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Orbits and emission spectra from the 2014 Camelopardalids

dc.contributor.authorZamorano Calvo, Jaime
dc.contributor.authorIzquierdo, Jaime
dc.contributor.authorSánchez De Miguel, Alejandro
dc.contributor.authorOcaña, Francisco
dc.date.accessioned2023-06-19T13:28:14Z
dc.date.available2023-06-19T13:28:14Z
dc.date.issued2014-12-11
dc.descriptionThis article has been accepted for publication in Monthly notices of the Royal Astronomical Society. © 2014 The Autors. Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved. Meteor stations deployed at Sevilla, La Hita, Huelva, El Arenosillo, Sierra Nevada and La Pedriza have been funded by the first author. We acknowledge partial support from the Spanish Ministry of Science and Innovation (projects AYA2011-26522, AYA2012-31277 and AYA2012-30717). We thank the AstroHita Foundation for its continuous support in the operation of the meteor observing station located at La Hita Astronomical Observatory.
dc.description.abstractWe have analysed the meteor activity associated with meteoroids of fresh dust trails of Comet 209P/LINEAR, which produced an outburst of the Camelopardalid meteor shower (IAU code #451, CAM) in 2014 May. With this aim, we have employed an array of high-sensitivity CCD video devices and spectrographs deployed at 10 meteor observing stations in Spain in the framework of the Spanish Meteor Network. Additional meteoroid flux data were obtained by means of two forward-scatter radio systems. The observed peak zenithal hourly rate was much lower than expected, of around 20 meteors h(-1). Despite of the small meteor flux in the optical range, we have obtained precise atmospheric trajectory, radiant and orbital information for 11 meteor and fireball events associated with this stream. The ablation behaviour and low tensile strength calculated for these particles reveal that Camelopardalid meteoroids are very fragile, mostly pristine aggregates with strength similar to that of the Orionids and the Leonids. The mineral grains seem to be glued together by a volatile phase. We also present and discuss two unique emission spectra produced by two Camelopardalid bright meteors. These suggest a non-chondritic nature for these particles, which exhibit Fe depletion in their composition.
dc.description.departmentDepto. de Física de la Tierra y Astrofísica
dc.description.facultyFac. de Ciencias Físicas
dc.description.refereedTRUE
dc.description.sponsorshipSpanish Ministry of Science and Innovation
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/28472
dc.identifier.doi10.1093/mnras/stu1990
dc.identifier.issn0035-8711
dc.identifier.officialurlhttp://dx.doi.org/10.1093/mnras/stu1990
dc.identifier.relatedurlhttp://mnras.oxfordjournals.org/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/33796
dc.issue.number3
dc.journal.titleMonthly notices of the Royal Astronomical Society
dc.language.isoeng
dc.page.final3314
dc.page.initial3309
dc.publisherWiley
dc.relation.projectIDAYA2011-26522
dc.relation.projectIDAYA2012-31277
dc.relation.projectIDAYA2012-30717
dc.rights.accessRightsopen access
dc.subject.cdu52
dc.subject.keywordOctober draconids outburst
dc.subject.keywordFireball spectroscopy
dc.subject.keywordMeteoroids
dc.subject.ucmAstrofísica
dc.subject.ucmAstronomía (Física)
dc.subject.ucmFísica atmosférica
dc.subject.unesco2501 Ciencias de la Atmósfera
dc.titleOrbits and emission spectra from the 2014 Camelopardalids
dc.typejournal article
dc.volume.number445
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dspace.entity.typePublication
relation.isAuthorOfPublication949589a4-3398-4ac6-805c-5dcf70d066f2
relation.isAuthorOfPublication9938be75-8360-4566-8763-c7afe78f3614
relation.isAuthorOfPublication.latestForDiscovery949589a4-3398-4ac6-805c-5dcf70d066f2

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