Astronomical Seeing from the Summits of the Antarctic Plateau

From the South Pole, microthermal turbulence within a narrow surface boundary layer some 200m thick provides the dominant contribution to the astronomical seeing. We present results for the seeing at a wavelength of 2.4um. The narrow turbulence layer above the site, confined close to the surface, pr...

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Main Author: Marks, R D
Language:English
Published: 2001
Subjects:
Online Access:http://cds.cern.ch/record/529260
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spelling ftcern:oai:cds.cern.ch:529260 2023-05-15T13:44:15+02:00 Astronomical Seeing from the Summits of the Antarctic Plateau Marks, R D 2001-12-04 http://cds.cern.ch/record/529260 eng eng http://cds.cern.ch/record/529260 astro-ph/0112068 oai:cds.cern.ch:529260 Astrophysics and Astronomy 2001 ftcern 2018-07-28T05:15:40Z From the South Pole, microthermal turbulence within a narrow surface boundary layer some 200m thick provides the dominant contribution to the astronomical seeing. We present results for the seeing at a wavelength of 2.4um. The narrow turbulence layer above the site, confined close to the surface, provides greatly superior conditions for adaptive optics correction than do temperate latitude sites. An analysis of the available meteorological data for the Antarctic plateau suggests that sites on its summit, such as Domes A and C, probably experience significantly better boundary layer seeing than does the South Pole. In addition, the inversion layers may be significantly narrower, lending the sites even further to adaptive optics correction than does the Pole. Other/Unknown Material Antarc* Antarctic South pole South pole CERN Document Server (CDS) Antarctic South Pole The Antarctic
institution Open Polar
collection CERN Document Server (CDS)
op_collection_id ftcern
language English
topic Astrophysics and Astronomy
spellingShingle Astrophysics and Astronomy
Marks, R D
Astronomical Seeing from the Summits of the Antarctic Plateau
topic_facet Astrophysics and Astronomy
description From the South Pole, microthermal turbulence within a narrow surface boundary layer some 200m thick provides the dominant contribution to the astronomical seeing. We present results for the seeing at a wavelength of 2.4um. The narrow turbulence layer above the site, confined close to the surface, provides greatly superior conditions for adaptive optics correction than do temperate latitude sites. An analysis of the available meteorological data for the Antarctic plateau suggests that sites on its summit, such as Domes A and C, probably experience significantly better boundary layer seeing than does the South Pole. In addition, the inversion layers may be significantly narrower, lending the sites even further to adaptive optics correction than does the Pole.
author Marks, R D
author_facet Marks, R D
author_sort Marks, R D
title Astronomical Seeing from the Summits of the Antarctic Plateau
title_short Astronomical Seeing from the Summits of the Antarctic Plateau
title_full Astronomical Seeing from the Summits of the Antarctic Plateau
title_fullStr Astronomical Seeing from the Summits of the Antarctic Plateau
title_full_unstemmed Astronomical Seeing from the Summits of the Antarctic Plateau
title_sort astronomical seeing from the summits of the antarctic plateau
publishDate 2001
url http://cds.cern.ch/record/529260
geographic Antarctic
South Pole
The Antarctic
geographic_facet Antarctic
South Pole
The Antarctic
genre Antarc*
Antarctic
South pole
South pole
genre_facet Antarc*
Antarctic
South pole
South pole
op_relation http://cds.cern.ch/record/529260
astro-ph/0112068
oai:cds.cern.ch:529260
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