2005: First measurements of the infrared sky brightness at Dome

ABSTRACT. Dome C, Antarctica, (75 south, 123 east, 3250 m) is one of the coldest and driest locations on Earth, with exceptionally low winds throughout the atmosphere. It therefore has the potential to be an ideal site for astronomical observations. It is also an excellent site for the validation of...

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Main Authors: V. P. Walden, M. S. Town, B. Halter, J. W. V. Storey
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.561.4370
http://www.webpages.uidaho.edu/~vonw/pubs/WaldenEtAl_PASP_2005.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.561.4370 2023-05-15T13:56:22+02:00 2005: First measurements of the infrared sky brightness at Dome V. P. Walden M. S. Town B. Halter J. W. V. Storey The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.561.4370 http://www.webpages.uidaho.edu/~vonw/pubs/WaldenEtAl_PASP_2005.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.561.4370 http://www.webpages.uidaho.edu/~vonw/pubs/WaldenEtAl_PASP_2005.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.webpages.uidaho.edu/~vonw/pubs/WaldenEtAl_PASP_2005.pdf text ftciteseerx 2016-01-08T12:03:51Z ABSTRACT. Dome C, Antarctica, (75 south, 123 east, 3250 m) is one of the coldest and driest locations on Earth, with exceptionally low winds throughout the atmosphere. It therefore has the potential to be an ideal site for astronomical observations. It is also an excellent site for the validation of satellite instruments. A Fourier transform infrared interferometer was deployed at Dome C during two austral summer seasons (2003 January and 2003 December/2004 January) for the purpose of acquiring satellite validation data. However, these data are also useful for understanding the infrared characteristics of the atmosphere for future astronomical experiments at Dome C. The Polar Atmospheric Emitted Radiance Interferometer measured the downwelling infrared radiance from the atmosphere (sky brightness) from 3 to 20 mm. Over 100 radiosondes were also launched during this time period. Typical measured values of the sky brightness in the clearest portions of the M, N, and Q bands are 0.9, 43, and 310 Jy arcsec2, respectively. The lowest measured values of sky brightness within these bands are 0.4, 34, and 200 Jy arcsec2. The spectral region of the Q band from about 18.7 to 19 mm is expected to be an excellent window for observations made from the Antarctic Plateau. The sky brightness has been measured between 10.60 and 11.30 mm in the N band for comparisons to earlier studies at South Pole Station; the values in this band are similar to those in the 8.20–8.40 mm band. For the period of time covered by our observations, the sky brightness in the dark portions of the N band was less than about 50–60 Jy arcsec2 for about 10 % of Text Antarc* Antarctic Antarctica South pole South pole Unknown Antarctic Austral South Pole The Antarctic
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description ABSTRACT. Dome C, Antarctica, (75 south, 123 east, 3250 m) is one of the coldest and driest locations on Earth, with exceptionally low winds throughout the atmosphere. It therefore has the potential to be an ideal site for astronomical observations. It is also an excellent site for the validation of satellite instruments. A Fourier transform infrared interferometer was deployed at Dome C during two austral summer seasons (2003 January and 2003 December/2004 January) for the purpose of acquiring satellite validation data. However, these data are also useful for understanding the infrared characteristics of the atmosphere for future astronomical experiments at Dome C. The Polar Atmospheric Emitted Radiance Interferometer measured the downwelling infrared radiance from the atmosphere (sky brightness) from 3 to 20 mm. Over 100 radiosondes were also launched during this time period. Typical measured values of the sky brightness in the clearest portions of the M, N, and Q bands are 0.9, 43, and 310 Jy arcsec2, respectively. The lowest measured values of sky brightness within these bands are 0.4, 34, and 200 Jy arcsec2. The spectral region of the Q band from about 18.7 to 19 mm is expected to be an excellent window for observations made from the Antarctic Plateau. The sky brightness has been measured between 10.60 and 11.30 mm in the N band for comparisons to earlier studies at South Pole Station; the values in this band are similar to those in the 8.20–8.40 mm band. For the period of time covered by our observations, the sky brightness in the dark portions of the N band was less than about 50–60 Jy arcsec2 for about 10 % of
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author V. P. Walden
M. S. Town
B. Halter
J. W. V. Storey
spellingShingle V. P. Walden
M. S. Town
B. Halter
J. W. V. Storey
2005: First measurements of the infrared sky brightness at Dome
author_facet V. P. Walden
M. S. Town
B. Halter
J. W. V. Storey
author_sort V. P. Walden
title 2005: First measurements of the infrared sky brightness at Dome
title_short 2005: First measurements of the infrared sky brightness at Dome
title_full 2005: First measurements of the infrared sky brightness at Dome
title_fullStr 2005: First measurements of the infrared sky brightness at Dome
title_full_unstemmed 2005: First measurements of the infrared sky brightness at Dome
title_sort 2005: first measurements of the infrared sky brightness at dome
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.561.4370
http://www.webpages.uidaho.edu/~vonw/pubs/WaldenEtAl_PASP_2005.pdf
geographic Antarctic
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South Pole
The Antarctic
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Austral
South Pole
The Antarctic
genre Antarc*
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South pole
South pole
genre_facet Antarc*
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Antarctica
South pole
South pole
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http://www.webpages.uidaho.edu/~vonw/pubs/WaldenEtAl_PASP_2005.pdf
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