Mrs. Paulus
Home
Biology
Anatomy
General Science II
8 Science
7 Science
Wellness 8
Genetics Vocabulary
Home
Biology
Anatomy
General Science II
8 Science
7 Science
Wellness 8
Genetics Vocabulary
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Figure G
Atmosphere Review
Atmosphere Review
Use Chapter 15. This is worth 20 points.
Screenshot to include BOTH score and name. Turn in on Edmodo. SOME TERMS WILL BE USED MORE THAN ONCE!!!
Our atmosphere is approximately 78%
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
, 21%
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
, and 1% other gases.
Use Figure A to identify each layer:
1 -
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
2 -
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
3 -
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
4 -
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
What is the layer above 4?
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
The layer where weather occurs is the
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
.
The white area marked 5 is called the
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
, while the yellow area marked 6 is the
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
.
The different layers of the atmosphere are determined by how the
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
changes. In the troposphere the temperature
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
as you go up. In the stratosphere the temperature
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
as you go up. As you go up in the atmosphere the atmospheric (air) pressure
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
.
The ozone layer is extremely important to Earth because it protects us from
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
. It has been weakened by
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
.
Heat flows from
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
to
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
objects. It is transferred three ways in the atmosphere. Energy transferred by waves is
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
. Heat transferred by the flow of materials is
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
. Heat transferred by direct contact is
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
. Identify the transfer shown in: Figure B –
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
… Figure C –
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
… Figure D –
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
.
All of the waters on Earth are part of the
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
. The waters all go through changes in the
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
. Identify the steps of this cycle using Figure E. Process X-
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
, process Y-
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
, and process Z-
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
.
Winds are caused by the heating of the air by the sun. Warm air is
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
dense than cold air. This causes different areas of
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
. Identify the different global winds in Figure F:
Q –
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
R –
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
S –
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
T –
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
Narrow belts of strong winds at the top of the troposphere are the
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
. Areas near large bodies of water will experience a
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
breeze at night and a
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
breeze during the day. This happens because the water and land gain and lose
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
at different rates.
Look at Figure G. The airplane appears to curve due to the
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
. This is caused by the Earth's
CFCs
air pressure
colder
condensation
conduction
convection
coriolis effect
decreases
doldrums
evaporation
exosphere
heat
hotter
hydrosphere
increases
ionosphere
jet stream
land
less
mesosphere
nitrogen
oxygen
ozone layer
polar easterlies
precipitation
radiation
rotation
sea
stratosphere
temperature
thermosphere
trade winds
troposphere
ultraviolet radiation
water cycle
westerlies
.
Check
OK
Home
Biology
Anatomy
General Science II
8 Science
7 Science
Wellness 8
Genetics Vocabulary