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dc.contributor.authorReiter, Elmar R.
dc.date.accessioned2017-06-09T16:34:12Z
dc.date.available2017-06-09T16:34:12Z
dc.date.copyright1963/12/01
dc.date.issued1963
dc.identifier.issn0021-8952
dc.identifier.otherams-7016.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4211912
dc.description.abstractDuring September 1961 a series of balloon ascents made from Flin Flon, Canada, carrying scintillation counters sensitive to gamma radiation, revealed the existence of shallow stable atmospheric layers carrying radioactive debris, presumably from the Russian test series during the same month. The debris layers encountered on 14 and 15 September have been studied in particular. The debris detected over Flin Flon on 14 September, 2221 GCT, at 650 mb had undergone strong sinking motion. One may conclude that it came from the region immediately underneath the tropopause shortly prior to 13 September, 12 GCT, entering the middle troposphere through the stable layer underneath the jet core, sometimes referred to as a ?jet-stream front.? Beginning with 17 September a distinct area of radioactive fallout begins to appear at the surface over the eastern United States. Some of this debris seems to be identical with the one detected over Flin Flon, and it apparently was transported by the same jet stream. Part of the fallout seems to be associated with a small collapsing cold dome travelling ahead of this jet stream.
dc.publisherAmerican Meteorological Society
dc.titleA Case Study of Radioactive Fallout
dc.typeJournal Paper
dc.journal.volume2
dc.journal.issue6
dc.journal.titleJournal of Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1963)002<0691:ACSORF>2.0.CO;2
dc.journal.fristpage691
dc.journal.lastpage705
dc.treeJournal of Applied Meteorology:;1963:;volume( 002 ):;issue: 006
dc.contenttypeFulltext


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