THE BOW ECHO and MCV EXPERIMENT Observations and Opportunities
THE BOW ECHO AND MCV EXPERIMENT Observations and Opportunities BY CHRISTOPHER DAVIS, NOLAN ATKINS, DIANA BARTELS, LANCE BOSART, MICHAEL CONIGLIO, GEORGE BRYAN, WILLIAM COTTON, DAVID DOWELL, BRIAN JEWETT, ROBERT JOHNS,* DAVID JORGENSEN, JASON KNIEVEL, KEVIN KNUPP, WEN-CHAU LEE, GREGORY MCFARQUHAR, JAMES MOORE, RON PRZYBYLINSKI, ROBERT RAUBER, BRADLEY SMULL, ROBERT TRAPP, STANLEY TRIER, ROGER WAKIMOTO, MORRIS WEISMAN, AND CONRAD ZIEGLER The field campaign, involving multiple aircraft and ground-based instruments, documented numerous long-lived mesoscale convective systems, many producing strong surface winds and exhibiting mesoscale rotation. hile the observational study of mesoscale Kansas Preliminary Regional Experiment for convective systems (MCSs) has been active Stormscale Operational and Research Meteorology W since the 1940s (e.g., Newton 1950 and ref- (STORM)-Central (PRE-STORM) (Cunning 1986) erences within), until the Bow Echo and Mesoscale were geographically fixed by the ground-based instru- Convective Vortex Experiment (BAMEX) there were ment networks employed. The unique observing no studies designed to sample multiscale aspects of strategy of BAMEX relied on the deployment of these systems throughout the majority of their life highly mobile observing systems, both airborne and cycles. Previous field studies such as the Oklahoma- ground based, supported by the enhanced operational AFFILIATIONS: DAVIS, BRYAN, DOWELL, KNIEVEL, BARTELS, LEE, Missouri; SMULL—NSSL, and University of Washington, Seattle, TRIER, AND WEISMAN—National
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