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contributor authorRosinski, Jan
contributor authorKnight, Charles A.
contributor authorNagamoto, Clarence T.
contributor authorMorgan, Griffith M.
contributor authorKnight, Nancy C.
contributor authorProdi, Franco
date accessioned2017-06-09T14:20:48Z
date available2017-06-09T14:20:48Z
date copyright1979/05/01
date issued1979
identifier issn0022-4928
identifier otherams-17702.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153626
description abstractResults of a previous study have been confirmed by additional measurements on many hailstones from several different areas. They indicate that relatively clear hailstone embryos, interpreted as frozen drops, are associated with large soil or organic particles. Opaque (bubbly) embryos do not contain foreign particles larger than 40 ?m diameter. The difference is observed even when the two hailstone embryo types occur in a single hailfall. The results suggest that different embryo types originate in different parts of a storm and are carried by the thunderstorm airflow into a common final growth and fallout region.
publisherAmerican Meteorological Society
titleFurther Studies of Large, Water-Insoluble Particles within Hailstones
typeJournal Paper
journal volume36
journal issue5
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1979)036<0882:FSOLWI>2.0.CO;2
journal fristpage882
journal lastpage891
treeJournal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 005
contenttypeFulltext


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