In this study, a synthetic PAR data tool is applied to two tornadic cases (24 May 2011 El Reno, Oklahoma, tornado and the 24 May 2016 Dodge City, Kansas, tornadoes) and one non-tornadic case (17 April 2013 near Lawton/Medicine Park, Oklahoma). Range and azimuth averaging are applied (only in the horizontal due to vertical data limitations in the datasets) over different windows to emulate different standoff ranges more comparable to operational, fixed-site radars. Using dealiased velocity data, intensity of synthetic PAR tornado vortex signatures (TVSs) is analyzed using a measure of the rotational intensity (Delta-V) as a function of time and height for each standoff range as well as for pencil beam scans versus spoiled imaging beams. The impacts of PAR-enabled imaging are analyzed using planned position indicators (PPIs). A comparison of tornadic and non-tornadic cases will be presented to illustrate simulated operational PAR examples. Results indicate that despite increasing standoff ranges and using imaging modes, an operational PAR should still observe a similar mode of tornadogenesis as mobile systems (i.e., non-descending TVS) with a slight delay in observing intensification at increasing standoff ranges. The PAR-enabled imaging mode shows promising results in enabling targeted and more complete data on vertical TVS evolution (through denser vertical sampling). Ultimately, through understanding the meteorological benefits from the synthetic PAR data, we should be able to contribute to improved planning for future all-digital operational PARs and warning decisions for tornadic storms.

