Effects of the Magnetospheric Currents on the Sq-Field and a New Magnetic Index Characterizing Sq Dynamo Current Intensity

13Citations
Citations of this article
7Readers
Mendeley users who have this article in their library.

Abstract

The magnetic fields caused by the magnetospheric and ionospheric current systems are calculated. These current systems are Chapman-Ferraro current system (C-F), magnetotail current system (MTL), symmetric ring current system (SRC), region 1 field-aligned current system (FAC1), partial ring current-region 2 field-aligned current-ionospheric current system (PRFI), and the ionospheric dynamo current system (IDC). The variable magnetic fields recorded at the ground surface are the superposition of these fields and other disturbance fields. The spatial-temporal characteristics of these fields are comparatively studied, and a method for separating dynamo-field from the total field is developed. In order to describe conveniently dynamo-field intensity, a new magnetic index, “Sq index”, is proposed. © 1992, Society of Geomagnetism and Earth, Planetary and Space Sciences. All rights reserved.

Cite

CITATION STYLE

APA

Xu, W. Y. (1992). Effects of the Magnetospheric Currents on the Sq-Field and a New Magnetic Index Characterizing Sq Dynamo Current Intensity. Journal of Geomagnetism and Geoelectricity, 44(6), 449–458. https://doi.org/10.5636/jgg.44.449

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free