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dc.contributor.authorLodge, James P.
dc.contributor.authorMcDonald, James E.
dc.contributor.authorBaer, Ferdinand
dc.date.accessioned2017-06-09T14:11:02Z
dc.date.available2017-06-09T14:11:02Z
dc.date.copyright1954/08/01
dc.date.issued1954
dc.identifier.issn0095-9634
dc.identifier.otherams-14088.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149610
dc.description.abstractMelander's experimental results on the apparent production of salt nuclei by evaporation of salt solutions are examined both theoretically and experimentally. It is concluded theoretically that the rate of evaporative escape of molecular sodium chloride or other salts from sea water is too low by a factor of 1018 to account for the formation of the nuclei active in cloud condensation. It is shown experimentally that the rate of collection of salt particles of diameter in excess of 0.05 micron over evaporating salt solution is too low by a factor of at least 106 to account for the observed rate of atmospheric condensation. Therefore, there appears to be no basis for accepting Wright's suggestion that Melander's work provides an answer to Simpson's long-standing objection to the sea-salt hypothesis of condensation nuclei.
dc.publisherAmerican Meteorological Society
dc.titleAN INVESTIGATION OF THE MELANDER EFFECT
dc.typeJournal Paper
dc.journal.volume11
dc.journal.issue4
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1954)011<0318:AIOTME>2.0.CO;2
dc.journal.fristpage318
dc.journal.lastpage322
dc.treeJournal of Meteorology:;1954:;volume( 011 ):;issue: 004
dc.contenttypeFulltext


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