Research output: Contribution to journal › Article › peer-review
A new mechanism for interpreting the motion of auroral arcs in the nightside ionosphere. / Semenov, V. S.; Bogdanova, Y. V.; Rijnbeek, R. P.; Buchan, M. J.
In: Geophysical Research Letters, Vol. 26, No. 15, 1999GL900526, 01.08.1999, p. 2367-2370.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - A new mechanism for interpreting the motion of auroral arcs in the nightside ionosphere
AU - Semenov, V. S.
AU - Bogdanova, Y. V.
AU - Rijnbeek, R. P.
AU - Buchan, M. J.
PY - 1999/8/1
Y1 - 1999/8/1
N2 - A new mechanism is proposed for predicting and interpreting the motion of auroral arcs observed in the nightside ionosphere during the expansion phase of a substorm. This mechanism is centred on the idea that such arcs act as visible manifestations of the arrival of earthward-propagating shock waves in the near-Earth magnetosphere. These shock waves are generated at a near-Earth X-line, and propagate at the local Alfvén speed. Because of the non-uniform nature of the magnetised plasma in the magnetotail, dispersion results in a change in the shape of the wave fronts as the shocks propagate towards the ionosphere. Theoretical analysis shows that a variety of arc motions can occur as a result of this dispersion, depending on factors such as the reconnection rate, the location of the re-connection site, and gradients in the magnetic field strength and plasma density.
AB - A new mechanism is proposed for predicting and interpreting the motion of auroral arcs observed in the nightside ionosphere during the expansion phase of a substorm. This mechanism is centred on the idea that such arcs act as visible manifestations of the arrival of earthward-propagating shock waves in the near-Earth magnetosphere. These shock waves are generated at a near-Earth X-line, and propagate at the local Alfvén speed. Because of the non-uniform nature of the magnetised plasma in the magnetotail, dispersion results in a change in the shape of the wave fronts as the shocks propagate towards the ionosphere. Theoretical analysis shows that a variety of arc motions can occur as a result of this dispersion, depending on factors such as the reconnection rate, the location of the re-connection site, and gradients in the magnetic field strength and plasma density.
UR - http://www.scopus.com/inward/record.url?scp=0033429621&partnerID=8YFLogxK
U2 - 10.1029/1999GL900526
DO - 10.1029/1999GL900526
M3 - Article
AN - SCOPUS:0033429621
VL - 26
SP - 2367
EP - 2370
JO - Geophysical Research Letters
JF - Geophysical Research Letters
SN - 0094-8276
IS - 15
M1 - 1999GL900526
ER -
ID: 53087702