dc.contributor.author |
Sastri, J. H |
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dc.contributor.author |
Rao, J. V. S. V |
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dc.contributor.author |
Rao, D. R. K |
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dc.contributor.author |
Pathan, B. M |
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dc.date.accessioned |
2008-08-06T05:42:35Z |
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dc.date.available |
2008-08-06T05:42:35Z |
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dc.date.issued |
2001-12 |
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dc.identifier.citation |
Journal of Geophysical Research-Space Physics, Vol. 106, No. A12, pp. 29925 – 29933 |
en |
dc.identifier.issn |
0148-0227 |
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dc.identifier.uri |
http://hdl.handle.net/2248/3037 |
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dc.description |
Open Access |
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dc.description.abstract |
Observations are presented from the Indian magnetometer network (dipole latitude range 1.2°S to 13.5°N) of short-lived (<1 hr) disturbances in the daytime equatorial geomagnetic H field associated with specific phases of isolated substorms. Three well-documented substorms are examined here, of which the expansion onset of each is closely associated with sudden transitions of interplanetary magnetic field (IMF) Bz /By after a >40-min interval of southward Bz . A positive baylike perturbation is found to prevail during the substorm growth phase, followed by a negative baylike disturbance starting precisely at the onset of expansion phase activity. The amplitude of the positive as well as negative bay-type disturbance showed a clear-cut enhancement at locations inside the equatorial electrojet belt when compared with stations away from the electrojet influence, indicative of a significant contribution of ionospheric currents to the bays. This pattern of response, which is found in two out of the three events studied, constitutes the first-time evidence for the occurrence of equatorial H field perturbations related to the growth phase as well as the expansion phase onset for individual substorms. The H field perturbations are suggested to be signatures of prompt penetration by electric fields associated with rapid changes in magnetospheric convection brought about by the swift transitions in the IMF Bz , before shielding by the ring current becomes effective. In the third event, where the growth phase is weak and prolonged, there is no perceptible simultaneous disturbance in the equatorial H field, while the expansion phase onset is associated with a positive bay of very small amplitude (≤4 nT). |
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dc.format.extent |
3894 bytes |
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dc.format.mimetype |
application/pdf |
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dc.language.iso |
en |
en |
dc.publisher |
American Geophysical Union |
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dc.relation.uri |
http://www.agu.org/pubs/crossref/2001/2001JA900120.shtml |
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dc.subject |
Isolated Substorms |
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dc.subject |
Interplanetary Magnetic Field (IMF) |
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dc.subject |
Ionospheric Currents |
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dc.subject |
Magnetospheric Convection |
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dc.title |
Daytime equatorial geomagnetic H field response to the growth phase and expansion phase onset of isolated substorms: Case studies and their implications |
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dc.type |
Article |
en |