Kinematic parameters derived from the dual-Doppler wind field show multiple centers of large magnitude vertical vorticity (up to 10-2 s-1) concentrated in the lowest levels of the atmosphere. While not of the same spatial scale as the tornadoes produced, it is noted that many of these vorticity cores line up well with tracks of the MCV-produced tornadoes over Marshall and Jackson Counties. Vertical motion magnitudes were relatively weak (< 10 m s-1) and peaked below 6 km AGL, consistent with the shallow extent of the reflectivity field (generally below 8 km AGL) and lack of observed lightning. Dual-polarimetric observations from the ARMOR permit an investigation of hydrometeor distribution. Initial results suggest a centrifuge-like separation of targets.
In addition to discussing the radar-derived structures, we will attempt to evaluate the governing dynamics of the MCV feature and assess the possible impact of its passage over more heterogeneous terrain. Of particular interest is the question of why the MCV became such a prolific tornado producer. The entity had produced few tornadoes (an EF-3 in Walker County, and an EF-2 in Cullman County) from its development, but once it reached the Lake Guntersville area, it spawned a flurry of weaker tornadoes, some of which occurred simultaneously.