Inverse modeling of salinity–temperature–depth relationships: Application to the upper eastern North Atlantic subtropical gyre

We test the skill of a polynomial fit to reproduce the upper ocean (down to 750 m) salinity in the eastern North Atlantic (from the Canary Islands to the Iberian Peninsula, approximately 12° × 12°) as a function of temperature and depth. A historical database, constructed by merging several regional...

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Veröffentlicht in:	Journal of marine systems 2010-03, Vol.80 (3), p.144-159
Hauptverfasser:	Machín, F., Herraiz, L., Pelegrí, J.L., Marrero-Díaz, A., Font, J., Rodríguez-Santana, A.
Format:	Artikel
Sprache:	eng
Schlagworte:	10.5–5.5 °W/33.5–37.5 °N Analysis of variance Basins Estimating Expandable bathythermograph Inverse Inverse model Marine Mathematical models Peninsulas Salinity Upper ocean
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