lecture for wednesday aug 27 - atmos.uw.edubitz/111/aug27.pdf · the greenhouse effect ghe glass...

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Lecture for Wednesday Aug 27 Lecture: Global warming theory Causes/Consequences of climate change Ac*vity: Media and climate change Reading for Tomorrow: Houghton p 56‐68

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Page 1: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Lecture for Wednesday Aug 27

Lecture:GlobalwarmingtheoryCauses/Consequencesofclimatechange

Ac*vity:Mediaandclimatechange

ReadingforTomorrow:Houghtonp56‐68

Page 2: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Visible and Infrared Satellite Pictures

a)Whichisthe"visible"image?Howcanyoutell?

d)Ontheinfraredimage,arehighertemperatureslighterordarker?Howcanyoutell?

c)WhichismorereflecJve:oceanorland?

infrared(LW) visible(SW)

b)WhatisemiKngtheradiaJonineachcase?

Page 3: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Height

Temperature

Lowest10koftheatmos.(wheremostofthemassis)temperaturedecreaseswithheight

Wherearetheclouds?

Whyisthesurfacewarm?

Whyisthestratospherewarm?

Medium

cold

Earth

Fromsatellite:warmareasareprobablyatorclosetothegroundandcoldareasareprobablytallcloudtops

warm

IRSatelliteViewExplained

Page 4: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Emission/AbsorpJon

Earthandcloudsare“blackbodies”‐emitandabsorbwithperfectefficiency(solidcurve)

GHG‐HypotheJcalimperfectEmiXer/absorberatThesameT

PeakwavelengthindicatestemperatureIsabout15degC

FluxorRa

diance(W

/m2 )

200

0

Wavelength(micrometers)

15 20

100

25

Page 5: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

ButEarthisgenerallywarmerthanatmosphere

GHG‐peakindicatesT=‐15C

EarthpeakwavelengthIndicatesT=15degC

FluxorRa

diance(W

/m2 )

200

0

Wavelength(micrometers)

15 20

100

25

Page 6: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

LWSpectrumofEarthwithAtmos.

SeedipsatwavelengthswhereGHGaregoodabsorbers/emiXers.ThecurvedipsbecausetheGHGarecolderthanthesurface

HoughtonFig2.4

WhereGHGarebadabsorbers/emiXers,thefluxfromthesurfacepassesthroughtheatmosphere“window”

Page 7: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

AddingmoreGHG,shrinksthewindowsAndlowerstheoutgoingLWflux

Page 8: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

PlanetaryEnergyBalance

AtEquilibrium(asteadyclimate):

EnergyFluxin=EnergyFluxout FIN=FOUT

Foraplanet:

Absorbedsolarenergy=Heatenergylosttospace*

*dependsontemperatureT

oftheearthandatmosphere

Page 9: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Houghton Fig 2.6

343‐103=240(W/m2) 40+35+165=240 (W/m2)

visiblesatelliteimage

infraredsatelliteimage

FIN=FOUT?

Page 10: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

MainCons*tuentsofEarth’sAtmosphere

N2Nitrogen 78%

O2Oxygen 21%

ArArgon 1%

H2OWaterVapor 0‐4%

CO2CarbonDioxide 0.0385%(increasing)

Whichonescontributetothegreenhouseeffect?

LikeHoughtontable2.1

Page 11: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Houghton Fig 2.2

• Termcomesfrom1827Jean‐BapJsteFourier

• Absorbedsunlightheatsplantsandsoil

• PlantsandsoilemitIRandheatglasswall

• GlasswallsemitIRbacktowardsplantswarm

TheGreenhouseEffectGHE

glass

Page 12: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Houghton Fig 2.2

Notreally,becausethemainreasonagreenhouseiswarmisbecausetheytraprisingwarmair

Absorbedsunlightcauses“thermals”

ResultsinconvecJon=risingwarmairandsinkingcoldair

warm

IstheGHELikeAGreenhouse?

glass

Page 13: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

ASlightlyBecerFigureFortheGHE

Houghton Fig 2.5

greenhousegases

Earth'ssurface

Warm

Cold

Warm

Page 14: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

ConsiderEarthwithNoAtmos.

Earth

SW LW

HereIhaveletarrowlengthsindicaterelaJveamountofflux.Earthisinbalance.

ReasonableesJmatesgivesanaveragetemperaturebelowfreezing!

Page 15: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

EarthwithaSimple1‐LayerAtmos.

Earth

SW LW

SimpleAtmosphere

GHE

Page 16: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

The Greenhouse Effect: Tyndall JohnTyndall*,1862(riveranalogy):

"Asadambuiltacrossarivercausesalocaldeepeningofthestream,soouratmosphere,thrownasabarrieracrosstheterrestrialrays,producesalocalheighteningofthetemperatureattheEarth'ssurface."

*Bri*shphysicist,chemist,inventor,andearlyatmosphericscien*st;measuredabsorp*onspectraofvariousgasesandscaceringproper*esofgasesandpar*cles;discoveredchemicalnatureofozone;firsturbanairqualitystudies

Page 17: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

TheGreenhouseEffect

Makesuswarmerby20to30C

Itisonlynatural!ItisnolongerdebatedbyscienJsts

Page 18: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Blanketsalsowarmbyreducingconvec*on.

Houghtonusestheterm“radia*onblanket”

Human‐inducedglobalwarming:addmoreblankets?

IstheGHELikeABlanket?

Page 19: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Current paradigm –forcing

10,000 5,000 0Yearsbeforepresent

CharlesD.Keeling(1925‐2005)

CO2hasrisenbyover35%

IPCC WG1 SPM Fig 1

Page 20: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

EnhancedorAnthropogenicGHE

Earth

SW LW

SimpleAtmosphereX TooSimplebecauseitdoesn’tchangeiftherearemoreGHGs

Rememberthattheatmosphereiscolderalop

IncreasingtheGHGconcentra*onreducestheoutgoingLW(coldmaceremitslessheatthanwarmmacer.

Page 21: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

AddingmoreGHGislikeaddingmorehighclouds.

Lessheatescapes,so

FOUTdecreases

Atfirst,energyisnotinbalance

WhichisbiggerFINorFOUT?

Page 22: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

ImaginetheCO2LevelDoubledInstantly

Lessheatescapes,so

FOUTdecreases

“Radia*veForcing”

ΔF=FIN‐FOUT=3.7W/m2

(es*matedtowithinafewtenths)

Page 23: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Energybalancetheoryofclimatechange

ΔT = λ ΔF

Note: Δ: common symbol to refer to change in some quantity

ΔF: radiative forcing (change in energy balance) ΔT: response (change in surface temperature) λ: climate sensitivity (everything else)

TheOnlyEqua*onYouNeedtoKnow

λ: does not represent the wavelength of light here!

Page 24: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Energybalancetheoryofclimatechange

ΔT = λ ΔF

RunaClimateModelwithDoubleCO2

RunmodelunJltheoceancomesintoequilibriumwiththeatmosphereandfindΔT isabout2‐4.5degC.

Soλ is?

Page 25: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

WhyCan’tWeUsetheRealEarth?

Page 26: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Currentparadigm–forcing

Source: IPCC 2001 WG1, SPM, Fig 4

Response:ObservedWarming

Page 27: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

WeCANNOTUsetheRealEarthVeryEasily

BecausetheforcingisnotjustfromCO2

AND

Theoceanisnotinequilibriumwiththeatmosphere,sothefullsurfacewarmingisdelayed

Page 28: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

New York Times Climate Experts Tussle Over Details. Public Gets Whiplash.

By ANDREW C. REVKIN July 29, 2008

Page 29: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Revkin writes, “How fast is Greenland shedding ice? Did human-caused warming wipe out frogs …? These questions endure even as the basic theory of a rising human influence on climate has steadily solidified.”

“Scientists see persistent disputes as the normal stuttering journey toward improved understanding of how the world works.”

Remind you of something Prof Ackerman said?

Page 30: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Example: Are Hurricane strengthening from global warming? Many papers on both sides of debate.

“ “not as an evolution of objective scientific understanding but as a proliferation of contradictory opinions.” ” according to W. Tad Pfeffer.

Are scientists partly to blame for public disengagement? A public divided and confused?

Page 31: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Revkin writes, “Morris Ward, the editor of the Yale effort says that it will be up to the public to choose to be better informed on momentous issues that do not fit the normal template for news or clash with their ingrained worldviews. “At some point,” he said, “the public at large has to step up to the plate in terms of scientific and policy literacy, in terms of commitment to education and strong and effective political leadership, and in terms of their own general self-improvement.” ”

Page 32: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Revkin writes, “The news media sometimes overplayed the uncertainty by balancing opposing views in a story without characterizing the overall level of confidence in either side”

The Columbia Journalism Review's Division Over Dissent IS GLOBAL WARMING NOW BEYOND DEBATE?

By Ron Rosenbaum Posted Friday, Aug. 8, 2008, at 6:09 PM ET

Rosenbaum criticizing other article that says, “Scientists look for consistency among several reports before concluding something is true.”

Page 33: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

June 27, 2008 North Pole could be ice-free this summer, scientists say

By Alan Duke CNN

"We kind of have an informal betting pool going around in our center and that betting pool is 'does the North Pole melt out this summer?' and it may well," said the center's senior research scientist, Mark Serreze.

Page 34: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river
Page 35: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

A more conservative ice scientist, Cecilia Bitz at the University of Washington, put the odds of a North Pole without ice closer to 1 in 4. Even that is far worse than climate models had predicted, which was 1 in 70 sometime in the next decade, she said.

But both she and Serreze agree it’s just a matter of time.

Page 36: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

The first scene from 31 January 2002 shows the shelf in late austral summer with dark bluish melt ponds dotting its surface. In the next two scenes minor retreat takes place, amounting to about 800 km2. The main collapse is seen in the last two scenes, on 5 March and 7 March. The last phases of the retreat totaled ~2600 km2.

Page 37: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

In-class activity: Enhanced GHE EnergybalanceequaJon…

FOUTenergy emitted

by Earth

FINenergy absorbed

by Earth

=

IfyouaddCO2totheatmosphere,whichtermchangesanddoesitincreaseordecrease?

“GlobalWarmingTheory”

Step 1: GHG increases, FOUTinstantly decreases, so FOUT < FIN

Step 2: In time Tsurface will go up until balance is restored, because

surface warming makes FOUT go up again

Page 38: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

What is the change to the top of atmosphere radiation balance in

step 1 known as:

ΔF = FOUT-FIN ?

Radiative Forcing Or Climate Forcing

Page 39: Lecture for Wednesday Aug 27 - atmos.uw.edubitz/111/Aug27.pdf · The Greenhouse Effect GHE glass ... Simple Atmosphere GHE The Greenhouse Effect: Tyndall John Tyndall*, 1862 (river

Source: IPCC 2007 WG1, SPM, Fig 2