G'day guys, interesting discussion. There were some great storms around on that day.
Whilst hail flare echos (or TBSS) from an S-Band radar like Mt Stapleton would typically indicate hail >2cm, it's hard for me to see the spike in these images. Here's my reasoning...
As an example, take the bottom-right panel of the image that David posted earlier. Note that the spike is very even and uniform along the beam propagation path.
Now, look at some radials from the 3rd image:
There is a 'spike', but it's not consistent with the azimuth from the Mt Stapleton site. I notice Les Lemon as a contributor to that PDF that Jimmy supplied the link for. Hold on to your hat Jimmy, but I could possibly have greater admiration for this guy than our mate Josh.
In the 90's there was a lot of talk about hail spikes within the NWS/NOAA from Nexrad scans, and Les produced an interesting fact - the length of the flare is determined by the maximum slant range (shown as 'r') in the cone below:
This makes it easy to differentiate between hail flares and other artifacts (such as microwave interference) ; hail spikes will end after a certain distance, interference will not.
My 2c worth...
Mal