Tornadoes in the Central United States and the "clash of air masses"

David M. Schultz, Yvette P. Richardson, Paul M. Markowski, Charles A. Doswell

Research output: Contribution to journalArticlepeer-review

17 Scopus citations

Abstract

Media reports that clashing air masses produce tornadoes in the Central US mischaracterize the abundant new observational and modeling research on how tornadoes form. The consistent message in the media is that tornadoes form along the boundaries between air masses, such as cold fronts or drylines, with tornado formation being directly linked to the intensity of the 'clashing' between adjacent air masses. The reality is that air masses clash all the time, but frontal zones only produce tornadoes on relatively few occasions. Many tornadoes also occur outside of regions where air masses are clashing. In the relatively flat central United States, continental polar, continental tropical, and maritime tropical air masses meet easily, which is a factor in creating the baroclinic environments that favor extra-tropical cyclones.

Original languageEnglish (US)
Pages (from-to)1704-1712
Number of pages9
JournalBulletin of the American Meteorological Society
Volume95
Issue number11
DOIs
StatePublished - Nov 1 2014

All Science Journal Classification (ASJC) codes

  • Atmospheric Science

Fingerprint

Dive into the research topics of 'Tornadoes in the Central United States and the "clash of air masses"'. Together they form a unique fingerprint.

Cite this