Non-Convective High Winds Associated with Extratropical Cyclones
2011; Wiley; Volume: 5; Issue: 2 Linguagem: Inglês
10.1111/j.1749-8198.2010.00395.x
ISSN1749-8198
AutoresJohn A. Knox, John D. Frye, Joshua D. Durkee, Christopher M. Fuhrmann,
Tópico(s)Meteorological Phenomena and Simulations
ResumoGeography CompassVolume 5, Issue 2 p. 63-89 Non-Convective High Winds Associated with Extratropical Cyclones John A. Knox, John A. Knox Department of Geography, University of GeorgiaSearch for more papers by this authorJohn D. Frye, John D. Frye Department of Geography, Kutztown UniversitySearch for more papers by this authorJoshua D. Durkee, Joshua D. Durkee Meteorology Program, Department of Geography and Geology, Western Kentucky UniversitySearch for more papers by this authorChristopher M. Fuhrmann, Christopher M. Fuhrmann Department of Geography, University of North Carolina at Chapel HillSearch for more papers by this author John A. Knox, John A. Knox Department of Geography, University of GeorgiaSearch for more papers by this authorJohn D. Frye, John D. Frye Department of Geography, Kutztown UniversitySearch for more papers by this authorJoshua D. Durkee, Joshua D. Durkee Meteorology Program, Department of Geography and Geology, Western Kentucky UniversitySearch for more papers by this authorChristopher M. Fuhrmann, Christopher M. Fuhrmann Department of Geography, University of North Carolina at Chapel HillSearch for more papers by this author First published: 01 February 2011 https://doi.org/10.1111/j.1749-8198.2010.00395.xCitations: 21Read the full textAboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onEmailFacebookTwitterLinkedInRedditWechat Abstract Non-convective high winds are a damaging and potentially life-threatening weather phenomenon that occurs in the absence of thunderstorms, tornadoes and tropical cyclones. The vast majority of non-convective high wind events develop in association with extratropical cyclones in mid-latitude regions. Interest in non-convective high winds is growing due to their societal impact, gaps in the scientific understanding of the triggering mechanisms for these events, and possible future changes in their frequency and intensity caused by climate change. In this article, non-convective high winds are examined first in terms of their historical and cultural significance and climatological characteristics. Then, four possible mechanisms for the development of non-convective high winds in extratropical cyclones are discussed and critiqued: topography; the isallobaric wind; tropopause folds associated with stratospheric intrusions and dry slots; and sting jets associated with marine frontal cyclones. Evidence for past and future trends in non-convective high wind event frequency and intensity is also briefly examined. New avenues for future work in this emerging area of research are suggested that unite applied and basic research as well as climatological and case-study perspectives. References M. H. Abrams, et al. (eds) (1979). The Norton anthology of English literature, vol. 1. 4th ed. New York: W.W. Norton and Company. Google Scholar Ackerman, S. A. and Knox, J. A. (2007). Meteorology: understanding the atmosphere. 2nd ed. Belmont, CA: Brooks/Cole. Google Scholar Angel, J. R. (1996). Cyclone climatology of the Great Lakes. Publication 172. 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