Kinematic and polarimetric radar observations of the 10 May 2010, Moore-Choctaw, Oklahoma, tornadic debris signature

The unique polarimetric signature associated with lofted debris is called the tornadic debris signature (TDS). While ties between TDS characteristics and tornado- and storm-scale kinematic processes have been speculated upon or investigated using photogrammetry and single-Doppler analyses, little work has been done to document the three-dimensional wind field associated with the TDS.