Tropical transition: Tropical cyclone formation from extratropical disturbances

Christopher A. Davis, Lance F. Bosart

Research output: AbstractPaperpeer-review

1 Scopus citations

Abstract

Two pathways of tropical transition (TT), one involving initially strong extratropical precursors and the other involving perturbations that mainly organize convection but do not grow from baroclinic energy conversion, were analyzed. The two classes of precursors were referred to as strong extratropical (SE) and weak extratropical (WE). In SE cases, a low-latitude frontal cyclone developed to an intensity sufficient to trigger wind-induced surface heat exchange. In WE cases, precursor disturbances can be weak baroclinic waves.

Original languageEnglish
Pages30-31
Number of pages2
StatePublished - 2004
Event26th Conference on Hurricanes and Tropical Meteorolgy - Miami, FL., United States
Duration: May 3 2004May 7 2004

Conference

Conference26th Conference on Hurricanes and Tropical Meteorolgy
Country/TerritoryUnited States
CityMiami, FL.
Period05/3/0405/7/04

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