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dc.contributor.authorFussen, D.
dc.contributor.authorBingen, C.
dc.contributor.authorVanhellemont, F.
dc.date1998
dc.date.accessioned2017-05-19T11:16:15Z
dc.date.available2017-05-19T11:16:15Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/5423
dc.descriptionA simple and robust model is presented for describing the extinction coefficient of stratospheric aerosols in the UV-visible range. In a first version, four basic volcanic modes are distinguished. The parameters of the vertical profiles take the latitudinal dependence into account. Future improvements are presented.
dc.languageeng
dc.titleA climatological model for the extinction coefficient of stratospheric aerosols
dc.typeConference
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.subject.freeClimatology
dc.subject.freeMathematical models
dc.subject.freeRadiation
dc.subject.freeRemote sensing
dc.subject.freeRobustness (control systems)
dc.subject.freeUpper atmosphere
dc.subject.freeStratospheric aerosols
dc.subject.freeAerosols
dc.source.titleProceedings of SPIE - The International Society for Optical Engineering
dc.source.volume3439
dc.source.page578-584
Orfeo.peerreviewedNo
dc.identifier.doi10.1117/12.325664
dc.identifier.scopus2-s2.0-0032223998


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