Editorial Type:
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Article Type:
Research Article

Close-Range Observations of Tornadoes in Supercells Made with a Dual-Polarization, X-Band, Mobile Doppler Radar

Howard B. Bluestein School of Meteorology, University of Oklahoma, Norman, Oklahoma

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Michael M. French School of Meteorology, University of Oklahoma, Norman, Oklahoma

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Robin L. Tanamachi School of Meteorology, University of Oklahoma, Norman, Oklahoma

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Stephen Frasier Microwave Remote Sensing Laboratory, Department of Computer and Electrical Engineering, University of Massachusetts, Amherst, Amherst, Massachusetts

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Kery Hardwick Microwave Remote Sensing Laboratory, Department of Computer and Electrical Engineering, University of Massachusetts, Amherst, Amherst, Massachusetts

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Francesc Junyent Microwave Remote Sensing Laboratory, Department of Computer and Electrical Engineering, University of Massachusetts, Amherst, Amherst, Massachusetts

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Andrew L. Pazmany Microwave Remote Sensing Laboratory, Department of Computer and Electrical Engineering, University of Massachusetts, Amherst, Amherst, Massachusetts

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Print Publication:
01 Apr 2007
DOI:
https://doi.org/10.1175/MWR3349.1
Page(s):
1522–1543
Restricted access

Abstract

A mobile, dual-polarization, X-band, Doppler radar scanned tornadoes at close range in supercells on 12 and 29 May 2004 in Kansas and Oklahoma, respectively. In the former tornadoes, a visible circular debris ring detected as circular regions of low values of differential reflectivity and the cross-correlation coefficient was distinguished from surrounding spiral bands of precipitation of higher values of differential reflectivity and the cross-correlation coefficient. A curved band of debris was indicated on one side of the tornado in another. In a tornado and/or mesocyclone on 29 May 2004, which was hidden from the view of the storm-intercept team by precipitation, the vortex and its associated “weak-echo hole” were at times relatively wide; however, a debris ring was not evident in either the differential reflectivity field or in the cross-correlation coefficient field, most likely because the radar beam scanned too high above the ground. In this case, differential attenuation made identification of debris using differential reflectivity difficult and it was necessary to use the cross-correlation coefficient to determine that there was no debris cloud. The latter tornado’s parent storm was a high-precipitation (HP) supercell, which also spawned an anticyclonic tornado approximately 10 km away from the cyclonic tornado, along the rear-flank gust front. No debris cloud was detected in this tornado either, also because the radar beam was probably too high.

* Current affiliation: ProSensing, Inc., Amherst, Massachusetts

Corresponding author address: Dr. Howard B. Bluestein, School of Meteorology, University of Oklahoma, 120 David L. Boren Blvd., Suite 5900, Norman, OK 73072. Email: hblue@ou.edu

Abstract

A mobile, dual-polarization, X-band, Doppler radar scanned tornadoes at close range in supercells on 12 and 29 May 2004 in Kansas and Oklahoma, respectively. In the former tornadoes, a visible circular debris ring detected as circular regions of low values of differential reflectivity and the cross-correlation coefficient was distinguished from surrounding spiral bands of precipitation of higher values of differential reflectivity and the cross-correlation coefficient. A curved band of debris was indicated on one side of the tornado in another. In a tornado and/or mesocyclone on 29 May 2004, which was hidden from the view of the storm-intercept team by precipitation, the vortex and its associated “weak-echo hole” were at times relatively wide; however, a debris ring was not evident in either the differential reflectivity field or in the cross-correlation coefficient field, most likely because the radar beam scanned too high above the ground. In this case, differential attenuation made identification of debris using differential reflectivity difficult and it was necessary to use the cross-correlation coefficient to determine that there was no debris cloud. The latter tornado’s parent storm was a high-precipitation (HP) supercell, which also spawned an anticyclonic tornado approximately 10 km away from the cyclonic tornado, along the rear-flank gust front. No debris cloud was detected in this tornado either, also because the radar beam was probably too high.

* Current affiliation: ProSensing, Inc., Amherst, Massachusetts

Corresponding author address: Dr. Howard B. Bluestein, School of Meteorology, University of Oklahoma, 120 David L. Boren Blvd., Suite 5900, Norman, OK 73072. Email: hblue@ou.edu

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