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Title: Global Ten-Moment Multifluid Simulations of the Solar Wind Interaction with Mercury: From the Planetary Conducting Core to the Dynamic Magnetosphere

Abstract

In this work, we explore for the first time the tightly coupled interior-magnetosphere system of Mercury by employing a three-dimensional ten-moment multifluid model. This novel fluid model incorporates the nonideal effects including the Hall effect, electron inertia, and tensorial pressures that are critical for collisionless magnetic reconnection; therefore, it is particularly well suited for investigating collisionless magnetic reconnection in Mercury's magnetotail and at the planet's magnetopause. Additionally, the model is able to reproduce the observed magnetic field vectors, field-aligned currents, and cross-tail current sheet asymmetry (beyond magnetohydrodynamic approach), and the simulation results are in good agreement with spacecraft observations. We also study the magnetospheric response of Mercury to a hypothetical extreme event with an enhanced solar wind dynamic pressure, which demonstrates the significance of induction effects resulting from the electromagnetically coupled interior. More interestingly, plasmoids (or flux ropes) are formed in Mercury's magnetotail during the event, indicating the highly dynamic nature of Mercury's magnetosphere.

Authors:
ORCiD logo [1]; ORCiD logo [1]; ORCiD logo [2]; ORCiD logo [1]; ORCiD logo [3]; ORCiD logo [4]; ORCiD logo [5]
  1. Princeton Univ., NJ (United States). Dept. of Astrophysical Sciences; Princeton Plasma Physics Lab. (PPPL), Princeton, NJ (United States). Princeton Center for Heliophysics
  2. Princeton Plasma Physics Lab. (PPPL), Princeton, NJ (United States). Princeton Center for Heliophysics
  3. Univ. of Michigan, Ann Arbor, MI (United States)
  4. NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States)
  5. Univ. of New Hampshire, Durham, NH (United States). Space Science Center
Publication Date:
Research Org.:
Princeton Plasma Physics Laboratory (PPPL), Princeton, NJ (United States)
Sponsoring Org.:
USDOE Office of Science (SC); National Aeronautics and Space Administration (NASA); National Science Foundation (NSF)
OSTI Identifier:
1648040
Alternate Identifier(s):
OSTI ID: 1573062
Grant/Contract Number:  
SC0006670; AGS-0962698; AGS-1338944; 80NSSC19K0621; NNH13AW51I; 80NSSC18K0288; AC05-00OR22725; AC02-05CH11231
Resource Type:
Accepted Manuscript
Journal Name:
Geophysical Research Letters
Additional Journal Information:
Journal Volume: 46; Journal Issue: 21; Journal ID: ISSN 0094-8276
Publisher:
American Geophysical Union
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES; Mercury's dynamic magnetosphere; induction response from Mercury's conducting core; ten-moment multifluid model; collisionless magnetic reconnection and flux ropes; field-aligned current; magnetotail asymmetry

Citation Formats

Dong, Chuanfei, Wang, Liang, Hakim, Ammar, Bhattacharjee, Amitava, Slavin, James A., DiBraccio, Gina A., and Germaschewski, Kai. Global Ten-Moment Multifluid Simulations of the Solar Wind Interaction with Mercury: From the Planetary Conducting Core to the Dynamic Magnetosphere. United States: N. p., 2019. Web. doi:10.1029/2019gl083180.
Dong, Chuanfei, Wang, Liang, Hakim, Ammar, Bhattacharjee, Amitava, Slavin, James A., DiBraccio, Gina A., & Germaschewski, Kai. Global Ten-Moment Multifluid Simulations of the Solar Wind Interaction with Mercury: From the Planetary Conducting Core to the Dynamic Magnetosphere. United States. https://doi.org/10.1029/2019gl083180
Dong, Chuanfei, Wang, Liang, Hakim, Ammar, Bhattacharjee, Amitava, Slavin, James A., DiBraccio, Gina A., and Germaschewski, Kai. Sun . "Global Ten-Moment Multifluid Simulations of the Solar Wind Interaction with Mercury: From the Planetary Conducting Core to the Dynamic Magnetosphere". United States. https://doi.org/10.1029/2019gl083180. https://www.osti.gov/servlets/purl/1648040.
@article{osti_1648040,
title = {Global Ten-Moment Multifluid Simulations of the Solar Wind Interaction with Mercury: From the Planetary Conducting Core to the Dynamic Magnetosphere},
author = {Dong, Chuanfei and Wang, Liang and Hakim, Ammar and Bhattacharjee, Amitava and Slavin, James A. and DiBraccio, Gina A. and Germaschewski, Kai},
abstractNote = {In this work, we explore for the first time the tightly coupled interior-magnetosphere system of Mercury by employing a three-dimensional ten-moment multifluid model. This novel fluid model incorporates the nonideal effects including the Hall effect, electron inertia, and tensorial pressures that are critical for collisionless magnetic reconnection; therefore, it is particularly well suited for investigating collisionless magnetic reconnection in Mercury's magnetotail and at the planet's magnetopause. Additionally, the model is able to reproduce the observed magnetic field vectors, field-aligned currents, and cross-tail current sheet asymmetry (beyond magnetohydrodynamic approach), and the simulation results are in good agreement with spacecraft observations. We also study the magnetospheric response of Mercury to a hypothetical extreme event with an enhanced solar wind dynamic pressure, which demonstrates the significance of induction effects resulting from the electromagnetically coupled interior. More interestingly, plasmoids (or flux ropes) are formed in Mercury's magnetotail during the event, indicating the highly dynamic nature of Mercury's magnetosphere.},
doi = {10.1029/2019gl083180},
journal = {Geophysical Research Letters},
number = 21,
volume = 46,
place = {United States},
year = {Sun Nov 03 00:00:00 EDT 2019},
month = {Sun Nov 03 00:00:00 EDT 2019}
}

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Works referencing / citing this record:

An extended MHD study of the 16 October 2015 MMS diffusion region crossing
text, January 2019