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Viudez, A., Tintoré, J., & Haney, R. L. (1996). Circulation in the alboransea as determined
by quasi-synoptic hydrographic observations. part i:Three-dimensional structure of the two
anticyclonic gyres. Journal of Physical Oceanography, p.p.684-705.
the winters of 1982 and 1983. (Vol. V). In Annales geophysicae.Series B. Terrestrial and
planetary physics.
Send, U., Font, J., et al. (1999). Recent advances in observing the physical oceanography of
the western mediterranean sea. Progress in Oceanography, p.p.37-64.
Send, U., Mertens, C., et al. (1996). Recent observation indicates convection'role in deep water
circulation. 61-65. Eos, Transactions American Geophysical Union.
Sotillo, M.G., Cailleau, S., et al. (2015). The MyOcean IBI Ocean Forecast and Reanalysis
Systems: operational products and roadmap to the future Copernicus Service. Journal of
Operational Oceanography.
Takahashi, T. B. (1985). Redfield ratio based on chemical data from isopycnal surfaces. J.
Geophys. Res.
Testor, P., Béranger, K., & Mortier, L. (2005). Modeling the deep eddy field in the
southwestern mediterranean: The life cycle of sardinian eddies. Geophysical research letters.
Tréguier, A.M. (2002). Modélisation pour l'océanographie physique. Annalzs Mathématique
BlaisePascal, Tome 9, p.p.345-361.
Tsimplis, M., & Bryden, H. (2000). Estimation of the transports through the Strait of Gibraltar.
Deep-Sea Research Part I-Oceanographic Research Papers, p.p.2219-2242.
Vargas-Yanez, M., Plaza, F., et al. (2002). About the seasonal variability of the alboran sea
circulation. Journal of Marine Systems, p.p.229-248.
Vazquez-Cuervo, J., Font, J., & Martinez-Benjamin, J. J. (1996). Observations on the
circulation in the alboran sea using ersi altimetry and sea surface temperature data. Journal of
Physical Oceanography.
Vidal-Vijande, E., Pascual, A., et al. (2012). Multiparametric analysis and validation in the
western mediterranean of three global ogcm hindcasts. Scientia Marina, p.p.147-164.
Viudez, A., Tintoré, J., & Haney, R. L. (1996). Circulation in the alboransea as determined
by quasi-synoptic hydrographic observations. part i:Three-dimensional structure of the two
anticyclonic gyres. Journal of Physical Oceanography, p.p.684-705.