+ All Categories
Home > Documents > 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100...

200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100...

Date post: 28-Mar-2015
Category:
Upload: tavion-arness
View: 228 times
Download: 2 times
Share this document with a friend
Popular Tags:
51
200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read? Say What?
Transcript
Page 1: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

200

300

400

500

100

200

300

400

500

100

200

300

400

500

100

200

300

400

500

100

200

300

400

500

100

Energy Transfer

AtmosphereGlobal

WarmingDid you

read?Say What?

Page 2: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Energy that flows from an object of higher temperature to an object of lower temperature

Page 3: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

HEAT

Page 4: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

50 % of the sun’s energy is either directly or indirectly _____________ by Earth’s surface.

Page 5: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

ABSORBED

Page 6: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Heat is transferred through the atmosphere in three ways. Name them.

Page 7: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

RadiationConvectionConduction

Page 8: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

What type of energy from the sun warms your face?

Page 9: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

RADIANT

Page 10: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

The transfer of energy when molecules bump into each other. This is the reason why your feet get hot on the sandy beach on a hot August day.

Page 11: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

CONDUCTION

Page 12: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Earth’s early atmosphere contained ________ and _______ from erupting volcanoes.

Page 13: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Carbon Dioxide and

Nitrogen

Page 14: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

What protective layer in the atmosphere allowed green plants to flourish?

Page 15: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

OZONE LAYER

Page 16: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Describe the composition of Earth’s atmosphere.

Page 17: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

NitrogenOxygenArgon

Carbon DioxideTrace elements

Solid, liquid, and gas particles

Page 18: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

True or false. There are solid particles in the atmosphere. If it’s true, explain the statement. If it’s false, explain why it is false.

Page 19: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

True. There are pollen and dust particles in the

atmosphere.

Page 20: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Put the layers of the atmosphere in the right order starting with the one closest to Earth’s surface.

Page 21: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

TroposphereStratosphereMesosphere

ThermosphereExosphere

Page 22: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Name a greenhouse gas.

Page 23: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

MethaneCarbon Dioxide

Water vapor

Page 24: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Too much exposure to ____________ radiation can cause skin cancer.

Page 25: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

ULTRAVIOLETRADIATION

Page 26: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Once used in refrigerators, air conditioners, and hair sprays, these molecules can break up ozone molecules in the atmosphere.

Page 27: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

CFCs or

Chlorofluorocarbons

Page 28: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Which part of a CFC molecule could break apart a molecule of ozone?

Page 29: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

The chlorine atom

Page 30: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Explain why during the day the radio only receives AM

radio stations from a nearby city, while at night, you are able to hear AM

radio stations from a distant city.

Page 31: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Ionosphere – The layer of electrically-charged particles between the mesosphere and the thermosphere.

Page 32: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Heated air at the equator is _____dense than the cold air near the Poles.

Page 33: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

LESS

Page 34: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Warmer, less dense air will(rise above or sink below)colder, denser air.

Page 35: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

RISE ABOVE

Page 36: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

This effect is caused bythe rotation of earth which results in air and waterappearing to move rightnorth of the equator and to the left south of the equator.

Page 37: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Coriolis Effect

Page 38: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Daily Double:

The windless, rainy zone by the equator is known as the

________.

Page 39: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

DOLDRUMS

Page 40: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Jet pilots and even airlines take advantage of these strong winds blowing near the top of the troposphere.

Page 41: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

JET STREAMS

Page 42: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

These winds are created when solar radiation warms the land more so than the water.

Page 43: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Sea breezes

Page 44: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Why doesn’t life exist on Mars or Venus?

Page 45: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Venus – gases in its atmosphere trap the sun’s energy resulting in temperatures being extremely hot on its surface.

Mars – extremely cold. Atmosphere is too thin to hold in the sun’s energy.

Page 46: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

True or False.

The water cycle affectsEarth’s climate.

Page 47: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

TRUE

Page 48: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

DAILY DOUBLE

Water vapor turns into liquid water

Page 49: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

CONDENSATION

Page 50: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

Describe how altitude affects the amount of atmospheric pressure you experience.

Page 51: 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 200 300 400 500 100 Energy Transfer Atmosphere Global Warming Did you read?

The higher in elevation you go, there is less atmospheric pressure because there are

less air molecules.


Recommended