2009
DOI: 10.1175/2008jtecha1084.1
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3D Convective Storm Identification, Tracking, and Forecasting—An Enhanced TITAN Algorithm

Abstract: Storm identification, tracking, and forecasting make up an essential part of weather radar and severe weather surveillance operations. Existing nowcasting algorithms using radar data can be generally classified into two categories: centroid and cross-correlation tracking. Thunderstorm Identification, Tracking, and Nowcasting (TITAN) is a widely used centroid-type nowcasting algorithm based on this paradigm. The TITAN algorithm can effectively identify, track, and forecast individual convective storm cells, but… Show more

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Cited by 140 publications
(127 citation statements)
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“…Although existing algorithms designed to detect thunderstorms, mesocyclones and tornado vortex signatures, such as thunderstorm identification, tracking, analysis and nowcasting (TITAN; Dixon and Wiener, 1993); storm cell identification and tracking (SCIT; Johnson et al, 1998); the National Severe Storms Laboratory (NSSL) Tornado vortex signature detection algorithm (TDA; Mitchell et al, 1998); the NSSL mesocyclone detection algorithm (MDA; Stumpf et al, 1998); w2segmotion (Lakshmanan et al, 2007(Lakshmanan et al, , 2009; Thunderstorm observation by radar (ThOR; Barjenbruch and Houston, 2006;Barjenbruch, 2008;Lahowetz et al, 2010) and enhanced-TITAN (E-TITAN; Han et al, 2009) include a tracking component, many recommendations to improve tracking in legacy algorithms have been proposed. For example, Johnson et al (1998) propose that SCIT should incorporate different estimates of initial storm motion throughout the domain and impose limits upon the ability of tracks to change direction.…”
Section: Introductionmentioning
confidence: 99%
“…Although existing algorithms designed to detect thunderstorms, mesocyclones and tornado vortex signatures, such as thunderstorm identification, tracking, analysis and nowcasting (TITAN; Dixon and Wiener, 1993); storm cell identification and tracking (SCIT; Johnson et al, 1998); the National Severe Storms Laboratory (NSSL) Tornado vortex signature detection algorithm (TDA; Mitchell et al, 1998); the NSSL mesocyclone detection algorithm (MDA; Stumpf et al, 1998); w2segmotion (Lakshmanan et al, 2007(Lakshmanan et al, , 2009; Thunderstorm observation by radar (ThOR; Barjenbruch and Houston, 2006;Barjenbruch, 2008;Lahowetz et al, 2010) and enhanced-TITAN (E-TITAN; Han et al, 2009) include a tracking component, many recommendations to improve tracking in legacy algorithms have been proposed. For example, Johnson et al (1998) propose that SCIT should incorporate different estimates of initial storm motion throughout the domain and impose limits upon the ability of tracks to change direction.…”
Section: Introductionmentioning
confidence: 99%
“…Previous studies defined the convective cell as a group of 3D contiguous grids that exceed the reflectivity and volume thresholds (Dixon and Wiener, 1993;Johnson et al, 1998;Han et al, 2009a). The same definition is used in this study.…”
Section: Identification Of Convective Cellsmentioning
confidence: 99%
“…However, other issues such as sensitivities to the convective area radius and spatial reflectivity gradient in the algorithm may be raised and should be tested in detail. The variable or multi-reflectivity threshold method was alternatively suggested for use to alleviate sensitivity to the fixed single reflectivity threshold (Johnson et al, 1998;Handwerker, 2002;Han et al, 2009a). This method has advantages in identifying multiple convective cores with higher reflectivity within convective regions.…”
Section: Identification Of Convective Cellsmentioning
confidence: 99%
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