Interplanetary Protons versus Interacting Protons in the 2017 September 10 Solar Eruptive Event

dc.contributor.authorKocharov L
dc.contributor.authorPesce-Rollins M
dc.contributor.authorLaitinen T
dc.contributor.authorMishev A
dc.contributor.authorKuhl P
dc.contributor.authorKlassen A
dc.contributor.authorJin M
dc.contributor.authorOmodei N
dc.contributor.authorLongo F
dc.contributor.authorWebb DF
dc.contributor.authorCane HV
dc.contributor.authorHeber B
dc.contributor.authorVainio R
dc.contributor.authorUsoskin I
dc.contributor.organizationfi=avaruustutkimuslaboratorio|en=Space Research Laboratory|
dc.contributor.organization-code1.2.246.10.2458963.20.47833719389
dc.converis.publication-id47015615
dc.converis.urlhttps://research.utu.fi/converis/portal/Publication/47015615
dc.date.accessioned2022-10-28T14:06:29Z
dc.date.available2022-10-28T14:06:29Z
dc.description.abstractWe analyze the relativistic proton emission from the Sun during the eruptive event on 2017 September 10, which caused a ground-level enhancement (GLE 72) registered by the worldwide network of neutron monitors. Using the neutron monitor data and interplanetary transport modeling both along and across interplanetary magnetic field (IMF) lines, we deduce parameters of the proton injection into the interplanetary medium. The inferred injection profile of the interplanetary protons is compared with the profile of the >100 MeV gamma-ray emission observed by the Fermi Large Area Telescope, attributed to pion production from the interaction of >300 MeV protons at the Sun. GLE 72 started with a prompt component that arrived along the IMF lines. This was followed by a more prolonged enhancement caused by protons arriving at the Earth across the IMF lines from the southwest. The interplanetary proton event is modeled using two sources-one source at the root of the Earth-connected IMF line and another source situated near the solar western limb. The maximum phase of the second injection of interplanetary protons coincides with the maximum phase of the prolonged >100 MeV gamma-ray emission that originated from a small area at the solar western limb, below the current sheet trailing the associated coronal mass ejection (CME). A possible common source of interacting protons and interplanetary protons is discussed in terms of proton acceleration at the CME bow shock versus coronal (re-)acceleration in the wake of the CME.
dc.identifier.eissn1538-4357
dc.identifier.jour-issn0004-637X
dc.identifier.olddbid186302
dc.identifier.oldhandle10024/169396
dc.identifier.urihttps://www.utupub.fi/handle/11111/36818
dc.identifier.urnURN:NBN:fi-fe2021042825119
dc.language.isoen
dc.okm.affiliatedauthorVainio, Rami
dc.okm.discipline115 Astronomy and space scienceen_GB
dc.okm.discipline115 Avaruustieteet ja tähtitiedefi_FI
dc.okm.internationalcopublicationinternational co-publication
dc.okm.internationalityInternational publication
dc.okm.typeA1 ScientificArticle
dc.publisherIOP PUBLISHING LTD
dc.publisher.countryUnited Kingdomen_GB
dc.publisher.countryBritanniafi_FI
dc.publisher.country-codeGB
dc.relation.articlenumberARTN 13
dc.relation.doi10.3847/1538-4357/ab684e
dc.relation.ispartofjournalAstrophysical Journal
dc.relation.issue1
dc.relation.volume890
dc.source.identifierhttps://www.utupub.fi/handle/10024/169396
dc.titleInterplanetary Protons versus Interacting Protons in the 2017 September 10 Solar Eruptive Event
dc.year.issued2020

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