Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/91195
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dc.contributor.authorLi, G.-
dc.contributor.authorNing, B.-
dc.contributor.authorWan, W.-
dc.contributor.authorReid, I.-
dc.contributor.authorHu, L.-
dc.contributor.authorYue, X.-
dc.contributor.authorYounger, J.-
dc.contributor.authorDolman, B.-
dc.date.issued2014-
dc.identifier.citationGeophysical Research Letters, 2014; 41(19):6583-6589-
dc.identifier.issn0094-8276-
dc.identifier.issn1944-8007-
dc.identifier.urihttp://hdl.handle.net/2440/91195-
dc.description.abstractWhether radar meteor echoes occur at high altitudes (above ~130 km) in the Earth's atmosphere is a long-standing question within the meteor radar community. Using observations from the Sanya VHF coherent radar interferometer during 11 July to 10 August 2013, we have found a new class of range-spread high-altitude meteor trail echoes (HAMEs), some of which appeared at ~170 km altitude lasting more than 10 s. A statistical analysis on the local time dependence of the identified HAME events shows a maximum around 00–04 LT. The results imply that there could be much more meteor mass input due to meteoroid sputtering at high altitudes in the Earth's atmosphere than previously thought.-
dc.description.statementofresponsibilityGuozhu Li, Baiqi Ning, Weixing Wan, I. M. Reid, Lianhuan Hu, Xinan Yue, J. P. Younger and B.K. Dolman-
dc.language.isoen-
dc.publisherAGU-
dc.rights© 2014 American Geophysical Union. All rights reserved-
dc.source.urihttp://dx.doi.org/10.1002/2014gl061478-
dc.titleObservational evidence of high-altitude meteor trail from radar interferometer-
dc.typeJournal article-
dc.identifier.doi10.1002/2014GL061478-
pubs.publication-statusPublished-
dc.identifier.orcidReid, I. [0000-0003-2340-9047]-
dc.identifier.orcidYounger, J. [0000-0003-2918-1709]-
dc.identifier.orcidDolman, B. [0000-0001-9119-8742]-
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