Abstract
Abstract The relatively rare case of an explosive land cyclone that occurred on I5–17 November 1989 over the United States and Canada is investigated to determine the physical mechanisms responsible for its development. Hourly surface and 12-h upper-air data are analyzed for this storm for the 36-h period beginning on 0000 UTC 15 November. The system appears to develop through favorable positioning of the surface low with respect to a 5OO-hPa short-wave trough and 250-hPa jet streak and yields the greatest deepening of 13 hPa in 12 h. Through an analysis of the terms in the quasigeostrophic height tendency equation, quasigeostrophic theory is deemed to be qualitatively inaccurate in diagnosing the development of this system. The performance of the National Meteorological Center's (currently known as the National Centers for Environmental Prediction) operational models is viewed, and errors in model forecasts of surface low position and intensity are attributed in large part to faulty initialization. A com...
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.