The formation of 44° parhelia differs from other halos in that it's not caused directly from sun rays, but from light rays of another halo - namely the common 22° parhelia. In other words, it is the parhelia of parhelia. Formation of 44° parhelia seem to require diamond dust conditions and very bright 22° parhelia. According to Jarmo Moilanen, also low sun elevation is essential to ensure there are enough ice crystals between the sun and observer. Here the sun elevation is 2°.
List of photographed occurrences of 44° parhelia:
- 3 Dec 1970, Saskatoon, Canada, Earle Ripley (photos not shown)
- 23 Jan 2002, Vaala, Finland, Jarmo Moilanen (drawing shown)
- June 2002, Greenland, Matthew Hyde
- 30 Dec 2002, Juva, Finland, Jari Piikki (drawing shown)
- 3 Jan 2004, Minnesota, USA
- 21 Nov 2004, Teuva, Finland, Heikki Mahlamäki
- 21 Dec 2005, Viitasaari, Finland, Jaakko Tähti
- 3 Jan 2006, Stockholm, Sweden, Yvonne Primé
Jaakko Tähti deserves congratulations!
VálaszTörlésFor completeness of the records, the Minnesota display was on 3rd January
2004. A low sun display. Bright left and right hand 44° parhelia were photographed. The 46° halo was bright and this allows the precise angle of the parhelia to be measured by comparison of their position with that of the 46° halo.