Automatically-generated vector field, composed of the fields surface_eastward_sea_water_velocity and surface_northward_sea_water_velocity

Sea Surface Salinity Climatology in April (spatial resolution 1/8*1/8). The product is based on the SeaDataNet regional climatologies produced by aggregated datasets for the period 1900-2013. Developed by DIVA software v4.6.10 - mask: relative error threshold 0.5. https://doi.org/10.13155/50381

Automatically-generated vector field, composed of the fields eastward_sea_water_velocity and northward_sea_water_velocity

Sea Surface Salinity Climatology in May (spatial resolution 1/8*1/8). The product is based on the SeaDataNet regional climatologies produced by aggregated datasets for the period 1900-2013. Developed by DIVA software v4.6.10 - mask: relative error threshold 0.5. https://doi.org/10.13155/50381

EMODnet Physics - SICE_005 - The products integrates Sea Ice Coverage Extend in Antarctic Sea (based on OSI SAF, developed by SIW-METNO-OSLO-NO, distribuited by CMEMS prd. id. 011_005) together with in operational situ data collected by platforms deployed/operating in Antarctic Sea

Automatically-generated vector field, composed of the fields eastward_sea_water_velocity and northward_sea_water_velocity

Sea Surface Salinity Climatology in March (spatial resolution 1/8*1/8). The product is based on the SeaDataNet regional climatologies produced by aggregated datasets for the period 1900-2013. Developed by DIVA software v4.6.10 - mask: relative error threshold 0.5. https://doi.org/10.13155/50381

Automatically-generated vector field, composed of the fields eastward_sea_water_velocity and northward_sea_water_velocity

Sea Surface Salinity Climatology in June (spatial resolution 1/8*1/8). The product is based on the SeaDataNet regional climatologies produced by aggregated datasets for the period 1900-2013. Developed by DIVA software v4.6.10 - mask: relative error threshold 0.5. https://doi.org/10.13155/50381

EMODnet Physics River PROXY – The product is 1D MOHID model that represent estuaries (i.e. proxy) schematically. The estuary is represented in the model by 10 grid cells in only one direction; 12x3 cells domain including the ocean open boundary and the land limits. In the open boundary, the model receives tides and water properties such as salinity and temperature. The model includes the local tides since the grid open boundary is georeferred and we can use global tidal models to provide realistic tides for each estuary. Tides were imposed using the Finite Element Solution 2014 (FES2014; Carrère et al., 2016) as the global tidal solution. In the land boundary, the model is forced in the innermost cell by river flow and temperature. River salinity values were considered as freshwater (0.01). Atmospheric forcing was not included.