Published 1980 | Version v1
Book

What is a magnetospheric substorm

  • 1. Alaska Univ., Fairbanks (USA). Geophysical Inst.

Description

It is suggested that if the solar wind-magnetosphere energy coupling, epsilon, increases above about 1018 erg/sec, the magnetosphere suddenly develops a more efficient energy dissipation process than that operating during periods of epsilon < 1018 erg/sec. It appears that the magnetosphere achieves this enhanced energy dissipation by interrupting the cross-tail current in the magnetotail and diverting it into the ionosphere, causing an enhanced Joule heat production in the ionosphere. The good correlation between epsilon and the total energy dissipated in the magnetosphere suggests that the substorm is more like a process directly driven by the solar wind, rather than an unloading process of energy accumulated prior to the onset. (Auth.)

Additional details

Publishing Information

Publisher
D. Reidel.
Imprint Place
Dordrecht, Netherlands
ISBN
90-277-1052-X
Imprint Title
Dynamics of the magnetosphere
Journal Volume
78
Series
Astrophysics and space science library proceedings.
Journal Page Range
p. 447-460.

Conference

Title
A.G.U. Chapman conference on magnetospheric substorms and related plasma processes.
Dates
9 - 13 Oct 1978.
Place
Los Alamos, NM, USA.

INIS

Country of Publication
Netherlands
Country of Input or Organization
Netherlands
INIS RN
11543708
Subject category
S58: GEOSCIENCES;
Resource subtype / Literary indicator
Conference, Numerical Data
Descriptors DEI
EARTH MAGNETOSPHERE; ENERGY LOSSES; EXPERIMENTAL DATA; GRAPHS; INTERPLANETARY MAGNETIC FIELDS; IONOSPHERE; MAGNETIC STORMS; MAGNETOTAIL; PLASMA SHEET; RING CURRENTS; SOLAR WIND
Descriptors DEC
CURRENTS; DATA; DATA FORMS; EARTH ATMOSPHERE; ELECTRIC CURRENTS; INFORMATION; MAGNETIC FIELDS; NUMERICAL DATA; SOLAR ACTIVITY

Optional Information

Notes
Imprint:Includes author and subject indexes.