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dc.contributor.authorAlonso del Rosario, José Juan 
dc.contributor.authorBlázquez Gómez, Elizabeth 
dc.contributor.authorVidal Pérez, Juan Manuel 
dc.contributor.authorMartin Rey, Faustino
dc.contributor.authorSilva Ramírez, Esther Lydia 
dc.contributor.otherCiencias de la Tierraes_ES
dc.contributor.otherCiencias y Técnicas de la Navegación y Construcciones Navaleses_ES
dc.contributor.otherFísica Aplicadaes_ES
dc.contributor.otherIngeniería Informáticaes_ES
dc.date.accessioned2025-01-03T17:45:47Z
dc.date.available2025-01-03T17:45:47Z
dc.date.issued2024-09
dc.identifier.issn2077-1312
dc.identifier.urihttp://hdl.handle.net/10498/34222
dc.description.abstractThe ATLAZUL project is an Interreg effort among 18 partners from Spain and Portugal along the Atlantic Iberian coasts. One of its objectives is the development of new methods and data processing for oceanic information to produce useful products for private and public stakeholders. This study proposes a new insight on the sea surface dynamic of the ATLAZUL area based on almost two years of multiscale high resolution sea surface temperature imagery. The use of techniques such as the Karhunen–Loève transform (Empirical Orthogonal Function) and the Maximum Entropy Spectral Analysis were applied to study long- and short-term features in the sea surface temperature imagery. Mathematical Morphology and the Geometrical Theory of Measure are utilized to compute the Medial Axis Transform and the Hausdorff dimension. The results can be summarized as follows: (i) the tow upwelling areas are identified along the Galician–Portugal coast as indicated in the second and third modes of KLT/EOF analysis, and they are partially affected by wind; (ii) the tow warm water outflows from the Bay of Cádiz to the Gulf of Cádiz are identified as the second and third modes of KLT/EOF analysis, which are also influenced by wind; (iii) the skeletons of the surface signature of the upwelling and of the warmer water outflow, along with their fractal dimensions, indicate a chaotic pattern of spatial distribution and (iv) the harmonic prediction model should be combined with the wind prediction.es_ES
dc.formatapplication/pdfes_ES
dc.language.isoenges_ES
dc.publisherMDPIes_ES
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.sourceJournal of Marine Science and Engineering, Vol. 12, Núm. 9, 2024es_ES
dc.subjectAtlantic Iberian coastes_ES
dc.subjectKarhunen–Loève transform (EOF)es_ES
dc.subjectMathematical Morphologyes_ES
dc.subjectfractal dimensiones_ES
dc.subjectharmonic predictiones_ES
dc.titleA New Insight on the Upwelling along the Atlantic Iberian Coasts and Warm Water Outflow in the Gulf of Cadiz from Multiscale Ultrahigh Resolution Sea Surface Temperature Imageryes_ES
dc.typejournal articlees_ES
dc.rights.accessRightsopen accesses_ES
dc.identifier.doi10.3390/jmse12091580
dc.type.hasVersionVoRes_ES


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Attribution-NonCommercial-NoDerivatives 4.0 Internacional
This work is under a Creative Commons License Attribution-NonCommercial-NoDerivatives 4.0 Internacional