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
Journal ArticleDOI

Polar cap patch segmentation of the tongue of ionization in the morning convection cell

TL;DR: In this paper, two types of poleward moving plasma concentration enhancements (PMPCEs) were observed during a sequence of pulsed reconnection events, both in the morning convection cell: Type L (low density) was associated with a cusp flow channel and seems likely to have been produced by ionization associated with particle precipitation, while Type H (high density) appeared to originate from the segmentation of the tongue of ionization by the processes which produced the Type L events.
Journal ArticleDOI

The statistical cusp: a flux transfer event model

TL;DR: In this paper, the authors predict precipitation signatures associated with transient magnetopause reconnection, following recent observations of the dependence of dayside ionospheric convection on the orientation of the IMF, and employ a simple model of the longitudinal motion of FTE signatures to show how such events can easily reproduce the local time distribution of cusp occurrence probabilities.
Journal ArticleDOI

High-latitude plasma convection from Cluster EDI: variances and solar wind correlations

TL;DR: Haaland et al. as mentioned in this paper constructed a database of high-latitude ionospheric convection velocities and associated solar wind and magnetospheric activity parameters based on drift velocity measurements of the EDI instruments on Cluster during the years 2001?2006.
Journal ArticleDOI

The role of the ionosphere in aurora and space weather

TL;DR: In this paper, it was shown that the behavior of intense aurora is controlled by magnetospheric-ionospheric coupling, with the solar cycle variations arising from a surprising source: variations in solar EUV flux.
Journal ArticleDOI

MESSENGER Observations of Large Dayside Flux Transfer Events: Do They Drive Mercury's Substorm Cycle?

TL;DR: In this article, the authors assessed the contribution of flux transfer events (FTEs) at the dayside magnetopause to the redistribution of magnetic flux in Mercury's magnetosphere with magnetic field data acquired in orbit about Mercury by the Magnetometer on the MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) spacecraft.
Related Papers (5)