2011
DOI: 10.1016/j.atmosres.2010.10.011
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An F3 downburst in Austria—A case study with special focus on the importance of real-time site surveys

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Cited by 20 publications
(6 citation statements)
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“…The surface data (Figure 6) show a 180° wind shift and a rise in pressure but little change in temperature. Given this behavior, the evolution of the radial velocity field away from a strong outflow (Figure 5) and a fine line moving ahead of the leading edge of the system suggest a weakening of the cold pool and the likely generation of an atmospheric bore (e.g., Haghi et al, 2017; Kingsmill & Wakimoto, 1991; Pistotnik et al, 2011; Roberts & Wilson, 1989; Takayama et al, 1997; Wakimoto & Bringi, 1988). Evidence supporting this statement can be found in the Haghi et al (2017) study that utilized past analyses in the literature to classify fine lines in the nocturnal environment.…”
Section: Observational Analysismentioning
confidence: 98%
“…The surface data (Figure 6) show a 180° wind shift and a rise in pressure but little change in temperature. Given this behavior, the evolution of the radial velocity field away from a strong outflow (Figure 5) and a fine line moving ahead of the leading edge of the system suggest a weakening of the cold pool and the likely generation of an atmospheric bore (e.g., Haghi et al, 2017; Kingsmill & Wakimoto, 1991; Pistotnik et al, 2011; Roberts & Wilson, 1989; Takayama et al, 1997; Wakimoto & Bringi, 1988). Evidence supporting this statement can be found in the Haghi et al (2017) study that utilized past analyses in the literature to classify fine lines in the nocturnal environment.…”
Section: Observational Analysismentioning
confidence: 98%
“…Because PV intrusions have been observed in association with cold-season derechos (e.g. Pistotnik et al, 2011), we also analysed fields of potential vorticity (PV) on the 320 K isentropic surface. We used archived GFS charts of wetter3.de (http://www1.wetter3.de/Archiv/), concentrating on PV intrusions as indicated by sharp PV gradients and large PV values of more than 1.5 PV units (PVU; 1 PVU = 10 −6 Kkg −1 m 2 s −1 ); PV was only available for years after 1998.…”
Section: Methodsmentioning
confidence: 99%
“…In contrast to the examples of German warm-season type derechos, German cold-season type derechos form within north-westerly large-scale flow (Gatzen et al, 2011;Pistotnik et al, 2011;Mathias et al, 2018). In particular, Pistotnik et al (2011) describe a mid-troposphere PV intrusion in one of the cold-season type derechos. Cold-season type derechos form along narrow cold-frontal rainbands in an environment similar to high-shear-low-CAPE situations described for the United States (e.g.…”
mentioning
confidence: 94%
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