Magnetosheath jet evolution as a function of lifetime: global hybrid-Vlasov simulations compared to MMS observations
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Published:2021-03-12
Issue:2
Volume:39
Page:289-308
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ISSN:1432-0576
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Container-title:Annales Geophysicae
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language:en
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Short-container-title:Ann. Geophys.
Author:
Palmroth MinnaORCID, Raptis SavvasORCID, Suni JonasORCID, Karlsson Tomas, Turc LucileORCID, Johlander Andreas, Ganse UrsORCID, Pfau-Kempf YannORCID, Blanco-Cano XochitlORCID, Akhavan-Tafti MojtabaORCID, Battarbee MarkusORCID, Dubart MaximeORCID, Grandin MaximeORCID, Tarvus Vertti, Osmane Adnane
Abstract
Abstract. Magnetosheath jets are regions of high dynamic pressure, which can traverse
from the bow shock towards the magnetopause. Recent modelling efforts, limited
to a single jet and a single set of upstream conditions, have provided the
first estimations about how the jet parameters behave as a function of
position within the magnetosheath. Here we expand the earlier results by
doing the first statistical investigation of the jet dimensions and
parameters as a function of their lifetime within the magnetosheath. To verify
the simulation behaviour, we first identify jets from Magnetosphere
Multiscale (MMS) spacecraft data (6142 in total) and confirm the Vlasiator
jet general behaviour using statistics of 924 simulated individual jets. We
find that the jets in the simulation are in quantitative agreement with the
observations, confirming earlier findings related to jets using Vlasiator. The
jet density, dynamic pressure, and magnetic field intensity show a sharp jump
at the bow shock, which decreases towards the magnetopause. The jets appear
compressive and cooler than the magnetosheath at the bow shock, while during
their propagation towards the magnetopause they thermalise. Further, the shape
of the jets flatten as they progress through the magnetosheath. They are able
to maintain their flow velocity and direction within the magnetosheath flow,
and they end up preferentially to the side of the magnetosheath behind the
quasi-parallel shock. Finally, we find that Vlasiator jets during low solar
wind Alfvén Mach number MA are shorter in duration, smaller in their extent, and
weaker in terms of dynamic pressure and magnetic field intensity as compared
to the jets during high MA.
Funder
Horizon 2020 Luonnontieteiden ja Tekniikan Tutkimuksen Toimikunta European Research Council
Publisher
Copernicus GmbH
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geology,Astronomy and Astrophysics
Reference64 articles.
1. Archer, M. O. and Horbury, T. S.: Magnetosheath dynamic pressure enhancements: occurrence and typical properties, Ann. Geophys., 31, 319–331, https://doi.org/10.5194/angeo-31-319-2013, 2013. a, b, c, d, e, f, g, h, i, j, k, l 2. Archer, M. O., Horbury, T. S., and Eastwood, J. P.: Magnetosheath pressure pulses: Generation downstream of the bow shock from solar wind discontinuities, J. Geophys. Res.-Space, 117, A05228, https://doi.org/10.1029/2011JA017468, 2012. a 3. Archer, M. O., Hietala, H., Hartinger, M. D., Plaschke, F., and Angelopoulos, V.: Direct observations of a surface eigenmode of the dayside magnetopause, Nat. Commun., 10, 615, https://doi.org/10.1038/s41467-018-08134-5, 2019. a 4. Battarbee, M. and the Vlasiator team: Analysator: python analysis toolkit, Zenodo, https://doi.org/10.5281/zenodo.4462515, 2020. a 5. Battarbee, M., Ganse, U., Pfau-Kempf, Y., Turc, L., Brito, T., Grandin, M., Koskela, T., and Palmroth, M.: Non-locality of Earth's quasi-parallel bow shock: injection of thermal protons in a hybrid-Vlasov simulation, Ann. Geophys., 38, 625–643, https://doi.org/10.5194/angeo-38-625-2020, 2020. a, b
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