English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/99317
Share/Impact:
Statistics
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:

DC FieldValueLanguage
dc.contributor.authorHernández Carrasco, Ismael-
dc.contributor.authorLópez, Cristóbal-
dc.contributor.authorOrfila, Alejandro-
dc.contributor.authorHernández-García, Emilio-
dc.date.accessioned2014-07-02T11:47:46Z-
dc.date.available2014-07-02T11:47:46Z-
dc.date.issued2013-10-31-
dc.identifierdoi: 10.5194/npg-20-921-2013-
dc.identifierissn: 1023-5809-
dc.identifier.citationNonlinear Processes in Geophysics 20(5): 921-933 (2013)-
dc.identifier.urihttp://hdl.handle.net/10261/99317-
dc.description.abstractCoastal transport in the Bay of Palma, a small region in the island of Mallorca, Spain, is characterized in terms of Lagrangian descriptors. The data sets used for this study are the output for two months (one in autumn and one in summer) of a high resolution numerical model, ROMS (Regional Ocean Model System), forced atmospherically and with a spatial resolution of 300 m. The two months were selected because of their different wind regime, which is the main driver of the sea dynamics in this area. Finite-size Lyapunov exponents (FSLEs) were used to locate semi-persistent Lagrangian coherent structures (LCS) and to understand the different flow regimes in the bay. The different wind directions and regularity in the two months have a clear impact on the surface bay dynamics, whereas only topographic features appear clearly in the bottom structures. The fluid interchan. © 2013. CC Attribution 3.0 License.-
dc.description.sponsorshipI. Hernández-Carrasco, C. López and E. Hernández-García acknowledge support from MICINN and FEDER through projects FISICOS (FIS2007-60327), INTENSE@COSYP (FIS2012-30634), and ESCOLA (CTM2012-39025-C02-01). A. Orfila acknowledges financial support from MICINN and EU-Med Programme through projects BUS2 (CGL2011-22964) and TOSCA (2GMED-09-425). We acknowledge the ICMAT Severo Ochoa project (SEV-2011-0087) for funding the publication charges of this article.-
dc.publisherAmerican Geophysical Union-
dc.publisherEuropean Geosciences Union-
dc.publisherCopernicus Publications-
dc.relation.isversionofPublisher's version-
dc.rightsopenAccess-
dc.subjectMediterranean Sea-
dc.subjectMajorca-
dc.subjectBalearic Islands-
dc.subjectWind direction-
dc.subjectNumerical model-
dc.subjectLagrangian analysis-
dc.subjectSpain-
dc.subjectTopography-
dc.subjectCoastal zone-
dc.subjectSpatial resolution-
dc.titleLagrangian transport in a microtidal coastal area: The Bay of Palma, island of Mallorca, Spain-
dc.typeartículo-
dc.identifier.doi10.5194/npg-20-921-2013-
dc.relation.publisherversionhttp://dx.doi.org/10.5194/npg-20-921-2013-
dc.date.updated2014-07-02T11:47:46Z-
dc.description.versionPeer Reviewed-
dc.language.rfc3066eng-
dc.rights.licensehttps://creativecommons.org/licenses/by/3.0/-
dc.contributor.funderMinisterio de Ciencia e Innovación (España)-
dc.contributor.funderEuropean Commission-
dc.relation.csic-
dc.identifier.funderhttp://dx.doi.org/10.13039/501100004837es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100000780es_ES
Appears in Collections:(IFISC) Artículos
(IMEDEA) Artículos
Files in This Item:
File Description SizeFormat 
Hernandez-Carrasco-NPG-2013-v20-n5-p921.pdf1,11 MBAdobe PDFThumbnail
View/Open
Show simple item record
 

Related articles:


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.