Observing CMB polarisation through ice

Ice crystal clouds in the upper troposphere can generate polarisation signals at the uK level. This signal can seriously affect very sensitive ground based searches for E- and B-mode of Cosmic Microwave Background polarisation. In this paper we estimate this effect within the ClOVER experiment obser...

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Main Authors: Pietranera, L, Bühler, S, Calisse, P G, Emde, C, Hayton, D, John, V O, Maffei, B, Piccirillo, L, Pisano, G, Savini, G, Sreerekha, T R
Language:English
Published: 2006
Subjects:
Online Access:http://cds.cern.ch/record/1000246
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author Pietranera, L
Bühler, S
Calisse, P G
Emde, C
Hayton, D
John, V O
Maffei, B
Piccirillo, L
Pisano, G
Savini, G
Sreerekha, T R
author_facet Pietranera, L
Bühler, S
Calisse, P G
Emde, C
Hayton, D
John, V O
Maffei, B
Piccirillo, L
Pisano, G
Savini, G
Sreerekha, T R
author_sort Pietranera, L
collection CERN Document Server (CDS)
description Ice crystal clouds in the upper troposphere can generate polarisation signals at the uK level. This signal can seriously affect very sensitive ground based searches for E- and B-mode of Cosmic Microwave Background polarisation. In this paper we estimate this effect within the ClOVER experiment observing bands (97, 150 and 220 GHz) for the selected observing site (Llano de Chajnantor, Atacama desert, Chile). The results show that the polarisation signal from the clouds can be of the order of or even bigger than the CMB expected polarisation. Climatological data suggest that this signal is fairly constant over the whole year in Antarctica. On the other hand the stronger seasonal variability in Atacama allows for a 50% of clean observations during the dry season.
genre Antarc*
Antarctica
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Antarctica
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spelling ftcern:oai:cds.cern.ch:1000246 2025-01-16T19:04:51+00:00 Observing CMB polarisation through ice Pietranera, L Bühler, S Calisse, P G Emde, C Hayton, D John, V O Maffei, B Piccirillo, L Pisano, G Savini, G Sreerekha, T R 2006-11-21 http://cds.cern.ch/record/1000246 eng eng http://cds.cern.ch/record/1000246 astro-ph/0611678 oai:cds.cern.ch:1000246 Astrophysics and Astronomy 2006 ftcern 2018-07-28T08:37:56Z Ice crystal clouds in the upper troposphere can generate polarisation signals at the uK level. This signal can seriously affect very sensitive ground based searches for E- and B-mode of Cosmic Microwave Background polarisation. In this paper we estimate this effect within the ClOVER experiment observing bands (97, 150 and 220 GHz) for the selected observing site (Llano de Chajnantor, Atacama desert, Chile). The results show that the polarisation signal from the clouds can be of the order of or even bigger than the CMB expected polarisation. Climatological data suggest that this signal is fairly constant over the whole year in Antarctica. On the other hand the stronger seasonal variability in Atacama allows for a 50% of clean observations during the dry season. Other/Unknown Material Antarc* Antarctica CERN Document Server (CDS)
spellingShingle Astrophysics and Astronomy
Pietranera, L
Bühler, S
Calisse, P G
Emde, C
Hayton, D
John, V O
Maffei, B
Piccirillo, L
Pisano, G
Savini, G
Sreerekha, T R
Observing CMB polarisation through ice
title Observing CMB polarisation through ice
title_full Observing CMB polarisation through ice
title_fullStr Observing CMB polarisation through ice
title_full_unstemmed Observing CMB polarisation through ice
title_short Observing CMB polarisation through ice
title_sort observing cmb polarisation through ice
topic Astrophysics and Astronomy
topic_facet Astrophysics and Astronomy
url http://cds.cern.ch/record/1000246