 Due to the short time scale (scale analysis reveals the Coriolis acceleration in the vorticity equation is negligible on short time scales ), the areas of vorticity result in low pressure (perturbations) on the flanks of the convective updraft.Given favorable environmental thermodynamics (sufficient buoyancy and negligible convective inhibition {CIN}) these pressure perturbations will induce mass flux from below, initiating new convective updrafts.These new updrafts are now located "off" the hodograph, with one to the left and one to the right, both co-located with the previously mentioned pressure perturbations.