july 7 2009 night time supercell

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July 7 2009 Night time Supercell • Convection developed over Central NY and then intensified into two discrete line segments in low CAPE/high shear environment. One of these segments developed a low topped supercell tracking se along the Lower Hudson Valley/NE NJ border into Nassau County. Severe hail and winds were experienced with this storm.

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Page 1: July 7 2009 Night time Supercell

July 7 2009 Night time Supercell

• Convection developed over Central NY and then intensified into two discrete line segments in low CAPE/high shear environment. One of these segments developed a low topped supercell tracking se along the Lower Hudson Valley/NE NJ border into Nassau County. Severe hail and winds were experienced with this storm.

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Radar

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Reflectivity Storm Relative Velocity

Velocity Tornado Vortex algorithm output

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Developing Supercell

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Supercell…with nice inflow notch and strong mesocyclone

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TVS signature

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Instability

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Only marginal elevated instability to work with

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Marginal to little surface instability

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Surface Analysis

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Weak surface trough…providing low-level convergence and moisture pooling

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Weak surface low providing some low-level convergence and shear

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There is not much instability, and only a weak surface low…so what was the forcing for these storms?

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100 kt upper level jet streak approaching region!!…with strong upper level divergence

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60 kt 0-6 km shear!!

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Strong jet dynamics and deep layer shear were able to overcome weak nightime instability to explosively strengthen storms into supercell. Low-level shear and helicity environment was less than ideal for tornadic formation…but the supercell had a subtle surface boundary and surface low to work with…which locally enhanced low level shear and convergence.

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Severe Radar Signatures

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4 Panel Reflectivity

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3 body scatter spike…w/ 75 dbz at 17500 ft...(-12c at 16kft) at 323z – Guaranteed Sign of Severe Hail !!

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Nice inflow notch, wer and 3 body scatter spike at 327z

Golf ball size hail reported in Yonkers!

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4 Panel SRM

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Strong and persistent mesocyclone indicative of strong updrafts…a supercell.

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30 kt Vr shear on 0.5deg slice at about 3500 ft at 331z

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4-panel Vel

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50 kt inbounds on 0.5 deg slice at about 4kft.

Lots of trees down in NE Bergen, S Westchester, and NW Nassau Counties. 100 mph winds estimated in Yonkers. 17000 without power at one point in Westchester.

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Derived Radar Products

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50-55 Vil. Vil threshold at the time was 40-45.

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Echo Tops only 30-35 kft…indicative of low topped convection