15A.2 1 Dual-Frequency Simulations of Radar Observations of Tornadoes
15A.2 1 DUAL-FREQUENCY SIMULATIONS OF RADAR OBSERVATIONS OF TORNADOES David J. Bodine1 ;2 ;3 ;,∗ Robert D. Palmer2 ;3 , Takashi Maruyama4 , Caleb J. Fulton3 ;5 , and Boon Leng Cheong3 ;5 1 Advanced Study Program, National Center for Atmospheric Research, Boulder, CO, USA 2 School of Meteorology, University of Oklahoma, Norman, OK, USA 3 Advanced Radar Research Center, University of Oklahoma, Norman, OK, USA 4 Disaster Prevention Research Institute, Kyoto University, Kyoto, Japan 5 School of Electrical and Computer Engineering, University of Oklahoma, Norman, OK, USA 1. INTRODUCTION based on radar reflectivity factor. A limitation to this technique is that the dominant scatterers must be rain Radars measure reflectivity-weighted particle velocities drops or small objects with similar electromagnetic and rather than air velocities, resulting in measurement errors aerodynamic characteristics, otherwise the correction is when Doppler velocities are used to estimate tornado wind underestimated. Polarimetric radar observations frequently speeds. Snow (1984) and Dowell et al. (2005) show that reveal areas of low co-polar cross-correlation coefficient debris is centrifuged outward relative to the air, and the radial (ρHV ) at S (Ryzhkov et al. 2005; Kumjian and Ryzhkov 2008; Bodine et al. 2013), C (Palmer et al. 2011; Schultz et al. difference between air and particle velocities (ur) depends on vortex dynamics and particle characteristics. Moreover, 2012a,b), and X bands (Bluestein et al. 2007; Snyder and Dowell et al. (2005) also showed that the tangential and Bluestein 2014), even in rural areas where perhaps larger vertical velocities of debris are reduced relative to the air scatterers are less common.
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