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Greenhouse Effect & Global Warming The Earth s Atmosphere

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Greenhouse Effect & Global Warming The Earth s Atmosphere 2 elements Nitrogen (N2) and Oxygen (O2) make up 99% of the volume of clean, dry air. – PowerPoint PPT presentation

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Title: Greenhouse Effect & Global Warming The Earth s Atmosphere


1
Greenhouse Effect Global Warming
2
The Earths Atmosphere
  • 2 elements Nitrogen (N2) and Oxygen (O2) make up
    99 of the volume of clean, dry air.
  • Remaining 1 of gases are inert gaseous elements
    like Argon. These gases are sometimes called
    Trace gases and are often referred to as the
    Greenhouse Gases- ( they function much like the
    glass plates found on a greenhouse used for
    growing plants.) http//www.rcn27.dial.pipex.com/c
    loudsrus/images/atmosc20compos.jpg

3
Earths Atmosphere
  • composed of gases (like CO2 and CH4 ) of just the
    right types in the right amounts to warm the
    earth to temperatures suitable for life.
  • The effect of the atmosphere to trap heat is the
    "greenhouse effect."www.solcomhouse.com

4
The Goldilocks Principle
  • "Venus is too hot, Mars is too cold, and Earth is
    just right.
  • Earth has an average surface temperature
    comfortably between the boiling point and
    freezing point of water, and is suitable for our
    life.
  • This cannot be explained by simply suggesting
    that our planet orbits at just the right distance
    from the sun to absorb just the right amount of
    solar radiation.
  • Our moderate temperatures are also the result of
    having just the right kind of atmosphere.

5
Goldilocks
  • A Venus-type atmosphere would produce hellish,
    Venus-like conditions on our planet a Mars
    atmosphere would leave us shivering in a
    Martian-type deep freeze. http//www.ucar.edu/lear
    n/1_3_1.htm

6
Our atmosphere is Just Right
  • Parts of our atmosphere (greenhouse gases-like
    CO2) act as an insulating blanket of just the
    right thickness, trapping sufficient solar energy
    to keep the global average temperature in a
    pleasant range.
  • The Martian blanket is too thin, and the Venusian
    blanket is way too thick!

7
Global Insulators
  • Greenhouse gases, like water vapor (H20 ), carbon
    dioxide (CO2) and methane (CH4), all act as
    effective global insulators.
  • Lets see How

8
Energy from the Sun
  • Absorbed by land, oceans, and vegetation at the
    surface, visible light is transformed into heat
    and re-radiates in the form of invisible infrared
    radiation.
  • If this was ALL that happened, then during the
    day earth would heat up, but at night, all the
    accumulated energy would radiate back into space
    and the planet's surface temperature would fall
    far below zero very rapidly!
  • This doesn't happen b/c the earth's atmosphere
    contains molecules (CO2) that absorb the heat and
    re-radiate the heat in all directions. This
    reduces the heat radiated out to space
  • These greenhouse gases serve to hold heat in
    like the glass walls of a greenhouse, and are
    responsible for the fact that the earth enjoys
    temperatures suitable for life.

9
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10
Carbon dioxide (CO2)A Greenhouse Gas
  • CO2 is made up of 1 carbon atom with an oxygen
    atom bonded to each side. When its atoms are
    bonded tightly together, the carbon dioxide
    molecule can absorb infrared radiation and the
    molecule starts to vibrate.
  • The vibrating molecule will emit the radiation
    again, and it will likely be absorbed by yet
    another greenhouse gas molecule. This
    absorption-emission-absorption cycle serves to
    keep the heat near the surface, effectively
    insulating the surface from the cold of space.
  • For demo go to http//www.ucar.edu/learn/1_3_1.h
    tm

11
What do Greenhouse gases have in common?
  • Carbon dioxide, water vapor, methane , nitorus
    oxide, and a few other gases are greenhouse
    gases. They all are molecules composed of more
    than two component atoms, bound loosely enough
    together to be able to vibrate with the
    absorption of heat. The major components of the
    atmosphere Nitrogen and Oxygen are two-atom
    molecules too tightly bound together to vibrate
    and thus they do not absorb heat and contribute
    to the greenhouse effect.

12
Greenhouse effect
  • Natural situation in which HEAT is retained in
    Earths atmosphere by Carbon dioxide, Methane,
    Water Vapor and other gases. (pg. 87)

13
Climates Past
  • Our evolutionary origins lie in the warm
    equatorial Africa, but our ancestors battled the
    cold, harsh, and unforgiving climate of the last
    ice age in order to spread across the planet.

14
Climate History
  • We know that the earth's climate has changed over
    time. Throughout the earth's history, there have
    been periods of glaciation followed by warming
    trends in which the glaciers retreated toward
    higher altitudes and latitudes. Today's concerns
    focus on the current and projected rate of
    climate change based, in large part, on human
    activities.
  • Some 10,000 years age, the ice age ended. We
    developed agriculture, civilization, industry,
    and technology generally in a global climate that
    was warm, pleasant, and mostly predictable.
    Regional climates have changed, sometimes
    drastically and disastrously for local human
    populations, but by and large the global climate
    has not dealt any significant long-term blows to
    the spread and development of human civilization.

15
Fossil Fuels
  • One of the most significant accomplishments of
    our species is the discovery of fossil fuels and
    the means of turning the energy trapped within
    them into heat, transportation, and the basis for
    manufacturing and construction

16
Changing the world forever?
  • On an ancient warmer Earth with a high
    concentration of carbon dioxide in the
    atmosphere, photosynthetic organisms (algae and
    higher plants) absorbed carbon dioxide , and used
    it to produce abundant organic material. When
    these organisms died, they were buried deep
    within the earth and slowly turned into coal and
    oil.
  • Since the 1800s, we've been burning vast
    quantities of these fossil fuels to power our
    developing technological and global civilization.
  • So, we've been releasing the CO2 trapped in the
    fuels in the form of energy-rich organic
    molecules back into the atmosphere, increasing
    the atmospheric concentration of CO2 .

17
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18
So What?
  • Since the 1800s, CO2 concentrations worldwide
    have increased from approximately 280 ppm (or
    0.028) to around 365 ppm (0.0365). The increase
    might seem trivial, but it also means that some 3
    gigatons (3 billion metric tons) of CO2 are
    being added to the atmosphere every year!
  • Knowing that CO2 is a GREENHOUSE gas, what might
    Increased Concentrations of this gas do to our
    climate?

19
CO2
  • CO2 is a powerful greenhouse gas!
  • We can therefore conclude that the earth's
    temperature should go up as CO2 concentrations
    increase.

20
Climatologists have detected a steady but small
increase in global average temperatures over the
last few decades, based on weather data collected
all around the world. Six of the last ten were
the hottest years on record.
21
Global Warming
  • An increase in the Average Temperature of the
    Earth (pg. 159) http//www.weatherquestions.com/gl
    obal_warming_Jones.jpg

22
  • Why is the carbon cycle so important when looking
    at climate change issues?

23
  • What major events in human history are thought to
    be factors in changing the earth's atmosphere?

24
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