Sparta, NJ: 12 August 2000
Low-centroid, warm-topped, terrain-locked convection
Post-frontal moist ENE flow into terrain rise, high RH
Unimpressive PW’s and Td’s unless one considers the overall cool anomaly that existed
High moisture relative the low thickness values
Very active low-level precipitation growth due to enhanced low-level vertical motion where low-level wind max is normal to terrain
Northeastern Topography Map