An Illustrated Guide to Climate Pollution

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    An endless sky? Think again.

    A pers

    of th

    back (

    time marat

    If o

    thi

    be

    of t

    The lowest five to ten

    miles of the atmosphere

    is where weather forms

    and planes fly.

    1The atmosphere is surprisingly thin. Space

    begins about 300 miles from Earths surface,

    which is where the blue coating around the

    Earth in this picture ends.

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    The atmosphere is Earths blanket.

    The atmosphere is naturally

    filled with gas molecules.

    Gases with asymmetrical structures

    absorb low-energy heat because

    they bend, stretch, or rotate.

    These gases trap heat in the Earth

    and keep us warm like a blanket.

    Without

    would be 6

    and uGases are mostly

    unaffected by

    high-energy

    sunlight.

    N2

    O2 H2O

    CH4

    O3

    N2O

    These gases include

    water vapor (H2O),carbon dioxide (CO

    2),

    methane (CH4),

    ozone (O3), and

    nitrous oxide (N2O).

    Earth cools off by emitting low-energy heat into space.

    2CO2

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    Human activitiessuch as burning coal for electricityare increasing the

    amount of heat-trapping gases in the atmosphere, thickening the Earths blanket.

    Some gases, such as CO2, can

    remain in the atmosphere for

    over a thousand years.

    So whats the problem? Too much of a good thing

    3

    CO2, CH4, and N2O concentrations40%, 150%, and 20% since

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    Unnatural warming is changing the climate with

    4UNNATURAL OVERDOSE

    OF GREENHOUSE EFFECT

    HUMAN SO

    NATURAL WO

    CHANGING CLIMATE

    CONDITIONS

    WARMING PLANET AND

    MOIST ATMOSPHERE

    Human activities are

    emitting large

    amounts of

    heat-trapping gases

    into the atmosphere.

    Some gases, such asmethane, break down

    to create even more

    greenhouse gases.

    Snow and ice melting

    Sea level rising

    Hot days increasing

    Flooding intensifying

    Powerful,

    damaging

    storms

    Intense, long

    droughts

    Dryness fuels

    wildfires

    Death, illness fro

    extremes, insect

    air quality

    Extra heat warms

    air and ocean

    Warmer air

    holds more

    moisture

    Warmer

    ocean

    evaporates

    more water

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    But hasnt the climate changed in the past, befor

    5

    HIGHER

    TEMPERATURE

    MORE CO2IN

    ATMOSPHERE

    aw

    armeroceanandmeltingicereleaseCO2intotheatmosph

    ere

    CO2preventsheatfromescapingtospaceBOTH

    natural and humanfactors can trigger

    the initiation of a

    feedback loop that

    increases global

    temperatures

    volcanic

    eruptions

    s

    ac

    na

    var

    cutting/burning

    down forests

    electricity

    generation

    Scientists use instruments

    that chemically separate the

    kinds of carbon found in fossil

    fuels from those in air and water. Scientists can therefore detect

    that the increasing CO2today is

    from human sources.

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    This means we can do something about it!

    6To reduce emissions of

    heat-trapping gases,individual actions are not

    enough. We also need

    visionary action from

    local, state, and

    national governments,

    and unprecedented

    internationalcooperation.

    Climate change is a global

    problem becauseemissions come from

    all levels and the

    pollution can last

    for hundreds

    of years.

    Individuals

    Communities

    Worldwide

    Local, State, National Governments

    Many d

    techPROBLEM SOLUTION

    TECHNOLOGICAL

    BEHAVIORAL

    ECONO

    POLITICAL

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