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contributor authorLodge, James P.
contributor authorMcDonald, James E.
contributor authorBaer, Ferdinand
date accessioned2017-06-09T14:11:02Z
date available2017-06-09T14:11:02Z
date copyright1954/08/01
date issued1954
identifier issn0095-9634
identifier otherams-14088.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149610
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.
publisherAmerican Meteorological Society
titleAN INVESTIGATION OF THE MELANDER EFFECT
typeJournal Paper
journal volume11
journal issue4
journal titleJournal of Meteorology
identifier doi10.1175/1520-0469(1954)011<0318:AIOTME>2.0.CO;2
journal fristpage318
journal lastpage322
treeJournal of Meteorology:;1954:;volume( 011 ):;issue: 004
contenttypeFulltext


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