Observations of Tornadoes and Other Convective Phenomena with a Mobile, 3-mm Wavelength, Doppler Radar: The Spring 1999 Field Experiment

By H. Bluestein, A. Pazmany. 2000

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Dust devils on Earth and Mars (2006, methodology): “Vh values up to 25 m s 1 have been measured in situ in approximate agreement with remote sensing measurements for Vh made using lidar of 11 m s 1 [Bluestein and Pazmany, 2000] and 22 m s 1 [Schwiesow and Cupp, 1975].”
THE SECOND VERIFICATION OF THE ORIGINS OF ROTATION IN TORNADOES EXPERIMENT (2012, background): “The most frequent observations have been by mobile radars at close range to tornadoes (e.g., Wurman et al. 1996a,b, 1997; Wurman and Gill 2000; Bluestein and Pazmany 2000; Wurman 2002; Lee and Wurman 2005; Bluestein et al. 2004; Wurman and Alexander 2005; Alexander and Wurman 2005; Bluestein et al.…”
Centrifuging of Hydrometeors and Debris in Tornadoes: Radar-Reflectivity Patterns and Wind-Measurement Errors (2005, background): “Significant radar scatterers in high-reflectivity regions could include hydrometeors, insects, gravel, plant material, and debris from man-made structures; in the case of millimeter-wavelength radar observations, smaller scatterers might also be significant (Bluestein and Pazmany 2000).”
The Multiple-Vortex Structure of a Tornado (2002, background): “Subsequent observations from a 3-mm-wavelength mobile radar revealed evidence of multiple vortices in one of the tornadoes that occurred during the 3 May 1999 Oklahoma tornado outbreak (Bluestein and Pazmany 2000).”