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http://hdl.handle.net/10261/123609
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dc.contributor.author | Troupin, Charles | es_ES |
dc.contributor.author | Pascual, Ananda | es_ES |
dc.contributor.author | Valladeau, Guillaume | es_ES |
dc.contributor.author | Pujol, Isabelle | es_ES |
dc.contributor.author | Lana, Arantxa | es_ES |
dc.contributor.author | Heslop, Emma | es_ES |
dc.contributor.author | Ruiz, Simón | es_ES |
dc.contributor.author | Torner, Marc | es_ES |
dc.contributor.author | Picot, Nicolas | es_ES |
dc.contributor.author | Tintoré, Joaquín | es_ES |
dc.date.accessioned | 2015-10-20T11:08:54Z | - |
dc.date.available | 2015-10-20T11:08:54Z | - |
dc.date.issued | 2014-09-16 | - |
dc.identifier.citation | Advances in Space Research 55(1): 51-59 (2014) | es_ES |
dc.identifier.issn | 1879-1948 | - |
dc.identifier.uri | http://hdl.handle.net/10261/123609 | - |
dc.description.abstract | © 2014 COSPAR. Published by Elsevier Ltd. All rights reserved. Satellite altimetry measurements from SARALAltiKa are analysed in the coastal ocean using the results of the GAltiKa mission (15 August 2013), which combined altimeter, HF radar and glider data coincident with the satellite track, southwest of Ibiza Island, in the Western Mediterranean Sea. The absolute dynamic topography, computed from 1 Hz and 40 Hz altimetry data, and the dynamic height, computed from glider temperature and salinity, both exhibited a weak signal with amplitudes of order 2 cm. The resulting geostrophic and HF radar velocities along the track depicted a northwestward coastal current with a maximal velocity larger than 20 cm s1. This demonstrates that the AltiKa altimeter is able to resolve SLA signals of more than 2 cm, and gradients in those signals over several tens of kilometres. After filtering, the 40 Hz data depicted a signal consistent with the other platforms, up to a distance of order 10 km from the coast | es_ES |
dc.description.sponsorship | SARAL IGDR are produced by CNES SPA Team as part of the SSALTO ground processing segment, and distributed by AVISO, with support from CNES SALP project. GAltiKa experiment was carried out in the frame of MyOcean2 EU FP7 funded project, with substantial support from SOCIB. Glider operations were partially funded by JERICO and PERSEUS FP7 projects. Additional funding from the Local Government of the Balearic Islands (CAIB51/ 2011 Grant) is also acknowledged. C. Troupin postdoctoral position was funded by MyOcean2 EU FP7 project | es_ES |
dc.language.iso | eng | es_ES |
dc.publisher | Elsevier | es_ES |
dc.relation | info:eu-repo/grantAgreement/EC/FP7/262584 | - |
dc.relation | info:eu-repo/grantAgreement/EC/FP7/283367 | - |
dc.relation | info:eu-repo/grantAgreement/EC/FP7/287600 | - |
dc.relation.isversionof | Postprint | es_ES |
dc.rights | openAccess | en_EN |
dc.subject | Radar Altimetry | es_ES |
dc.subject | Mesoscale eddies | es_ES |
dc.subject | Ocean Gliders | es_ES |
dc.subject | Northwestern Mediterranean Sea | es_ES |
dc.subject | Ibiza Channel | es_ES |
dc.subject | HF radar | es_ES |
dc.title | Illustration of the emerging capabilities of SARAL/AltiKa in the coastal zone using a multiplatform approach | es_ES |
dc.type | artículo | es_ES |
dc.identifier.doi | 10.1016/j.asr.2014.09.011 | - |
dc.description.peerreviewed | Peer reviewed | es_ES |
dc.relation.publisherversion | http://dx.doi.org/10.1016/j.asr.2014.09.011 | es_ES |
dc.embargo.terms | 2016-09-17 | es_ES |
dc.contributor.funder | Govern de les Illes Balears | es_ES |
dc.contributor.funder | European Commission | es_ES |
dc.relation.csic | Sí | es_ES |
dc.identifier.funder | http://dx.doi.org/10.13039/501100000780 | es_ES |
dc.type.coar | http://purl.org/coar/resource_type/c_6501 | es_ES |
item.openairetype | artículo | - |
item.grantfulltext | open | - |
item.cerifentitytype | Publications | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
item.languageiso639-1 | en | - |
Aparece en las colecciones: | (IMEDEA) Artículos |
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Illustration_Troupin.pdf | 9,01 MB | Adobe PDF | Visualizar/Abrir |
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