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Echo Storm download1/1/2024 A weak tornado was observed in that shear region. Most of the damage was collocated with the strongest Doppler winds but some of the damage occurred beneath the strongest signature of azimuthal shear. The vortex developed at a shear line that was formed by the downdraft outflow of an earlier thunderstorm cell. The damage track can be attributed to a strong radar-observed vortex of 2–7-km diameter. Updraft impulses followed each other in time steps of typically 5 min. The storm reached a weak-evolution mode when the damage occurred. Volume-scan radar data in the direction of the approaching storm are available every 2.5 min. Damage data, meteorological data from a ground micronet, and Doppler radar data are analyzed. Wind damage occurred along a track 15 km long and some 100 m wide. A severe bow-echo storm over northern Switzerland is investigated.
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