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I think that a convergence-line/surface trough was in my neighourhood and caused this change of movement of the shower. It is possible that a pre-existing vortice in the surface windfield became stretched in the updraft and caused the observed rotation. Perhaps the late day-time/weak instability prehibited the forming of a real funnel.
This was not the first time that showers/thunderstorms in a (modified) polar airmass showed some nice visual sights.
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Here a bonus-image of the sunset of 23 July with dissipating convection (at that time the airmass was still warm and humid).
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