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dc.contributor.authorBanola, S.
dc.contributor.authorDhar, Ajay
dc.contributor.authorRajaram, G.
dc.date.accessioned2015-09-15T11:03:39Z
dc.date.accessioned2021-02-12T09:27:46Z
dc.date.available2015-09-15T11:03:39Z
dc.date.available2021-02-12T09:27:46Z
dc.date.issued1997
dc.identifier.citationThirteenth Indian Expedition to Antarctica, Scientific Report, 1997, DOD Technical Publication No.11, p.91-105en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/422
dc.description.abstractDuring the 13th Summer Indian Antarctic Expedition (Dec 1993 - March 1994), fluxgate magnetometers were operated at the Indian Antarctic locations MAITRI (MAI) and DAKSHIN GANGOTRI (DG). The variations of the X, Y, Z geomagnetic components when compared between magnetically Quiet days, moderately Disturbed days, and clearly Disturbed days, indicate that during quiet times, the Indian stations occupy a sub-auroral position; with increasing disturbance, they come into the auroral oval, and then the geomagnetic variations bear the signature of the auroral electrojet (AE) and field-aligned currents (FAC). Ionospheric horizontal current densities in the north-south and east-west directions are estimated from the variations in the geomagnetic components using the Biot-Savart law. They indicate that the current densities over MAI and DG increase with increasing electromagnetic disturbance in geospace, more sharply in the Dawn sector than in the Dusk sector.en_US
dc.language.isoenen_US
dc.subjectAuroral ovalen_US
dc.subjectIndian Antarctic stationen_US
dc.subjectElectrojeten_US
dc.subjectAuroral fielden_US
dc.subjectMaitrien_US
dc.titleMovement of Indian Antarctic station Maitri into auroral oval during geomagnetic disturbanceen_US
dc.typeArticleen_US
dc.identifier.accession090920
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