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Convective Systems: Squall lines and Bow Echoes . ASP Colloquium 2006. Morris Weisman (NCAR/MMM). Radar Composite 7 May 1995 VORTEX. Radar Composite 26 May 1997. Radar Composite 11 June 2001. Squall Line Environments:. Bow Echoes: Fujita 1978. Bow Echoes: Fujita 1978.
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Convective Systems: Squall lines and Bow Echoes ASP Colloquium 2006 Morris Weisman (NCAR/MMM)
15 July 1995 Tree Blow Down in Adirondacks, 8 killed
So, how well do numerical models reproduce this observed spectrum?? Comet Web Modules: htpp://meted.ucar.edu/topics_convective.php • Convective Storm Matrix • MCS Matrix
RKW Theory Rotunno et al. (JAS, 1988) C/∆u > 1 “Optimal”condition for cold pool lifting C/∆u = 1 C/∆u < 1
Early System Evolution “Optimal” C/∆u << 1 C/∆u ~ 1
Mature System: C/∆u > 1
How can we systematically produce the observed line-end vortex pattern?
Line-end vortex mechanisms: Early Phase:
Line-end vortex mechanisms: Mature Phase:
Role of Line-End Vortices Focuses and Intensifies Rear-Inflow Jet
Symmetric-to-asymmetric evolution represents a generic property of finite-length squall lines in the presence of Coriolis forcing.
X Upscale Growth of Convection Chris Davis (NCAR/MMM) Bow echoes 0540 UTC 10 June, 2003 MCV 0600 UTC 10 June, 2003 MCSs 11 June, 2003