This improved understanding of the variability and trends in tornadoes should be of immense value to public planners, businesses, and insurance-based risk management agencies. SOI and AO explain the cyclical variability in Dixie Alley. PDO and AMO are also contributing to this multi-time scale variability. NAO and the interplay between NAO and ENSO explained the interannual to multi-decadal variability in Tornado Alley. The step-increase induced due to the installation of the Doppler Radar systems explains the long-term trend in Tornado Alley. Population density explains the long-term trend in Dixie Alley. The influence of the anthropogenic factors and the large-scale climate variables are modeled in a nested framework to unravel secular trend from cyclical variability. The model provides a robust way of estimating the response coefficients by considering pooling of information across groups of states that belong to Tornado Alley, Dixie Alley, and Other States, thereby reducing their uncertainty. Large-scale climate variables include El Niño Southern Oscillation (ENSO), Southern Oscillation Index (SOI), North Atlantic Oscillation (NAO), Pacific Decadal Oscillation (PDO), Arctic Oscillation (AO), and Atlantic Multi-decadal Oscillation (AMO). Anthropogenic factors include increases in population density and better detection systems since the mid-1990s. The annual frequency of tornadoes during 1950–2018 across the major tornado-impacted states were examined and modeled using anthropogenic and large-scale climate covariates in a hierarchical Bayesian inference framework.
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