Thermal infrared sky background for a High-Arctic mountain observatory

Nighttime zenith sky spectral brightness in the 3.3–20 μm wavelength region is reported for an observatory site nearby Eureka on Ellesmere Island in the Canadian High Arctic. Measurements are derived from an automated Fourier-transform spectrograph that operated there continuously over three consecu...

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Published in:Publications of the Astronomical Society of the Pacific
Main Author: Steinbring, Eric
Format: Article in Journal/Newspaper
Language:English
Published: IOP Publishing 2016
Subjects:
Online Access:https://doi.org/10.1088/1538-3873/129/971/015003
https://nrc-publications.canada.ca/eng/view/object/?id=5598921a-4113-4c62-9f0e-5cb8ccbade81
https://nrc-publications.canada.ca/fra/voir/objet/?id=5598921a-4113-4c62-9f0e-5cb8ccbade81
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spelling ftnrccanada:oai:cisti-icist.nrc-cnrc.ca:cistinparc:23003403 2023-05-15T14:57:08+02:00 Thermal infrared sky background for a High-Arctic mountain observatory Steinbring, Eric 2016-11-30 text https://doi.org/10.1088/1538-3873/129/971/015003 https://nrc-publications.canada.ca/eng/view/object/?id=5598921a-4113-4c62-9f0e-5cb8ccbade81 https://nrc-publications.canada.ca/fra/voir/objet/?id=5598921a-4113-4c62-9f0e-5cb8ccbade81 eng eng IOP Publishing issn:0004-6280 issn:1538-3873 Publications of the Astronomical Society of the Pacific, Volume: 129, Issue: 971, Publication date: 2016-11-30 doi:10.1088/1538-3873/129/971/015003 site testing article 2016 ftnrccanada https://doi.org/10.1088/1538-3873/129/971/015003 2021-09-01T06:17:01Z Nighttime zenith sky spectral brightness in the 3.3–20 μm wavelength region is reported for an observatory site nearby Eureka on Ellesmere Island in the Canadian High Arctic. Measurements are derived from an automated Fourier-transform spectrograph that operated there continuously over three consecutive winters. During that time, the median through the most transparent portion of the Q window was 460 Jy arcsec^-2, falling below 32 Jy arcsec^-2 in the N band, and to sub-Jansky levels by M and shortward, reaching only 36 mJy arcsec^-2 within L. Nearly six decades of twice-daily balloonsonde launches from Eureka, together with contemporaneous meteorological data plus a simple model, allows characterization of background stability and extrapolation into K band. This suggests that the study location has dark skies across the whole thermal infrared spectrum, typically sub-200 μJy arcsec^-2 at 2.4 μm. That background is comparable to South Pole and more than an order of magnitude less than estimates for the best temperate astronomical sites, all at much higher elevation. Considerations relevant to future facilities, including for polar transient surveys, are discussed. Peer reviewed: Yes NRC publication: Yes Article in Journal/Newspaper Arctic Ellesmere Island South pole National Research Council Canada: NRC Publications Archive Arctic Ellesmere Island Eureka ENVELOPE(-85.940,-85.940,79.990,79.990) South Pole Publications of the Astronomical Society of the Pacific 129 971 015003
institution Open Polar
collection National Research Council Canada: NRC Publications Archive
op_collection_id ftnrccanada
language English
topic site testing
spellingShingle site testing
Steinbring, Eric
Thermal infrared sky background for a High-Arctic mountain observatory
topic_facet site testing
description Nighttime zenith sky spectral brightness in the 3.3–20 μm wavelength region is reported for an observatory site nearby Eureka on Ellesmere Island in the Canadian High Arctic. Measurements are derived from an automated Fourier-transform spectrograph that operated there continuously over three consecutive winters. During that time, the median through the most transparent portion of the Q window was 460 Jy arcsec^-2, falling below 32 Jy arcsec^-2 in the N band, and to sub-Jansky levels by M and shortward, reaching only 36 mJy arcsec^-2 within L. Nearly six decades of twice-daily balloonsonde launches from Eureka, together with contemporaneous meteorological data plus a simple model, allows characterization of background stability and extrapolation into K band. This suggests that the study location has dark skies across the whole thermal infrared spectrum, typically sub-200 μJy arcsec^-2 at 2.4 μm. That background is comparable to South Pole and more than an order of magnitude less than estimates for the best temperate astronomical sites, all at much higher elevation. Considerations relevant to future facilities, including for polar transient surveys, are discussed. Peer reviewed: Yes NRC publication: Yes
format Article in Journal/Newspaper
author Steinbring, Eric
author_facet Steinbring, Eric
author_sort Steinbring, Eric
title Thermal infrared sky background for a High-Arctic mountain observatory
title_short Thermal infrared sky background for a High-Arctic mountain observatory
title_full Thermal infrared sky background for a High-Arctic mountain observatory
title_fullStr Thermal infrared sky background for a High-Arctic mountain observatory
title_full_unstemmed Thermal infrared sky background for a High-Arctic mountain observatory
title_sort thermal infrared sky background for a high-arctic mountain observatory
publisher IOP Publishing
publishDate 2016
url https://doi.org/10.1088/1538-3873/129/971/015003
https://nrc-publications.canada.ca/eng/view/object/?id=5598921a-4113-4c62-9f0e-5cb8ccbade81
https://nrc-publications.canada.ca/fra/voir/objet/?id=5598921a-4113-4c62-9f0e-5cb8ccbade81
long_lat ENVELOPE(-85.940,-85.940,79.990,79.990)
geographic Arctic
Ellesmere Island
Eureka
South Pole
geographic_facet Arctic
Ellesmere Island
Eureka
South Pole
genre Arctic
Ellesmere Island
South pole
genre_facet Arctic
Ellesmere Island
South pole
op_relation issn:0004-6280
issn:1538-3873
Publications of the Astronomical Society of the Pacific, Volume: 129, Issue: 971, Publication date: 2016-11-30
doi:10.1088/1538-3873/129/971/015003
op_doi https://doi.org/10.1088/1538-3873/129/971/015003
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