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Improvement of the WSR-88D Mesocyclone Algorithm

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Improvement of the WSR-88D Mesocyclone Algorithm Accepted for publication in Weather and Forecasting 1998 IMPROVEMENT OF THE WSR-88D MESOCYCLONE ALGORITHM Robert R. Lee*1 and Anderson White1 1 WSR-88D Operational Support Facility (OSF), Norman, Oklahoma Submitted to: Weather and Forecasting Draft: 15 December 1997 ABSTRACT distracted by false alarms from the radar. In turn, the programmer must balance the radar software such that The Build 9 Weather Surveillance Radar - 1988, it detects most mesocyclonic circulations yet warns Doppler (WSR-88D) Mesocyclone Algorithm (B9MA) is mainly on those with the potential for becoming severe. designed to locate mesocyclones (rotating thunderstorm updrafts with diameters between 1.8 - 9.2 km (1 - 5 nm)). The purposes of this paper are: to explain some of the Because there is less than a one to one correspondence inner workings and limitations of the (current) Build 9 between tornadoes and mesocyclones, the B9MA alerts WSR-88D Mesocyclone Algorithm,hereafter B9MA; to forecasters when it detects circulations that meet its outline steps forecast offices may take to adjust the criteria but tornadoes may not be observed. On the other algorithm for optimum performance in their local warning hand, some tornadoes are not accompanied by large areas; and report on an Integrated Rotational Strength scale meoscyclonic circulations. Weather radars can not index, a potential improvement to mesocyclone resolve small scale tornadic circulations, and the B9MA evaluation by the WSR-88D. may fail to alert forecasters that a tornado is present. The B9MA is only one of many tools that forecasters should The paper is organized as follows: There is a general use to predict tornado formation. discussion of mesocyclones and tornadoes that may or may not be detected by Doppler weather radar. Next, This paper describes limitations of the B9MA and how to there is an explanation of how the B9MA processes data improve its performance. The correlation between and a description of initial attempts to regionalize the algorithmic detections and severe weather occurrence algorithm through the use of adaptable parameters to may be optimized under the premise that storms with minimize the number of false detections and reduce the strong, deep rotations are more likely to be associated bias toward Great Plains storms. This is followed by a with severe weather. Some tornadic circulations missed historical perspective on operational rules of thumb by the B9MA can be detected when the value of pertaining to mesocyclone strength analysis coupled with Threshold Pattern Vector (TPV), a B9MA adaptable recent strategies to incorporate these rules into parameter, is lowered. When a rotational strength filter is calculating an Integrated Rotational Strength index. added to the program logic, some algorithm detections of Results of several studies are presented. Finally, a nontornadic mesocyclones can be eliminated. summary and conclusions are offered along with suggestions for future research. 1. INTRODUCTION 2. LIMITATIONS OF DETECTING MESOCYCLONES Storms containing strong, deep, rotating updrafts have BY DOPPLER WEATHER RADAR a high likelihood of producing tornadoes, large hail (>2.0 cm diameter), and damaging wind (Fujita, 1963); yet, The first step forecasters can take towards improving based on a 20 year study of Doppler radar data in B9MA performance is to consider several limitations. The Oklahoma, Burgess et al. (1963) observed only 30% to conceptual model is too simplistic. All mesocyclones do 50% of supercell mesocyclones actually produce not produce tornadoes. Radar geometry limits detection tornadoes. This dichotomy creates a dilemma both for of smaller scale rotational features. Incorrectly dealiased the forecast meteorologist and for the Doppler velocities may cause misses or false alarms. programmer-meteorologist who designs and fine-tunes algorithms for the Weather Surveillance Radar - 1988 The B9MA examines Doppler velocity data, identifies Doppler (WSR-88D). The forecaster wants to be alerted regions of cyclonic shear, and models flow after a to those mesocyclonic circulations potentially associated Rankine-combined vortex (Hennington and Burgess with tornadoes but at the same time cannot afford to be 1981; Wood and Brown 1983; Zrnic et al. 1984). Applying simplistic assumptions to complex, dynamic flow fields such as gust fronts and squall lines results in algorithm * Corresponding author address: Robert R. Lee, WSR- detections that alert forecasters to isolated, rotating 88D Operational Support Facility, 1200 Westheimer Drive updrafts and potentially severe circulations that are not Norman, OK 73069; e-mail: [email protected] present. Desrochers and Harris (1996) examined and questioned range from the radar. If cyclonic shear exists, Doppler the assumptions inherent in the Rankine-combined vortex velocity increases from the first bin to the second and an paradigm and developed a more sophisticated model. "open" or incomplete pattern vector is created They proposed a nonsymmetrical flow model based on at the azimuth and range of the first velocity bin. The vorticity and divergence rather than on the Rankin- procedure continues for the next two radials, and so on, combined vortex design used as the basis of fielded until cyclonic shear no longer is detected and the pattern WSR-88D software and National Severe Storms vector is “closed.” In this manner all pattern vectors within Laboratory (NSSL) developmental algorithms (Stumpf the radar volume scan are identified. 1998). Momentum and shear values are calculated for each Non-supercell tornados such as waterspouts and pattern vector as follows: landspouts (associated with gust fronts, squall lines, hurricanes, derechos, and microbursts) are not usually and accompanied by larger scale (1.8 - 9.2 km (1 - 5 nm)) mesocyclonic circulations. Since individual tornadic where VIn and VOut are maximum base velocity values vorticies are too small to be identified by the B9MA toward and away from the radar, respectively (Zrnic et al. except at very close range, forecasters should not expect 1984). Momentum and shear values are compared to the the algorithm, in general, to detect non-supercell following adaptable parameters: Threshold High tornadoes. Momentum (THM), Threshold High Shear (THS), Threshold Low Momentum (TLM), and Threshold Low Some F0, F1, and mini-supercell tornadoes form within Shear (TLS). A discussion of these parameters may be rotating thunderstorm updrafts that are shallow (less than found in Zrnic et al. (1984) and Szoke (1988). The three 9.1 km (30 kft) deep) and small in diameter (less than 1.8 letter adaptable parameter designators are provided for km (1 nm)) (Burgess et al. 1995; Grant and Prentice WSR-88D operators so the names of the parameters 1996). Radar limitations such as beam broadening, contained in WSR-88D adaptable parameter menus can range/height dependency, and range folding work against be correlated with their function. Pattern vectors that pass a radar based algorithm attempting to detect tornadic momentum and shear tests are expected to be mesocyclones that form from small-scale, low-level characteristic of mesocyclones. Two-dimensional rotations. features are formed when a minimum number of pattern vectors (adaptable parameter Threshold Pattern Vector The WSR-88D velocity dealiasing algorithm determines (TPV)) are in close proximity to each other. Two- velocity values for each data bin within the area of radar dimensional features are combined in the vertical to form coverage. In regions of high shear, the dealiasing three-dimensional features and mesocyclones are algorithm may assign erroneous or missing velocity identified. For a full description of B9MA processing, see values. Erroneous values have been known to cause the Tipton et al. (1998). B9MA to generate false mesocyclone detections, and missing velocity values have caused circulations to be After the first WSR-88D radars were fielded at several missed. locations around the country, forecasters noted the Mesocyclone Algorithm identified many circulations not The B9MA alerts forecasters to storms that need no associated with tornadoes. Since the Mesocyclone warning and fails, at times, to detect tornadic circulations. Algorithm is designed to detect velocity signatures with These limitations can be mitigated, to some degree, by different size, strength, and shape characteristics, OSF fine-tuning algorithm adaptable parameters; however, the personnel experimented with several case studies and B9MA will never perform perfectly because there is much raised threshold values of shear, momentum, and TPV to more to tornado genesis than the presence of a make the algorithm less sensitive. Algorithmic detections mesocyclone. The next section outlines how the B9MA of nontornadic circulations decreased, but some tornadic processes velocity data to locate mesocyclonic mesocyclones, detected previously, were missed. circulations and discusses initial attempts to optimize algorithm performance using adaptable parameters. The WSR-88D has been fielded throughout the entire country and additional data have been collected. 3. ALGORITHM DESIGN AND ADAPTABLE Forecasters note when default adaptable parameter PARAMETERS values are used in the B9MA, some tornadic mesocyclones are missed. The default adaptable The B9MA searches for cyclonic azimuthal shear patterns parameters are based on research conducted in (pattern vectors) in Doppler velocity data which are Oklahoma (Zrnic et al. 1984) and are shown in Table 1. partitioned into 0.25
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