Standard

Earthward flow bursts, auroral streamers, and small expansions. / Nakamura, R.; Baumjohann, W.; Schödel, R.; Brittnacher, M.; Sergeev, V. A.; Kubyshkina, M.; Mukai, T.; Liou, K.

в: Journal of Geophysical Research: Space Physics, Том 106, № A6, 2000JA000306, 01.06.2001, стр. 10791-10802.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Nakamura, R, Baumjohann, W, Schödel, R, Brittnacher, M, Sergeev, VA, Kubyshkina, M, Mukai, T & Liou, K 2001, 'Earthward flow bursts, auroral streamers, and small expansions', Journal of Geophysical Research: Space Physics, Том. 106, № A6, 2000JA000306, стр. 10791-10802.

APA

Nakamura, R., Baumjohann, W., Schödel, R., Brittnacher, M., Sergeev, V. A., Kubyshkina, M., Mukai, T., & Liou, K. (2001). Earthward flow bursts, auroral streamers, and small expansions. Journal of Geophysical Research: Space Physics, 106(A6), 10791-10802. [2000JA000306].

Vancouver

Nakamura R, Baumjohann W, Schödel R, Brittnacher M, Sergeev VA, Kubyshkina M и пр. Earthward flow bursts, auroral streamers, and small expansions. Journal of Geophysical Research: Space Physics. 2001 Июнь 1;106(A6):10791-10802. 2000JA000306.

Author

Nakamura, R. ; Baumjohann, W. ; Schödel, R. ; Brittnacher, M. ; Sergeev, V. A. ; Kubyshkina, M. ; Mukai, T. ; Liou, K. / Earthward flow bursts, auroral streamers, and small expansions. в: Journal of Geophysical Research: Space Physics. 2001 ; Том 106, № A6. стр. 10791-10802.

BibTeX

@article{166d8a0bf48f4f7892e0c8fb1acd0c64,
title = "Earthward flow bursts, auroral streamers, and small expansions",
abstract = "Earthward flow bursts associated with small auroral expansions, including pseudobreakups, and auroral streamers are studied by using Geotail plasma and magnetic field data and Polar ultraviolet imager data. These flow bursts are accompanied by dipolarization and decrease in the plasma pressure, which are consistent with the characteristics of so-called bubbles, and have a timescale of 2.5 min on average. Based on a statistical study of the flow bursts, it is shown that the location of the flows are centered about 0.4 hour magnetic local time east of the center of auroral expansion and are localized with a width of 3 - 5 RE. This relationship supports the idea that a dawn-to-dusk polarization electric field is created in the bubble to enhance the flows. The flow bursts associated with the small expansions, which are mainly observed in the region earthward of 15 RE, show more distinct signatures of compression at the front side of the flow, which possibly leads to the stopping of these flows. Flow bursts related to auroral streamers, which are observed mainly tailward of 15 RE, take place during relatively thick plasma sheet configurations, and are accompanied by stronger flow shear.",
author = "R. Nakamura and W. Baumjohann and R. Sch{\"o}del and M. Brittnacher and Sergeev, {V. A.} and M. Kubyshkina and T. Mukai and K. Liou",
year = "2001",
month = jun,
day = "1",
language = "English",
volume = "106",
pages = "10791--10802",
journal = "Journal of Geophysical Research: Biogeosciences",
issn = "0148-0227",
publisher = "American Geophysical Union",
number = "A6",

}

RIS

TY - JOUR

T1 - Earthward flow bursts, auroral streamers, and small expansions

AU - Nakamura, R.

AU - Baumjohann, W.

AU - Schödel, R.

AU - Brittnacher, M.

AU - Sergeev, V. A.

AU - Kubyshkina, M.

AU - Mukai, T.

AU - Liou, K.

PY - 2001/6/1

Y1 - 2001/6/1

N2 - Earthward flow bursts associated with small auroral expansions, including pseudobreakups, and auroral streamers are studied by using Geotail plasma and magnetic field data and Polar ultraviolet imager data. These flow bursts are accompanied by dipolarization and decrease in the plasma pressure, which are consistent with the characteristics of so-called bubbles, and have a timescale of 2.5 min on average. Based on a statistical study of the flow bursts, it is shown that the location of the flows are centered about 0.4 hour magnetic local time east of the center of auroral expansion and are localized with a width of 3 - 5 RE. This relationship supports the idea that a dawn-to-dusk polarization electric field is created in the bubble to enhance the flows. The flow bursts associated with the small expansions, which are mainly observed in the region earthward of 15 RE, show more distinct signatures of compression at the front side of the flow, which possibly leads to the stopping of these flows. Flow bursts related to auroral streamers, which are observed mainly tailward of 15 RE, take place during relatively thick plasma sheet configurations, and are accompanied by stronger flow shear.

AB - Earthward flow bursts associated with small auroral expansions, including pseudobreakups, and auroral streamers are studied by using Geotail plasma and magnetic field data and Polar ultraviolet imager data. These flow bursts are accompanied by dipolarization and decrease in the plasma pressure, which are consistent with the characteristics of so-called bubbles, and have a timescale of 2.5 min on average. Based on a statistical study of the flow bursts, it is shown that the location of the flows are centered about 0.4 hour magnetic local time east of the center of auroral expansion and are localized with a width of 3 - 5 RE. This relationship supports the idea that a dawn-to-dusk polarization electric field is created in the bubble to enhance the flows. The flow bursts associated with the small expansions, which are mainly observed in the region earthward of 15 RE, show more distinct signatures of compression at the front side of the flow, which possibly leads to the stopping of these flows. Flow bursts related to auroral streamers, which are observed mainly tailward of 15 RE, take place during relatively thick plasma sheet configurations, and are accompanied by stronger flow shear.

UR - http://www.scopus.com/inward/record.url?scp=39449138811&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:39449138811

VL - 106

SP - 10791

EP - 10802

JO - Journal of Geophysical Research: Biogeosciences

JF - Journal of Geophysical Research: Biogeosciences

SN - 0148-0227

IS - A6

M1 - 2000JA000306

ER -

ID: 18138898