Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/12516
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dc.contributor.authorGibson-Wilde, D.en
dc.contributor.authorVincent, R.en
dc.contributor.authorSouprayen, C.en
dc.contributor.authorGodin, S.en
dc.contributor.authorHertzog, A.en
dc.contributor.authorEckermann, S.en
dc.date.issued1997en
dc.identifier.citationGeophysical Research Letters, 1997; 24(13):1627-1630en
dc.identifier.issn0094-8276en
dc.identifier.urihttp://hdl.handle.net/2440/12516-
dc.description.abstractA case study is presented of 6.5 h of simultaneous colocated stratospheric Differential Absorption Lidar (DIAL) measurements of ozone concentration and Rayleigh-Mie Doppler (RD) lidar measurements of horizontal wind velocity from the Observatoire de Haute Provence (OHP), France (44°N, 6°E). The RD lidar observations reveal a distinct gravity wave motion at ∼12–18 km, while the DIAL data show laminated ozone structures in the same height range. We combine these data to show that advection due to the gravity wave cannot produce the large ozone lamina at ∼14km.en
dc.description.statementofresponsibilityGibson‐Wilde, D. E. ; Vincent, R. A. ; Souprayen, C. ; Godin, S. ; Hertzog, A. ; Eckermann, S. D.en
dc.language.isoenen
dc.publisherAMER GEOPHYSICAL UNIONen
dc.rightsCopyright 1997 by the American Geophysical Union.en
dc.titleDual-lidar observations of mesoscale fluctuations of ozone and horizontal windsen
dc.typeJournal articleen
dc.identifier.rmid0030003967en
dc.identifier.doi10.1029/97GL01609en
dc.identifier.pubid67973-
pubs.library.collectionPhysics publicationsen
pubs.verification-statusVerifieden
pubs.publication-statusPublisheden
dc.identifier.orcidVincent, R. [0000-0001-6559-6544]en
Appears in Collections:Physics publications

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