Structuring of intermediate scale equatorial spread F irregularities during intense geomagnetic storm of solar cycle 24

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dc.contributor.author Kakad, Bharati
dc.contributor.author Gurram, P.
dc.contributor.author Sundari, P.N.B. Tripura
dc.date.accessioned 2017-11-06T09:57:01Z
dc.date.accessioned 2021-02-12T09:58:38Z
dc.date.available 2017-11-06T09:57:01Z
dc.date.available 2021-02-12T09:58:38Z
dc.date.issued 2016
dc.identifier.citation JGR, 121, doi: 10.1002/2016JA022635 en_US
dc.identifier.uri http://localhost:8080/xmlui/handle/123456789/1055
dc.description.abstract Here we examine the structuring of equatorial plasma bubble (EPB) during intense geomagnetic storm of solar cycle (SC) 24 that occurred on 17 March 2015 using spaced receiver scintillation observations on a 251 MHz radio signal, recorded by a network of stations in Indian region. As yet, this is the strongest geomagnetic storm (Dstmin ∼ −223nT) that occurred in present SC. Present study reveals that the structuring of equatorial spread F (ESF) irregularities was significantly different on 17 March as compared to quiet days of corresponding month. ESF irregularities of intermediate scale (100 m to few kilometers) are observed at unusually higher altitudes (≥ 800 km) covering wider longitudinal-latitudinal belt over Indian region. A presence of large-scale irregularity structures with stronger ΔN at raised F peak with small-scale irregularities at even higher altitudes is observed. It caused strong focusing effect (S4 >1) that prevails throughout premidnight hours at dip equatorial station Tirunelveli. Other observational aspect is that zonal irregularity drifts over low-latitude station Kolhapur exhibited a large deviation of ∼230 m/s from their average quiet time pattern. During this geomagnetic storm, two southward turnings of significant strength (BZ ≤−15 nT) occurred at 11.4 IST (Indian standard time) and 17.9 IST. The later southward turning of interplanetary magnetic field (IMF) BZ resulted in a large eastward prompt penetration electric field (PPEF) close to sunset hours in Indian longitude. Estimates of PPEF obtained from real-time ionospheric model are too low to explain the observed large upliftment of F region in the post sunset hours. Possible reason for observed enhanced PPEF-linked effects is discussed. en_US
dc.language.iso en en_US
dc.subject ESF irregularities en_US
dc.subject Equatorial Plasma bubble en_US
dc.subject Spread F irregularities en_US
dc.subject EPB en_US
dc.subject Solar cycle 24 en_US
dc.subject Geomagnetic storm en_US
dc.title Structuring of intermediate scale equatorial spread F irregularities during intense geomagnetic storm of solar cycle 24 en_US
dc.type Article en_US
dc.identifier.accession 091597


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