Energetic Electron Pitch-angle Distributions in the Martian Space Environment: Pancake

We perform a statistical investigation of the occurrence rates of energetic electron (100–500 eV) pancake pitch-angle distributions (PADs) in the Martian space environment by utilizing 6 yr of MAVEN data. In the Martian ionosphere, we find the following: (1) at the same altitude in the terminator and night regions, the occurrences rates in the center of the southern magnetic anomaly regions are very low, but at the edges of strong magnetic fields, they increase significantly; (2) the occurrence rates of energetic electron perpendicular anisotropies on the Martian dayside increase with altitude; and (3) some closed magnetic lines in the 10°S–55°S, 30°W–125°W region at 400–800 km altitude gradually become open during the rotation of Mars from duskside to dawnside, while more closed magnetic lines are produced in the 40°S–65°S, 35°E–90°E region. In the Martian induced magnetosphere, we find the following: (1) the high-energy electron perpendicular anisotropy in the magnetosheath is the most significant; (2) the occurrence rates in the southern (Z MSO ≤−1 R M) magnetosheath are higher than those in the northern (Z MSO ≥ 1 R M) magnetosheath; (3) in the region of ∣Z MSO∣ < 0.5 R M, these high-energy electron pancake PADs are mainly concentrated in the magnetosheath region with Y MSO ∈ [−1.4RM, 2R M]; (4) the occurrence rates in the dawnside (Y MSO ≤−1 R M) magnetosheath are higher than those in the duskside (Y MSO ≥ 1 R M) magnetosheath; and (5) in the region of ∣Y MSO∣ < 0.5 R M, the occurrence rates throughout the magnetosheath are very high.

[1]  Y. Liu,et al.  Characteristics of Electron Pitch-angle Distribution in the Flapping Magnetotail , 2022, The Astrophysical Journal.

[2]  Y. Liu,et al.  First Observation of Lower Hybrid Drift Waves at the Edge of the Current Sheet in the Martian Magnetotail , 2022, The Astrophysical Journal.

[3]  Z. Wang,et al.  Electron Thermalization and Electrostatic Turbulence Caused by Flow Reversal in Dipolarizing Flux Tubes , 2022, The Astrophysical Journal.

[4]  Y. Liu,et al.  Electron Rolling-pin Distribution Inside Magnetic Hole , 2022, The Astrophysical Journal.

[5]  Z. Zhang,et al.  In Situ Detection of Kinetic-size Magnetic Holes in the Martian Magnetosheath , 2021, The Astrophysical Journal.

[6]  B. Ni,et al.  Bidirectional electron conic observations for photoelectrons in the Martian ionosphere , 2020, Earth and Planetary Physics.

[7]  E. Grigorenko,et al.  Magnetotail dipolarization fronts and particle acceleration: A review , 2019, Science China Earth Sciences.

[8]  B. Jakosky,et al.  The global current systems of the Martian induced magnetosphere , 2019, Nature Astronomy.

[9]  F. Sahraoui,et al.  The Role of Upper Hybrid Waves in the Magnetotail Reconnection Electron Diffusion Region , 2019, The Astrophysical Journal.

[10]  Xiaocan Li,et al.  Energetic Electron Acceleration in Unconfined Reconnection Jets , 2019, The Astrophysical Journal.

[11]  Y. Liu,et al.  Parallel Electron Heating by Tangential Discontinuity in the Turbulent Magnetosheath , 2019, The Astrophysical Journal.

[12]  A. Vaivads,et al.  Super-efficient Electron Acceleration by an Isolated Magnetic Reconnection , 2019, The Astrophysical Journal.

[13]  H. Fu,et al.  Electron Acceleration by Dipolarization Fronts and Magnetic Reconnection: A Quantitative Comparison , 2018 .

[14]  C. Russell,et al.  Magnetospheric Multiscale Observations of Electron Vortex Magnetic Hole in the Turbulent Magnetosheath Plasma , 2016, 1612.08787.

[15]  J. Rouzaud,et al.  The MAVEN Solar Wind Electron Analyzer , 2016 .

[16]  J. Connerney,et al.  The MAVEN Magnetic Field Investigation , 2015 .

[17]  A. Vaivads,et al.  Energetic electron acceleration by unsteady magnetic reconnection , 2013, Nature Physics.

[18]  Robert J. Lillis,et al.  Nightside electron precipitation at Mars: Geographic variability and dependence on solar wind conditions , 2013 .

[19]  M. Kelley,et al.  The Mars Atmosphere and Volatile Evolution (MAVEN) Mission , 2013 .

[20]  D. Mitchell,et al.  Tectonic implications of Mars crustal magnetism. , 2005, Proceedings of the National Academy of Sciences of the United States of America.

[21]  M. Acuna,et al.  Martian shock and magnetic pile-up boundary positions and shapes determined from the Phobos 2 and Mars Global Surveyor data sets , 2004 .

[22]  Ness,et al.  Global distribution of crustal magnetization discovered by the mars global surveyor MAG/ER experiment , 1999, Science.

[23]  Ness,et al.  Magnetic Field and Plasma Observations at Mars: Initial Results of the Mars Global Surveyor Mission , 1998, Science.