GUMICS-4 analysis of interplanetary coronal mass ejection impact on Earth during low and typical Mach number solar winds

dc.contributor.authorLakka A
dc.contributor.authorPulkkinen TI
dc.contributor.authorDimmock AP
dc.contributor.authorKilpua E
dc.contributor.authorAla-Lahti M
dc.contributor.authorHonkonen I
dc.contributor.authorPalmroth M
dc.contributor.authorRaukunen O
dc.contributor.organizationfi=fysiikan ja tähtitieteen laitos|en=Department of Physics and Astronomy|
dc.contributor.organization-code1.2.246.10.2458963.20.55477946762
dc.converis.publication-id41781911
dc.converis.urlhttps://research.utu.fi/converis/portal/Publication/41781911
dc.date.accessioned2022-10-27T11:55:41Z
dc.date.available2022-10-27T11:55:41Z
dc.description.abstractWe study the response of the Earth's magnetosphere to fluctuating solar wind conditions during interplanetary coronal mass ejections (ICMEs) using the Grand Unified Magnetosphere-Ionosphere Coupling Simulation (GUMICS-4). The two ICME events occurred on 15-16 July 2012 and 29-30 April 2014. During the strong 2012 event, the solar wind upstream values reached up to 35 particles cm(-3), speeds of up to 694 km s(-1), and an interplanetary magnetic field of up to 22 nT, giving a Mach number of 2.3. The 2014 event was a moderate one, with the corresponding upstream values of 30 particles cm(-3), 320 km s(-1) and 10 nT, indicating a Mach number of 5.8. We examine how the Earth's space environment dynamics evolves during both ICME events from both global and local perspectives, using well-established empirical models and in situ measurements as references. We show that on the large scale, and during moderate driving, the GUMICS-4 results are in good agreement with the reference values. However, the local values, especially during high driving, show more variation: such extreme conditions do not reproduce local measurements made deep inside the magnetosphere. The same appeared to be true when the event was run with another global simulation. The cross-polar cap potential (CPCP) saturation is shown to depend on the Alfven-Mach number of the upstream solar wind. However, care must be taken in interpreting these results, as the CPCP is also sensitive to the simulation resolution.
dc.format.pagerange561
dc.format.pagerange579
dc.identifier.jour-issn0992-7689
dc.identifier.olddbid172862
dc.identifier.oldhandle10024/155956
dc.identifier.urihttps://www.utupub.fi/handle/11111/54992
dc.identifier.urnURN:NBN:fi-fe2021042821961
dc.language.isoen
dc.okm.affiliatedauthorRaukunen, Osku
dc.okm.discipline114 Physical sciencesen_GB
dc.okm.discipline115 Astronomy and space scienceen_GB
dc.okm.discipline1171 Geosciencesen_GB
dc.okm.discipline114 Fysiikkafi_FI
dc.okm.discipline115 Avaruustieteet ja tähtitiedefi_FI
dc.okm.discipline1171 Geotieteetfi_FI
dc.okm.internationalcopublicationinternational co-publication
dc.okm.internationalityInternational publication
dc.okm.typeA1 ScientificArticle
dc.publisherCOPERNICUS GESELLSCHAFT MBH
dc.publisher.countryGermanyen_GB
dc.publisher.countrySaksafi_FI
dc.publisher.country-codeDE
dc.relation.doi10.5194/angeo-37-561-2019
dc.relation.ispartofjournalAnnales Geophysicae
dc.relation.issue4
dc.relation.volume37
dc.source.identifierhttps://www.utupub.fi/handle/10024/155956
dc.titleGUMICS-4 analysis of interplanetary coronal mass ejection impact on Earth during low and typical Mach number solar winds
dc.year.issued2019

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