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Description

The determination of DS variation of magnetic storms as a function of storm time is critically examined. The regular changes in the phase angles of harmonics for DS, found by Yokouchi (1958), are attributed to irregular features that are not adequately averaged out. This apparently paradoxical circumstance is explained with an illustrative example.

Publication Date

9-17-1961

Keywords

Geomagnetism, Magnetic storms

Handle

http://hdl.handle.net/11122/15431

A note on the DS variation of geomagnetic storms : a critical examination of method of analysis.

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