Formation of Foreshock Transients and Associated Secondary Shocks

Upstream of shocks, the foreshock is filled with hot ions. When these ions are concentrated and thermalized around a discontinuity, a diamagnetic cavity bounded by compressional boundaries, referred to as a foreshock transient, forms. Sometimes, the upstream compressional boundary can further steepen into a secondary shock, which has been observed to accelerate particles and contribute to the primary shock acceleration. However, secondary shock formation conditions and processes are not fully understood. Using particle-in-cell simulations, we reveal how secondary shocks are formed. From 1D simulations, we show that electric fields play a critical role in shaping the shock’s magnetic field structure, as well as in coupling the energy of hot ions to that of the shock. We demonstrate that larger thermal speed and concentration ratio of hot ions favor the formation of a secondary shock. From a more realistic 2D simulation, we examine how a discontinuity interacts with foreshock ions leading to the formation of a foreshock transient and a secondary shock. Our results imply that secondary shocks are more likely to occur at primary shocks with higher Mach number. With the secondary shock’s previously proven ability to accelerate particles in cooperation with a planetary bow shock, it is even more appealing to consider them in particle acceleration of high Mach number astrophysical shocks.

[1]  B. Mauk,et al.  Microscopic, Multipoint Characterization of Foreshock Bubbles With Magnetospheric Multiscale (MMS) , 2020, Journal of Geophysical Research: Space Physics.

[2]  V. Angelopoulos,et al.  Magnetospheric Multiscale (MMS) Observations of Magnetic Reconnection in Foreshock Transients , 2020, Journal of Geophysical Research: Space Physics.

[3]  V. Angelopoulos,et al.  Relativistic electrons generated at Earth’s quasi-parallel bow shock , 2019, Science Advances.

[4]  C. Niemann,et al.  Three Regimes and Four Modes for the Resonant Saturation of Parallel Ion-beam Instabilities , 2019, The Astrophysical Journal.

[5]  M. Balikhin,et al.  The First Direct Observational Confirmation of Kinematic Collisionless Relaxation in Very Low Mach Number Shocks Near the Earth , 2019, Journal of Geophysical Research: Space Physics.

[6]  J. G. Sample,et al.  The Space Physics Environment Data Analysis System (SPEDAS) , 2019, Space Science Reviews.

[7]  D. Baker,et al.  Autogenous and efficient acceleration of energetic ions upstream of Earth’s bow shock , 2018, Nature.

[8]  V. Angelopoulos,et al.  Ion Acceleration Inside Foreshock Transients , 2018 .

[9]  V. Angelopoulos,et al.  Fermi acceleration of electrons inside foreshock transient cores , 2017, 1706.05047.

[10]  V. Angelopoulos,et al.  Statistical study of particle acceleration in the core of foreshock transients , 2017, 1706.04993.

[11]  C. Niemann,et al.  Collisionless momentum transfer in space and astrophysical explosions , 2017, Nature Physics.

[12]  V. Angelopoulos,et al.  Relativistic Electrons Produced by Foreshock Disturbances Observed Upstream of Earth's Bow Shock. , 2016, Physical review letters.

[13]  V. Angelopoulos,et al.  Observations of a new foreshock region upstream of a foreshock bubble's shock , 2016 .

[14]  M. Gedalin Collisionless relaxation of non-gyrotropic downstream ion distributions: dependence on shock parameters , 2015 .

[15]  B. Jakosky,et al.  A hot flow anomaly at Mars , 2015 .

[16]  W. Gekelman,et al.  Electrostatic structure of a magnetized laser-produced plasma. , 2015, Physical review. E, Statistical, nonlinear, and soft matter physics.

[17]  V. Angelopoulos,et al.  THEMIS observations of tangential discontinuity‐driven foreshock bubbles , 2015 .

[18]  T. Horbury,et al.  Global impacts of a Foreshock Bubble: Magnetosheath, magnetopause and ground-based observations , 2014, 1409.0390.

[19]  V. Angelopoulos,et al.  First observations of foreshock bubbles upstream of Earth's bow shock: Characteristics and comparisons to HFAs , 2013 .

[20]  A. Szabo,et al.  Shocklets, SLAMS, and field‐aligned ion beams in the terrestrial foreshock , 2012, 1207.5561.

[21]  E. Möbius,et al.  Ion Acceleration at the Earth’s Bow Shock , 2012 .

[22]  V. Angelopoulos,et al.  Multispacecraft observations of a foreshock-induced magnetopause disturbance exhibiting distinct plasma flows and an intense density compression , 2011 .

[23]  J. Giacalone,et al.  Interaction between inclined current sheets and the heliospheric termination shock , 2010 .

[24]  N. Omidi,et al.  Foreshock bubbles and their global magnetospheric impacts , 2010 .

[25]  S. Schwartz,et al.  Hot flow anomalies at Saturn's bow shock , 2009 .

[26]  R. Treumann Fundamentals of collisionless shocks for astrophysical application, 1. Non-relativistic shocks , 2009 .

[27]  D. Sibeck,et al.  Formation of hot flow anomalies and solitary shocks , 2007 .

[28]  R. Treumann,et al.  The Foreshock , 2005 .

[29]  Y. Lin Global hybrid simulation of hot flow anomalies near the bow shock and in the magnetosheath , 2002 .

[30]  Jean-Luc Vay,et al.  A new absorbing layer boundary condition for the wave equation , 2000 .

[31]  M. Dunlop,et al.  Conditions for the formation of hot flow anomalies at Earth's bow shock , 2000 .

[32]  David G. Sibeck,et al.  Comprehensive study of the magnetospheric response to a hot flow anomaly , 1999 .

[33]  M. Thomsen,et al.  Hybrid simulation of the formation of a hot flow anomaly , 1991 .

[34]  H. Lühr,et al.  Ion thermalization in quasi-perpendicular shocks involving reflected ions , 1990 .

[35]  S. Schwartz,et al.  Ion distributions and thermalization at perpendicular and quasi‐perpendicular supercritical collisionless shocks , 1989 .

[36]  D. Burgess On the effect of a tangential discontinuity on ions specularly reflected at an oblique shock , 1989 .

[37]  C. Russell,et al.  On the origin of hot diamagnetic cavities near the Earth's bow shock , 1988 .

[38]  K. Papadopoulos,et al.  Collisionless coupling in the AMPTE artificial comet , 1987 .

[39]  C. Russell,et al.  Hot, diamagnetic cavities upstream from the Earth's bow shock , 1986 .

[40]  B. Klecker,et al.  COMETARY PICK-UP IONS OBSERVED NEAR GIACOBINI-ZINNER. , 1986 .

[41]  S. Schwartz,et al.  An active current sheet in the solar wind , 1985, Nature.

[42]  C. Russell,et al.  Evolution of ion distributions across the nearly perpendicular bow shock: Specularly and non‐specularly reflected‐gyrating ions , 1983 .

[43]  B. Brosowski,et al.  The interaction of the solar wind with a comet , 1967 .