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    Rights statement: An edited version of this paper was published by AGU. Copyright 2018 American Geophysical Union. Kimura, T., Hiraki, Y., Tao, C., Tsuchiya, F., Delamere, P. A., Yoshioka, K., et al. (2018). Response of Jupiter's aurora to plasma mass loading rate monitored by the Hisaki satellite during volcanic eruptions at Io. Journal of Geophysical Research: Space Physics, 123, 1885–1899. https://doi.org/10.1002/2017JA025029 To view the published open abstract, go to http://dx.doi.org and enter the DOI.

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Response of Jupiter's Aurora to Plasma Mass Loading Rate Monitored by the Hisaki Satellite During Volcanic Eruptions at Io

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Response of Jupiter's Aurora to Plasma Mass Loading Rate Monitored by the Hisaki Satellite During Volcanic Eruptions at Io. / Kimura, T.; Hiraki, Y.; Tao, C. et al.
In: Journal of Geophysical Research: Space Physics, Vol. 123, No. 3, 03.2018, p. 1885-1899.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Kimura, T, Hiraki, Y, Tao, C, Tsuchiya, F, Delamere, PA, Yoshioka, K, Murakami, G, Yamazaki, A, Kita, H, Badman, SV, Fukazawa, K, Yoshikawa, I & Fujimoto, M 2018, 'Response of Jupiter's Aurora to Plasma Mass Loading Rate Monitored by the Hisaki Satellite During Volcanic Eruptions at Io', Journal of Geophysical Research: Space Physics, vol. 123, no. 3, pp. 1885-1899. https://doi.org/10.1002/2017JA025029

APA

Kimura, T., Hiraki, Y., Tao, C., Tsuchiya, F., Delamere, P. A., Yoshioka, K., Murakami, G., Yamazaki, A., Kita, H., Badman, S. V., Fukazawa, K., Yoshikawa, I., & Fujimoto, M. (2018). Response of Jupiter's Aurora to Plasma Mass Loading Rate Monitored by the Hisaki Satellite During Volcanic Eruptions at Io. Journal of Geophysical Research: Space Physics, 123(3), 1885-1899. https://doi.org/10.1002/2017JA025029

Vancouver

Kimura T, Hiraki Y, Tao C, Tsuchiya F, Delamere PA, Yoshioka K et al. Response of Jupiter's Aurora to Plasma Mass Loading Rate Monitored by the Hisaki Satellite During Volcanic Eruptions at Io. Journal of Geophysical Research: Space Physics. 2018 Mar;123(3):1885-1899. Epub 2018 Feb 27. doi: 10.1002/2017JA025029

Author

Kimura, T. ; Hiraki, Y. ; Tao, C. et al. / Response of Jupiter's Aurora to Plasma Mass Loading Rate Monitored by the Hisaki Satellite During Volcanic Eruptions at Io. In: Journal of Geophysical Research: Space Physics. 2018 ; Vol. 123, No. 3. pp. 1885-1899.

Bibtex

@article{ffc62408e12f467c882a829a27cd21b1,
title = "Response of Jupiter's Aurora to Plasma Mass Loading Rate Monitored by the Hisaki Satellite During Volcanic Eruptions at Io",
abstract = "The production and transport of plasma mass are essential processes in the dynamics of planetary magnetospheres. At Jupiter, it is hypothesized that Io's volcanic plasma carried out of the plasma torus is transported radially outward in the rotating magnetosphere and is recurrently ejected as plasmoid via tail reconnection. The plasmoid ejection is likely associated with particle energization, radial plasma flow, and transient auroral emissions. However, it has not been demonstrated that plasmoid ejection is sensitive to mass loading because of the lack of simultaneous observations of both processes. We report the response of plasmoid ejection to mass loading during large volcanic eruptions at Io in 2015. Response of the transient aurora to the mass loading rate was investigated based on a combination of Hisaki satellite monitoring and a newly developed analytic model. We found that the transient aurora frequently recurred at a 2-6day period in response to a mass loading increase from 0.3 to 0.5t/s. In general, the recurrence of the transient aurora was not significantly correlated with the solar wind, although there was an exceptional event with a maximum emission power of similar to 10TW after the solar wind shock arrival. The recurrence of plasmoid ejection requires the precondition that an amount comparable to the total mass of magnetosphere, similar to 1.5Mt, is accumulated in the magnetosphere. A plasmoid mass of more than 0.1Mt is necessary in case that the plasmoid ejection is the only process for mass release.",
keywords = "Jupiter, aurora, Io, volcano, plasma, transport, CASSINI UVIS OBSERVATIONS, JOVIAN INNER MAGNETOSPHERE, INTERCHANGE INSTABILITY, AZIMUTHAL VARIABILITY, RADIAL VARIATIONS, PARTICLE BURSTS, IOGENIC PLASMA, JANUARY 2014, TORUS, TRANSPORT",
author = "T. Kimura and Y. Hiraki and C. Tao and F. Tsuchiya and Delamere, {P. A.} and K. Yoshioka and G. Murakami and A. Yamazaki and H. Kita and Badman, {S. V.} and K. Fukazawa and I. Yoshikawa and M. Fujimoto",
note = "An edited version of this paper was published by AGU. Copyright 2018 American Geophysical Union. Kimura, T., Hiraki, Y., Tao, C., Tsuchiya, F., Delamere, P. A., Yoshioka, K., et al. (2018). Response of Jupiter's aurora to plasma mass loading rate monitored by the Hisaki satellite during volcanic eruptions at Io. Journal of Geophysical Research: Space Physics, 123, 1885–1899. https://doi.org/10.1002/2017JA025029 To view the published open abstract, go to http://dx.doi.org and enter the DOI.",
year = "2018",
month = mar,
doi = "10.1002/2017JA025029",
language = "English",
volume = "123",
pages = "1885--1899",
journal = "Journal of Geophysical Research: Space Physics",
issn = "2169-9380",
publisher = "Blackwell Publishing Ltd",
number = "3",

}

RIS

TY - JOUR

T1 - Response of Jupiter's Aurora to Plasma Mass Loading Rate Monitored by the Hisaki Satellite During Volcanic Eruptions at Io

AU - Kimura, T.

AU - Hiraki, Y.

AU - Tao, C.

AU - Tsuchiya, F.

AU - Delamere, P. A.

AU - Yoshioka, K.

AU - Murakami, G.

AU - Yamazaki, A.

AU - Kita, H.

AU - Badman, S. V.

AU - Fukazawa, K.

AU - Yoshikawa, I.

AU - Fujimoto, M.

N1 - An edited version of this paper was published by AGU. Copyright 2018 American Geophysical Union. Kimura, T., Hiraki, Y., Tao, C., Tsuchiya, F., Delamere, P. A., Yoshioka, K., et al. (2018). Response of Jupiter's aurora to plasma mass loading rate monitored by the Hisaki satellite during volcanic eruptions at Io. Journal of Geophysical Research: Space Physics, 123, 1885–1899. https://doi.org/10.1002/2017JA025029 To view the published open abstract, go to http://dx.doi.org and enter the DOI.

PY - 2018/3

Y1 - 2018/3

N2 - The production and transport of plasma mass are essential processes in the dynamics of planetary magnetospheres. At Jupiter, it is hypothesized that Io's volcanic plasma carried out of the plasma torus is transported radially outward in the rotating magnetosphere and is recurrently ejected as plasmoid via tail reconnection. The plasmoid ejection is likely associated with particle energization, radial plasma flow, and transient auroral emissions. However, it has not been demonstrated that plasmoid ejection is sensitive to mass loading because of the lack of simultaneous observations of both processes. We report the response of plasmoid ejection to mass loading during large volcanic eruptions at Io in 2015. Response of the transient aurora to the mass loading rate was investigated based on a combination of Hisaki satellite monitoring and a newly developed analytic model. We found that the transient aurora frequently recurred at a 2-6day period in response to a mass loading increase from 0.3 to 0.5t/s. In general, the recurrence of the transient aurora was not significantly correlated with the solar wind, although there was an exceptional event with a maximum emission power of similar to 10TW after the solar wind shock arrival. The recurrence of plasmoid ejection requires the precondition that an amount comparable to the total mass of magnetosphere, similar to 1.5Mt, is accumulated in the magnetosphere. A plasmoid mass of more than 0.1Mt is necessary in case that the plasmoid ejection is the only process for mass release.

AB - The production and transport of plasma mass are essential processes in the dynamics of planetary magnetospheres. At Jupiter, it is hypothesized that Io's volcanic plasma carried out of the plasma torus is transported radially outward in the rotating magnetosphere and is recurrently ejected as plasmoid via tail reconnection. The plasmoid ejection is likely associated with particle energization, radial plasma flow, and transient auroral emissions. However, it has not been demonstrated that plasmoid ejection is sensitive to mass loading because of the lack of simultaneous observations of both processes. We report the response of plasmoid ejection to mass loading during large volcanic eruptions at Io in 2015. Response of the transient aurora to the mass loading rate was investigated based on a combination of Hisaki satellite monitoring and a newly developed analytic model. We found that the transient aurora frequently recurred at a 2-6day period in response to a mass loading increase from 0.3 to 0.5t/s. In general, the recurrence of the transient aurora was not significantly correlated with the solar wind, although there was an exceptional event with a maximum emission power of similar to 10TW after the solar wind shock arrival. The recurrence of plasmoid ejection requires the precondition that an amount comparable to the total mass of magnetosphere, similar to 1.5Mt, is accumulated in the magnetosphere. A plasmoid mass of more than 0.1Mt is necessary in case that the plasmoid ejection is the only process for mass release.

KW - Jupiter

KW - aurora

KW - Io

KW - volcano

KW - plasma

KW - transport

KW - CASSINI UVIS OBSERVATIONS

KW - JOVIAN INNER MAGNETOSPHERE

KW - INTERCHANGE INSTABILITY

KW - AZIMUTHAL VARIABILITY

KW - RADIAL VARIATIONS

KW - PARTICLE BURSTS

KW - IOGENIC PLASMA

KW - JANUARY 2014

KW - TORUS

KW - TRANSPORT

U2 - 10.1002/2017JA025029

DO - 10.1002/2017JA025029

M3 - Journal article

VL - 123

SP - 1885

EP - 1899

JO - Journal of Geophysical Research: Space Physics

JF - Journal of Geophysical Research: Space Physics

SN - 2169-9380

IS - 3

ER -