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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
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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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Time-of-day/time-of-year response functions of planetary geomagnetic indices

TL;DR: In this paper, the effect of the position of a geomagnetic observatory on its sensitivity to solar forcing is investigated. But the authors focus on the effect on the geomagnetism of the stations and do not consider the effects of the location of the station on the response of the other stations.
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A numerical model of the ionospheric signatures of time-varying magnetic reconnection: III. Quasi-instantaneous convection responses in the Cowley-Lockwood paradigm

TL;DR: In this article, a numerical implementation of the cowlock92 model of flow excitation in the magnetosphere-ionosphere (MI) system was used to show that both an expanding and a quasi-instantaneous response in ionospheric convection to the onset of magnetopause reconnection can be accommodated by the Cowley-Lockwood conceptual framework.
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Solar wind modulation of cusp particle signatures and their associated ionospheric flows

TL;DR: In this article, a multi-instrument case study of the northern polar cusp at a variety of altitudes in conjunction with solar wind measurements is presented, and the authors conclude that the solar wind Alfven waves modulate the dayside interaction, producing periodic flux transfer events resulting in the pulsed cusp particle signatures and PMRAFs.
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Relationship between interplanetary parameters and the magnetopause reconnection rate quantified from observations of the expanding polar cap

TL;DR: In this article, the authors measured the dependence of the magnetopause reconnection rate on interplanetary parameters from the OMNI data set and found that the reconnection rates are determined by the magnetic flux transport in the solar wind across a channel approximately 4 RE in width.
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