A re-evaluation of surface layer turbulence from Antarctic data

A data set of velocity and temperature variances measured in the surface layer over a glacier in Antarctica is analysed in terms of the Monin-Obukhov Similarity Theory. The presence of surface inhomogeneities, flow unsteadiness, and other uncontrolled disturbances affects the shape of the distributi...

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Main Authors: Tampieri, F., Maurizi, A.
Format: Article in Journal/Newspaper
Language:English
Published: Societa italiana di fisica 2008
Subjects:
Online Access:http://eprints.bice.rm.cnr.it/16409/
http://eprints.bice.rm.cnr.it/16409/1/ncc9337.pdf
https://www.sif.it/riviste/sif/ncc/econtents/2008/031/05-06/article/12
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spelling ftcnrroma:oai:eprints.bice.rm.cnr.it:16409 2023-05-15T14:00:11+02:00 A re-evaluation of surface layer turbulence from Antarctic data Tampieri, F. Maurizi, A. 2008 text http://eprints.bice.rm.cnr.it/16409/ http://eprints.bice.rm.cnr.it/16409/1/ncc9337.pdf https://www.sif.it/riviste/sif/ncc/econtents/2008/031/05-06/article/12 en eng Societa italiana di fisica http://eprints.bice.rm.cnr.it/16409/1/ncc9337.pdf Tampieri, F. and Maurizi, A. (2008) A re-evaluation of surface layer turbulence from Antarctic data. Il nuovo cimento C, 31 (5\6). pp. 711-722. ISSN 1826-9885 551.6 Climatologia e tempo atmosferico (Classificare qui i lo studio dei Cambiamenti climatici) Article PeerReviewed 2008 ftcnrroma 2022-02-24T22:10:20Z A data set of velocity and temperature variances measured in the surface layer over a glacier in Antarctica is analysed in terms of the Monin-Obukhov Similarity Theory. The presence of surface inhomogeneities, flow unsteadiness, and other uncontrolled disturbances affects the shape of the distribution of normalised variances for intervals of the stability parameter. The modal value of the distribution, instead of the mean, is used to estimate the numerical coefficients of the similarity functions to minimize the influence of the (positive) outliers on the estimates. The overall agreement of the present results with previuos investigations is good, and also the spread of the numerical values noted by different authors is confirmed. In particular the investigation points out the need to use a similarity function for the temperature variance which diverges in near neutral conditions, as the heat flux goes to zero, and the occurrence of a large stability region where the variances of velocity and temperature are characterised by a behaviour almost independent of the momentum flux. Article in Journal/Newspaper Antarc* Antarctic Antarctica CNR Solar (Scientific Open-access Literature Archive and Repository - National Research Council) Antarctic
institution Open Polar
collection CNR Solar (Scientific Open-access Literature Archive and Repository - National Research Council)
op_collection_id ftcnrroma
language English
topic 551.6 Climatologia e tempo atmosferico (Classificare qui i lo studio dei Cambiamenti climatici)
spellingShingle 551.6 Climatologia e tempo atmosferico (Classificare qui i lo studio dei Cambiamenti climatici)
Tampieri, F.
Maurizi, A.
A re-evaluation of surface layer turbulence from Antarctic data
topic_facet 551.6 Climatologia e tempo atmosferico (Classificare qui i lo studio dei Cambiamenti climatici)
description A data set of velocity and temperature variances measured in the surface layer over a glacier in Antarctica is analysed in terms of the Monin-Obukhov Similarity Theory. The presence of surface inhomogeneities, flow unsteadiness, and other uncontrolled disturbances affects the shape of the distribution of normalised variances for intervals of the stability parameter. The modal value of the distribution, instead of the mean, is used to estimate the numerical coefficients of the similarity functions to minimize the influence of the (positive) outliers on the estimates. The overall agreement of the present results with previuos investigations is good, and also the spread of the numerical values noted by different authors is confirmed. In particular the investigation points out the need to use a similarity function for the temperature variance which diverges in near neutral conditions, as the heat flux goes to zero, and the occurrence of a large stability region where the variances of velocity and temperature are characterised by a behaviour almost independent of the momentum flux.
format Article in Journal/Newspaper
author Tampieri, F.
Maurizi, A.
author_facet Tampieri, F.
Maurizi, A.
author_sort Tampieri, F.
title A re-evaluation of surface layer turbulence from Antarctic data
title_short A re-evaluation of surface layer turbulence from Antarctic data
title_full A re-evaluation of surface layer turbulence from Antarctic data
title_fullStr A re-evaluation of surface layer turbulence from Antarctic data
title_full_unstemmed A re-evaluation of surface layer turbulence from Antarctic data
title_sort re-evaluation of surface layer turbulence from antarctic data
publisher Societa italiana di fisica
publishDate 2008
url http://eprints.bice.rm.cnr.it/16409/
http://eprints.bice.rm.cnr.it/16409/1/ncc9337.pdf
https://www.sif.it/riviste/sif/ncc/econtents/2008/031/05-06/article/12
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_relation http://eprints.bice.rm.cnr.it/16409/1/ncc9337.pdf
Tampieri, F. and Maurizi, A. (2008) A re-evaluation of surface layer turbulence from Antarctic data. Il nuovo cimento C, 31 (5\6). pp. 711-722. ISSN 1826-9885
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