(Sub-)inertial wave boundary turbulence in the Gulf of Valencia
7 pages, 6 figures
| Autores: | , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 2013 |
| País: | España |
| Institución: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/77442 |
| Acceso en línea: | http://hdl.handle.net/10261/77442 |
| Access Level: | acceso abierto |
| Palabra clave: | 50-m high K-H billows Inertial wave turbulence Gulf of Valencia |
| id |
ES_89ffe1230dccfcf95ffe8dcd24f68663 |
|---|---|
| oai_identifier_str |
oai:digital.csic.es:10261/77442 |
| network_acronym_str |
ES |
| network_name_str |
España |
| repository_id_str |
|
| spelling |
(Sub-)inertial wave boundary turbulence in the Gulf of Valenciavan Haren, H.Ribó, MartaPuig, Pere50-m high K-H billowsInertial wave turbulenceGulf of Valencia7 pages, 6 figuresThe bottom boundary layer above sloping topography can be highly turbulent, even in deep seas. This is demonstrated here using high-resolution 1-Hz sampling temperature sensors that were moored for 5 months every 0.5 m between 6.5 and 61 m above a 572 m deep seafloor promontory on the continental slope off Valencia, Spain. Using these data, turbulence parameters have been estimated. With time and in the vertical, values vary over four orders of magnitude. They have a dominant local inertial period which is modulated by an about 11 day periodicity associated with variations in a baroclinic unstable boundary current. When this current is strong and Eastward, the upslope phase of inertial wave generates convective turbulence which reaches closest to the bottom and therefore can effect sediment dispersal. In late winter, equally strong shear-induced turbulence in 50 m high Kelvin-Helmholtz (K-H) overturns is forced by 0.2 m s−1 off/downslope motions, which are preceded by periods of warming of a few 0.01°C before the cooler near-bottom water is suddenly flushed over the promontory into the basin. Such anomalously large K-H overturns occurred 6 times in the investigated winter periodThis research was supported by the project COSTEM (CTM2009-07806). We thank the captain and the crew of the R/V Garcia del Cid for their kind assistance. We thank Martin Laan for all his enthusiastic development of NIOZ-thermistors. We are grateful to the UTM technicians for providing assistance during the data acquisition. M. R. is supported by a FPI grant (Ref. BES-2010-029949) from the Spanish Ministry of Economy and CompetitivenessPeer reviewedWiley-BlackwellAmerican Geophysical Union2013info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501http://hdl.handle.net/10261/77442reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Ingléshttps://doi.org/10.1002/jgrc.20168info:eu-repo/semantics/openAccessoai:digital.csic.es:10261/774422026-05-22T06:33:51Z |
| dc.title.none.fl_str_mv |
(Sub-)inertial wave boundary turbulence in the Gulf of Valencia |
| title |
(Sub-)inertial wave boundary turbulence in the Gulf of Valencia |
| spellingShingle |
(Sub-)inertial wave boundary turbulence in the Gulf of Valencia van Haren, H. 50-m high K-H billows Inertial wave turbulence Gulf of Valencia |
| title_short |
(Sub-)inertial wave boundary turbulence in the Gulf of Valencia |
| title_full |
(Sub-)inertial wave boundary turbulence in the Gulf of Valencia |
| title_fullStr |
(Sub-)inertial wave boundary turbulence in the Gulf of Valencia |
| title_full_unstemmed |
(Sub-)inertial wave boundary turbulence in the Gulf of Valencia |
| title_sort |
(Sub-)inertial wave boundary turbulence in the Gulf of Valencia |
| dc.creator.none.fl_str_mv |
van Haren, H. Ribó, Marta Puig, Pere |
| author |
van Haren, H. |
| author_facet |
van Haren, H. Ribó, Marta Puig, Pere |
| author_role |
author |
| author2 |
Ribó, Marta Puig, Pere |
| author2_role |
author author |
| dc.subject.none.fl_str_mv |
50-m high K-H billows Inertial wave turbulence Gulf of Valencia |
| topic |
50-m high K-H billows Inertial wave turbulence Gulf of Valencia |
| description |
7 pages, 6 figures |
| publishDate |
2013 |
| dc.date.none.fl_str_mv |
2013 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article http://purl.org/coar/resource_type/c_6501 |
| format |
article |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10261/77442 |
| url |
http://hdl.handle.net/10261/77442 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
https://doi.org/10.1002/jgrc.20168 |
| dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
| eu_rights_str_mv |
openAccess |
| dc.publisher.none.fl_str_mv |
Wiley-Blackwell American Geophysical Union |
| publisher.none.fl_str_mv |
Wiley-Blackwell American Geophysical Union |
| dc.source.none.fl_str_mv |
reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC instname:Consejo Superior de Investigaciones Científicas (CSIC) |
| instname_str |
Consejo Superior de Investigaciones Científicas (CSIC) |
| reponame_str |
DIGITAL.CSIC. Repositorio Institucional del CSIC |
| collection |
DIGITAL.CSIC. Repositorio Institucional del CSIC |
| repository.name.fl_str_mv |
|
| repository.mail.fl_str_mv |
|
| _version_ |
1869412668553560064 |
| score |
15,811543 |