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dc.contributor.authorEllis, Kelsey N.
dc.contributor.authorTrepanier, Jill C.
dc.contributor.authorHodges, Robert E.
dc.date.accessioned2017-06-09T16:51:03Z
dc.date.available2017-06-09T16:51:03Z
dc.date.copyright2016/04/01
dc.date.issued2016
dc.identifier.issn1558-8424
dc.identifier.otherams-75269.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4217586
dc.description.abstracthe characteristics and conditions favoring extreme hurricanes remain largely unknown because of their small number in the observational record. Synthetic tracks are capable of providing a large, representative sample of these events, which provides an opportunity to further understanding of extreme characteristics as compared with those of more common tropical cyclones. The authors compare 300 synthetic extreme (100-yr event, ≥48.9 m s?1) and 300 common (5-yr event, ≤33.6 m s?1) tropical cyclones for Charleston, South Carolina, for differences in spatial, temporal, and other characteristics. Results suggest that extreme hurricanes have a more-defined spatial and temporal behavior, generally forming off the coast of Africa and making a direct landfall at Charleston. Common tropical cyclones sometimes make prior landfalls, may approach from either the Gulf of Mexico or the Atlantic Ocean, and often decay well before reaching Charleston. They are likely to occur through much of the hurricane season, whereas extreme events are most common during a short period toward the end of August. There is no significant difference between common and extreme translational velocity at landfall. This study demonstrates the opportunity that synthetic tracks provide for understanding the rarest hurricanes and provides initial insight into those affecting Charleston.
dc.publisherAmerican Meteorological Society
dc.titleUsing Synthetic Tropical Cyclones to Characterize Extreme Hurricanes Affecting Charleston, South Carolina
dc.typeJournal Paper
dc.journal.volume55
dc.journal.issue4
dc.journal.titleJournal of Applied Meteorology and Climatology
dc.identifier.doi10.1175/JAMC-D-15-0215.1
dc.journal.fristpage883
dc.journal.lastpage892
dc.treeJournal of Applied Meteorology and Climatology:;2016:;volume( 055 ):;issue: 004
dc.contenttypeFulltext


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