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Environmental Science Brewer 1 ES 2.1: The Thin Blue Blanket atmosphere: a mixture a gases that surrounds the planet Earth. 78% nitrogen 21% oxygen the atmosphere is held to the Earth by the force of gravity. Due to the smaller mass of planets like Mercury, less atmosphere can be held in place. Thinner atmosphere means less insulation. Therefore, Mercury has greater temperature extremes (840 to 275 Fahrenheit)

ES 2.1: The Thin Blue Blanket Earth by the force of gravity.images.pcmac.org/SiSFiles/Schools/AL/MobileCounty/DavidsonHigh... · Environmental Science Brewer 1 ES 2.1: The Thin Blue

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  • EnvironmentalScience

    Brewer 1

    ES2.1:TheThinBlueBlanket

    atmosphere:amixtureagasesthatsurroundstheplanetEarth.

    78%nitrogen

    21%oxygen

    theatmosphereisheldtotheEarthbytheforceofgravity.

    DuetothesmallermassofplanetslikeMercury,lessatmospherecanbeheldinplace.

    Thinneratmospheremeanslessinsulation.

    Therefore,Mercuryhasgreatertemperatureextremes(840to275Fahrenheit)

  • EnvironmentalScience

    Brewer 2

    ES2.1:TheThinBlueBlanket

    ConsidertheplanetVenus

    approximatelythesamesizeandmassasEarth

    96%oftheatmosphereiscomposedofthegreenhousegascarbondioxide.

    temperaturesareneverbelow750Fahrenheit

    ConsiderUranus

    gasgiantwiththickcloudsofdeadlymethanegas

    temperaturesaverage360Fahrenheit

    NotehowmuchlargerUranusisthantheEarth.

    WhateffectwouldtherelativesizeofUranushaveonthetotalatmosphereoftheplanet?

  • EnvironmentalScience

    Brewer 3

    ES2.1:TheThinBlueBlanket

    TherelativethicknessoftheEarth'satmospheretotherestoftheEarthcanbecomparedtotheskinofanapplecomparedtotherestofanapple

  • EnvironmentalScience

    Brewer 4

    ES2.1:TheThinBlueBlanket

    TheEarth'satmospherebecomesthinnerwithincreasingelevation.

    Thisisduetoadecreaseintheforceofgravitywithincreasingdistancefromacenterofmass(i.e.centeroftheEarth)

    mountainclimberw/O2tank

    warmclothingduetolowtemperaturescausedbythinningatmosphere

  • EnvironmentalScience

    Brewer 5

    ES2.1:TheThinBlueBlanket

    TheOzoneShieldaNaturalSunscreen

    Recallapproximately21%oftheatmosphereisO2

    O2moleculescanbesplitbyultravioletlightandlightning.

    ThesefreeOatomsthencombinewithotherO2moleculestoformozone,O3

    MoleculeBuildingactivity

  • EnvironmentalScience

    Brewer 6

  • EnvironmentalScience

    Brewer 7

    ES2.1:TheThinBlueBlanket

    TheOzoneShieldaNaturalSunscreen

    Ozoneismeasureinpartspermillion(ppm)byvolume

    Thecycleofozonecreation(UVlight)anddestruction(nitricoxide)iscontinuousandnatural.

    OzoneformationdependsontheamountofUVlightandtemperature

    Equilibriumisachievedwhentherateofcreationequalstherateofdestructionofozone.

    Ozonedepletionoccurswhentherateofdestructionisgreaterthanthatofcreation.

  • EnvironmentalScience

    Brewer 8

    ES2.1:TheThinBlueBlanket

    CFCsTheRisksandBenefitsofTechnology

    Beginninginthe1970's,scientistsbegantostudytheeffectofchemicalsproducedbyhumanactivitiesontheozoneshield

    PaulCrutzendiscoveredthatnitrogenoxidesfromsupersonicjetscoulddamagetheozonelayer.

  • EnvironmentalScience

    Brewer 9

    ES2.1:TheThinBlueBlanket

    chlorofluorocarbons(CFC's):compoundscontainingcarbon,fluorine,andchlorinethatcandestroytheozonelayer

    WhenCFCsmeetOzone.mpeg

    CharacteristicsofCFC's:1)nontoxic2)nonflammable3)inexpensivetoproduce

    Usedasareplacementcoolantinrefrigeratorsandairconditionersbecausethemethylchlorideusedwastoxic.

    Extremelystableinthetroposphere,whereUVlightsplitschlorinefromCFC's.AsingleClatomcanthendestroy100,000ozonemolecules.

    CFC'seventuallyreturntotheloweratmosphereandarewashedoutbyrain.

    SMART Notebook

  • EnvironmentalScience

    Brewer 10

    ES2.1:TheThinBlueBlanket

    OzoneReactions

    FormationofOzone

    O2+UVlight>O+O

    O+O+2O2+catalyst>2O3

    Net:3O2>2O3

    NaturalDestructionofOzone

    O3+NO>O2+NO2

    O3+UVlight>O2+O

    NO2+O>NO+O2

    Net:2O3>3O2

    OzoneAccumulation

    3O2>2O3

    3O2

  • EnvironmentalScience

    Brewer 11

    CFC'sAttackonOzoneReaction

    CFCl3+UVlight>CFCl2+Cl

    Cl+O3>ClO+O2

    O3+UVlight>O2+O

    ClO+O>Cl+O2

    Cl+O3>ClO+O2

    Result2O3>3O2

  • EnvironmentalScience

    Brewer 12

    ES2.1:TheThinBlueBlanket

    BiologicalEffects

    OzoneprotectslifefromharmfulUV(blacklight)

    UVtypes(bywavelength)

    UVA:necessaryforsynthesisofvitaminDintheskin

    UVB:causesagingoftheskin,skincancers,cataracts,andmayimpairimmunesystemresponse

    notnecessaryforphotosynthesis,andcanbeharmfultoplantsandmicrobes

    plantsbecomemoresusceptibletoinsectsandpathogens

    UVC:mostdeadlyformofUV,butabsorbedbyozoneandoxygeninatmosphere

  • EnvironmentalScience

    Brewer 13

    ES2.1:TheThinBlueBlanket

    BiologicalEffects

    CO2,H2O,nutrientsandheatarefactorsinhowmucheffectUVradiationwillhaveonplants

    UVmayalsoreducetherateofphotosynthesisofphytoplanktonintheocean.

    FrogeggsandcoralreefsarealsosensitivetoUVlightandinterfereswiththeirdevelopment.

    Marineecosystemsnearthepolesexperiencethegreatesteffects.

  • EnvironmentalScience

    Brewer 14

    ES2.1:TheThinBlueBlanket

    WarningNotHeeded

    ScientistsfirstdiscoveredthelinkbetweenCFC'sandozonedepletionin1974.

    In1977theU.S.,Canada,andothersbannedtheuseofCFC'sinaerosols

    Althoughothersourcesexistedatthattime,industrylobbyistsenticedpoliticianstoallowindustrialuseofCFC's.

    Presently,theozoneisbeingdestroyedatafasterratethanitisbeingproduced.

    OzonedepletionisgreatestoverAntarctica.Duringthespring,Antarctica'suniqueweatherpatterns furtherthedepletion.

    Contrarytopopularbelief,thereisnophysical"hole"intheozonerather,theozonelayerisverythinintheseregions.

  • EnvironmentalScience

    Brewer 15

    ES2.1:TheThinBlueBlanket

    TheMontrealProtocol

    ThemajorcauseofozonedestructionischlorinefromCFC's

    Solutions:

    1.StopproductionofCFC's

    2.PreventthereleaseofCFC'sintheatmosphere

    ProtocolnowseekstotaleliminationofCFC's

    Theglobalnatureofozonerequiresinternationalcooperationinordertoprovideprotection

    Ozonewillnotreturntopre1980levelsuntil2065.

  • EnvironmentalScience

    Brewer 16

    ES2.1:TheThinBlueBlanket

    FindingAlternatives

    CFC'sarebannedinindustrializedcountries

    exceptions:whennootheroptionisavailable

    DevelopingcountriesstilluseCFC's

    RecycledCFC'scanbeusedforequipment

    HighcostofreplacementsencouragesillegaluseofCFC's

    HCFC'sarelessstableandfewermoleculesreachtheatmosphere

    productionmuststopby2030

    replacementchemicalmustbe:

    1.nonflammable

    2.noncorrosive

    3.lowtoxicity

    4.reasonablypriced

    Halonsareusedinfireexstinguishers

    replacementbyCO2

    CO2onlyworksforcertainkindsoffires

    CO2weighsmore(impracticalforairplanes)

    HCFCmolecule

    CFCmolecule

  • EnvironmentalScience

    Brewer 17

    ES2.1:TheThinBlueBlanket

    WhatYouCanDo

    Recycleyourrefrigerants(don'tforgetyourcar)

    Avoidthesunbetween10and3

    UsesunscreenthatblocksUVAandUVB

    WearsunglassesthatblockUVradiation

  • Attachments

    WhenCFCsmeetOzone.mpeg

    SMART Notebook

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