Magnetospheric Response to a Pressure Pulse in a Three‐Dimensional Hybrid‐Vlasov Simulation

Author:

Horaites K.1ORCID,Rintamäki E.1ORCID,Zaitsev I.1,Turc L.1ORCID,Grandin M.1ORCID,Cozzani G.1ORCID,Zhou H.1ORCID,Alho M.1ORCID,Suni J.1ORCID,Kebede F.1,Gordeev E.1,George H.12ORCID,Battarbee M.1ORCID,Bussov M.1ORCID,Dubart M.1,Ganse U.1ORCID,Papadakis K.1,Pfau‐Kempf Y.1ORCID,Tarvus V.1,Palmroth M.13ORCID

Affiliation:

1. Department of Physics University of Helsinki Helsinki Finland

2. Now at Laboratory for Atmospheric and Space Physics University of Colorado Boulder Boulder CO USA

3. Finnish Meteorological Institute Space and Earth Observation Centre Helsinki Finland

Abstract

AbstractVlasiator is a high‐performance ion‐kinetic code that is now conducting 3D hybrid‐Vlasov simulations of the global magnetosphere. We use Vlasiator to investigate the impact of a pressure pulse with southward‐oriented magnetic field on the Earth's magnetosphere. The simulation driving parameters are comparable to conditions that have led to geomagnetic storms. Our pressure pulse simulation reproduces many physical effects, namely the expansion of the auroral oval, the development of field‐aligned currents, enhanced particle precipitation near the open/closed field line boundary, and compression of Earth's magnetopause. This demonstrates the effectiveness of the hybrid‐Vlasov approach for moderate driving conditions. Our investigation of the time‐dependent magnetopause compression motivates a generalization of the existing theory. Specifically, we find that accounting for the finite transition time of the solar wind dynamic pressure improves the model's description of the magnetopause oscillations.

Funder

European Research Council

Partnership for Advanced Computing in Europe AISBL

Academy of Finland

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Geophysics

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