Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/66672
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dc.contributorDepartment of Land Surveying and Geo-Informaticsen_US
dc.creatorKumar, Sen_US
dc.creatorChen, Wen_US
dc.creatorLiu, ZZen_US
dc.creatorJi, SYen_US
dc.date.accessioned2017-05-22T02:26:34Z-
dc.date.available2017-05-22T02:26:34Z-
dc.identifier.issn2169-9380en_US
dc.identifier.urihttp://hdl.handle.net/10397/66672-
dc.language.isoenen_US
dc.publisherWiley-Blackwellen_US
dc.rights©2016. American Geophysical Union. All Rights Reserved.en_US
dc.subjectEquatorial plasma bubbleen_US
dc.subjectSolar activityen_US
dc.subjectGeomagnetic stormen_US
dc.titleEffects of solar and geomagnetic activity on the occurrence of equatorial plasma bubbles over Hong Kongen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage9164en_US
dc.identifier.epage9178en_US
dc.identifier.volume121en_US
dc.identifier.issue9en_US
dc.identifier.doi10.1002/2016JA022873en_US
dcterms.abstractIn the present study, the occurrence and characteristics of equatorial plasma bubble (EPB) has been analyzed using the GPS data from continuously operating reference stations network over Hong Kong during 2001–2012. The analysis found maximum EPB occurrences during the equinoctial months and minimum EPB occurrences during the December solstice throughout 2001–2012 except during the solar minimum in 2007–2009. The maximum EPB occurrences were observed in June solstice during 2007–2008, whereas for 2009, EPB occurrences were quite higher for June solstice but slightly smaller than the March equinox. The seasonal maximum in EPB occurrences have been discussed in terms of plasma density seed perturbation caused by gravity waves as well as the post sunset F-layer rise due to the pre-reversal enhancement of zonal electric field. Generally, EPB occurrences are found to be more prominent during nighttime hours (19:00–24:00 h) than daytime hours. The day and nighttime EPB occurrences were inferred and found to vary linearly with solar activity and have an annual correlation coefficient (R) of ~ 0.92 with F10.7 cm solar flux and ~0.88 with sunspot number. Moreover, the impact of solar activity on EPB occurrences is found to be dependent on seasons with maximum during the equinox (R = 0.80) and minimum during the summer season (R = 0.68). The detail study of EPB occurrences during two typical cases of geomagnetic storms on 6 November and 24 November 2001 found that the storm on 24 November triggered the EPB occurrence whereas storm on 6 November suppressed the EPB occurrence. The enhancement/suppression of EPB occurrences during storms periods is a consequence of a storm-induced prompt penetration electric field as well as disturbance dynamo electric field effects associated with the main phase of the geomagnetic storm.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of geophysical research : space physics, Sept. 2016, v. 121, no. 9, p. 9164-9178en_US
dcterms.isPartOfJournal of geophysical research : space physicsen_US
dcterms.issued2016-09-
dc.identifier.isiWOS:000385844000066-
dc.identifier.ros2016004112-
dc.identifier.eissn2169-9402en_US
dc.identifier.rosgroupid2016004033-
dc.description.ros2016-2017 > Academic research: refereed > Publication in refereed journalen_US
dc.description.validate201804_a bcmaen_US
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberLSGI-0428-
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextHong Kong Polytechnic University; National Natural Science Foundation of Chinaen_US
dc.description.pubStatusPublisheden_US
dc.identifier.OPUS6679774-
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