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இது விக்கிமீடியா பொதுக்கோப்பகத்தில் இருக்கும் ஒரு கோப்பாகும். இக்கோப்பைக் குறித்து அங்கே காணப்படும் படிம விளக்கப் பக்கத்தை இங்கே கீழே காணலாம்.
பொதுக்கோப்பகம் ஒரு கட்டற்ற கோப்புகளின் சேமிப்பகமாகும். நீங்களும் உதவலாம்.
விளக்கம்
English: Drawing of passage of "auroral beam" of November 17, 1882.

Drawing of passage of "auroral beam" of November 17, 1882, by astronomer and aurora expert Rand Capron, Guildown Observatory, Surrey, UK. Also described by prominent British astronomer Edward Walter Maunder. Drawing first published in Philosophical Magazine, May 1883. Reprinted by astronomer Morris K. Jessup in "The Case for the UFO," 1955, p. 32, Citadel Press. Electronic version of Jessup book with illustration online

Maunder in The Observatory journal of the Royal Greenwich Observatory, in June 1883 and April 1916, described the phenomenon as about 30 degrees long, 2-3 degrees wide, with distinct edges and an opaque central portion. It was whitish or whitish-green, about the same color as auroral displays, but much brighter. It moved steadily across the sky from (magnetic) east to west in under 2 minutes. It moved "as the Sun, Moon, stars and planets move but nearly a thousand times as quickly." When first seen it was low down in the E.N.E. and circular or disc-like in shape, but as it moved it turned into "a very elongated ellipse", variously described as "cigar-shaped," "like a torpedo," "a spindle", or a "shuttle." In 1916, Maunder likened it to "just like a Zeppelin."

In 1916, Maunder commented that it was "a celestial object unique in my experience" and "unlike any other celestial object that I have ever seen. The quality of its light, and its occurrence while a great magnetic storm and a bright aurora were in progress, seem to establish its auroral origin. But it differed very widely in appearance from any other aurora that I have ever seen."

The described phenomenon has some similarity in appearance to Upper Tangent arc, frequent in the northern regions, described and studied by meteorologists. Upper Tangent arc is produced by horizontally orientated column-shaped ice crystals reflecting the sunlight (articles in Arbeitskreis Meteore e.V. ). However, the 1882 phenomenon, according to Maunder, moved rapidly across the sky, whereas Upper Tangent arc would remain relatively stationary and can only occur during daytime, since it is created by and is tied to the position of the sun.
நாள்
மூலம் Philosophical Magazine
ஆசிரியர் Rand Capron
ஒத்தக்கோப்பு English Wikipedia

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மே 1883Gregorian

கோப்பின் வரலாறு

குறித்த நேரத்தில் இருந்த படிமத்தைப் பார்க்க அந்நேரத்தின் மீது சொடுக்கவும்.

நாள்/நேரம்நகம் அளவு சிறுபடம்அளவுகள்பயனர்கருத்து
தற்போதைய06:07, 15 அக்டோபர் 200806:07, 15 அக்டோபர் 2008 இலிருந்த பதிப்புக்கான சிறு தோற்றம்400 × 210 (27 KB)Kakoui{{Information |Description=Drawing of passage of "auroral beam" of November 17, 1882 |Source=Philosophical Magazine |Date=May 1883 |Author=Rand Capron |Permission={{PD-old}} |other_versions=[[:w:en:Image:Maunder auroral be

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