The surface layer observed by a high-resolution sodar at DOME C, Antarctica
One year field experiment has started on December 2011 at the French - Italian station of Concordia at Dome C, East Antarctic Plateau. The objective of the experiment is the study of the surface layer turbulent processes under stable/very stable stratifications, and the mechanisms leading to the for...
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ftdoajarticles:oai:doaj.org/article:21817bf825d0439d96b29b520df5dcbb 2023-05-15T13:59:25+02:00 The surface layer observed by a high-resolution sodar at DOME C, Antarctica Stefania Argentini Igor Petenko Angelo Viola Giangiuseppe Mastrantonio Ilaria Pietroni Giampietro Casasanta Eric Aristidi Christophe Genthon 2014-01-01T00:00:00Z https://doi.org/10.4401/ag-6347 https://doaj.org/article/21817bf825d0439d96b29b520df5dcbb EN eng Istituto Nazionale di Geofisica e Vulcanologia (INGV) http://www.annalsofgeophysics.eu/index.php/annals/article/view/6347 https://doaj.org/toc/1593-5213 https://doaj.org/toc/2037-416X 1593-5213 2037-416X doi:10.4401/ag-6347 https://doaj.org/article/21817bf825d0439d96b29b520df5dcbb Annals of Geophysics, Vol 56, Iss 5 (2014) Antarctica Boundary layer Mixing layer height Sodar Gravity Waves Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 article 2014 ftdoajarticles https://doi.org/10.4401/ag-6347 2022-12-31T04:12:28Z One year field experiment has started on December 2011 at the French - Italian station of Concordia at Dome C, East Antarctic Plateau. The objective of the experiment is the study of the surface layer turbulent processes under stable/very stable stratifications, and the mechanisms leading to the formation of the warming events. A sodar was improved to achieve the vertical/time resolution needed to study these processes. The system, named Surface Layer sodar (SL-sodar), may operate both in high vertical resolution (low range) and low vertical resolution (high range) modes. In situ turbulence and radiation measurements were also provided in the framework of this experiment. A few preliminary results, concerning the standard summer diurnal cycle, a summer warming event, and unusually high frequency boundary layer atmospheric gravity waves are presented. Article in Journal/Newspaper Antarc* Antarctic Antarctica Directory of Open Access Journals: DOAJ Articles Antarctic Annals of Geophysics 56 5 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Antarctica Boundary layer Mixing layer height Sodar Gravity Waves Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 |
spellingShingle |
Antarctica Boundary layer Mixing layer height Sodar Gravity Waves Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 Stefania Argentini Igor Petenko Angelo Viola Giangiuseppe Mastrantonio Ilaria Pietroni Giampietro Casasanta Eric Aristidi Christophe Genthon The surface layer observed by a high-resolution sodar at DOME C, Antarctica |
topic_facet |
Antarctica Boundary layer Mixing layer height Sodar Gravity Waves Meteorology. Climatology QC851-999 Geophysics. Cosmic physics QC801-809 |
description |
One year field experiment has started on December 2011 at the French - Italian station of Concordia at Dome C, East Antarctic Plateau. The objective of the experiment is the study of the surface layer turbulent processes under stable/very stable stratifications, and the mechanisms leading to the formation of the warming events. A sodar was improved to achieve the vertical/time resolution needed to study these processes. The system, named Surface Layer sodar (SL-sodar), may operate both in high vertical resolution (low range) and low vertical resolution (high range) modes. In situ turbulence and radiation measurements were also provided in the framework of this experiment. A few preliminary results, concerning the standard summer diurnal cycle, a summer warming event, and unusually high frequency boundary layer atmospheric gravity waves are presented. |
format |
Article in Journal/Newspaper |
author |
Stefania Argentini Igor Petenko Angelo Viola Giangiuseppe Mastrantonio Ilaria Pietroni Giampietro Casasanta Eric Aristidi Christophe Genthon |
author_facet |
Stefania Argentini Igor Petenko Angelo Viola Giangiuseppe Mastrantonio Ilaria Pietroni Giampietro Casasanta Eric Aristidi Christophe Genthon |
author_sort |
Stefania Argentini |
title |
The surface layer observed by a high-resolution sodar at DOME C, Antarctica |
title_short |
The surface layer observed by a high-resolution sodar at DOME C, Antarctica |
title_full |
The surface layer observed by a high-resolution sodar at DOME C, Antarctica |
title_fullStr |
The surface layer observed by a high-resolution sodar at DOME C, Antarctica |
title_full_unstemmed |
The surface layer observed by a high-resolution sodar at DOME C, Antarctica |
title_sort |
surface layer observed by a high-resolution sodar at dome c, antarctica |
publisher |
Istituto Nazionale di Geofisica e Vulcanologia (INGV) |
publishDate |
2014 |
url |
https://doi.org/10.4401/ag-6347 https://doaj.org/article/21817bf825d0439d96b29b520df5dcbb |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Antarctica |
genre_facet |
Antarc* Antarctic Antarctica |
op_source |
Annals of Geophysics, Vol 56, Iss 5 (2014) |
op_relation |
http://www.annalsofgeophysics.eu/index.php/annals/article/view/6347 https://doaj.org/toc/1593-5213 https://doaj.org/toc/2037-416X 1593-5213 2037-416X doi:10.4401/ag-6347 https://doaj.org/article/21817bf825d0439d96b29b520df5dcbb |
op_doi |
https://doi.org/10.4401/ag-6347 |
container_title |
Annals of Geophysics |
container_volume |
56 |
container_issue |
5 |
_version_ |
1766267959489069056 |