Layers of Atmosphere Slides for Earth Environmental.ppt

This document is used in my Earth Environmental class to discuss the atmosphere layers and related topics.

1. LAYERS OF GASES SURROUNDING EARTH LAYERS OF GASES SURROUNDING EARTH
Atmosphere

2. % of gases in the atmosphere% of gases in the atmosphere
•78% Nitrogen
•21% Oxygen
•0.04% Carbon dioxide, CO
2
•0.4% water vapor

3. •Gravity pulls the gases of atmosphere toward
earth’s surface & holds them
•Most gases are found within 32 km (20 miles)
•Air (atmospheric) pressure – pressure exerted
on a surface by the atmosphere
•Less air at higher altitudes means less weight
pushing down = Air pressure is HIGHER at
LOWER altitudes & Lower at Higher altitudes

4. 5 Layers 5 Layers
of the Atmosphereof the Atmosphere
Layers are divided by Layers are divided by
TEMPERATURE!TEMPERATURE!

5. 1) Troposphere1) Troposphere
•Layer closest to the Earth (sea level to 10 miles)
•Contains 90% of the atmosphere’s mass,
making it the MOST DENSE LAYER!
•Temperature decreases as altitude increases
•Contains almost all of the CO2, water vapor,
clouds, weather, air pollution

6. 1) Troposphere1) Troposphere
Warmest
temperatures at the
bottom
Temperatures
decrease with height
Top layer is called the
tropopause

7. 2) Stratosphere2) Stratosphere
•Above Troposphere (10-30 miles)
•Very little water vapor or clouds
•Absorbs UV radiation from sun
•Temps increase as altitude
increases
•Contains Ozone: made of 3 oxygen
molecules
(not the usual 2)

8. OzoneOzone
Center region of
stratosphere is called the
OZONOSPHERE
Ozone molecules
ABSORB UV rays from
the Sun
Temperature increases

9. OzoneOzone
•Ozone layer is reduced by chemical interaction with
CFCs (Chlorofluorocarbons) which are released from
refrigerators, air conditioners, and aerosol cans.

10. 3) Mesosphere3) Mesosphere
•Sits on top of stratopause
•Temperatures decrease with
height- it is the coldest layer
of the atmosphere reaching -130 F
–(-93
o
C)
•Protects Earth’s surface from meteoroids

11. 4) Thermosphere4) Thermosphere
•layer above Mesosphere
•Little atmosphere, very low density
•Temperatures increase with altitude
reaching 3,632
o
F due to decreasing air

12. 4) Thermosphere4) Thermosphere
•Contains Ionosphere- lower layer of
thermosphere, energy from Sun tears
gasses apart, electrically charging
particles
•This releases lights that we call the Aurora
borealis!

13. 5) Exosphere5) Exosphere
•Exosphere - uppermost layer
•Space shuttle orbits here
•Temperature increases with altitude
before blending into space
•Composition of Oxygen, Nitrogen, and
Helium

14. Solar Energy Solar Energy
•Our atmosphere is heated by the transfer of
energy from the sun in several ways:
•A) radiation – all forms of energy from waves
in space ex. radio, infrared, visible, ultraviolet
(UV), & X-rays
•B) conduction – when heat (E) is transferred
from 1 object to another by direct contact
•C) convection – the movement of GASES or
LIQUIDS when they are heated unevenly

15. •Most solar energy that reaches the Earth’s
atmosphere is ABSORBED by the surface
•Solar – energy from the sun is trapped in
the lower atmosphere by “greenhouse
gases” & prevented from escaping back
into space
•Greenhouse gases:
–CO – burning of wood & fossil fuels
–CO
2
– use of coal, natural gas, & oil
–CH
4 – farming and industrial activity

16. Global WarmingGlobal Warming
•Energy trapped by gases in our
atmosphere has caused the overall global
temperature of Earth to rise over the past
100 years.
•Human activity such as burning fossil fuels
& deforestation, may be increasing the
levels of greenhouse gases in our
atmosphere

17. WindWind
•Wind- movement of air due to uneven
atmospheric pressure
•Coriolis Effect – rotation of Earth causes
surface winds in the Northern Hemisphere
to turn to the LEFT and surface winds in
the Southern Hemisphere to the RIGHT

18. •When air gets warmer it becomes less
dense, as it rises it begins to move toward
the POLES.
•The longer it is high in the air, it becomes
More DENSE and SINKS down to the
Earth’s surface again where it is warmed.
•Air flowing from the equator completes
Continuous looping patterns of flow called
“wind cells.”