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Vertical ozone distribution over Uccle during a passage of the polar front

dc.contributor.authorDe Muer, D.
dc.coverage.spatialUccle/Ukkel
dc.coverage.temporal20th century
dc.date1979
dc.date.accessioned2016-03-07T17:13:43Z
dc.date.accessioned2021-12-09T09:57:54Z
dc.date.available2016-03-07T17:13:43Z
dc.date.available2021-12-09T09:57:54Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/9517
dc.descriptionData from a series of ozone soundings taken at Uccle during a pronounced polar front passage have been used to study the vertical distribution of ozone in relation to the synoptic situation. The analysis of these data shows a large influx of ozone-rich polar air in the lower stratosphere as the upper-air trough approaches. There is also evidence of an instrsion of stratospheric air into the troposhere in the region of the tropopause break near the polar front jet stream.
dc.languageeng
dc.publisherIRM
dc.publisherKMI
dc.publisherRMI
dc.relation.ispartofseriesPublications série B - Publicaties Serie B
dc.titleVertical ozone distribution over Uccle during a passage of the polar front
dc.typeBook
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceGeneral Public
dc.audienceScientific
dc.subject.freeOzone
dc.subject.freeUccle
dc.subject.freepolar front
dc.subject.freemeteorology and atmospheric sciences
dc.subject.freeClimatic research
dc.source.volume104
dc.source.page20
Orfeo.peerreviewedYes


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