 In this idealized environment, as new updrafts are initiated due to the pressure perturbations from the original split, additional crosswise vorticity will be tilted into the vertical on the flanks of the new updrafts.This will result in the continuation of the process that results in splitting, with a continuous propagation of new updrafts to the right and left of the hodograph.This allows each split to start the process over, splitting again and again until the environmental vertical wind shear no longer favors splitting supercells, or the storms have moved into an unfavorable thermodynamic environment.