Specialissueeditorial-PlasmaInteractionswithSolarSystemObjects:AnticipatingRosetta,MavenandMarsOrbiterMission
A.J.Coates1.2,A.Wellbrock1,2andM.Yamauchi3
1.MullardSpaceScienceLaboratory,UniversityCollegeLondon,HolmburyStMary,Dorking,SurreyRH56NT,UK
2.CentreforPlanetaryScienceatUCL-Birkbeck,GowerSt,LondonWC1E6BT
3.SwedishInstituteofSpacePhysics,POBox812,SE-98128Kiruna,Sweden
Abstract
Withinoursolarsystem,theplanets,moons,cometsandasteroidsallhaveplasmainteractions.Theinteractiondependsonthenatureoftheobject,particularlythepresenceofanatmosphereandamagneticfield.Eventhesizeoftheobjectmattersthroughthefinitegyroradiuseffectandthescaleheightofcoldionsofexosphericorigin.Italsodependsontheupstreamconditions,includingpositionwithinthesolarwindorthepresencewithinaplanetarymagnetosphere.SoonafterESA'sRosettareachedcometChuryumov-Gerasimenko,NASA'sMavenandISRO'sMarsOrbiterMission(MOM)reachedMars,andESA'sVenusExpressmissionwascompleted,thisissueexploresourunderstandingofplasmainteractionswithcomets,Mars,Venus,andmoonsinthesolarsystem.Weexploretheprocesseswhichcharacterisetheinteractions,suchasionpickupandfielddraping,andtheireffectssuchasplasmaescape.Papersarebasedondatafromcurrentandrecentspacemissions,modellingandtheory,asweexploreourlocalpartofthe'plasmauniverse'.
Introduction
Theissuerepresentspredictionsformissionswhichhaverecentlyreachedtheirtargets.Someofthepaperswerepresentedatthe6thAlfvenConferenceonPlasmaInteractionswithSolarSystemObjects:AnticipatingRosetta,MAVENandMarsOrbiterMission,heldatUniversityCollegeLondonon7-11July2014(seeFigure1).Theconferenceincluded65oral(including19invited)papersand19posterpresentations.Thestructureoftheconferenceincludedsectionsoncomets,Mars,Venus,moons,missionsandcomparisonsbetweentheinteractions.Thespecialissuewasopentopaperpresentersandtothewiderscientificcommunity,andhasresultedinthe12papersincludedhere.
Summaryofpapers
Comets:
Ionpickupisoneessentialelementofacomet’sinteractionwiththesolarwind.AsacometnearstheSun,waterandothermoleculessublimeawayfromthenucleus.Theseareeventuallyionisedandthenareacceleratedbythesolarwindconvectiveelectricfield,andtheythengyratearoundthefieldtoformaringdistributioninvelocityspace.Thisisunstableandashelldistribution,andplasmawaves,result.Severalboundariesoccurincludingabowshockandacontactsurface.
Matteinietal.(2015)usehybridsimulationstostudytheionpickupprocess.Bisphericalandnon-gyrotropicdistributionsarestudied,andtheresultingwavesserveaspredictionsforcomet67P(Churyumov-Gerasimenko,Rosetta’starget).Gunelletal.(2015)usehybridsimulationsbutalsoincludeachargeddustpopulation,andmakepredictionsforthemorphology,effectivenessandtimingofdustaccelerationat67P.Nordheimetal.(2015)modelthesurfacepotentialandelectricfieldatthesurfaceof67Pat3.5and3AU,findingpositivepotentialsonthesunlitsideandthepossibilityofsubstantialcharginginthewake.
Venus:
Venushasadenseatmosphereandanionosphere,butnomagneticfield.Thesolarwindinteractionregionincludestheionopause,inducedmagnetosphere,drapedmagneticfield,asheathregionwiththermalisedanddeceleratedsolarwind,andabowshock.
Luhmannetal.(2015)re-examinePVOandVenusExpressdataandcomparewithMHDsimulationstoexploreapreviouslydiscoveredhemisphericbiasinthemagneticfieldlowinthewakeregion.Theyfindthatalthoughsomeaspectsoftheresultsareconsistentwithaweakglobalmagneticfield,thiscanberuledoutinpreferenceforothereffects,suchashemisphericasymmetriesintheinteractionorthepossibilityofexternalfielddiffusionthroughtheplanet.
Mars:
TheMarsinteractionwiththesolarwindissomewhatsimilartoVenusexceptthattheratiooftheiongyroradiustotheobstaclesizeislarger,andMarshascrustalmagneticfieldswhichdistorttheinteractiontosomeextent.Atmosphericescapeisakeyissueoverthe3.8billionyearssinceMarslostitsglobalmagneticfield,studiedoverthelastsolarcyclebyMarsExpressandstudiesarebeginningwiththecomprehensively-instrumentedMAVENmission.
Holmstrometal.(2015)useahybridmodeltostudytheMars-solarwindinteractiononalargescale,findingapolarplumeofionsandescapealongthetail.Theescaperateincreasesastheassumedproductionrateincreases,andcomparisonsaremadewithacomet.
Yamauchietal.(2015a)presentMarsExpressASPERA-3observationsoftheMartianforeshock.Theyfindprotonsand,forthefirsttime,oxygenionsupstreamofthebowshock.Theydiscusshowthismaybeanadditionalescapemechanisminvolvingaccelerationinthebowshock-sheathregion.
Yamauchietal.(2015b)studypickupprotonsinthesolarwindnearMarsover8years,findingthattheamountofpickupionsisrelatedtotheSun-Marsdistance.ThisindicatesthattheUVfluxplaysamajorroleinpickupionproductionbutothereffectsareimportanttoo,atopicforMAVEN.
Xuetal.(2015)studytheproductionofphotoelectronsintheMartianionosphereusingthreedifferentsolarirradiancemodels.Theyfindafactor~2variationinthemodelledphotoelectronfluxes.
Vaisberg(2015)reviewsionescapemechanismsatMars,includingpickupions,tailescapeandionosphericescape.Simulationsarealsodiscussed,discrepanciesbetweenobservationsandsimulationsareidentified,andsuggestionsaremadeforfutureresearchincludingMAVENandMOM.
Fraenzetal.(2015)useASPERA-3andMARSISdatatoestimateMartianescaperates.Byincludingthepreviouslyunderestimatedcoldioncomponenttheyfindhighertotalescaperates(2.8±0.4x1025s-1)thanpreviouslyreported,andinagreementwithsomemodellingstudies.
Alhoetal.(2015)useahybridsimulationtostudytheshieldingeffectofanearlyMarsmagneticfield,startingatareasonableassumedlevelanddecliningtotoday’sinducedmagnetosphere.TheyfindsignificantshieldingispresentonearlyMarsagainstsolarenergeticparticles,causedbythesolarwindinteraction.
Moons:
Poppeetal.(2015)studythechargingenvironmentofairlessbodiesforarangeofanglesbetweentheincidentflowandthesolardirection,relevantforthemoonsofMarsandsomeouterplanetmoonsaswellasEarth’sMoon.Theyfindsomecomplexpotentialstructurescanexistnearthesurfaces.
Acknowledgments
WewishtothanktheScientificandLocalOrganisingCommitteesfortheirhelpwiththeconference,andtherefereesfortheirhelpwiththeindividualpapers.WeparticularlythanktheLOCfortheirhardworkbefore,duringandafterthemeeting.Wethankthesponsorsofthemeetingfortheirgeneroussupport–ESA(includingtheRosettaproject),RAS,STFC,UKSA,RosettaprojectandADS(UK)
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Figure1-Attendeesatthe6thAlfvénConference,10July2014