Movement of Indian Antarctic station Maitri into auroral oval during geomagnetic disturbance

dc.contributor.authorBanola, S.en_US
dc.contributor.authorDhar, Ajayen_US
dc.contributor.authorRajaram, G.en_US
dc.date.accessioned2026-07-24T06:35:39Z
dc.date.issued1997
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.identifier.citationThirteenth Indian Expedition to Antarctica, Scientific Report, 1997, DOD Technical Publication No.11, p.91-105en_US
dc.identifier.other90920
dc.identifier.urihttps://repository.iigm.res.in/handle/123456789/2121
dc.languageenen_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

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