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Chapter 3 Giant planets(第1页)

Chapter3 Gias

&hebodiesthatdomiheSolarSystem–providedyouthinkitissizethatmatters,andarewilliheSuhefiasareillustratedtosthelowerhalfofFigure3,showinghowpreheheirsizeovershadowstheterrestrialplaheviewofUranusisfromtheHubbleSpaceTelesorbitabouttheEarth,whereastheiasareasseenbyvisitiheirdominationbymassisnotquites,becausetheyarelessdeheterrestrialplaer’sdensityisonly24%oftheEarth’s,andSaturnisevenlessdenseandwouldfloatifdroppedintoasuffitlylarge(ahetical)bucketofwater。AllofthemhaveriorialplahoughournandUranusaresuffitlypromiobevisibleihslooksolid,theyaremadeofmyriadspartidareextremelyinsubstantial。Theyarediscussed,alongwiththegiaellites,ier。

By,thesizeofagiaismeasuredfromthetopofitsclouds。Theseotheplaroposphere,abovewhicharelargelytraandprogressivelylessdenselayersclassifiableinthesamewayasfortheEarth’satmosphere。Thebaseofagiaroposphereishardtodefineandhasneverbeenexploredevenier,wherein1995aryprobereleasedbytheGalileospacecraftreachedadepthof160kilometresbelowthecloud-topsbeforepressure(22atmospheres)aure(153°C)putpaidtoit。Probably,thetroposphereofeatplamergesseamlesslyintoafluidiemperaturesandpressuressohighthatthereisnodistiweengasandliquid。ly,thereisnosolidsurfacethatahumaandupon。

Basicdatafiasaregivehepolardiametersquotedtherearelessthaorialdiameters,becauserapidrateofrotatioable2)flattenstheirshapes。Jupiter’spolardiameteris6。5%less,andSaturhanitspolardiameter。Thedifferenlyabout2%forthelessgassyandmoreslUraune(ahaerrestrialpla)。

Interiors

Thereisostudytheinteriiaweuseatmospheriposition(99%hydrogenandhelium)andeneralktheSolarSystemasawholeismadeoftostructamodelthatistwithitsmeasureddensity,andwiththeinteriorpressuresthatweferfromthis。Belohere,eatplahaveazoingmostlyenmolecules(H2)aoms(He),iisbettertocall‘fluid’ratherthaher‘liquid’aseous’。Attheverytre,thereisprobablyaroercore,ofaboutthreeEarth-massesierandSaturn,andaboutoh-massinsideUraune。Surroundingtheihereoughttobeanoutercoreof‘iposedofunknownproportionsofwater,ammonia,aingtoabouttwicethemassoftheEarthier,maybesixEarth-massesiurn,twelveinsideUranus,andfifteeukheseouterandinneroltenorsolid,becausealthoughweestimatethepressure(astaggering50milliohetreofJupiter),wedonotkionandhaveonlyavagueideaofthelikelytemperature(rangingfrominexcessof15,000°thetreofJupitertoabout2,200°Cattheeofune’score)。ofhowmaterialsbehaveundersuchextremesissketgwhethermetallicoulddiffereheroktowardstheanihecoresofUrauevenbeuedmixturesofidrock。

Table5 Basicdatafiaethatthemassuhousandtimesbiggertharialplaable3

Agforthecoresleaveslittlemorethah-massforthehydrogeeriorsofUraune,prisi6,000kilometresthick。Hasgiants’JupiterandSaturnhavemuchdeeperenvelopesenandheliumsurroundingtheirexcessof300ah-masses,respectively。Hydrogeomodelthaniceorrodstistsareprettytthatatpressuresgreaterthanabout2millionatmospheres,hydrogenatomsaresqueezedsotightlytogetherthatelesarenolongeredaboutspes。Iheyareablethaseaenthatbehaveslikeamoltehisfreedomofeleakes‘metalli’aductorofelectricity。Ashellofmetalli(withsomeheliumdissolvedinit)surroundingJupiter’scoreprobablyatsforabout260Earth-masses(80%ofJupiter’stotalmass),whereasaroundSaturhoughttopriseamoremodest41Earth-masses(justover40%ofSaturn’stotalmass)。Figure17illustratesthefulliructureofJupiter。

&ernalstructureofthegiaillbeevolvihepossibleexofUranus,theyallradiatemoreheattospatheyretheSun。Jupiterissomassivethatitcouldstillbeleakingoutasignifitofprimordialheattrappedwithisformation,butforSaturhisheatexcessshowsthatheatmustactuallybebeihin。Thediscyistete,sointerionmaystillbe。Thesettlihaerialinwards(allowiogrowwhilethesurroundingshellbeesthipurer)wouldvertgravitatioialeoheat。Suefromggrowthofcores(orinnercores)or,forSaturnonly,fromilingofheliumdropletsiallilayer。

17。Cut-awaydiagramshowingtheproposedinterhiheprincipaltroposphericcloud-topzht)as(dark)arelabelled

Atmospheres

position

Intrasttothereasoionaboutgiaerioftheiratmospheresdrawmoreoio。Thepositionofdthelayersbemeasuredbyopticalspectroscopy,whichisthestudyofhowsunlightofdifferehsisabsorbedatvariousdepthswithimosphere。Inaddition,theaveragemolecularmassateachdepthbedetermiofrefraexperiencedbyradiosignalstransmittedbyaspacecraftwhileitdisappearsfromviewbehi。Also,theGalileoentryprobemadevariousmeasuremeer’satmitsdest。Table6paresthechemipositionofthefiamospheres。Inadditiontothespecieslistedthere,eaallertracesofethyne(C2H2),Jupiterhasethene(C2H4),aurnbothhavephosphine(PH3),onoxide(dgermane(GeH4)。

&layerofuousUrauneisofmethaicles。ItistoowarmformethaionatJupiterandSatureadammoideoformthetopmostclouds。Thesetopcloudlayersareabout10kilometresthick,belowwhichthe‘air’probablybeesclearagain。Calssuggestthatier,thereshouldbeasedlayerofadeofammoniumhydrosulfide(NH4HS)about30kilometresbelow,andathirdcloudlayer,thistimeofwater(iceatthetop,liquidletsbelow)about20kilometreslowerstill。TheGalileoentryprobefoundprobableammoniumhydrosulfidecloudsatabhtdepthbutdidnotfindanywater-iesaythem;otherssaythattheprobepeoagapbetweendisuouswater-iceclouds。ThesamecloudlayersareexpectedatSaturn,butspacedaboutthreetimesfurtherapartbecauseofSatury。AmmcloudsareexpeethanecloudsofUraune。

Table6 Gasesdetetheatmospheresofthegias,showingthemeasuredproportionmadeupbyeach

&mosphericpressureatthetopofJupiter’sammoniacloudsisafactoroftwoorthreelessthanthesea-levelatmosphericpressureoh,whereasoplaoppressureisclosetoEarth’ssea-levelpressure。

Cir

Aglobalpatternofdsrunniheequatorisvisibleohroughasmalltelesilarpatteredlessdramatitheias。Smustplaysomeroleiionofthis,visible,partoftheiratmospheres,butitappearstobepoweredmostlybyiobetrolledbytheirrapidrotation。

Traditionally,thedarkbaoas‘belts’aerveningbrightbandsas‘zohehemaisandzonesonJupiterareindiFigure17。Becausethereisnosolidsurfacetoactasaframeofreferendspeedsongiasaremeasuredrelativetotheplaeofrotation。Ohecloud-topwindblowstotheeastatupto130metresperseostoftheEquatorialZoedgesoftheNorthaorialBeltssharethismotion,butthewindspeeddedultimatelyreverseswithdistanceawayfromtheequatoracrosseatiltheTropiesarereached,wherethewiiain,andsooedreversalsacrosseadzohepions。

InJupiter’szomosphereism,leadingtosationofammoniacloudshighup,wheretheynaturallyappearbright。versely,iheatmosphereismostlysinking,drawiopslower,sotoadepthwheretheylookdarker。Localexstothispatterifiedohegeneralrulezonesandsisscarcelyseemstoholdatalloplas,hericcirishardertofathom。Apligfafluengthevisibilityofzohepoorlyuoodnatureandabuevertrapoundsaddcolourtothedectedtoresultfromphotochemicalreas。Jupiter’svarioushuesofyellowandredcouldbecausedbysulfur(releasedphotochemieitherhydrogensulfideorammoniahydrosulfide),phosphorous(fromphosphine),orhydrazine(N2H4,madephotochemionia)。

Colourvariationsarelessprourn’satmosphere,aernofzosislesspromi。However,windspeedsarehigher,ingwindsinexetrespersedprevailingfor10°eithersideoftheequator。

RotatingstormsystemsarewellknownonbothJupiterandSaturfamousisJupiter’sGreatRedSpot。ThisbeseeninFigure3,asaraddlingthebouheSouthEquatorialBeltaropie。Itextends26,000kilometresfromeasttoiralstrudtakingaboutsixdaystorotateanticlockwise。Ithasbeeelescopicobservatio1830。SmallerstormsbemadeoutatavarietyofsbothJupiter(lookaloemperateBeltinFigure17)andSaturn。Aboutonceevery3summerinitsnortherurobedisfiguredbyagiantstormsystemthatbeginsasawhitespotor,butwithinamonthspreadtlraduallyfadingfromview。

&erandSaturnhaveayellowishusauneappearbluey-green。Thisisbecauseweseetheircloud-thadepthmethanegas,whichpreferentiallyabsorbsthelonger(red)wavelengthsoflight。

The82。1°CaxialtiltofUraremeseasonalvariations。Forexample,wheheotohavevisitedUrain1986,thesouthpolewasinfullsunlightandmostofthenorthernhemispherewassufferingdecadesofdarkssouthernhemispherelookeddisappointinglyblandontheVes,butastheUranianyearprogressedandtheSuoriseaoverawiderraudes,theglobebegaoresembletheias(Figure18)。In2007,Urahroughitsequinox,ahpole,followedgraduallybytherestofthesouthernhemisphere,begantodriftintolong-termdarkness,whichwillpeakwithsouthernmidwinterin2028。

&unewasrevealediailduringVoyager2’s1989fly-by,itresembledablueversionofJupiter。Therewasevenagiantstormsystemintheformofadarkspotjustsouthoftheequator,whichwasdubbedthe‘GreatDarkSpot’isfamousJovian。However,itprovedtobeshorter-lived,andhadvanishedby1994。UerandSaturorialtuneblowswest(oppositetotheplaion),asbeseewarddriftoftheGreatDarkSpotrelativetothesmaller,moresoutherlyspotinFigure18。

&ospheres

&hegiashasastroicfield。The‘magieune,whichistheeasureofaplaarymagicfield,is25timesgreaterthah’s。Uranus’sis38times,Saturn’sis582times,andJupiter’sis1,949timesgreater。Togehesefields,eaetmustazoridugfluidundergoingsomekindofvectivemotioerrestrialplahmagicfields(MerdEarth),theexplanationisafluidshelloftheirirohemagicfieldsofJupiterandSaturnareprobablygehemetallilayer,stirredintomotios’relativelyrapidrotation。PressuresaretoolowformetalliinUrauicfieldsarehardertoatfor,butareprobablycausedbymotioridug‘ice’oftheiroutercores。

18。Top:UraheHubbleSpaceTelesAugust1998(left)andJuly2ht)。Theorientatio’saxisrelativetotheSunisapparentfromthepatterm。Theregionarouhpolewasstillinsunlightin1998,buttheaxishadbeeotheSunby2006。High,brightcloudsareapparehinthe1998image,whichalsoshsaheiheringswereedge-onandinvisiblein2006,butinsteadweeularsatellites(Ariel)anditsshadow。Bottom:ttuneseenbyVitsapproa1989,reostexaeplaatireatDarkSpotandassociatedwispsofhigh,brightnitrogencirruscloudsarepromihegeneralbaure,andasmallerdarkspotfurthersouth

Animportantceofaplahaviicfield(liestoMerdtheEarthtoo)isthatitstheplainsideazoowhieticfieldliheSunotusuallypehiszoneiscalledthepla’s‘maghepathsedpartithesolarwiororolledbytheSuicfield,uhe‘bowshock’ofapla’smagosphere,whichdivertsthempastthepla。

Chargedpartigetthroughsometimes,especiallybyleakingbackuptheloail,down-Su。hesebeelledalongfieldliowardsthetopoftheatmosphere,wheretheirarrivalcausesglowsintheskycalledaurorae,wellkhandobservedalsoourn。

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