The 18Z vLaps initiated with the one cell but unfortunately did not produce the cluster of storms that developed across central Indiana behind the original one (upper left). You can see the Maximum base reflectivity (upper right) also produces some convection too far south and west. The surface simulated brightness temperature (bottom left) shows the one storm but doesn’t account for the other ones as you can see on the actual IR Satellite image (bottom right). We will see if the 19z run does better!













