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   Lowitz Arcs  

  
  


Two aspects of a 1988 Lowitz arc display observed by Robert Gorkin at Dover, Delaware, USA.

Lowitz arcs extend upwards and downwards from the parhelion towards the 22° halo. But, as usual, they are faint and indistinct.

Much clearer is the upper Lowitz arc extending up from the 22 degree halo, crossing the upper tangent arc and meeting the Parry arc. Look in this region when the sun is 15 - 30 degrees high for the best chance to see a Lowitz.



















































 

 

Lowitz arcs were the most controversial of the halos. They were first recorded in 1790, but even until the 1990s their existence was doubted. Now, see the gallery, digital cameras, easy Internet communication and much increased interest in atmospheric optics combine to produce images each year. Nonetheless, Lowitz arcs remain rare. When they are seen they are usually fleeting, faint and indistinct.

Looking for a Lowitz arc? The traditional search is for arcs extending from a sundog to the nearby 22° halo. Do this, but look out for other features. The 22° halo at 10 and 2 o’clock is often brighter where a Lowitz arc touches it. The 22° halo is conversely rather weaker next to the parhelion. The upper Lowitz arc can be most evident above the 22° halo.

Lowitz arcs are closely related to Parry arcs and the upper Lowitz arc is always tangential to a suncave Parry. Therefore, look closely at the region between a Parry arc and upper tangent arc. With luck, a faint Lowitz arc will be seen curving downwards. When the sun is low and the twin ‘V’s of an upper tangent and suncave Parry are visible, look also for a middle Lowitz arc touching the Parry.

The classical explanation for Lowitz arc formation is via Lowitz oriented plate crystals. These ‘rotate’ or take all rotational positions about a near horizontal ‘Lowitz axis’. Lowitz rays pass between two prism side faces inclined at 60°. As with Parry arcs, there are three possible routes and for Lowitz oriented crystals they produce upper, middle and lower arcs. The Lowitz orientation is unusual and perhaps not aerodynamically very favourable. This might account for the arcs’ rarity but there may be other factors.

Recently Marko Riikonen et.al.* analysed several Lowitz displays with clear and well defined arcs and concluded that, for some, the classical explanation was not adequate. The arc relative intensities were better simulated using semi-regular hexagonal plates or prisms rather than the regular ones previously assumed. Furthermore, the observed extent of arcs suggest that crystals take limited orientations about the Lowitz axis rather than all rotational positions. The Lowitz story is not over yet.



Riikonen, M., Cowley, L., Schroeder, M., Pekkola, M, Öhman, T. and Hinz, C.,
The Lowitz Arcs
, Weather, September 2007, Vol.62, No.9, pp252-6