Hybrid-Vlasov simulation of auroral proton precipitation in the cusps: Comparison of northward and southward interplanetary magnetic field driving
Particle precipitation is a central aspect of space weather, as it strongly couples the magnetosphere and the ionosphere and can be responsible for radio signal disruption at high latitudes. We present the first hybrid-Vlasov simulations of proton precipitation in the polar cusps. We use two runs fr...
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doaj-5b09a7de98464143b48e1510264671a52021-04-02T14:30:38ZengEDP SciencesJournal of Space Weather and Space Climate2115-72512020-01-01105110.1051/swsc/2020053swsc200058Hybrid-Vlasov simulation of auroral proton precipitation in the cusps: Comparison of northward and southward interplanetary magnetic field drivingGrandin Maxime0https://orcid.org/0000-0002-6373-9756Turc Lucile1https://orcid.org/0000-0002-7576-3251Battarbee Markus2https://orcid.org/0000-0001-7055-551XGanse Urs3https://orcid.org/0000-0003-0872-1761Johlander Andreas4https://orcid.org/0000-0001-7714-1870Pfau-Kempf Yann5https://orcid.org/0000-0001-5793-7070Dubart Maxime6https://orcid.org/0000-0003-0549-0371Palmroth Minnahttps://orcid.org/0000-0003-4857-1227Department of Physics, University of HelsinkiDepartment of Physics, University of HelsinkiDepartment of Physics, University of HelsinkiDepartment of Physics, University of HelsinkiDepartment of Physics, University of HelsinkiDepartment of Physics, University of HelsinkiDepartment of Physics, University of HelsinkiParticle precipitation is a central aspect of space weather, as it strongly couples the magnetosphere and the ionosphere and can be responsible for radio signal disruption at high latitudes. We present the first hybrid-Vlasov simulations of proton precipitation in the polar cusps. We use two runs from the Vlasiator model to compare cusp proton precipitation fluxes during southward and northward interplanetary magnetic field (IMF) driving. The simulations reproduce well-known features of cusp precipitation, such as a reverse dispersion of precipitating proton energies, with proton energies increasing with increasing geomagnetic latitude under northward IMF driving, and a nonreversed dispersion under southward IMF driving. The cusp is also found more polewards in the northward IMF simulation than in the southward IMF simulation. In addition, we find that the bursty precipitation during southward IMF driving is associated with the transit of flux transfer events in the vicinity of the cusp. In the northward IMF simulation, dual lobe reconnection takes place. As a consequence, in addition to the high-latitude precipitation spot associated with the lobe reconnection from the same hemisphere, we observe lower-latitude precipitating protons which originate from the opposite hemisphere’s lobe reconnection site. The proton velocity distribution functions along the newly closed dayside magnetic field lines exhibit multiple proton beams travelling parallel and antiparallel to the magnetic field direction, which is consistent with previously reported observations with the Cluster spacecraft. In both runs, clear electromagnetic ion cyclotron waves are generated in the cusps and might further increase the calculated precipitating fluxes by scattering protons to the loss cone in the low-altitude cusp. Global kinetic simulations can improve the understanding of space weather by providing a detailed physical description of the entire near-Earth space and its internal couplings.https://www.swsc-journal.org/articles/swsc/full_html/2020/01/swsc200058/swsc200058.htmlpolar cuspparticle precipitationnumerical simulationsmagnetosphereemic waves |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Grandin Maxime Turc Lucile Battarbee Markus Ganse Urs Johlander Andreas Pfau-Kempf Yann Dubart Maxime Palmroth Minna |
spellingShingle |
Grandin Maxime Turc Lucile Battarbee Markus Ganse Urs Johlander Andreas Pfau-Kempf Yann Dubart Maxime Palmroth Minna Hybrid-Vlasov simulation of auroral proton precipitation in the cusps: Comparison of northward and southward interplanetary magnetic field driving Journal of Space Weather and Space Climate polar cusp particle precipitation numerical simulations magnetosphere emic waves |
author_facet |
Grandin Maxime Turc Lucile Battarbee Markus Ganse Urs Johlander Andreas Pfau-Kempf Yann Dubart Maxime Palmroth Minna |
author_sort |
Grandin Maxime |
title |
Hybrid-Vlasov simulation of auroral proton precipitation in the cusps: Comparison of northward and southward interplanetary magnetic field driving |
title_short |
Hybrid-Vlasov simulation of auroral proton precipitation in the cusps: Comparison of northward and southward interplanetary magnetic field driving |
title_full |
Hybrid-Vlasov simulation of auroral proton precipitation in the cusps: Comparison of northward and southward interplanetary magnetic field driving |
title_fullStr |
Hybrid-Vlasov simulation of auroral proton precipitation in the cusps: Comparison of northward and southward interplanetary magnetic field driving |
title_full_unstemmed |
Hybrid-Vlasov simulation of auroral proton precipitation in the cusps: Comparison of northward and southward interplanetary magnetic field driving |
title_sort |
hybrid-vlasov simulation of auroral proton precipitation in the cusps: comparison of northward and southward interplanetary magnetic field driving |
publisher |
EDP Sciences |
series |
Journal of Space Weather and Space Climate |
issn |
2115-7251 |
publishDate |
2020-01-01 |
description |
Particle precipitation is a central aspect of space weather, as it strongly couples the magnetosphere and the ionosphere and can be responsible for radio signal disruption at high latitudes. We present the first hybrid-Vlasov simulations of proton precipitation in the polar cusps. We use two runs from the Vlasiator model to compare cusp proton precipitation fluxes during southward and northward interplanetary magnetic field (IMF) driving. The simulations reproduce well-known features of cusp precipitation, such as a reverse dispersion of precipitating proton energies, with proton energies increasing with increasing geomagnetic latitude under northward IMF driving, and a nonreversed dispersion under southward IMF driving. The cusp is also found more polewards in the northward IMF simulation than in the southward IMF simulation. In addition, we find that the bursty precipitation during southward IMF driving is associated with the transit of flux transfer events in the vicinity of the cusp. In the northward IMF simulation, dual lobe reconnection takes place. As a consequence, in addition to the high-latitude precipitation spot associated with the lobe reconnection from the same hemisphere, we observe lower-latitude precipitating protons which originate from the opposite hemisphere’s lobe reconnection site. The proton velocity distribution functions along the newly closed dayside magnetic field lines exhibit multiple proton beams travelling parallel and antiparallel to the magnetic field direction, which is consistent with previously reported observations with the Cluster spacecraft. In both runs, clear electromagnetic ion cyclotron waves are generated in the cusps and might further increase the calculated precipitating fluxes by scattering protons to the loss cone in the low-altitude cusp. Global kinetic simulations can improve the understanding of space weather by providing a detailed physical description of the entire near-Earth space and its internal couplings. |
topic |
polar cusp particle precipitation numerical simulations magnetosphere emic waves |
url |
https://www.swsc-journal.org/articles/swsc/full_html/2020/01/swsc200058/swsc200058.html |
work_keys_str_mv |
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