The Flare Echo: Reflectivity and Velocity Signature
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Abstract The characteristics and causes of a radar artifact called a flare echo are described. The spike or flare-shaped echo typically has reflectivities <20 dBZ, and approaching Doppler velocities. It extends radially 10–20 km downrange of some intense radar storm echoes. Zrnic recently proposed a three-body scattering scenario to explain its occurrence, which consists of scattering by the hydrometeors to the ground, backscattering by the ground to the hydrometeors and scattering by the hydrometeors to the radar. In addition he developed relationships that predict the behavior of the flare reflectivities and velocities. The data presented here support Zrnic's three-body scattering explanation and relationship, indicating that the flare echo power is dependent on the inverse cube of the distance from the large hydrometeors to the ground. The flue Doppler velocities depend on the radial velocity and fall speed of the hydrometeors responsible for producing the flare. However, it was found that Zrnic's theo...