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dc.contributor.authorKing, Michael D.
dc.contributor.authorHarshvardhan
dc.contributor.authorArking, Albert
dc.date.accessioned2017-06-09T14:00:17Z
dc.date.available2017-06-09T14:00:17Z
dc.date.copyright1984/07/01
dc.date.issued1984
dc.identifier.issn0733-3021
dc.identifier.otherams-10750.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145902
dc.description.abstractAn accurate multiple-scattering model has been employed to examine the effect of an aerosol layer at 25 mb, corresponding to the EL Chichon observations, on the reflection, transmission and absorption of radiation by the stratosphere as a function of latitude, optical thickness and aerosol size distribution. Results are presented and parameterized for each of two wavelength intervals in the shortwave region and 17 wavelength intervals in the longwave region for three models of the aerosol size distribution. They include one model representing the unperturbed stratospheric aerosol plus two models based on measurements of the EL Chichon aerosol size distribution. In addition to models of the radiative properties of the aerosol layer, a simple model of the latitudinal distribution of aerosol optical thickness as a function of time is developed, based on diffusive transport in latitude and exponential decay in time. These parameterizations for solar and infrared radiation, together with the dispersion model, permit climate models to account for the evolution of an aerosol size distribution from post-volcanic conditions to background conditions.
dc.publisherAmerican Meteorological Society
dc.titleA Model of the Radiative Properties of the EL Chichon Stratospheric Aerosol Layer
dc.typeJournal Paper
dc.journal.volume23
dc.journal.issue7
dc.journal.titleJournal of Climate and Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1984)023<1121:AMOTRP>2.0.CO;2
dc.journal.fristpage1121
dc.journal.lastpage1137
dc.treeJournal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 007
dc.contenttypeFulltext


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