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contributor authorTwomey, S.
date accessioned2017-06-09T14:11:02Z
date available2017-06-09T14:11:02Z
date copyright1954/08/01
date issued1954
identifier issn0095-9634
identifier otherams-14090.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149613
description abstractThe composition of the larger (> 10?12 g) hygroscopic particles in the atmosphere was investigated, with use of a phase-transition method. Particles were collected on stretched spider webs exposed from an aircraft, and samples were taken in both maritime and continental air in different meteorological and geographical situations. It was found that the great majority of hygroscopic particles was composed of sea salt, sometimes in combination with insoluble material. A chemical test on individual particles indicated that no appreciable decrease in chloride content or replacement of chlorides by carbonates took place. Only occasionally were large soluble particles, other than sea salt, detected.
publisherAmerican Meteorological Society
titleTHE COMPOSITION OF HYGROSCOPIC PARTICLES IN THE ATMOSPHERE
typeJournal Paper
journal volume11
journal issue4
journal titleJournal of Meteorology
identifier doi10.1175/1520-0469(1954)011<0334:TCOHPI>2.0.CO;2
journal fristpage334
journal lastpage338
treeJournal of Meteorology:;1954:;volume( 011 ):;issue: 004
contenttypeFulltext


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