Chapter 1: Earth`s Changing Atmosphere
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Transcript Chapter 1: Earth`s Changing Atmosphere
Earths Atmosphere
Chapter 1:
Earth’s Changing Atmosphere
1.1 Earth’s Atmosphere Supports Life
Air – mixture of gases
Atmosphere – layer of air that surrounds the
Earth
1. Supports life and protects it
2. Keeps Earth warm
3. Transports energy
Characteristics of the
Atmosphere
Altitude – distance above sea level
The thickness or thinness of air is
measured by its density.
Density – the amount of mass in a given
volume of a substance
*Atmosphere’s density decreases as you
travel upward.
Gases in the atmosphere:
Nitrogen (N2) – 78%
Oxygen (O2) – 21%
Carbon Dioxide (CO2), argon, other gases – 1%
Nitrogen – promotes plant growth
Oxygen – animals and plants perform life
processes
Carbon dioxide – plants use to make food
Cycles – processes that are repeated
over and over again
1. Carbon Cycle :
a. Oxygen inhaled by animals, exhales
Carbon Dioxide (CO2)
b. CO2 taken in by plants, releases
Oxygen (O2)
2. Nitrogen Cycle :
a. tiny organisms (living things) remove N2 from
air, changes it into other chemicals and
returns it to the soil.
b. plants/animals use solids/liquids that contain
N2, then return to soil when they die & decay.
c. soil slowly releases N2 back in the air
3. Water Cycle:
a. Liquid water from oceans & lakes changes into
gas (evaporates) and enters atmosphere
b. Plants release water vapor from leaves
c. Liquid water falls back to atmosphere as
precipitation – rain, snow, sleet, or hail.
Sudden Changes:
**Volcanic eruptions, forest fires,
dust storms can cause changes in
the atmosphere
Volcanic Eruptions – shoots gases and ash into the
atmosphere.
Forest Fires – when forests burn, carbon that makes up
the trees enters the atmosphere as carbon dioxide.
Dust Storms – Adds huge amounts of particles to the
air.
Section 1.2: The Sun Supplies the
Atmosphere’s Energy
Two main things happen to sunlight
when it hits the Earth:
1. Sunlight is reflected – you see most
objects by reflected sunlight
2. Sunlight is absorbed – sand absorbs
sunlight & becomes warm
The Atmosphere Moves Energy
Processes that move Energy from place to place:
Radiation - Energy that travels distances in waves, can be
absorbed or reflected.
Conduction – Transfer of heat energy from one substance to
another by direct contact.
Convection – Transfer of energy by the motion of gas or liquid.
Movement of gases up and down. Warm air rises, cool air
sinks.
Example:
1. Radiation from sun warms the sand
2. Hot sand conducts energy to feet, air –or
anything that touches the sand
3. Warm air carries energy upward by
convection
1.3 - Gases in the Atmosphere
pgs. 22-25
Atmosphere effects light in 4 ways:
Absorb light
Reflect light
Let it pass through
Give off light – emit light
1.3 - Two types of radiation
(energy):
1. Ultraviolet radiation – waves of
energy you can’t see, causes
sunburn.
2. infrared radiation – warms the
materials that absorb it.
1.3 - Earth’s Protection:
Ozone layer – ozone gases in the stratosphere,
protects life on earth by absorbing harmful
ultraviolet rays from sun.
Greenhouse effect – traps heat – absorbs
gases (carbon dioxide, methane, etc.) and
keeps earth warm – allows heat to go back into
space.
Keeps Earth’s average surface temp. around
59 degrees.
Air Masses 3.1 – pgs. 79-82
Air Mass – large body of air. covers
thousands of miles.
Characteristics of Air Mass: depends on
where it forms and the temperature
1st word tells where it forms (land or
water)
2nd word tells temp. (near or far from
equator)
Four Types:
Continental Tropical – dry and warm
Continental Polar – dry and cool
Maritime Tropical – moist and warm
Maritime Polar – moist and cool
Air Masses move from West to East – away
from where they start.
Takes on characteristics of earth’s surface
as it moves.
Front – boundary between air masses.
fronts are often cloudy or stormy
3 types:
Cold Front – cold air mass pushes a warm air mass.
Produces cumulonimbus clouds. Brief heavy
storms.
Cool weather
Warm Front – warm air mass pushes cold air mass.
Hours of rain or snow – warm air
Stationary Front – Two air masses push against each
other and stop moving.
Becomes warm or cold when one air mass
advances.
Storms: 3.2 – 3.3 pgs. 87 – 97
Storms – 3.2
High pressure system – can bring clear
skies, calm air, gentle breezes
Low Pressure system – brings stormy
weather
Tropical Storm – low pressure system
that starts at the equator – winds 40 mph
(65k)
Hurricanes
Hurricane – low pressure system – winds
74 mph (120k)
Hurricane strike between Aug. thru Oct. –
when water gets warm enough – loses
strength when reaches land
Eye of Hurricane – center of storm, calm
winds
Storm Surge – pushes huge mass of
ocean water onto coastal area.
Winter storms result of two air masses
colliding.
NWS – National Weather Service – alerts
people to dangerous weather.
Blizzards – Blinding snowstorms, winds
35mph, occur in northern and central
U.S.
Ice storms – rain falls onto freezing cold
ground.
covers everything with ice
Severe Storms – 3.3
Lightning – spark of electricity
Air around lightning is heated briefly to
temp. hotter than the surface of sun
Thunder – sharp wave of heated air that
travels away from lightning
Thunderstorm – storm with lightning and
thunder – get energy from humid air.
Effects of Thunderstorms:
Flash floods, winds, hail, lightning
Tornado – violently rotating column of air
– occurs mostly in spring - unpredictable