Mesoscale optical turbulence simulations above Dome C, Dome A and South Pole

In two recent papers the mesoscale model Meso-NH, joint with the Astro-Meso-NH package, has been validated at Dome C, Antarctica, for the characterization of the optical turbulence. It has been shown that the meteorological parameters (temperature and wind speed, from which the optical turbulence de...

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Main Authors: Lascaux, Franck, Masciadri, Elena, Hagelin, Susanna
Format: Text
Language:unknown
Published: arXiv 2010
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Online Access:https://dx.doi.org/10.48550/arxiv.1011.1413
https://arxiv.org/abs/1011.1413
id ftdatacite:10.48550/arxiv.1011.1413
record_format openpolar
spelling ftdatacite:10.48550/arxiv.1011.1413 2023-05-15T13:32:39+02:00 Mesoscale optical turbulence simulations above Dome C, Dome A and South Pole Lascaux, Franck Masciadri, Elena Hagelin, Susanna 2010 https://dx.doi.org/10.48550/arxiv.1011.1413 https://arxiv.org/abs/1011.1413 unknown arXiv https://dx.doi.org/10.1111/j.1365-2966.2010.17709.x arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Instrumentation and Methods for Astrophysics astro-ph.IM Atmospheric and Oceanic Physics physics.ao-ph FOS Physical sciences article-journal Article ScholarlyArticle Text 2010 ftdatacite https://doi.org/10.48550/arxiv.1011.1413 https://doi.org/10.1111/j.1365-2966.2010.17709.x 2022-04-01T14:24:11Z In two recent papers the mesoscale model Meso-NH, joint with the Astro-Meso-NH package, has been validated at Dome C, Antarctica, for the characterization of the optical turbulence. It has been shown that the meteorological parameters (temperature and wind speed, from which the optical turbulence depends on) as well as the Cn2 profiles above Dome C were correctly statistically reproduced. The three most important derived parameters that characterize the optical turbulence above the internal antarctic plateau: the surface layer thickness, the seeing in the free-atmosphere and in the total atmosphere showed to be in a very good agreement with observations. Validation of Cn2 has been performed using all the measurements of the optical turbulence vertical distribution obtained in winter so far. In this paper, in order to investigate the ability of the model to discriminate between different turbulence conditions for site testing, we extend the study to two other potential astronomical sites in Antarctica: Dome A and South Pole, which we expect to be characterized by different turbulence conditions. The optical turbulence has been calculated above these two sites for the same 15 nights studied for Dome C and a comparison between the three sites has been performed. : 13 pages, 5 figures, 9 tables, accepted in MNRAS Text Antarc* Antarctic Antarctica South pole South pole DataCite Metadata Store (German National Library of Science and Technology) Antarctic 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
Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
spellingShingle Instrumentation and Methods for Astrophysics astro-ph.IM
Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
Lascaux, Franck
Masciadri, Elena
Hagelin, Susanna
Mesoscale optical turbulence simulations above Dome C, Dome A and South Pole
topic_facet Instrumentation and Methods for Astrophysics astro-ph.IM
Atmospheric and Oceanic Physics physics.ao-ph
FOS Physical sciences
description In two recent papers the mesoscale model Meso-NH, joint with the Astro-Meso-NH package, has been validated at Dome C, Antarctica, for the characterization of the optical turbulence. It has been shown that the meteorological parameters (temperature and wind speed, from which the optical turbulence depends on) as well as the Cn2 profiles above Dome C were correctly statistically reproduced. The three most important derived parameters that characterize the optical turbulence above the internal antarctic plateau: the surface layer thickness, the seeing in the free-atmosphere and in the total atmosphere showed to be in a very good agreement with observations. Validation of Cn2 has been performed using all the measurements of the optical turbulence vertical distribution obtained in winter so far. In this paper, in order to investigate the ability of the model to discriminate between different turbulence conditions for site testing, we extend the study to two other potential astronomical sites in Antarctica: Dome A and South Pole, which we expect to be characterized by different turbulence conditions. The optical turbulence has been calculated above these two sites for the same 15 nights studied for Dome C and a comparison between the three sites has been performed. : 13 pages, 5 figures, 9 tables, accepted in MNRAS
format Text
author Lascaux, Franck
Masciadri, Elena
Hagelin, Susanna
author_facet Lascaux, Franck
Masciadri, Elena
Hagelin, Susanna
author_sort Lascaux, Franck
title Mesoscale optical turbulence simulations above Dome C, Dome A and South Pole
title_short Mesoscale optical turbulence simulations above Dome C, Dome A and South Pole
title_full Mesoscale optical turbulence simulations above Dome C, Dome A and South Pole
title_fullStr Mesoscale optical turbulence simulations above Dome C, Dome A and South Pole
title_full_unstemmed Mesoscale optical turbulence simulations above Dome C, Dome A and South Pole
title_sort mesoscale optical turbulence simulations above dome c, dome a and south pole
publisher arXiv
publishDate 2010
url https://dx.doi.org/10.48550/arxiv.1011.1413
https://arxiv.org/abs/1011.1413
geographic Antarctic
South Pole
geographic_facet Antarctic
South Pole
genre Antarc*
Antarctic
Antarctica
South pole
South pole
genre_facet Antarc*
Antarctic
Antarctica
South pole
South pole
op_relation https://dx.doi.org/10.1111/j.1365-2966.2010.17709.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.1011.1413
https://doi.org/10.1111/j.1365-2966.2010.17709.x
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