A 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 Imagery

Author:

del Rosario José J. Alonso1ORCID,Gómez Elizabeth Blázquez2ORCID,Pérez Juan Manuel Vidal3ORCID,Rey Faustino Martín4,Silva-Ramírez Esther L.5ORCID

Affiliation:

1. Department of Applied Physics, School of Naval Architecture and Ocean Engineering, CASEM, University of Cádiz, Avda. Rep Saharaui s/n, 11510 Puerto Real, Spain

2. Department of Earth Sciences, Faculty of Marine and Environmental Sciences, CASEM, University of Cádiz, Avda. Rep Saharaui s/n, 11510 Puerto Real, Spain

3. Department of Ship Building, School of Naval Architecture and Ocean Engineering, CASEM, University of Cádiz, Avda. Rep Saharaui s/n, 11510 Puerto Real, Spain

4. Integrated Center for Information Technologies, University of Cádiz, Avda. Rep Saharaui s/n, 11510 Puerto Real, Spain

5. Department of Computer Science and Engineering, Escuela Superior de Ingeniería, Universidad de Cádiz, Avda. de la Universidad s/n, 11510 Puerto Real, Spain

Abstract

The 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.

Funder

Interreg-ATLAZUL

Publisher

MDPI AG

Reference39 articles.

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2. Coupling between the Iberian basin-scale circulation and the Portugal boundary current system: A chemical study;Castro;Deep. Sea Res. Part I Oceanogr. Res. Pap.,2001

3. Surface circulation in the eastern North Atlantic from drifters and altimetry;Martins;J. Geophys. Ocean. Res.,2002

4. Winter upper ocean circulation in the western Iberia basin- fronts, eddies and poleward flows: An overview;Peliz;Deep Sea Res. I,2005

5. Robinson, A., and Brink, K.H. (2004). Oceanography and fisheries od the Canary current/Iberian region of the eastern North Atlantic. The Sea, Harvard University Press.

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