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contributor authorDitchek, Sarah D.;Nelson, T. Connor;Rosenmayer, Michaela;Corbosiero, Kristen L.
date accessioned2018-01-03T11:00:53Z
date available2018-01-03T11:00:53Z
date copyright3/15/2017 12:00:00 AM
date issued2017
identifier otherjcli-d-16-0554.1.pdf
identifier urihttp://138.201.223.254:8080/yetl1/handle/yetl/4246046
description abstractAbstractDespite recent improvements made to tropical cyclone intensity predictions, this study investigates a different approach than those attempted thus far. Here, the overall environmental setup at genesis is evaluated to determine whether it predisposes a storm to reach its future maximum intensity. Variables retrieved from ERA-Interim are used to generate storm-centered composites at the time of genesis for Atlantic basin, main development region TCs from 1979?2015. Composites are stratified by their maximum attained intensity: tropical depressions (GTD), tropical storms (GTS), minor hurricanes (GMN), or major hurricanes (GMJ). A multiple-parameter linear regression is then used to associate the eventual attained intensity of tropical cyclone to the obtained variables at genesis. The regression has an adjusted r2 of 0.39, which indicates that a statistical relationship is present. Regression coefficients, along with the spatial distribution of variables in the storm-centered composites, indicate that storms that reach higher intensities are associated at genesis with stronger, more compact, low-level vortices, better-defined outflow jets, a more compact region of high midlevel relative humidity, and higher atmospheric water vapor content.
publisherAmerican Meteorological Society
titleThe Relationship between Tropical Cyclones at Genesis and Their Maximum Attained Intensity
typeJournal Paper
journal volume30
journal issue13
journal titleJournal of Climate
identifier doi10.1175/JCLI-D-16-0554.1
journal fristpage4897
journal lastpage4913
treeJournal of Climate:;2017:;volume( 030 ):;issue: 013
contenttypeFulltext


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