On December 16, 2007, the skies above Oslo, Norway, were adorned with a breathtaking display of atmospheric optics known as a halo display. This phenomenon, caused by the interaction of light with ice crystals in the atmosphere, created a mesmerizing spectacle that captivated observers. The diamond dust display covered a wide area of approximately 30-40 kilometers, showcasing various prominent features.
Johannes Lillegaard, an avid sky watcher, managed to capture the essence of the halo display in three stunning images. These images showcased several key elements of the phenomenon:
As observers moved farther from the sun, additional captivating features came into view:
The halo display in Oslo showcased some unique and rarely observed atmospheric optics phenomena:
As the display extended outward from the sun, two specific phenomena caught the attention of observers:
Odd-Tore Saugerud, situated near Oslo's Kolsås, managed to capture stunning images of low sun halos caused by diamond dust in the valley. These images showcased several distinct features:
In conclusion, the halo display observed in Oslo, Norway on December 16, 2007, was a remarkable atmospheric optics event that showcased a wide range of captivating features. From the dominant upper tangent arc to the rare Moilanen and Parry arcs, as well as the supralateral arc and 46° halo in the outer regions, this display left observers in awe of the wonders of nature. The subhorizon arcs added another layer of complexity to the spectacle, providing a visual feast for those lucky enough to witness it.
The diamond dust display covered a wide 30-40 km
area. Johannes Lillegaard took the three images at top showing its main aspects; a dominant "V" shaped upper tangent arc, bright sundogs, a 22° halo, a parhelic circle and upper and lower sun pillars. Further from the sun, a colourful supralateral arc and a 46° halo shone.
There were other halos. A rare Moilanen arc was seen in one location. A bright sunvex Parry arc sat close above the upper tangent arc. From high ground and close to sunset the diamond dust created a lower tangent arc and subparhelia.
Moilanen arc - Steinar Midtskogen captured images 4 and 5. The lower one shows a rare Moilanen arc - the "V" shaped arc above the sun and halfway towards the 22° halo. The arc was possibly made by crystals nucleated by ski-slope snow machines 1.5 km to the north.
Parry arc - Signe Strøm Flugsrud's images (6,7) show the "V" shaped sunv
Moilanen arc - Steinar Midtskogen captured images 4 and 5. The lower one shows a rare Moilanen arc - the "V" shaped arc above the sun and halfway towards the 22° halo. The arc was possibly made by crystals nucleated by ski-slope snow machines 1.5 km to the north.
Parry arc - Signe Strøm Flugsrud's images (6,7) show the "V" shaped sunvex Parry arc above the upper tangent arc and mirroring its form.
Supralateral arc & 46° halo - Image (7) and that that of Odd-Tore Saugerud (8) reveal that the outer arcs twice as far from the sun as the 22° halo were a combined supralateral arc and the more rarely seen 46° circular halo. The supralateral arc always touches the (upward curving in images 7,8) circumzenithal arc. The lower arc is the 46° halo. Its separation from the supralateral arc varies with solar elevation and the low sun presented
a good opportunity to see them spaced
well apart.
Subhorizon arcs
Odd-Tore Saugerud captured these very low sun halos at Kolsås near Oslo. Diamond dust in the valley shows the lower half of the 22° halo and the narrow inverted V of a lower tangent arc. Above it is a narrow and intense lower sun pillar. The arms of are subparhelia link upwards to the sundogs.
Images (1)(2)(3) ©Johannes Lillegaard - Images (4)(5) ©Steinar Midtskogen, (6)(7) ©Signe Strøm Flugsrud, (8)(9)(10) ©Odd-Tore Saugerud.
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