I cannot remember which event, but I recall that while SFC Observations showed NE winds with the Wedge, there were observations made at both the Tops Of Stone Mountain (850 ft) and Mount Currahee (Toccoa, 1000 ft) from the SE while upper levels were SW with the jet. Temps and DP were some 10-15 degrees higher also The "ft" I listed is height above surrounding terrain . It shows how shallow wedges are, and the degree of shear. This could very well explain why we sometimes get cells that rapidly turn violent when running into the retreating wedges in NE GA. Also, just got me to thinking... if parcels from just above the surface are heated, while the true "surface" does not, what impact would those rising "near surface" parcels have toward surface based CAPE, etc.