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dc.contributor.authorFrank, W. M.
dc.contributor.authorGray, W. M.
dc.date.accessioned2017-06-09T17:40:22Z
dc.date.available2017-06-09T17:40:22Z
dc.date.copyright1980/02/01
dc.date.issued1979
dc.identifier.issn0021-8952
dc.identifier.otherams-9860.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233395
dc.description.abstractOver 8500 rawinsonde soundings within 8° radius of tropical cyclones in the northwest Pacific and West Indies regions are statistically analyzed to determine occurrence frequencies of 15 m s?1 (30 kt) winds at the sea surface. At any radius the likelihood of encountering winds >15 m s?1 is found to increase with increasing central wind speed and with increasing radius of the highest closed isobar. There are significant right-side wind maxima and left-side minima with respect to the direction of storm motion. This reflects the natural storm asymmetry. Much variability is found in the radius of 15 m s?1 winds between cyclones of similar inner core intensity.
dc.publisherAmerican Meteorological Society
dc.titleRadius and Frequency of 15 m s−1 (30 kt) Winds around Tropical Cyclones
dc.typeJournal Paper
dc.journal.volume19
dc.journal.issue2
dc.journal.titleJournal of Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1980)019<0219:RAFOMS>2.0.CO;2
dc.journal.fristpage219
dc.journal.lastpage223
dc.treeJournal of Applied Meteorology:;1979:;volume( 019 ):;issue: 002
dc.contenttypeFulltext


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