I see folks have already confirmed this is tornado debris.
But for those who want to learn you have to use CC in conjunction with other radar variables to confirm. You'll want to pair this CC up with differential reflectivity (ZDR), reflectivity (Z), and velocity (V or SRV). So the drop in CC must be collocated with sufficient Z (> 20 dBZ would be ideal if not higher), a V couplet, and near 0 ZDR (debris tumbles like hail and looks neither tall or wide to the radar).
Now one caveat is that Z and CC are sampled by the radar first, and then V. So it is possible that the couplet may be displaced slightly ahead of the TDS because of storm motion (especially in fast moving storms), but it shouldn't be far away.
A commonly misidentified TDS is in the inflow region of supercells. Dust, bugs, etc. are all very low in CC too, so a quick check of Z will show that dBZs aren't high enough to be a true TDS.