Chapter Thirteen: Atmosphere and Climate Change
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Transcript Chapter Thirteen: Atmosphere and Climate Change
CHAPTER THIRTEEN: ATMOSPHERE
AND CLIMATE CHANGE
Section One: Climate and Climate
Change
What Factors Determine Climate?
Climate:
the long-term prevailing weather conditions at
a particular place bases upon records taken
Things
that determine climate
Latitude
Atmospheric circulation patterns
Oceanic circulation patterns
Topography
Solar and volcanic activity
Section One: Climate and Climate
Change
Latitude
The
distance from the equator measured in degrees
north or south of the equator
Equator
is at 0˚ latitude
North Pole is at 90˚ latitude north
South Pole is at 90˚ latitude south
Low latitudes: closer to the equator and receive more
sunlight
High latitudes: closer to the poles and receive less sunlight
Section One: Climate and Climate
Change
Section One: Climate and Climate
Change
Atmospheric Circulation
How the air moves across
the earth
Cold air sinks because it is
denser than warm air (
compresses and warms as
it sinks)
Warm air rises (expands
and cools as it rises)
Warm air holds more
water vapor than cold air
(causes fog, rain and
snow)
Section One: Climate and Climate
Change
Atmospheric Circulation
1.
2.
The sun warms the ground
and warms the air above
the ground
Warm air rises, and cooler
air replaces it (wind)
Areas that get more
sunlight have more warm
air that rises and cools.
When it cools it can hold
less water vapor so
precipitation occurs.
Therefore, the more sunlight
an area receives, the more
precipitation it gets.
Section One: Climate and Climate
Change
Atmospheric
Circulation
Prevailing
Winds:
winds that blow
predominately in one
direction throughout
the year
To
the right of the
Northern Hemisphere,
or to the left of the
Southern Hemisphere
Section One: Climate and Climate
Change
Oceanic Circulation Patterns
Water
holds a large amount of heat
Ocean current movement mostly caused by wind
El Niño: the short term periodic change in the location
of warm and cold water masses in the Pacific Ocean
Warm
water is pushed eastward, and rainfall follows
More rainfall in southern U.S. and South America
La
Niña: the water in the eastern Pacific Ocean is
cooler than usual
Section One: Climate and Climate
Change
Section One: Climate and Climate
Change
Topography
Topography:
local geography of the area
Mountains and mountain ranges influence precipitation
and temperature
Section One: Climate and Climate
Change
Solar and Volcanic Activity
Sun
Emits
UV radiation which produces more ozone
More ozone causes the earth to also warm
Volcanoes
Causes
sulfur dioxide to be released
Sulfur dioxide mixes with water vapor to make haze
Haze reflects sunlight and causes a global temperature
decrease
Section One: Climate and Climate
Change
Seasonal Changes in Climate
Seasons
Causes
are a result of the tilt of the Earth’s axis
a change in the amount of sunlight received
Section Two: The Ozone Shield
Ozone Layer
Ozone
Layer: an area
in the stratosphere
where ozone is highly
concentrated
Chemicals that cause
Ozone Depletion
CFCs:
human made
chemicals that destroy
ozone molecules
Also causes a problem
in the bird population
Section Two: The Ozone Shield
The Ozone Hole
Ozone
Hole: a thinning of stratospheric ozone that
occurs over the poles during the spring
Section Two: The Ozone Shield
The Ozone Hole
Polar
Stratospheric Clouds: high altitude clouds made
of water and nitric acid
Where
CFCs are converted to chlorine
Chlorines are broken apart by UV
Chlorines destroy the ozone
Section Two: The Ozone Shield
The Ozone Hole
Effects
More
on Humans, Animals, and Plants
UV radiation can pass through the atmosphere
UV damages DNA and can cause skin cancer
Kills phytoplankton
Kills amphibian eggs
Interfering with photosynthesis
Section Two: The Ozone Shield
Protecting the Ozone Layer
Montreal
Protocol: nations agreed to limit their
production of CFCs
United
States pledged to ban all substances that harm the
ozone by 2000
Section Three: Global Warming
The Greenhouse Effect
Greenhouse
Effect: caused by atmospheric gases radiating
and not absorbing hear causing the gradual warming of the
Earth
Greenhouse gases
Water Vapor
Carbon Dioxide
CFCs
Methane
Nitrous Oxide
Section Three: Global Warming
The Greenhouse Effect
Carbon
dioxide level
decrease in the
summer and increase in
the winter
Photosynthesis
removes
carbon dioxide from
the atmosphere
Carbon
dioxide levels
are steadily rising
Section Three: Global Warming
Global Warming
Global
Warming: the increase in the average
temperature at Earth’s surface
Section Three: Global Warming
Consequences of a
Warmer Earth
Melting Ice and Rising
Sea levels
Global Weather Patterns
Change
Human Health Problems
Droughts Killing Crops
Shifts Geographical
Ranges of Plants and
Animals
Section Three: Global Warming
Recent Findings
Temperature
has increase 0.6˚C
Snow cover and ice have decreased
Average global sea level has risen
Reducing the Risk
Kyoto
Protocol: required developed countries to
decrease emissions of carbon dioxide and other
greenhouse gases by an average of 5% below their
1990 levels by 2012