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Excitation and decay of solar-wind driven flows in the magnetosphere-ionosphere system

Stanley W. H. Cowley, +1 more
- 01 Feb 1992 - 
- Vol. 10, pp 103-115
TLDR
In this paper, the authors considered the high-latitude ionospheric flows and their excitation and decay and proposed a flow-free equilibrium configuration for a magnetosphere which contains a given (arbitrary) amount of open flux.
Abstract
Basic concepts of the form of high-latitude ionospheric flows and their excitation and decay are discussed in the light of recent high time-resolution measurements made by ground-based radars. It is first pointed out that it is in principle impossible to adequately parameterize these flows by any single quantity derived from concurrent interplanetary conditions. Rather, even at its simplest, the flow must be considered to consist of two basic time-dependent components. The first is the flow driven by magnetopause coupling processes alone, principally by dayside reconnection. These flows may indeed be reasonably parameterized in terms of concurrent near-Earth interplanetary conditions, principally by the interplanetary magnetic field (IMF) vector. The second is the flow driven by tail reconnection alone. As a first approximation these flows may also be parameterized in terms of interplanetary conditions, principally the north-south component of the IMF, but with a delay in the flow response of around 30-60 min relative to the IMF. A delay in the tail response of this order must be present due to the finite speed of information propagation in the system, and we show how "growth" and "decay" of the field and flow configuration then follow as natural consequences. To discuss the excitation and decay of the two reconnection-driven components of the flow we introduce that concept of a flow-free equilibrium configuration for a magnetosphere which contains a given (arbitrary) amount of open flux. Reconnection events act either to create or destroy open flux, thus causing departures of the system from the equilibrium configuration. Flow is then excited which moves the system back towards equilibrium with the changed amount of open flux. We estimate that the overall time scale associated with the excitation and decay of the flow is about 15 min. The response of the system to both impulsive (flux transfer event) and continuous reconnection is discussed in these terms.

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Citations
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Journal ArticleDOI

Motion of the dayside polar cap boundary during substorm cycles: II. Generation of poleward-moving events and polar cap patches by pulses in the magnetopause reconnection rate

TL;DR: In this paper, the formation of ionospheric polar cap patches and their relationship to the magnetopause reconnection pulses identified in the companion paper by Lockwood et al. were studied using data from the EISCAT (European Incoherent Scatter) VHF and CUTLASS (Cooperative UK Twin-Located Auroral Sounding System) HF radars.
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Observational properties of dayside throat aurora and implications on the possible generation mechanisms

TL;DR: In this paper, the authors used 7'year continuous auroral observations obtained at Yellow River Station (magnetic latitude 76.24°N) to investigate the ionospheric signature of redistribution of reconnection rate on the magnetopause by cold magnetospheric plasma.
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Solar-wind-driven pulsed magnetic reconnection at the dayside magnetopause, Pc5 compressional oscillations, and field line resonances

TL;DR: A series of observations by satellites of the solar wind and magnetosphere, by HF radars of the F region, and by ground-based magnetometers of E region currents are presented in this article.
Journal ArticleDOI

Dayside and nightside contributions to the cross polar cap potential: placing an upper limit on a viscous-like interaction

TL;DR: In this paper, it was shown that Φ PC does not decrease to zero even for strongly northward IMF B z, and that this is the consequence of flows excited by tail reconnection.
Journal ArticleDOI

Geomagnetic storms over the last solar cycle: A superposed epoch analysis

TL;DR: In this article, the results of a superposed epoch analysis of geomagnetic storms over the last solar cycle were discussed, where the corresponding solar wind (SW) onset mechanisms were located by means of 1 min ACE OMNI data.
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