A template of atmospheric O2 circularly polarized emission for CMB experiments

We compute the circularly polarized signal from atmospheric molecular oxygen. Polarization of O2 rotational lines is caused by Zeeman effect in the Earth magnetic field. We evaluate the circularly polarized emission for various sites suitable for CMB measurements: South Pole and Dome C (Antarctica),...

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Main Authors: Spinelli, Sebastiano, Fabbian, Giulio, Tartari, Andrea, Zannoni, Mario, Gervasi, Massimo
Format: Text
Language:unknown
Published: arXiv 2011
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Online Access:https://dx.doi.org/10.48550/arxiv.1103.0160
https://arxiv.org/abs/1103.0160
id ftdatacite:10.48550/arxiv.1103.0160
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spelling ftdatacite:10.48550/arxiv.1103.0160 2023-05-15T13:34:17+02:00 A template of atmospheric O2 circularly polarized emission for CMB experiments Spinelli, Sebastiano Fabbian, Giulio Tartari, Andrea Zannoni, Mario Gervasi, Massimo 2011 https://dx.doi.org/10.48550/arxiv.1103.0160 https://arxiv.org/abs/1103.0160 unknown arXiv https://dx.doi.org/10.1111/j.1365-2966.2011.18625.x arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Instrumentation and Methods for Astrophysics astro-ph.IM Cosmology and Nongalactic Astrophysics astro-ph.CO FOS Physical sciences article-journal Article ScholarlyArticle Text 2011 ftdatacite https://doi.org/10.48550/arxiv.1103.0160 https://doi.org/10.1111/j.1365-2966.2011.18625.x 2022-04-01T14:14:51Z We compute the circularly polarized signal from atmospheric molecular oxygen. Polarization of O2 rotational lines is caused by Zeeman effect in the Earth magnetic field. We evaluate the circularly polarized emission for various sites suitable for CMB measurements: South Pole and Dome C (Antarctica), Atacama (Chile) and Testa Grigia (Italy). An analysis of the polarized signal is presented and discussed in the framework of future CMB polarization experiments. We find a typical circularly polarized signal (V Stokes parameter) of ~ 50 - 300 μK at 90 GHz looking at the zenith. Among the other sites Atacama shows the lower polarized signal at the zenith. We present maps of this signal for the various sites and show typical elevation and azimuth scans. We find that Dome C presents the lowest gradient in polarized temperature: ~ 0.3 μK/\circ at 90 GHz. We also study the frequency bands of observation: around ν \simeq 100 GHz and ν \simeq 160 GHz we find the best conditions because the polarized signal vanishes. Finally we evaluate the accuracy of the templates and the signal variability in relation with the knowledge and the variability of the Earth magnetic field and the atmospheric parameters. : 10 pages, 12 figures, accepted for publication on Mon. Not. R. Astron. Soc Text Antarc* Antarctica South pole South pole DataCite Metadata Store (German National Library of Science and Technology) South Pole
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Instrumentation and Methods for Astrophysics astro-ph.IM
Cosmology and Nongalactic Astrophysics astro-ph.CO
FOS Physical sciences
spellingShingle Instrumentation and Methods for Astrophysics astro-ph.IM
Cosmology and Nongalactic Astrophysics astro-ph.CO
FOS Physical sciences
Spinelli, Sebastiano
Fabbian, Giulio
Tartari, Andrea
Zannoni, Mario
Gervasi, Massimo
A template of atmospheric O2 circularly polarized emission for CMB experiments
topic_facet Instrumentation and Methods for Astrophysics astro-ph.IM
Cosmology and Nongalactic Astrophysics astro-ph.CO
FOS Physical sciences
description We compute the circularly polarized signal from atmospheric molecular oxygen. Polarization of O2 rotational lines is caused by Zeeman effect in the Earth magnetic field. We evaluate the circularly polarized emission for various sites suitable for CMB measurements: South Pole and Dome C (Antarctica), Atacama (Chile) and Testa Grigia (Italy). An analysis of the polarized signal is presented and discussed in the framework of future CMB polarization experiments. We find a typical circularly polarized signal (V Stokes parameter) of ~ 50 - 300 μK at 90 GHz looking at the zenith. Among the other sites Atacama shows the lower polarized signal at the zenith. We present maps of this signal for the various sites and show typical elevation and azimuth scans. We find that Dome C presents the lowest gradient in polarized temperature: ~ 0.3 μK/\circ at 90 GHz. We also study the frequency bands of observation: around ν \simeq 100 GHz and ν \simeq 160 GHz we find the best conditions because the polarized signal vanishes. Finally we evaluate the accuracy of the templates and the signal variability in relation with the knowledge and the variability of the Earth magnetic field and the atmospheric parameters. : 10 pages, 12 figures, accepted for publication on Mon. Not. R. Astron. Soc
format Text
author Spinelli, Sebastiano
Fabbian, Giulio
Tartari, Andrea
Zannoni, Mario
Gervasi, Massimo
author_facet Spinelli, Sebastiano
Fabbian, Giulio
Tartari, Andrea
Zannoni, Mario
Gervasi, Massimo
author_sort Spinelli, Sebastiano
title A template of atmospheric O2 circularly polarized emission for CMB experiments
title_short A template of atmospheric O2 circularly polarized emission for CMB experiments
title_full A template of atmospheric O2 circularly polarized emission for CMB experiments
title_fullStr A template of atmospheric O2 circularly polarized emission for CMB experiments
title_full_unstemmed A template of atmospheric O2 circularly polarized emission for CMB experiments
title_sort template of atmospheric o2 circularly polarized emission for cmb experiments
publisher arXiv
publishDate 2011
url https://dx.doi.org/10.48550/arxiv.1103.0160
https://arxiv.org/abs/1103.0160
geographic South Pole
geographic_facet South Pole
genre Antarc*
Antarctica
South pole
South pole
genre_facet Antarc*
Antarctica
South pole
South pole
op_relation https://dx.doi.org/10.1111/j.1365-2966.2011.18625.x
op_rights arXiv.org perpetual, non-exclusive license
http://arxiv.org/licenses/nonexclusive-distrib/1.0/
op_doi https://doi.org/10.48550/arxiv.1103.0160
https://doi.org/10.1111/j.1365-2966.2011.18625.x
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