A New Hypothesis for the Vertical Distribution of Atmospheric Aerosols

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dc.creatorSelvam, A. Mary
dc.creatorMurty, A. S. Ramachandra
dc.creatorRamanamurty, Bh. V.
dc.date1999-12-05
dc.date.accessioned2026-07-07T05:57:34Z
dc.date.available2026-07-07T05:57:34Z
dc.descriptionA simple model which can explain the observed vertical distribution and size spectrum of atmospheric aerosol has been proposed. The model is based on a new physical hypothesis for the vertical mass exchange between the troposphere and the stratosphere. The vertical mass excange takes place through a gravity wave feedback mechanism. There is a close agreement between the model predicted aerosol distribution and size spectrum and the observed distributions.
dc.description5 pages, 2 figures, Proc.of the XI Int. Conf. on Atmospheric Aerosols, Condensation and Ice Nuclei, 2-7 Sept.1984, Budapest, Hungary, 77-81
dc.identifierhttps://arxiv.org/abs/physics/9912014
dc.identifierhttp://arxiv.org/abs/physics/9912014
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/88028
dc.subjectGeneral Physics
dc.titleA New Hypothesis for the Vertical Distribution of Atmospheric Aerosols
dc.typetext

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