In a relative vorticity framework you get positive vorticity by either curvature (around a low) or by a positive change in wind speed to the right of the vector. Vort "lobes" tend to be produced by the curvature in, or in advance of a low, and the "ribbons" tend to be from areas of high wind shear across a horizontal distance.
Look at an H5 wind map, then look at at an H5 Rel. Vort map, then flip them back and forth. You'll see it.