Pyramid crystals and odd radius halos, part II

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More halo and crystal photos from the 20/21 January night. While this second crystal sampling and photographing session was under way, the display in the beam was photographed constantly, but again odd radius halos are not visible in the photos, expect perhaps for a suggestion of 35° halo at one stage (not shown). Yet again the sample was littered with classical pyramids as shown by the images in the gallery.

The picture above is an appearance of odd radius halos after the crystal business was over with. It is a “blue minus red” (br) of stack with total of 9m30s exposure and contains 9°, 18° and 35° halos. Three more halo images are in the gallery, first a single frame from the stack above, then two that are versions of another stack, the br displaying full 46° halo.

Jarmo Moilanen / Marko Riikonen

Pyramid crystals and odd radius halos, part I

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The night of January 20/21 in Rovaniemi was a night of odd radius halos. Here are shown mostly crystals collected during a half hour period. At the same time photos were taken continuously in the spotlight beam, below is one of those stacks. The sample contained plenty of traditional type pyramids – something we have not yet seen this winter. So it is curious that odd radius halos are not conspicuous in the beam photos and at times even completely absent. Maybe the abundant cavities in the crystals caused too much disturbance.

The stack is from a stage where the odd radius stuff was at its best, taken towards the end of the crystal collecting period. Visible are 9°, 18° and 35° halos. The temperature during the night was around -33° C.

Jarmo Moilanen / Marko Riikonen

Double Halos

During a sunrise on 2013, May 13th I saw from the Zugspitze (2963m) two pillars with different inclinations. The most remote pillar was diffuse and came from virga below altocumulus; the other one originated from nearby icefog and was narrow and distinct. Unfortunately in most of my photos the two pillars overlap, but at the end they show up separate. The 3-D impression was very fascinating.

Subsuns appear very often during wintertime. It may happen that they appear in two different ice clouds: one of them may be affected by sheer wind causing the crystals to be tilted. Then, two subsuns are visible, one of them being displaced from the solar vertical. A displaced subsun is often a indicator for imminent sheer winds at the observer’s spot.

Double subsun on Mt. Wendelstein (1838m).

Double Subsun on Mt. Zugspitze.

Double Subsuns on Mt. Wendelstein (above) and Mt. Zugspitze.

Author: Claudia Hinz