes a higher pressure zone over the land, which makes wind blow from the land up towards the water.

When at night, the cooler air on land causes a higher-pressure zone over the land, which makes wind blow from the land towards the water.

When during the day, the air above the land becomes warmer than the air above water, so that the colder, denser air over the water flows towards the land and pushes the warm air on the land upward.

At nightfall, the air along the mountain slopes cool and move into the valley

During the day, the sun warms the air along the mountain slopes faster than the air in the valleys, which results in uneven heating and air pressure.

During the day, the sun warms the air along the mountain slopes faster than the air in the valleys, which results in uneven heating and air pressure.

At nightfall, the air along the mountain slopes cool and move up into the valley