Downslope windstorm in High Tatras, 19 November 2004
Downslope windstorm in High Tatras, 19 November 2004
Downslope windstorm in High Tatras, 19 November 2004
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2.5 km hydrostatic run with physics• Extreme w<strong>in</strong>d speeds on the lee side: area of <strong>in</strong>creasedstatic stability and downslop<strong>in</strong>g isotherms of „θ“• Vertical velocities: effect similar to “hydraulic jump”NWPotential vorticity + w<strong>in</strong>dSEPot. Temperature + Vertical velocity (Pa/s)