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A survey of superthermal electron flux depressions, or “electron holes” within the illuminated Martian induced magnetosphere

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A survey of superthermal electron flux depressions, or “electron holes” within the illuminated Martian induced magnetosphere. / Hall, Benjamin Edward Stanley; Lester, Mark; Nichols, Jonathan et al.
In: Journal of Geophysical Research: Space Physics, Vol. 121, No. 5, 13.05.2016, p. 4835-4857.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Hall, BES, Lester, M, Nichols, J, Sánchez-Cano, B, Andrews, D, Opgenoorth, H & Fraenz, M 2016, 'A survey of superthermal electron flux depressions, or “electron holes” within the illuminated Martian induced magnetosphere', Journal of Geophysical Research: Space Physics, vol. 121, no. 5, pp. 4835-4857. https://doi.org/10.1002/2015JA021866

APA

Hall, B. E. S., Lester, M., Nichols, J., Sánchez-Cano, B., Andrews, D., Opgenoorth, H., & Fraenz, M. (2016). A survey of superthermal electron flux depressions, or “electron holes” within the illuminated Martian induced magnetosphere. Journal of Geophysical Research: Space Physics, 121(5), 4835-4857. https://doi.org/10.1002/2015JA021866

Vancouver

Hall BES, Lester M, Nichols J, Sánchez-Cano B, Andrews D, Opgenoorth H et al. A survey of superthermal electron flux depressions, or “electron holes” within the illuminated Martian induced magnetosphere. Journal of Geophysical Research: Space Physics. 2016 May 13;121(5):4835-4857. doi: 10.1002/2015JA021866

Author

Hall, Benjamin Edward Stanley ; Lester, Mark ; Nichols, Jonathan et al. / A survey of superthermal electron flux depressions, or “electron holes” within the illuminated Martian induced magnetosphere. In: Journal of Geophysical Research: Space Physics. 2016 ; Vol. 121, No. 5. pp. 4835-4857.

Bibtex

@article{e64567d9967948e4922f4e6334b6e394,
title = "A survey of superthermal electron flux depressions, or “electron holes” within the illuminated Martian induced magnetosphere",
abstract = "Since Mars lacks a global intrinsic magnetic field, the solar wind interacts directly with the Martian upper atmosphere and ionosphere. The presence of localized intense remnant crustal magnetic fields adds to this interaction, making the Martian plasma system a unique environment within the solar system. Rapid reductions in the electron flux, referred to as “electron holes,” occur within the Martian induced magnetosphere (IM). We present a statistical analysis of this phenomenon identified from proxy measurements of the electron flux derived from measurements by the Analyser of Space Plasmas and Energetic Neutral Atoms Electron Spectrometer experiment on board the Mars Express (MEX) spacecraft. The study is completed for the period of 9 February 2004 to 9 May 2014. Electron holes are observed within the IM in more than 56% of MEX orbits during this study period, occurring predominantly at altitudes less than 1300 km, with the majority in the negative X Mars-Centric Solar Orbital direction. The spatial distribution above the surface of Mars is observed to bear close resemblance to that of the crustal magnetic fields as predicted by the Cain et al. [2003] magnetic field model, suggesting that they play an important role in the formation of these phenomena.",
keywords = "Mars, Crustal Magnetic Fields, Electron Holes, Ionospheres, solar wind planetary interactions, unmagnetised bodies, Mars Express",
author = "Hall, {Benjamin Edward Stanley} and Mark Lester and Jonathan Nichols and Beatriz S{\'a}nchez-Cano and David Andrews and Hermann Opgenoorth and Markus Fraenz",
year = "2016",
month = may,
day = "13",
doi = "10.1002/2015JA021866",
language = "English",
volume = "121",
pages = "4835--4857",
journal = "Journal of Geophysical Research: Space Physics",
issn = "2169-9380",
publisher = "Blackwell Publishing Ltd",
number = "5",

}

RIS

TY - JOUR

T1 - A survey of superthermal electron flux depressions, or “electron holes” within the illuminated Martian induced magnetosphere

AU - Hall, Benjamin Edward Stanley

AU - Lester, Mark

AU - Nichols, Jonathan

AU - Sánchez-Cano, Beatriz

AU - Andrews, David

AU - Opgenoorth, Hermann

AU - Fraenz, Markus

PY - 2016/5/13

Y1 - 2016/5/13

N2 - Since Mars lacks a global intrinsic magnetic field, the solar wind interacts directly with the Martian upper atmosphere and ionosphere. The presence of localized intense remnant crustal magnetic fields adds to this interaction, making the Martian plasma system a unique environment within the solar system. Rapid reductions in the electron flux, referred to as “electron holes,” occur within the Martian induced magnetosphere (IM). We present a statistical analysis of this phenomenon identified from proxy measurements of the electron flux derived from measurements by the Analyser of Space Plasmas and Energetic Neutral Atoms Electron Spectrometer experiment on board the Mars Express (MEX) spacecraft. The study is completed for the period of 9 February 2004 to 9 May 2014. Electron holes are observed within the IM in more than 56% of MEX orbits during this study period, occurring predominantly at altitudes less than 1300 km, with the majority in the negative X Mars-Centric Solar Orbital direction. The spatial distribution above the surface of Mars is observed to bear close resemblance to that of the crustal magnetic fields as predicted by the Cain et al. [2003] magnetic field model, suggesting that they play an important role in the formation of these phenomena.

AB - Since Mars lacks a global intrinsic magnetic field, the solar wind interacts directly with the Martian upper atmosphere and ionosphere. The presence of localized intense remnant crustal magnetic fields adds to this interaction, making the Martian plasma system a unique environment within the solar system. Rapid reductions in the electron flux, referred to as “electron holes,” occur within the Martian induced magnetosphere (IM). We present a statistical analysis of this phenomenon identified from proxy measurements of the electron flux derived from measurements by the Analyser of Space Plasmas and Energetic Neutral Atoms Electron Spectrometer experiment on board the Mars Express (MEX) spacecraft. The study is completed for the period of 9 February 2004 to 9 May 2014. Electron holes are observed within the IM in more than 56% of MEX orbits during this study period, occurring predominantly at altitudes less than 1300 km, with the majority in the negative X Mars-Centric Solar Orbital direction. The spatial distribution above the surface of Mars is observed to bear close resemblance to that of the crustal magnetic fields as predicted by the Cain et al. [2003] magnetic field model, suggesting that they play an important role in the formation of these phenomena.

KW - Mars

KW - Crustal Magnetic Fields

KW - Electron Holes

KW - Ionospheres

KW - solar wind planetary interactions

KW - unmagnetised bodies

KW - Mars Express

U2 - 10.1002/2015JA021866

DO - 10.1002/2015JA021866

M3 - Journal article

VL - 121

SP - 4835

EP - 4857

JO - Journal of Geophysical Research: Space Physics

JF - Journal of Geophysical Research: Space Physics

SN - 2169-9380

IS - 5

ER -