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"Secondary maxima in ozone profiles"

dc.contributor.authorLemoine, R.
dc.contributor.authorDe Backer, H.
dc.contributor.authorCheymol, A.
dc.contributor.authorDelcloo, A.
dc.coverage.temporal21st century
dc.date2004
dc.date.accessioned2016-03-07T16:16:47Z
dc.date.accessioned2021-12-09T09:53:22Z
dc.date.available2016-03-07T16:16:47Z
dc.date.available2021-12-09T09:53:22Z
dc.identifierISBN 960-630-103-6, ISBN 960-630-101-1, ISBN 960-630-105-2, 392
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/8632
dc.descriptionOzone profiles from balloon soundings as well as SAGEII ozone profiles were used to detect anomalous large ozone concentrations of ozone in the lower stratosphere. These secondary ozone maxima are found to be the result of differential advection of ozone-poor and ozone-rich air associated with Rossby wave breaking events. The frequency and intensity of secondary ozone maxima and their geographical distribution is presented. The occurrence and amplitude of ozone secondary maxima is connected to ozone variability and trend at Uccle and account for a large part of the total ozone and lower stratospheric ozone variability.
dc.languageeng
dc.publisherIRM
dc.publisherKMI
dc.publisherRMI
dc.relation.ispartofseriesOzone, Proceedings of the XX Quadrennial Ozone Symposium, 1-8 June 2004, Kos, Greece, Edt. C.S. Zerefos,
dc.title"Secondary maxima in ozone profiles"
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceGeneral Public
dc.audienceScientific
dc.subject.freeOzone
dc.subject.freeSAGEII
dc.subject.freeRossby
dc.subject.freeUccle
dc.source.issueOzone, Proceedings of the XX Quadrennial Ozone Symposium, 1-8 June 2004, Kos, Greece, Edt. C.S. Zerefos,
Orfeo.peerreviewedNot pertinent


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