2008
DOI: 10.1016/j.rse.2007.04.020
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Retrieving ocean surface current by 4-D variational assimilation of sea surface temperature images

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Cited by 32 publications
(40 citation statements)
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“…resolution surface current maps obtained by means of the imagery processing (Korotaev et al, 2008) show that the Rim current has fine structure in the form of narrow and intense submesoscale jets. However the current grid size of the model (5 km) is able to resolve mesoscale eddies but not submesoscale structures.…”
Section: Profiling Floatsmentioning
confidence: 99%
“…resolution surface current maps obtained by means of the imagery processing (Korotaev et al, 2008) show that the Rim current has fine structure in the form of narrow and intense submesoscale jets. However the current grid size of the model (5 km) is able to resolve mesoscale eddies but not submesoscale structures.…”
Section: Profiling Floatsmentioning
confidence: 99%
“…Among those heuristics, the shallow water model [17] has been proven to be suitable for representing the surface circulation of closed seas, such as Black Sea [10]. These shallow water equations have also been successfully used to estimate the upper layer circulation of Black Sea from Sea Surface Temperature (SST) images [5,6] with a data assimilation method.…”
Section: Introductionmentioning
confidence: 99%
“…This 2D model has been proven to be suitable for representing the surface circulation of closed seas, such as Black Sea (Oguz et al, 1992). The shallow water equations have also been success-1 http://www.nemo-ocean.eu/ fully used to estimate the upper layer circulation of Black Sea from Sea Surface Temperature (SST) images (Korotaev et al, 2008;Huot et al, 2010) with a data assimilation method.…”
Section: Introductionmentioning
confidence: 99%