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dc.contributor.authorFussen, D.
dc.contributor.authorBingen, C.
dc.date1999
dc.date.accessioned2017-05-09T11:58:42Z
dc.date.available2017-05-09T11:58:42Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/5363
dc.descriptionWe present a climatological model of the extinction coefficient of stratospheric aerosols in the UV-visible range based on SAGE II data. The model is a function of wavelength, latitude, relative altitude with respect to the tropopause and depends on the volcanism level. The vertical structure describes the tropopause region, the Junge layer and the high altitude domain. The model is shown to predict realistic extinction profiles with an reasonable accuracy.
dc.languageeng
dc.titleA volcanism dependent model for the extinction profile of stratospheric aerosols in the uv-visible range
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeClimatology
dc.subject.freeLight extinction
dc.subject.freeMathematical models
dc.subject.freeUltraviolet radiation
dc.subject.freeUpper atmosphere
dc.subject.freeTropopause
dc.subject.freeVolcanism
dc.subject.freeAtmospheric aerosols
dc.subject.freeaerosol property
dc.subject.freeextinction
dc.subject.freemodel
dc.subject.freevolcanism
dc.source.titleGeophysical Research Letters
dc.source.volume26
dc.source.issue6
dc.source.page703-706
Orfeo.peerreviewedYes
dc.identifier.doi10.1029/1999GL900082
dc.identifier.scopus2-s2.0-0033559286


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