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dc.contributor.authorUlanowski, Zbigniew
dc.date.accessioned2011-11-08T12:01:19Z
dc.date.available2011-11-08T12:01:19Z
dc.date.issued2007
dc.identifier.citationUlanowski , Z 2007 , Alignment of atmospheric dust observed by high-sensitivity optical polarimetry . in Nucleation and Atmospheric Aerosols . vol. 10 , Springer Nature , pp. 1139-1144 , 17th International Conference, Nucleation and Atmospheric Aerosols , Galway , Ireland , 13/08/07 . https://doi.org/10.1007/978-1-4020-6475-3_226
dc.identifier.citationconference
dc.identifier.isbn978-1-4020-6474-6
dc.identifier.otherPURE: 444957
dc.identifier.otherPURE UUID: 39f5fc4d-e061-4c6b-a871-ab5e421436c8
dc.identifier.otherORCID: /0000-0003-4761-6980/work/32374658
dc.identifier.urihttp://hdl.handle.net/2299/6937
dc.description“The original publication is available at www.springerlink.com” Copyright Springer [Full text of this paper is not available in the UHRA]
dc.description.abstractOptical polarimetry observations on La Palma, Canary Islands, during a Saharan dust episode showed dichroic extinction, indicating the presence of vertically aligned particles in the atmosphere. It is postulated that the alignment was due to an electric field of the order of 1 kV/m or greater. Two alternative mechanisms for the origin of the field are examined, including the effect of reduced atmospheric conductivity and the presence of charged dust.en
dc.format.extent6
dc.language.isoeng
dc.publisherSpringer Nature
dc.relation.ispartofNucleation and Atmospheric Aerosols
dc.subjecttropospheric aerosol
dc.subjectmineral dust
dc.subjectalignment
dc.subjectelectric field
dc.subjectpolarimetry
dc.titleAlignment of atmospheric dust observed by high-sensitivity optical polarimetryen
dc.contributor.institutionSchool of Physics, Astronomy and Mathematics
dc.identifier.urlhttp://www.conference.ie/Conferences/index.asp?Conference=34
rioxxterms.versionofrecordhttps://doi.org/10.1007/978-1-4020-6475-3_226
rioxxterms.typeOther
herts.preservation.rarelyaccessedtrue


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