SMAGU: Submesoscale variability in the Agulhas Current Region
Pauline Tedesco
This model is forced using ROMS/CROCO. It has a horizontal resolution of ~0.75 km and uses the ~ 3km resolution WOES III (http://dap.saeon.ac.za/thredds/catalog/SAEON.EGAGASINI/2019.Penven/DAILY_MEANS/1_36_degree/catalog.html) as its oceanic boundary conditions. This is done offline. The surface forcing is daily ERA-ECMWF reanalysis product, with the relative wind formulation. The bathymetry is built from the General Bathymetric Chart of the Oceans 30-sec resolution (Gebco 2014). There are 100 topography following coordinates, distributed following LemariƩ et al. (2012) method with...