ESA 4DMED-Sea - Finite-Time Lagrangian Vorticity in the Mediterranean Sea derived from 4DVARNET8 geostrophic velocities (1/24°)

This product provides the Finite-Time Lagrangian Vorticity derived from surface geostrophic velocities result from the application of the 4DVARNET algorithm (Fablet et al., 2021; resolution of the dynamical model used for the learning/training (eNATL60-BLB02) downgraded to 1/8°) to altimetry L3-data (https://doi.org/10.5281/zenodo.10908416) at a resolution of 1/24° over the Mediterranean Sea and for the period from April 2016 to July 2022. 

Algorithm used to compute Finite-Time Lagrangian Vorticity was developed by I. Hernandez-Carrasco (Hernandez-Carrasco et al, 2011, Ocean modelling. https://doi.org/10.1016/j.ocemod.2010.12.006).

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Geographical coverage: Mediterranean Sea

Grid and horizontal spatial resolution: Evenly spaced 1/24º grid

Vertical levels: Only surface level

Temporal resolution: Daily (April 2016 - July 2022)

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Variables:

lon (1D)

lat (1D)

time (1D)

ftlv (2D)