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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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Citations
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Journal ArticleDOI

Average field-aligned current configuration parameterized by solar wind conditions

TL;DR: In this article, a large-scale comparison of the spatial distribution of field-aligned currents as measured by the Active Magnetosphere and Planetary Electrodynamics Response Experiment, with the location and brightness of the average auroral oval, determined from the Imager for Magnetopause-to-Aurora Global Exploration far ultraviolet instrument is presented.
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Ground-based observations of the auroral zone and polar cap ionospheric responses to dayside transient reconnection

TL;DR: In this paper, the EISCAT VHF incoherent scatter radar system in northern Norway, during a run of the common programme CP-4, reveal a series of poleward- propagating F-region electron density enhancements in the pre-noon sector on 23 November 1999.
Book ChapterDOI

Identifying the Open-Closed Field Line Boundary

TL;DR: In this paper, the authors look at the topological reconnection classes that can take place, both at the magnetopause and in the cross-tail current sheet and discuss the implications for identifying the open-closed boundary when reconnection is giving velocity filter dispersion of signatures.
Journal ArticleDOI

Conjugate observations of the day-side reconnection electric field: A GEM boundary layer campaign

TL;DR: In this paper, the day-side reconnection electric field was observed to be bursty in nature in the throat flow region of the Earth's magnetic field during a period of 4 hours around local magnetic noon.
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