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dc.contributor.authorSugiura, Masahisa
dc.date.accessioned2024-10-02T00:50:08Z
dc.date.available2024-10-02T00:50:08Z
dc.date.issued1961-09
dc.identifier.urihttp://hdl.handle.net/11122/15431
dc.descriptionUAG R-123; Scientific Report No. 4en_US
dc.description.abstractThe 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.en_US
dc.description.sponsorshipPrepared for Geophysics Research Directorate, Air Force Cambridge Research Laboratories, Air Force Office of Aerospace Research, United States Air Force, Bedford, Massachusetts; AFCRL 1013, Contract No. AF 19(604)-2163.en_US
dc.language.isoen_USen_US
dc.subjectGeomagnetismen_US
dc.subjectMagnetic stormsen_US
dc.titleA note on the DS variation of geomagnetic storms : a critical examination of method of analysis.en_US
dc.typeReporten_US
refterms.dateFOA2024-10-02T00:50:10Z


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