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・ Lyman Woodard
・ Lyman Wynne
・ Lyman Young
・ Lyman, California
・ Lyman, Maine
・ Lyman, Mississippi
・ Lyman, Nebraska
・ Lyman, New Hampshire
・ Lyman, South Carolina
・ Lyman, Utah
・ Lyman, Washington
・ Lyman, Wyoming
・ Lyman-alpha blob
・ Lyman-alpha blob 1
・ Lyman-alpha emitter
Lyman-alpha forest
・ Lyman-alpha line
・ Lyman-break galaxy
・ Lymania
・ Lymania alvimii
・ Lymania azurea
・ Lymania corallina
・ Lymania globosa
・ Lymania languida
・ Lymania marantoides
・ Lymania smithii
・ Lymania spiculata
・ Lymanopoda
・ Lymanske
・ Lymanske (urban-type settlement)


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Lyman-alpha forest : ウィキペディア英語版
Lyman-alpha forest

In astronomical spectroscopy, the Lyman-alpha forest is a series of absorption lines in the spectra of distant galaxies and quasars arising from the Lyman-alpha electron transition of the neutral hydrogen atom.
==History==
The Lyman-alpha forest was first discovered in 1970 by astronomer Roger Lynds in an observation of the quasar 4C 05.34. Quasar 4C 05.34 was the farthest object observed to that date, and Lynds noted an unusually large number of absorption lines in its spectrum. He suggested that most of the absorption lines were all due to the same Lyman-alpha transition. Follow-up observations by John Bahcall and Samuel Goldsmith confirmed the presence of the unusual absorption lines, though they were less conclusive about the origin of the lines. Subsequently, the spectra of many other high-redshift quasars were observed to have the same system of narrow absorption lines. Lynds was the first to describe them as the "Lyman-alpha forest". Jan Oort argued that the absorption features are due not to any physical interactions within the quasars themselves, but to absorption inside clouds of intergalactic gas in superclusters.

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