Central U.S. cyclones were discerned within the ERA5 reanalysis between 1980–2021 using a cyclone identification method adopted from previously published work (Wernli and Schwierz 2006; Sprenger et al. 2017). This unique dataset facilitated an analysis of the monthly and seasonal frequency of Central U.S. cyclones, in which few significant trends were observed during the 42-year period of study. Self-Organizing Maps (SOMs) trained using mean sea-level pressure anomalies from ERA5 were subsequently used to examine the variability in large-scale weather regimes conducive to lee cyclogenesis across the Central U.S. The extent to which the characteristics of cyclone environments (i.e., frontal structure, moisture sources, upper-level jet stream structure, etc.) vary as a function of the prevailing weather regime were also investigated.
References:
Sprenger, M., Fragkoulidis, G., Binder, H., Croci-Maspoli, M., Graf, P., Grams, C. M., Knippertz, P., Madonna, E., Schemm, S., Škerlak, B., & Wernli, H. (2017). Global Climatologies of Eulerian and Lagrangian Flow Features based on ERA-Interim, Bulletin of the American Meteorological Society, 98(8), 1739-1748.
Wernli, H., & Schwierz, C. (2006). Surface Cyclones in the ERA-40 Dataset (1958–2001). Part I: Novel Identification Method and Global Climatology, Journal of the Atmospheric Sciences, 63(10), 2486-2507.

