The traditional place to search for Lowitz arcs is, where Lowitz first recorded them in 1790, as small arcs extending sunwards from the sundogs and joining the 22° halo. That is perhaps one reason why they were so rarely observed.
The upper Lowitz arc is more frequently seen, as here, curving downwards from an upper Parry arc - crossing the upper tangent arc - and then merging with a 22° halo.
The HaloSim ray tracing at right shows Lowitz crystal arcs in red. Arcs near the sundogs are prominent because traditionally oriented Lowitz crystals were used. Those in Andrew Kirk's display might have been columnar and rocking back and forth around the Parry orientation. This strongly favours the upper arc that was observed. There is no evidence - see lower image - of arcs near the sundogs.
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