Part
2 Clinton, Essex, and Addison Counties
Convection
•Overall,
the storms were pulse like storms within a broken line of convection
•High
instability and low shear environment (2000 j/kg and 0-6km shear < 15 knots)
•Convective
updrafts were 5 to 15 nm wide and only lasted 20 to 30 minutes before dissipating
•Verification
was limited to do location of storms and no spotters in the vicinity (i.e. southern/central Essex
County, NY and western Clinton
County, NY
•Addison
County Storm collapsed/weakened before entering the county and did not produce any severe weather reports