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http://hdl.handle.net/2248/3037
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DC Field | Value | Language |
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dc.contributor.author | Sastri, J. H | - |
dc.contributor.author | Rao, J. V. S. V | - |
dc.contributor.author | Rao, D. R. K | - |
dc.contributor.author | Pathan, B. M | - |
dc.date.accessioned | 2008-08-06T05:42:35Z | - |
dc.date.available | 2008-08-06T05:42:35Z | - |
dc.date.issued | 2001-12 | - |
dc.identifier.citation | Journal of Geophysical Research-Space Physics, Vol. 106, No. A12, pp. 29925 – 29933 | en |
dc.identifier.issn | 0148-0227 | - |
dc.identifier.uri | http://hdl.handle.net/2248/3037 | - |
dc.description | Open Access | - |
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). | en |
dc.format.extent | 3894 bytes | - |
dc.format.mimetype | application/pdf | - |
dc.language.iso | en | en |
dc.publisher | American Geophysical Union | en |
dc.relation.uri | http://www.agu.org/pubs/crossref/2001/2001JA900120.shtml | en |
dc.subject | Isolated Substorms | en |
dc.subject | Interplanetary Magnetic Field (IMF) | en |
dc.subject | Ionospheric Currents | en |
dc.subject | Magnetospheric Convection | en |
dc.title | Daytime equatorial geomagnetic H field response to the growth phase and expansion phase onset of isolated substorms: Case studies and their implications | en |
dc.type | Article | en |
Appears in Collections: | IIAP Publications |
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Daytime equatorial geomagnetic H field response to the growth phase and expansion... | Open Access | 406.52 kB | Adobe PDF | View/Open |
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