Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/79259
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dc.contributorDepartment of Land Surveying and Geo-Informaticsen_US
dc.creatorYang, Zen_US
dc.creatorLiu, ZZen_US
dc.date.accessioned2018-11-05T01:45:12Z-
dc.date.available2018-11-05T01:45:12Z-
dc.identifier.issn2169-9380en_US
dc.identifier.urihttp://hdl.handle.net/10397/79259-
dc.language.isoenen_US
dc.publisherWiley-Blackwellen_US
dc.rights©2018. American Geophysical Union. All Rights Reserved.en_US
dc.subjectGlobal Positioning System (GPS)en_US
dc.subjectCOSMICen_US
dc.subjectROen_US
dc.subjectIonospheric irregularities and scintillationsen_US
dc.subjectRate of change of total electron content index (ROTI)en_US
dc.titleLow-latitude ionospheric density irregularities and associated scintillations investigated by combining COSMIC RO and ground-based global positioning system observations over a solar active perioden_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage3998en_US
dc.identifier.epage4014en_US
dc.identifier.volume123en_US
dc.identifier.issue5en_US
dc.identifier.doi10.1029/2017JA024199en_US
dcterms.abstractThis study for the first time presents a locally integrated analysis of occurrences of ionospheric E and F region irregularities/scintillations in southeast China, by employing radio occultation (RO) profile data retrieved from Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMIC) satellites and observations from a ground-based Global Navigation Satellite System receiver over a solar active period from 2014 to 2015. Their occurrences in both nighttime and daytime were examined by using both amplitude scintillation index (S-4) and the rate of change of total electron content index. It is found that (1) F region irregularities occurred predominantly during 20-03 local time (LT) and exhibited maximum (minimum) during equinoxes (solstices) and equinoctial (solstice) asymmetry. Their geographic mapping reveals the maximum occurrence in the westward tilted structure of equatorial plasma bubbles. In addition, the altitude-time variations indicate that their occurrences at higher altitudes were prevailing at 20-22 LT. (2) The E region irregularities were found prominently during 15-00 LT at altitudes of 90-110 km with an even geographic distribution. Their occurrences with maximum in summer (May-August) were distinctly detected by RO observations but insignificantly by ground-based observations. (3) By examining simultaneous observations of E and F region irregularities, it is found that they appeared absent during 21-00 LT and predominant after midnight. This could be related to the weakening/disruption of sporadic E (Es) layers during the development of equatorial plasma bubbles. A sign of coupling of E and F regions during nighttime is likely revealed from RO profile data.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of geophysical research : space physics, May 2018, v. 123, no. 5, p. 3998-4014en_US
dcterms.isPartOfJournal of geophysical research : space physicsen_US
dcterms.issued2018-05-
dc.identifier.isiWOS:000435943300046-
dc.identifier.eissn2169-9402en_US
dc.identifier.rosgroupid2017005324-
dc.description.ros2017-2018 > Academic research: refereed > Publication in refereed journalen_US
dc.description.validate201810 bcrcen_US
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberLSGI-0308-
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextHong Kong Polytechnic Universityen_US
dc.description.pubStatusPublisheden_US
dc.identifier.OPUS6835897-
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