Signatures of the Solar Transient Disturbances Over the Low Latitude Ionosphere During 6 to 8 September 2017

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dc.contributor.author Bagiya, Mala S.
dc.contributor.author Thambi, Smitha V.
dc.contributor.author Hui, Deprub
dc.contributor.author Sunil, A.S.
dc.contributor.author Chakrabarty, D.
dc.contributor.author Choudhary, R.K.
dc.date.accessioned 2010-02-07T01:39:51Z
dc.date.accessioned 2021-02-12T10:20:10Z
dc.date.available 2010-02-07T01:39:51Z
dc.date.available 2021-02-12T10:20:10Z
dc.date.issued 2018
dc.identifier.citation JGR, , 123, 7598–7608, doi: 10.1029/2018JA025496 en_US
dc.identifier.uri http://localhost:8080/xmlui/handle/123456789/1488
dc.description.abstract Low latitude ionospheric behavior during solar transient disturbances of solar flares and storm time penetrating electric fields comprises an important part of the Earth’s space weather. The flares enhance the electron density of the sunlit ionosphere by supplying excess solar radiation. However, the degree of these density changes is subjective if a geomagnetic storm persists simultaneously. The present case study addresses the ionospheric variations over the Indian longitudes under the combined effects of the solar flares and a geomagnetic storm during 6 to 8 September 2017 and probably the first of its kind in delineating the effects of these two over the low latitude ionosphere. The X9.3 class flare of 6 September, which occurred during non-storm conditions, produced an intense E region ionization (~500% over the ambient). However, the total electron content response to this flare was comparatively weak. The flares on 7 and 8 September occurred during the 7–8 September geomagnetic storm. Though the 8 September flare occurred with higher intensity (M8.1) and early in local time compared to the flare of 7 September (M7.3), the equatorial electrojet current enhancement was lesser on 8 September (~75% over the ambient) than that of 7 September (~110% over the ambient). This aspect is discussed in view of the storm time convection effects over the low latitudes during 7–8 September storm. The total electron content did not respond to the flares of 7 and 8 September. This behavior is attributed to the varying center-to-limb distance of the solar active region 12673 during this period. en_US
dc.language.iso en_US en_US
dc.subject Ionosphere en_US
dc.subject Low latitude ionosphere en_US
dc.subject Space weather en_US
dc.subject Solar flare en_US
dc.subject Geomagnetic storm en_US
dc.subject Solar Transient Disturbances en_US
dc.title Signatures of the Solar Transient Disturbances Over the Low Latitude Ionosphere During 6 to 8 September 2017 en_US
dc.type Article en_US
dc.identifier.accession 091779


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