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Kinematic and Polarimetric Radar Observations of the 10 May 2010, Moore-Choctaw, Oklahoma, Tornadic Debris Signature

机译:Kinematic and Polarimetric Radar Observations of the 10 May 2010, Moore-Choctaw, Oklahoma, Tornadic Debris Signature

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摘要

Tornadoes are capable of lofting large pieces of debris that present irregular shapes, near-random orientations, and a wide range of dielectric constants to polarimetric radars. 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.

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