Accuracy in starphotometry

Starphotometry, the night-time counterpart of sunphotometry, has not yet achieved the commonly sought observational error level of 1 %: a spectral optical depth (OD) error level of 0.01. In order to address this issue, we investigate a large variety of systematic (absolute) uncertainty sources. The...

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Published in:Atmospheric Measurement Techniques
Main Authors: L. Ivănescu, K. Baibakov, N. T. O'Neill, J.-P. Blanchet, K.-H. Schulz
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2021
Subjects:
Online Access:https://doi.org/10.5194/amt-14-6561-2021
https://doaj.org/article/902b31e2e0644be0bd1224cbe2b7df4b
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author L. Ivănescu
K. Baibakov
N. T. O'Neill
J.-P. Blanchet
K.-H. Schulz
author_facet L. Ivănescu
K. Baibakov
N. T. O'Neill
J.-P. Blanchet
K.-H. Schulz
author_sort L. Ivănescu
collection Directory of Open Access Journals: DOAJ Articles
container_issue 10
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container_title Atmospheric Measurement Techniques
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description Starphotometry, the night-time counterpart of sunphotometry, has not yet achieved the commonly sought observational error level of 1 %: a spectral optical depth (OD) error level of 0.01. In order to address this issue, we investigate a large variety of systematic (absolute) uncertainty sources. The bright-star catalogue of extraterrestrial references is noted as a major source of errors with an attendant recommendation that its accuracy, particularly its spectral photometric variability, be significantly improved. The small field of view (FOV) employed in starphotometry ensures that it, unlike sun- or moonphotometry, is only weakly dependent on the intrinsic and artificial OD reduction induced by scattering into the FOV by optically thin clouds. A FOV of 45 arcsec (arcseconds) was found to be the best trade-off for minimizing such forward-scattering errors concurrently with flux loss through vignetting. The importance of monitoring the sky background and using interpolation techniques to avoid spikes and to compensate for measurement delay was underscored. A set of 20 channels was identified to mitigate contamination errors associated with stellar and terrestrial atmospheric gas absorptions, as well as aurora and airglow emissions. We also note that observations made with starphotometers similar to our High Arctic instrument should be made at high angular elevations (i.e. at air masses less than 5). We noted the significant effects of snow crystal deposition on the starphotometer optics, how pseudo OD increases associated with this type of contamination could be detected, and how proactive techniques could be employed to avoid their occurrence in the first place. If all of these recommendations are followed, one may aspire to achieve component errors that are well below 0.01: in the process, one may attain a total 0.01 OD target error.
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spelling ftdoajarticles:oai:doaj.org/article:902b31e2e0644be0bd1224cbe2b7df4b 2025-01-16T20:44:53+00:00 Accuracy in starphotometry L. Ivănescu K. Baibakov N. T. O'Neill J.-P. Blanchet K.-H. Schulz 2021-10-01T00:00:00Z https://doi.org/10.5194/amt-14-6561-2021 https://doaj.org/article/902b31e2e0644be0bd1224cbe2b7df4b EN eng Copernicus Publications https://amt.copernicus.org/articles/14/6561/2021/amt-14-6561-2021.pdf https://doaj.org/toc/1867-1381 https://doaj.org/toc/1867-8548 doi:10.5194/amt-14-6561-2021 1867-1381 1867-8548 https://doaj.org/article/902b31e2e0644be0bd1224cbe2b7df4b Atmospheric Measurement Techniques, Vol 14, Pp 6561-6599 (2021) Environmental engineering TA170-171 Earthwork. Foundations TA715-787 article 2021 ftdoajarticles https://doi.org/10.5194/amt-14-6561-2021 2022-12-31T11:39:35Z Starphotometry, the night-time counterpart of sunphotometry, has not yet achieved the commonly sought observational error level of 1 %: a spectral optical depth (OD) error level of 0.01. In order to address this issue, we investigate a large variety of systematic (absolute) uncertainty sources. The bright-star catalogue of extraterrestrial references is noted as a major source of errors with an attendant recommendation that its accuracy, particularly its spectral photometric variability, be significantly improved. The small field of view (FOV) employed in starphotometry ensures that it, unlike sun- or moonphotometry, is only weakly dependent on the intrinsic and artificial OD reduction induced by scattering into the FOV by optically thin clouds. A FOV of 45 arcsec (arcseconds) was found to be the best trade-off for minimizing such forward-scattering errors concurrently with flux loss through vignetting. The importance of monitoring the sky background and using interpolation techniques to avoid spikes and to compensate for measurement delay was underscored. A set of 20 channels was identified to mitigate contamination errors associated with stellar and terrestrial atmospheric gas absorptions, as well as aurora and airglow emissions. We also note that observations made with starphotometers similar to our High Arctic instrument should be made at high angular elevations (i.e. at air masses less than 5). We noted the significant effects of snow crystal deposition on the starphotometer optics, how pseudo OD increases associated with this type of contamination could be detected, and how proactive techniques could be employed to avoid their occurrence in the first place. If all of these recommendations are followed, one may aspire to achieve component errors that are well below 0.01: in the process, one may attain a total 0.01 OD target error. Article in Journal/Newspaper Arctic Directory of Open Access Journals: DOAJ Articles Arctic Atmospheric Measurement Techniques 14 10 6561 6599
spellingShingle Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
L. Ivănescu
K. Baibakov
N. T. O'Neill
J.-P. Blanchet
K.-H. Schulz
Accuracy in starphotometry
title Accuracy in starphotometry
title_full Accuracy in starphotometry
title_fullStr Accuracy in starphotometry
title_full_unstemmed Accuracy in starphotometry
title_short Accuracy in starphotometry
title_sort accuracy in starphotometry
topic Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
topic_facet Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
url https://doi.org/10.5194/amt-14-6561-2021
https://doaj.org/article/902b31e2e0644be0bd1224cbe2b7df4b