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contributor authorBirstein, S. J.
contributor authorAnderson, C. E.
date accessioned2017-06-09T14:11:08Z
date available2017-06-09T14:11:08Z
date copyright1955/02/01
date issued1955
identifier issn0095-9634
identifier otherams-14136.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149664
description abstractA careful study has been made of the nucleating ability of various chemicals. The nuclei were prepared in a nitrogen atmosphere, rather than air, to prevent a reaction at the hot filament with atmospheric oxygen. With use of these carefully controlled conditions, numerous materials previously reported as effective were found to be poor nucleating agents. The discrepancies among the various sets of data were found to be due to reaction at the filament of the solid material and oxygen in previous investigations. The results are examined to determine how they support prevailing theories on ice-crystal formation.
publisherAmerican Meteorological Society
titleTHE MECHANISM OF ATMOSPHERIC ICE FORMATION, I: THE CHEMICAL COMPOSITION OF NUCLEATING AGENTS
typeJournal Paper
journal volume12
journal issue1
journal titleJournal of Meteorology
identifier doi10.1175/1520-0469(1955)012<0068:TMOAIF>2.0.CO;2
journal fristpage68
journal lastpage73
treeJournal of Meteorology:;1955:;volume( 012 ):;issue: 001
contenttypeFulltext


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