As water freezes in the upper atmosphere, small, flat, six-sided, ice crystals might be formed. As these crystals flutter to the ground, much time is spent with their faces flat, parallel to the ground. An observer may pass through the same plane as many of the falling ice crystals near sunrise or sunset. During this alignment, each crystal can act like a miniature lens, refracting sunlight into our view and creating phenomena like parhelia, the technical term for sundogs. The above image was taken last year in Stockholm, Sweden. Visible in the image center is the Sun, while two bright sundogs glow prominently from both the left and the right. Also visible is the bright 22 degree halo -- as well as the rarer and much fainter 46 degree halo -- also created by sunlight reflecting off of atmospheric ice crystals.
10 January 2011
Sun halo
Today's Astronomy Picture of the Day:
When I was young, I learned the two bright spots that appear left and right were called "sun dogs".
ReplyDeleteSee: http://en.wikipedia.org/wiki/Sun_dog
um... isn't that what the post says? twice?
ReplyDeleteHahah! Indeed. I didn't read the post just the title and photo. What a fool I've been! I'm glad that some anonymous person on the internet corrected my mistake! ;o)
ReplyDelete