Proximity soundings for severe convection for Europe and the United States from reanalysis data

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Overshooting cloud top detections using MSG SEVIRI Infrared brightness temperatures and their relationship to severe weather over Europe (2011, background): “Sander et al. (2008), Brooks (2009), and Kaltenböck et al. (2009) found that severe storms in an environment with large 0–1 kmwind shear and a low lifted condensation level aremost likely to produce a significant tornado across Europe.”
A Review of Planetary Boundary Layer Parameterization Schemes and Their Sensitivity in Simulating Southeastern U.S. Cold Season Severe Weather Environments (2015, unknown): “Brooks (2009) shows that CAPE and deep-layer shear combinations associated with signiﬁcantly severe thun-derstorms in Europe are more similar to those associated with the southeastern U.S. cold season than the entire full-U.”
A Climatology of Tornadoes in Europe: Results from the European Severe Weather Database (2014, methodology): “Both Storm Data (e.g., Rasmussen and Blanchard 1998; Thompson et al. 2003; Craven and Brooks 2004), and the ESWD (Kaltenböck et al. 2009; Brooks 2009, 2013) have been used in such studies, combining storm reports with radiosonde measurements or data from numerical atmospheric models.”