Files

Download

Download file (427 KB)

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.

Share

COinS
 
 

To view the content in your browser, please download Adobe Reader or, alternately,
you may Download the file to your hard drive.

NOTE: The latest versions of Adobe Reader do not support viewing PDF files within Firefox on Mac OS and if you are using a modern (Intel) Mac, there is no official plugin for viewing PDF files within the browser window.