scispace - formally typeset
Open AccessJournal Article

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
Reads0
Chats0
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.

read more

Citations
More filters
Book ChapterDOI

Coherent-Scatter Radar Studies of the Dayside Cusp

TL;DR: In this paper, the authors consider the use of coherent scatter radars to study the ionospheric footprint of the cusp of the Earth's magnetic field in order to provide information on the dynamics of the magnetopause.

Simultaneous observations of the auroral ovals in both hemispheres under varying conditions

TL;DR: Stubbs et al. as discussed by the authors used simultaneous observations of the entire auroral ovals in both hemispheres to track their location and showed the expected IMF By-dependent asymmetry along the dawndusk meridian; however, there was an unexpected offset of both ovals toward dawn.
Journal ArticleDOI

An extensive survey of dayside diffuse aurora based on optical observations at Yellow River Station

TL;DR: In this paper, the authors performed an extensive survey for the dayside diffuse aurora (DDAs) and acquired observational results as follows: the unstructured and structured DDAs are mainly distributed in the morning and afternoon, but the structured DDA predominantly occurred around the magnetic local noon (MLN).
Journal ArticleDOI

SuperDARN Observations of the Two Component Model of Ionospheric Convection

TL;DR: In this paper , the authors used a 20-year database of Super Dual Auroral Radar Network (SuperDARN) observations to investigate the two component model of ionospheric convection.
Related Papers (5)