Local scaling characteristics of Antarctic surface layer turbulence
Over the past years, several studies have validated Nieuwstadt's local scaling hypothesis by utilizing turbulence observations from the mid-latitude, nocturnal stable boundary layers. In this work, we probe into the local scaling characteristics of polar, long-lived stable boundary layers by an...
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Copernicus Publications
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Online Access: | https://doi.org/10.5194/tc-4-325-2010 http://www.the-cryosphere.net/4/325/2010/tc-4-325-2010.pdf https://doaj.org/article/d863a4ab8ae444fa8c3a3480f8c3c51e |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:d863a4ab8ae444fa8c3a3480f8c3c51e 2023-05-15T13:37:01+02:00 Local scaling characteristics of Antarctic surface layer turbulence S. Basu A. Ruiz-Columbié J. A. Phillipson S. Harshan 2010-09-01 https://doi.org/10.5194/tc-4-325-2010 http://www.the-cryosphere.net/4/325/2010/tc-4-325-2010.pdf https://doaj.org/article/d863a4ab8ae444fa8c3a3480f8c3c51e en eng Copernicus Publications doi:10.5194/tc-4-325-2010 1994-0416 1994-0424 http://www.the-cryosphere.net/4/325/2010/tc-4-325-2010.pdf https://doaj.org/article/d863a4ab8ae444fa8c3a3480f8c3c51e undefined The Cryosphere, Vol 4, Iss 3, Pp 325-331 (2010) geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2010 fttriple https://doi.org/10.5194/tc-4-325-2010 2023-01-22T19:35:05Z Over the past years, several studies have validated Nieuwstadt's local scaling hypothesis by utilizing turbulence observations from the mid-latitude, nocturnal stable boundary layers. In this work, we probe into the local scaling characteristics of polar, long-lived stable boundary layers by analyzing turbulence data from the South Pole region of the antarctic plateau. Article in Journal/Newspaper Antarc* Antarctic South pole South pole The Cryosphere Unknown Antarctic South Pole The Antarctic The Cryosphere 4 3 325 331 |
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language |
English |
topic |
geo |
spellingShingle |
geo S. Basu A. Ruiz-Columbié J. A. Phillipson S. Harshan Local scaling characteristics of Antarctic surface layer turbulence |
topic_facet |
geo |
description |
Over the past years, several studies have validated Nieuwstadt's local scaling hypothesis by utilizing turbulence observations from the mid-latitude, nocturnal stable boundary layers. In this work, we probe into the local scaling characteristics of polar, long-lived stable boundary layers by analyzing turbulence data from the South Pole region of the antarctic plateau. |
format |
Article in Journal/Newspaper |
author |
S. Basu A. Ruiz-Columbié J. A. Phillipson S. Harshan |
author_facet |
S. Basu A. Ruiz-Columbié J. A. Phillipson S. Harshan |
author_sort |
S. Basu |
title |
Local scaling characteristics of Antarctic surface layer turbulence |
title_short |
Local scaling characteristics of Antarctic surface layer turbulence |
title_full |
Local scaling characteristics of Antarctic surface layer turbulence |
title_fullStr |
Local scaling characteristics of Antarctic surface layer turbulence |
title_full_unstemmed |
Local scaling characteristics of Antarctic surface layer turbulence |
title_sort |
local scaling characteristics of antarctic surface layer turbulence |
publisher |
Copernicus Publications |
publishDate |
2010 |
url |
https://doi.org/10.5194/tc-4-325-2010 http://www.the-cryosphere.net/4/325/2010/tc-4-325-2010.pdf https://doaj.org/article/d863a4ab8ae444fa8c3a3480f8c3c51e |
geographic |
Antarctic South Pole The Antarctic |
geographic_facet |
Antarctic South Pole The Antarctic |
genre |
Antarc* Antarctic South pole South pole The Cryosphere |
genre_facet |
Antarc* Antarctic South pole South pole The Cryosphere |
op_source |
The Cryosphere, Vol 4, Iss 3, Pp 325-331 (2010) |
op_relation |
doi:10.5194/tc-4-325-2010 1994-0416 1994-0424 http://www.the-cryosphere.net/4/325/2010/tc-4-325-2010.pdf https://doaj.org/article/d863a4ab8ae444fa8c3a3480f8c3c51e |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/tc-4-325-2010 |
container_title |
The Cryosphere |
container_volume |
4 |
container_issue |
3 |
container_start_page |
325 |
op_container_end_page |
331 |
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1766087025396547584 |