dc.creatorRastogi, Ram Gopal
dc.creatorChandra, Harish
dc.date.accessioned2018-11-21T15:11:59Z
dc.date.accessioned2023-05-24T14:23:05Z
dc.date.available2018-11-21T15:11:59Z
dc.date.available2023-05-24T14:23:05Z
dc.date.created2018-11-21T15:11:59Z
dc.date.issued2016-01
dc.identifierRastogi, R. G., & Chandra, H. (2016). Response of equatorial ionosphere during the super geomagnetic storm of april 2000.==$Indian Journal of Radio & Space Physics, 45$==(2), 67-78.
dc.identifierhttp://hdl.handle.net/20.500.12816/3774
dc.identifierIndian Journal of Radio & Space Physics
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/6429216
dc.description.abstractThe effects of super geomagnetic storm of 6 April 2000 on E and F-regions of the ionosphere at Thumba (India) and at Jicamarca (Peru) are studied. The geomagnetic storm started at 1630 hrs UT on 6 April 2000 with sudden increase in solar wind speed and ion density and southward turning of IMF-Bz from 0 to -25 nT. The event was unique with IMF-Bz steady southward for about 6 hours and later turning from -30 nT at 2300 hrs UT to 10 nT at 0200 hrs UT and large fluctuations around 1200 hrs UT on 7 April 2000. The southward turning of IMF-Bz on the night of 06-07 April 2000 inhibited the development of Spread-F irregularities at Thumba. The large excursions of IMF-Bz on 7 April 2000 inhibited the Es-q at Thumba. At Jicamarca, the southward turning of IMF-Bz on 6 April caused a very large enhancement of EEJ current and generated very strong Es-q. The northward turning of IMF-Bz on 7 April 2000 is associated with large rise of F-layer around midnight and ESF was seen at 0100 hrs LT; however, later, the F-layer descended and inhibited ESF irregularities. The results confirm the earlier suggestion of Rastogi & Patel [Effect of interplanetary magnetic field on the ionosphere over the magnetic equator, Proc Indian Acad Sci, A 82 (1975) pp 121-141] that northward (southward) turning of IMF-Bz generates an eastward (westward) electric field in night side of ionosphere and westward (eastward) electric field in the dayside of ionosphere. The effect of a solar space weather event on the equatorial ionosphere at different longitudes depends on the local solar time of the event.
dc.languageeng
dc.publisherNational Institute of Science Communication and Information Resources (NISCAIR)
dc.relationurn:issn:0367-8393
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.subjectMagnetic storms
dc.subjectE region
dc.subjectF region
dc.subjectIonosphere
dc.subjectSolar wind
dc.subjectInterplanetary magnetic fields
dc.subjectIonograms
dc.titleResponse of equatorial ionosphere during the super geomagnetic storm of april 2000
dc.typeinfo:eu-repo/semantics/article


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