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Polar confinement of Saturn's magnetosphere revealed by in situ Cassini observations

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Polar confinement of Saturn's magnetosphere revealed by in situ Cassini observations. / Pilkington, Nathan. M.; Achilleos, N.; Arridge, C. S. et al.
In: Journal of Geophysical Research: Space Physics, Vol. 119, No. 4, 04.2014, p. 2858-2875.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Pilkington, NM, Achilleos, N, Arridge, CS, Masters, A, Sergis, N, Coates, AJ & Dougherty, MK 2014, 'Polar confinement of Saturn's magnetosphere revealed by in situ Cassini observations', Journal of Geophysical Research: Space Physics, vol. 119, no. 4, pp. 2858-2875. https://doi.org/10.1002/2014JA019774

APA

Pilkington, N. M., Achilleos, N., Arridge, C. S., Masters, A., Sergis, N., Coates, A. J., & Dougherty, M. K. (2014). Polar confinement of Saturn's magnetosphere revealed by in situ Cassini observations. Journal of Geophysical Research: Space Physics, 119(4), 2858-2875. https://doi.org/10.1002/2014JA019774

Vancouver

Pilkington NM, Achilleos N, Arridge CS, Masters A, Sergis N, Coates AJ et al. Polar confinement of Saturn's magnetosphere revealed by in situ Cassini observations. Journal of Geophysical Research: Space Physics. 2014 Apr;119(4):2858-2875. doi: 10.1002/2014JA019774

Author

Pilkington, Nathan. M. ; Achilleos, N. ; Arridge, C. S. et al. / Polar confinement of Saturn's magnetosphere revealed by in situ Cassini observations. In: Journal of Geophysical Research: Space Physics. 2014 ; Vol. 119, No. 4. pp. 2858-2875.

Bibtex

@article{3d1e70905f3e4199a4c6bcb8e2e0e67c,
title = "Polar confinement of Saturn's magnetosphere revealed by in situ Cassini observations",
abstract = "Plasma rotation plays a large role in determining the size and shape of Saturn's disk-like magnetosphere. A magnetosphere more confined to the equator in the polar regions is expected as a result of the interaction between this type of obstacle and the solar wind. In addition, at times away from equinox, a north-south asymmetry is expected where the magnetopause will be further confined in one hemisphere but less confined in the opposite hemisphere. Examining the extent of this confinement has been limited by a lack of high-latitude spacecraft observations. Here for the first time, direct evidence for polar confinement of Saturn's magnetopause has been observed using in situ data obtained by the Cassini spacecraft during a series of high-inclination orbits between 2007 and 2009. Following techniques established by previous authors, we assume an equilibrium between the solar wind dynamic pressure (which Cassini is generally unable to measure directly), and the magnetic plus plasma pressure inside the magnetosphere. This assumption thus allows us to estimate the upstream solar wind dynamic pressure (D-P) for a series of magnetopause crossings, and hence to determine the expected location and global shape of the magnetopause as a function of D-P. A clear divergence from the familiar axisymmetric models of the magnetosphere is observed, which may be characterized by an apparent flattening parameter of 0.81+0.03/-0.06 (representing a simple dilation of the nominal axisymmetric boundary along the Z(KSM) axis such that the extent is reduced by approximately 19% in this direction). This figure is insensitive to variations in D-P.",
keywords = "Saturn, magnetopause, magnetosphere, polar flattening, Cassini, solar wind, SOLAR-WIND FLOW, MAGNETIC-FIELD, BOW SHOCK, PERIODIC PERTURBATIONS, JOVIAN MAGNETOPAUSE, ENCELADUS, PLASMA, SHAPE, PLANETS, MODEL",
author = "Pilkington, {Nathan. M.} and N. Achilleos and Arridge, {C. S.} and A. Masters and N. Sergis and Coates, {A. J.} and Dougherty, {M. K.}",
note = "{\textcopyright}2014. The Authors.",
year = "2014",
month = apr,
doi = "10.1002/2014JA019774",
language = "English",
volume = "119",
pages = "2858--2875",
journal = "Journal of Geophysical Research: Space Physics",
issn = "2169-9380",
publisher = "Blackwell Publishing Ltd",
number = "4",

}

RIS

TY - JOUR

T1 - Polar confinement of Saturn's magnetosphere revealed by in situ Cassini observations

AU - Pilkington, Nathan. M.

AU - Achilleos, N.

AU - Arridge, C. S.

AU - Masters, A.

AU - Sergis, N.

AU - Coates, A. J.

AU - Dougherty, M. K.

N1 - ©2014. The Authors.

PY - 2014/4

Y1 - 2014/4

N2 - Plasma rotation plays a large role in determining the size and shape of Saturn's disk-like magnetosphere. A magnetosphere more confined to the equator in the polar regions is expected as a result of the interaction between this type of obstacle and the solar wind. In addition, at times away from equinox, a north-south asymmetry is expected where the magnetopause will be further confined in one hemisphere but less confined in the opposite hemisphere. Examining the extent of this confinement has been limited by a lack of high-latitude spacecraft observations. Here for the first time, direct evidence for polar confinement of Saturn's magnetopause has been observed using in situ data obtained by the Cassini spacecraft during a series of high-inclination orbits between 2007 and 2009. Following techniques established by previous authors, we assume an equilibrium between the solar wind dynamic pressure (which Cassini is generally unable to measure directly), and the magnetic plus plasma pressure inside the magnetosphere. This assumption thus allows us to estimate the upstream solar wind dynamic pressure (D-P) for a series of magnetopause crossings, and hence to determine the expected location and global shape of the magnetopause as a function of D-P. A clear divergence from the familiar axisymmetric models of the magnetosphere is observed, which may be characterized by an apparent flattening parameter of 0.81+0.03/-0.06 (representing a simple dilation of the nominal axisymmetric boundary along the Z(KSM) axis such that the extent is reduced by approximately 19% in this direction). This figure is insensitive to variations in D-P.

AB - Plasma rotation plays a large role in determining the size and shape of Saturn's disk-like magnetosphere. A magnetosphere more confined to the equator in the polar regions is expected as a result of the interaction between this type of obstacle and the solar wind. In addition, at times away from equinox, a north-south asymmetry is expected where the magnetopause will be further confined in one hemisphere but less confined in the opposite hemisphere. Examining the extent of this confinement has been limited by a lack of high-latitude spacecraft observations. Here for the first time, direct evidence for polar confinement of Saturn's magnetopause has been observed using in situ data obtained by the Cassini spacecraft during a series of high-inclination orbits between 2007 and 2009. Following techniques established by previous authors, we assume an equilibrium between the solar wind dynamic pressure (which Cassini is generally unable to measure directly), and the magnetic plus plasma pressure inside the magnetosphere. This assumption thus allows us to estimate the upstream solar wind dynamic pressure (D-P) for a series of magnetopause crossings, and hence to determine the expected location and global shape of the magnetopause as a function of D-P. A clear divergence from the familiar axisymmetric models of the magnetosphere is observed, which may be characterized by an apparent flattening parameter of 0.81+0.03/-0.06 (representing a simple dilation of the nominal axisymmetric boundary along the Z(KSM) axis such that the extent is reduced by approximately 19% in this direction). This figure is insensitive to variations in D-P.

KW - Saturn

KW - magnetopause

KW - magnetosphere

KW - polar flattening

KW - Cassini

KW - solar wind

KW - SOLAR-WIND FLOW

KW - MAGNETIC-FIELD

KW - BOW SHOCK

KW - PERIODIC PERTURBATIONS

KW - JOVIAN MAGNETOPAUSE

KW - ENCELADUS

KW - PLASMA

KW - SHAPE

KW - PLANETS

KW - MODEL

U2 - 10.1002/2014JA019774

DO - 10.1002/2014JA019774

M3 - Journal article

VL - 119

SP - 2858

EP - 2875

JO - Journal of Geophysical Research: Space Physics

JF - Journal of Geophysical Research: Space Physics

SN - 2169-9380

IS - 4

ER -