Relay-Version: version B 2.10 5/3/83; site utzoo.UUCP Posting-Version: version B 2.10.2 9/18/84; site lanl.ARPA Path: utzoo!linus!decvax!genrad!wjh12!harvard!seismo!cmcl2!lanl!jlg From: jlg@lanl.ARPA Newsgroups: net.physics Subject: Re: Sunrise Phenomenon Message-ID: <15524@lanl.ARPA> Date: Fri, 2-Nov-84 15:03:21 EST Article-I.D.: lanl.15524 Posted: Fri Nov 2 15:03:21 1984 Date-Received: Sat, 3-Nov-84 21:55:03 EST References: <1345@drutx.UUCP> Sender: newsreader@lanl.ARPA Organization: Los Alamos National Laboratory Lines: 36 > > - > Can anyone out there explain the atmospheric phenomenon known as > the "rosy fingers of dawn" in reasonably plain English (that is, > without invoking quantum chromodynamics or other esoteric theory)? > In case this beautiful morning sight is known by another name, let > me explain: On a cloudless morning, just before the limb of the sun > breaks the horizon, deep pink shafts of light radiate from the hor- > izon to just beyond directly overhead but not quite to the western > horizon. There appears to be four or five very sharply defined > shafts of light, alternating with deep blue, growing with intensity > as the horizon is neared. One is reminded of the "rising sun" > Japanese flag symbol. Interestingly enough, I have never seen this > at sunset. Can it happen then, too? I have seen this a number of times at both sunrise and sunset. On one very dramatic occasion the cause of the phenomon was also directly in view. It was a distant mountain who's contours cast a shadow on the lower atmosphere. In the places where the mountain was lower, the sunlight reaches lower into the air above me, and a brighter shaft of light was produced. I don't know if this is the only cause of the phenomon, but it is certainly A cause. Try looking around for large obsticles on the horizon and position yourself so that it is between you and the setting (or rising) sun. You should be a sufficient distance away for the object to cast shadows on you only when the sun is at or below horizontal. Your best chance is on a day with thermal inversion layers in the atmosphere so that the difference in scattering between one atmospheric level and the next is most apparent. (This may be why you have only seen the effect at sunrise. Inversion layers form over cities at night, but are usually burned off by the sun during the day. Only in regions with shallow valleys bordered by mountains do inversion layers form during the day.) Good hunting!