Energetic particle acceleration and transport with the novel Icarus plus PARADISE model

dc.contributor.authorHusidic Edin
dc.contributor.authorWijsen Nicolas
dc.contributor.authorBaratashvili Tinatin
dc.contributor.authorPoedts Stefaan
dc.contributor.authorVainio Rami
dc.contributor.organizationfi=avaruustutkimuslaboratorio|en=Space Research Laboratory|
dc.contributor.organizationfi=fysiikan ja tähtitieteen laitos|en=Department of Physics and Astronomy|
dc.contributor.organization-code1.2.246.10.2458963.20.47833719389
dc.contributor.organization-code1.2.246.10.2458963.20.55477946762
dc.converis.publication-id393368555
dc.converis.urlhttps://research.utu.fi/converis/portal/Publication/393368555
dc.date.accessioned2025-08-27T23:12:05Z
dc.date.available2025-08-27T23:12:05Z
dc.description.abstract<p>With the rise of satellites and mankind’s growing dependence on technology, there is an increasing awareness of space weather phenomena related to high-energy particles. Shock waves driven by coronal mass ejections (CMEs) and corotating interaction regions (CIRs) occasionally act as potent particle accelerators, generating hazardous solar energetic particles (SEPs) that pose risks to satellite electronics and astronauts. Numerical simulation tools capable of modelling and predicting large SEP events are thus highly demanded. We introduce the new Icarus + PARADISE model as an advancement of the previous EUHFORIA + PARADISE model. Icarus, based on the MPI-AMRVAC framework, is a three-dimensional magnetohydrodynamic code that models solar wind configurations from 0.1 au onwards, encompassing transient structures like CMEs or CIRs. Differing from EUHFORIA’s uniform-only grid, Icarus incorporates solution adaptive mesh refinement (AMR) and grid stretching. The particle transport code PARADISE propagates energetic particles as test particles through these solar wind configurations by solving the focused transport equation in a stochastic manner. We validate our new model by reproducing EUHFORIA + PARADISE results. This is done by modelling the acceleration and transport of energetic particles in a synthetic solar wind configuration containing an embedded CIR. Subsequently, we illustrate how the simulation results vary with grid resolution by employing different levels of AMR. The resulting intensity profiles illustrate increased particle acceleration with higher levels of AMR in the shock region, better capturing the effects of the shock.<br></p>
dc.identifier.eissn2115-7251
dc.identifier.jour-issn2115-7251
dc.identifier.olddbid203585
dc.identifier.oldhandle10024/186612
dc.identifier.urihttps://www.utupub.fi/handle/11111/40278
dc.identifier.urlhttps://www.swsc-journal.org/articles/swsc/full_html/2024/01/swsc230063/swsc230063.html
dc.identifier.urnURN:NBN:fi-fe2025082786126
dc.language.isoen
dc.okm.affiliatedauthorHusidic, Edin
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.publisherEDP Sciences
dc.publisher.countryFranceen_GB
dc.publisher.countryRanskafi_FI
dc.publisher.country-codeFR
dc.relation.articlenumber11
dc.relation.doi10.1051/swsc/2024009
dc.relation.ispartofjournalJournal of Space Weather and Space Climate
dc.relation.volume14
dc.source.identifierhttps://www.utupub.fi/handle/10024/186612
dc.titleEnergetic particle acceleration and transport with the novel Icarus plus PARADISE model
dc.year.issued2024

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