234678 Global Warming 1

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    Global Warming

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    CO2 needs to be added to the list!

    Not regulated as apollutant under theU.S. Clean Air Act.

    But most emissionsare CO2

    A greenhouse gas Contributes to

    global climatechange

    In the US

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    Sources of C02

    US emissions

    1. 40 %

    Petroleum

    products

    2. 34 % coal

    3. 20 % naturalgas

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    Greenhouse Effect

    In a greenhouse, light enters but IR cannotescape

    CO2 in atmosphere allows light rays to enter

    but traps IR CO2 % in atmosphere has increased from 280

    ppm in pre-Industrial time to present day

    value of 375.64 ppm (2003 data), 387 ppm(2009 data)

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    Rise in atmospheric CO2 in the last 50 years

    Why the see-saw pattern? Why Mauna Loa?

    http://upload.wikimedia.org/wikipedia/commons/5/51/Mauna_Loa_Carbon_Dioxide-en.svghttp://upload.wikimedia.org/wikipedia/commons/5/51/Mauna_Loa_Carbon_Dioxide-en.svghttp://upload.wikimedia.org/wikipedia/commons/5/51/Mauna_Loa_Carbon_Dioxide-en.svghttp://upload.wikimedia.org/wikipedia/commons/5/51/Mauna_Loa_Carbon_Dioxide-en.svg
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    Other Greenhouse Gases

    Methane, water vapor, nitrous oxide

    Rice paddy, extraction of fossil fuel, raising of livestock (bovine flatulence) cause increase in methane

    Cutting of forests kills CO2 sink

    Some effects might be opposite of CO2: SO2

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    Increasing concentration of

    greenhouse gasesGas Historic Level Current Level Warming

    potential

    comapred to

    CO2

    Lifetime in

    Atmosphere

    (years)

    CO2 280 ppm 387 ppm 1 5-200

    CH4 700 ppb 1720 ppb 23 12

    N2O 275 ppb 314 ppb 300 114

    CFCs 0 ppt level 4000-8000 5-100

    Perfluoro-

    methane (PFC)

    40 pt 80 ppt 5700 50,000

    Sulfur

    Hexafluoride

    (SF6)

    0.01 ppt 3 ppt 22,000 3200

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    Greenhouse Effect: Is it Real?

    How much CO2=How much rise of T?

    More T = more evaporation = more cloud = LessTemp

    Real rise or natural fluctuation? Data for the last 10ka indicate upto 6 C fluctuation Little ice age (1450 1850)

    About 2/3rd of the centuries warming has taken place inthe last 25 years: 1990s were the warmest decade of the20th century

    Based on 14,000 land and sea records from all over theworld

    Ice core patternsvaried between 180 and 280 ppm in thelast half million years

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    Evidence to Support Global Warming

    Intergovernmental Panel on Climate Change (IPCC)

    An international panel of scientists and government officialsestablished in 1988

    Generated reports on the synthesis of scientific information

    concerning climate change 4th Assessment report 2007

    Documents observed trends in surface temperature, precipitationpatterns, snow and ice cover, sea levels, storm intensity

    The IPCC concluded that it is more than 90%likely that most global warming is due to humans

    The Debate over climate change is over 84% of people surveyed think humans contribute to global warming

    Predicts future changes

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    Effects of Global Warming

    Sea level rise

    Extreme weather

    Decreasing Biodiversity Decline in Food Production

    Effect on Health

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    Greatest air pollution problem: Global Warming

    www.nelson.wisc.edu/outreach/energy2006

    http://bp0.blogger.com/_iKGmOafHiwQ/SINKm0LsigI/AAAAAAAAAgA/cDnBZas-PUM/s1600-h/preaching+to+reduce+greenhouse+emissions.gif
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    Greenhouse Effect: Problems

    Increasing ocean temperature:

    0.06 C between 1955 and 1995

    Oceans hold 10X heat than what has been used to raisethe global temperature

    An increased amount of heat storage in the oceanspreceded all earlier rapid warming

    Rise of temperature : Drier climate?

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    Satellites that detect and observe different

    characteristics and features of the Earth's atmosphere,

    lands, and oceans are often referred to as environmental

    satellites.

    Most environmental satellites have one of two types of

    orbits: geosynchronous (GOES) or sun-synchronous(POES)

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    Sea Surface Temperature

    Sea surface-temperature is one important type ofdata that GOES and POES provide.

    Temperature changes influence the behavior offish, can cause the bleaching of corals, and

    affects weather along the coast. Satellite images of sea-surface temperature also

    show patterns of water circulation. Examplesinclude locations of upwelling, characterized bycold waters that rise up from the depths, often

    near the coasts; and warm water currents, suchas the Gulf Stream.

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    Steve Riser and ARGO lab3000 free floating package of sensors

    Crates a ocean temperature map upto 1500 m depth

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    http://www.argo.net/index_flash.html