Define it!
True or False?
Clouds
Hemispheres & Weather
Wind, More Clouds & Weather
Grab Bag
100

The point at which the earth is farthest from the sun.

Aphelion

100

The weather changes from day to day, but the climate does not.

True (Climate is what you generally expect from a region, but weather is what actually happens from day to day.)

100

List the four main types of clouds.

Cirrus, Cumulus, Stratus, Lenticular

100

The length of days in the N. Hemisphere between June 21 and Sept. 22 is more OR less than 12 hours.

More than 12 hours
(In the N. Hemisphere, June 21 is the summer solstice – when it is pointed toward the sun & has the longest days.)

100

These differences cause wind.

Temperature differences

100

This term is an abbreviation for incoming solar radiation.

Insolation

200

The point at which the earth is closest to the sun.

Perihelion

200

The main factors that affect the earth’s weather are thermal energy and the uneven distribution of thermal energy.

False (There is a 3rd main factor – water vapor in the atmosphere.)

200

These clouds are at the top of the troposphere and are made of ice crystals. They have a wispy, feathery appearance.

Cirrus clouds

200

In the S. Hemisphere, day lengths are less than 12 hours but are increasing between:
June 21 &  Sept. 22 OR Sept. 23 & Dec. 21.

June 21 & Sept. 22 (In the S. Hemisphere, Sept. 22 is exactly 12 hours long.)

200

Wind patterns bend in different regions of the globe because of this.

The Coriolis effect

200

This is a mix between two types of clouds that are high in the sky, made of ice crystals, yet fluffier than cirrus.

Cirrocumulus

300

Imaginary lines that run north and south across the earth.

Lines of Longitude

300

A lenticular cloud found higher than normal is an altolenticular cloud.

True

300

These clouds are in flat layers, relatively close to the ground.

Stratus clouds

300

Day length in the N. Hemisphere between the summer solstice (June 21) and September 22 is:
Increasing OR Decreasing.

Decreasing

300

This is why there is not a constant stream of wind blowing from the poles to the equator.

Because air temperature changes as it changes latitude (east-west motion, not north-south as from poles to equator).

300

This is a type of cumulus cloud, often referred to as a thunder cloud, typically dark at the bottom and whiter at the top. It is caused by unusually large, upward moving wind currents.

Cumulonimbus

400

Imaginary lines that run east and west across the earth.

Lines of Latitude

400

Humidity is high in a continental polar air mass.

False
(Since it is continental, humidity is low.)

400

These clouds are fluffy and look like piles of cotton in the sky.

Cumulus clouds

400

Day length in the S. Hemisphere between June 21 and Sept. 22 is: Increasing OR
Decreasing.

 Increasing

400

You should aim a missile from Alaska in this direction to hit a target at the equator, south of you, if you ignore the effects of wind and air resistance.

Southeast (The ground in AK rotates slower than at the equator, so the missile’s path will bend west relative to the ground.)

400

This is a stratus cloud found higher than normal.

Altostratus

500

The way in which the rotation of the earth bends the path of winds, sea currents, and objects that fly through different latitudes.

Coriolis Effect

500

A continental polar air mass is cold.

True
(Since it is polar, the air mass is cold. )

500

These clouds are generally found in mountainous regions in pockets of low pressure. They are usually lens-shaped, or oval.

Lenticular clouds

500

The N. Hemisphere’s summer is during: Aphelion OR Perihelion.

Aphelion (This is when the N. Hemisphere is pointed at, but is farthest from, the sun.)

500

This is why it is not possible to have altocirrus clouds.

Cirrus clouds are at the highest altitudes, and “alto” means higher than usual.

500

This is a cumulus cloud found higher than normal.

Altocumulus

600

A large body of air with relatively uniform pressure, temperature, and humidity.

Air Mass

600

The humidity in a maritime tropical air mass is high.

True
(Since it is maritime, the humidity is high.)

600

Dark clouds tell us this might happen.

Precipitation

600

This type of weather front causes clouds to slowly build over a couple of days before a gentle, long rain begins. It then continues for about 20 hours.

Warm front (If it were a stationary front, the rain would last several days.)

600

High elevations cool faster at night than low elevations. Local wind caused by this will blow: from the mountain to the valley OR 2. from the valley to the mountain

From the mountain to the valley (Along the earth’s surface, winds blow from cold to warm.)

600

This is a mix between two types of clouds. It appears lower in the sky, with the layer appearance of stratus clouds, but it is also fluffy.

Stratocumulus

700

A boundary between two air masses.

Weather Front

700

A maritime tropical air mass is cold.

False
(Since it is tropical, the air mass is warm.)

700

Because there can be a lot of water in warm air, low, flat stratus clouds can easily turn into this type of dark, rain-producing cloud.

Nimbostratus (stratonimbus is also correct)

700

Over a few days you see cirrus clouds form, followed by stratus and nimbostratus clouds. In just a few hours, though, you see evidence of this type of front when dark cumulonimbus “thunder” clouds form.

Occluded front (The cloud progression described is caused by this type of front)

700

In less than a day, dark cumulonimbus clouds form and unleash a thunderstorm that lasts just a few hours. When the sky clears, you expect: Cooler OR Warmer temperatures than before the clouds first formed.

Cooler temperatures (The cloud pattern and resulting rain indicate a cold front.)

700

This is a mix between two types of clouds. It  appears high in the sky, and is made of ice crystals which are not blown apart by the wind. It appears fluffier than regular cirrus clouds.

Cirrocumulus

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