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    Media Myths about ClimateBe skeptical be very skeptical !

    Concern about global warming is based on recenttemperature trends

    9 of the 10 hottest years on record

    If somebody could find some other cause for recentwarming, we could quit worrying

    Global warming is a theory based on complicatedcomputer models

    CO2is air pollution cutting emissions will leadto falling CO2 and therefore cooling

    If we stop burning coal, well freeze in the dark!

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    Global Warming isBased on Common Sense

    not computer models not recent temperatures

    not complicated!

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    Planetary Energy Balance

    Energy In = Energy Out

    2 2 4(1 ) 4S R R T

    o18 CT

    But the observed Ts is about 15 C

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    Dancing Molecules and Heat Rays!

    Nearly all of the air is

    made of oxygen (O2)and nitrogen (N2) inwhich two atoms ofthe same elementshare electrons

    Infrared (heat)

    energy radiated upfrom the surface canbe absorbed by thesemolecules, but not

    very well

    N N

    O O

    Diatomic molecules can

    vibrate back and forthl ike balls on a spring, but

    the ends are identical

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    Dancing Molecules and Heat Rays!

    Carbon dioxide (CO2)

    and water vapor (H2O)are different!

    They have many moreways to vibrate androtate, so they arevery good at absorbingand emitting infrared(heat) radiation

    Molecules that have manyways to wiggle are called

    Greenhouse molecules

    O OC

    H H

    O

    Absorption spectrum of CO2 was measured by John Tyndall in 1863

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    Common Sense

    Doubling CO2 wouldadd 4 watts toevery square meterof the surface of

    the Earth, 24/7 Doing that would

    make the surfacewarmer

    This was knownbefore light bulbswere invented!

    4 Watts

    John Tyndall , January 1863

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    Common Misconception #1Expectations of future warming are based on

    extrapolation of recent warming trends

    WRONG! They are based on the idea that whenwe add energy to the surface, it will warm up

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    19th Century Climate Physics(Svante Arrhenius, 1897)

    S0(1 )r2

    TS4 (4r2 )

    S0(1 ) 4TS4

    0 4TS

    4 4(4TS

    4 )

    Differentiate, apply chain rule

    TS

    TS

    4

    Ar rhenius worked out a simple formula

    for the change in sur face temperature

    given a change in effective

    atmospher ic emissivity due to CO2

    Earth

    Ts

    aS0

    esTs4

    S0

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    19th Century ClimatePhysics(contd)

    Plug in measured values

    TS TS

    4

    TS

    4 240 W m-2

    (from satellite data)

    ()(

    TS

    4

    ) 4 W m-2

    (for 2 x CO2

    from radiative transfer)

    4

    240

    Ts = 288 K

    TS

    288K

    4

    4

    240

    1.2K

    For CO2 alone (no feedback), expect about 2F warming for 2 x CO2

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    Climate Feedback Processes

    Positive Feedbacks(amplify changes) Water vapor

    Ice-albedo

    High clouds

    De DTS Dvapor

    D albedo

    DLW

    D hi cloud

    D lo cloud

    Negative feedbacks

    (damp changes) Longwave cooling Low clouds

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    Tiny Bubbles Priceless

    ice age ice age ice ageice age

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    Estimating Total Climate Sensitivity

    At the Last Glacial Maximum

    (~ 18k years ago) surface temp ~ 6C colder CO2 was ~ 180 ppm

    (weaker greenhouse, 4.1 W m-2 more LW)

    Brighter surface due to snow and ice, estimate3.4 W m-2 more reflected solar

    Or, for doubling of CO2: expect 4 x 0.8 = 3.2C of

    T

    S

    FTS(now)T

    S(then)

    F(now

    ) F

    (then

    )

    6K

    (4.1 3.4)Wm2 0.8

    K

    Wm2

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    Review: 19th Century Physics(updated using paleo-data)

    Forcing: changes in properties ofatmosphere as measured by spectroscopy(4 W m-2 per doubling of CO2)

    Feedback: both positive and negative, totalresponse to forcing estimated from Ice Ageclimate data (about 0.8C per W m-2)

    Response: about 3.2 C warming for 2 xCO2No climate models required just based on observations

    (modern calculations agree coincidence?)

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    CO2 and the Modern Age

    370 ppm in 2000

    Vostok (400k yr) Ice Core data (Petit et al, 1999)

    180

    230

    280

    330

    380

    -400000 -300000 -200000 -100000 0

    year

    Over the past 420,000

    years atmospheric CO2has varied between 180and 280 parts permillion, beating in timewith the last four glacialcycles

    Since the IndustrialRevolution, CO2 has risen

    very rapidly ice iceiceice

    CO2

    388 ppm in 2009

    f rom measurements

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    CO2 and the Future

    Vostok (400k yr) Ice Core data (Petit et al, 1999)

    0

    200

    400

    600

    800

    1000

    -400000 -300000 -200000 -100000 0

    year

    Over the past 420,000

    years atmospheric CO2has varied between 180and 280 parts permillion, beating in timewith the last four glacial

    cycles

    Since the IndustrialRevolution, CO2 has risenvery rapidly

    If China & India developusing 19th Centurytechnology, CO2 willreach 900 ppm in this

    century

    ice iceiceice

    CO2

    900 ppm in 2100

    388 ppm in 2009

    You aint seen nothing yet!

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    Climate vs. Weather

    Weather tells you what to wear today climate tells you what clothes to buy!

    Climate is an envelope of possibilitieswithin which the weather bounces around

    Weather depends very sensitively on theevolution of the system from one momentto the next (initial conditions)

    Climate is determined by the properties ofthe Earth system itself(the boundary conditions)

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    Climate Predictability

    Predicting the response of the climate to achange in the radiative forcing is notanalogousto weather prediction

    If the change in forcing is large and predictable,

    the response can also be predictable I cant predict the weather in Fort Collins on

    December 18, 2009 (nobody can!)

    I can predict with 100% confidence that theaverage temperature in Fort Collins forDecember, 2009 will be warmer than the averagefor July!

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    Climate Forcing

    Changes in climate often reflect changes in forcing, asamplified or damped by climate feedbacks Diurnal cycle

    Seasonal cycle

    Ice ages

    Response to volcanic aerosol

    Solar variability

    Greenhouse forcing

    If forcing is sufficiently strong, and the forcing itself is

    predictable, then the response of the climate can bepredictable too!