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Please use this identifier to cite or link to this item: http://library.iigm.res.in:8080/xmlui/handle/123456789/171
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dc.contributor.authorSridharan, M.
dc.contributor.authorRamasamy, A.M.S.
dc.date.accessioned2015-06-24T06:23:15Z
dc.date.accessioned2021-02-12T10:52:10Z-
dc.date.available2015-06-24T06:23:15Z
dc.date.available2021-02-12T10:52:10Z-
dc.date.issued2002
dc.identifier.citationJournal of Earth System Science, v.111/4, p.459-465, 2002, doi: 10.1007/BF02702058en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/171-
dc.description.abstractMultidimensional scaling is a powerful technique for analysis of data. The latitudinal dependence of geomagnetic field variation in horizontal component (H) during magnetic storms is analysed in this paper by employing this technique.en_US
dc.language.isoenen_US
dc.subjectMultidimensional scalingen_US
dc.subjectCovering distanceen_US
dc.subjectStorm time rangeen_US
dc.subjectMagnetic stormsen_US
dc.titleMultidimensional scaling technique for analysis of magnetic storms at Indian observatoriesen_US
dc.typeArticleen_US
dc.identifier.accession090690
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