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




TekijätHusidic Edin, Wijsen Nicolas, Baratashvili Tinatin, Poedts Stefaan, Vainio Rami

KustantajaEDP Sciences

Julkaisuvuosi2024

JournalJournal of Space Weather and Space Climate

Tietokannassa oleva lehden nimiJOURNAL OF SPACE WEATHER AND SPACE CLIMATE

Artikkelin numero11

Vuosikerta14

ISSN2115-7251

eISSN2115-7251

DOIhttps://doi.org/10.1051/swsc/2024009

Verkko-osoitehttps://www.swsc-journal.org/articles/swsc/full_html/2024/01/swsc230063/swsc230063.html

Rinnakkaistallenteen osoitehttps://research.utu.fi/converis/portal/detail/Publication/393368555

Preprintin osoitehttps://arxiv.org/abs/2404.12164


Tiivistelmä

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.


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Last updated on 2025-13-02 at 10:57