On June 12, 2017 as part of the Rivers of Vorticity in Supercells (RiVorS) project, a mobile observed sounding was gathered from NSSL’s P1 mobile mesonet to sample the pre-convective environment of a tornadic supercell near Cheyenne, WY. Based on this sounding, a tornadic supercell was modeled using CM1 at 125-m horizontal grid spacing, and a coherent SVC was indeed shown to be present. Simulated range-height indicator (RHI) data show the strongest vorticity in the SVC was concentrated in Kelvin-Helmholtz billows associated with the vertical wind shear characteristic of the region immediately behind the FFCB. Further simulations were run to test dependence of SVC magnitude and FFCB structure on grid spacing. Parcel trajectories and vorticity budgets were also analyzed to identify parcel paths relative to the baroclinic zone.
Throughout the spring of 2017 and 2018, the TTUKa radars were involved in two field campaigns: The Rivers of Vorticity in Supercells (RiVorS) and NSF National Robotics Initiative (NRI) projects, each seeking to learn more about supercell thunderstorm dynamics through intensive multi-platform observations. On June 12, 2018, a long-duration coordinated deployment involving both TTUKa radars took place on a nearly stationary supercell near Gate, OK. This supercell initially exhibited a strong boundary within the forward flank that was observed with both plan-position indicator and RHI strategies. Strong similarities between the modeled and radar-observed FFCB structure will be reported.