This paper introduces a new storm tracking algorithm that more reliably detects the critical features of a storm such as rear flank downdrafts and regions with high pressure perturbations by incorporating both updraft and reflectivity into the definition of a storm cell. The new storm cell definition improves the results presented in McGovern et al (2007) and Rosendahl (2007) and is designed to move toward a relational model that incorporates high level features such as rear flank downdrafts, updrafts, rain/hail regions and gust fronts and the relationships that exist between those high level features.
We also extend the data mining techniques in two ways. We first extend the rule-finding approach presented in McGovern et al (2007) and Rosendahl (2007) to include boosting. This significantly improves the results and gives us a more varied set of rules which can be used to improve our understanding of tornadogenesis. We also introduce preliminary results with a novel dynamic relational model: the dynamic relational probability tree. This model is designed to learn human-readable models of the critical storm processes and requires the new storm cell definition to identify the high-level features and relationships.
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