Layer thickness of the operational circulation model of the Federal Maritime and Hydrographic Agency of Germany (BSH), in the German Bight and the western Baltic Sea (horizontal resolution ca. 900 m). The model (HBM, HIROMB-BOOS-Model) is run four times each day in a configuration with a fine grid in the German Bight and western Baltic Sea (900 m resolution, this dataset) and a coarser grid which covers the North and Baltic Sea (5 km resolution, separate dataset). The model is forced by the weather forecast of the German Weather Service (DWD). More detailed information about the model configuration can be found in Brüning et al. (2021); https://doi.org/10.23784/HN118-01.

Layer thickness of the operational circulation model of the Federal Maritime and Hydrographic Agency of Germany (BSH), in the North and Baltic Sea (horizontal resolution ca. 5 km). The model (HBM, HIROMB-BOOS-Model) is run four times each day in a configuration with a fine grid in the German Bight and western Baltic Sea (900 m resolution, separate dataset) and a coarser grid which covers the North and Baltic Sea (5 km resolution, this dataset). The model is forced by the weather forecast of the German Weather Service (DWD). More detailed information about the model configuration can be found in Brüning et al. (2021); https://doi.org/10.23784/HN118-01.

Modelled current forecast of the operational circulation model of the Federal Maritime and Hydrographic Agency of Germany (BSH), in the North and Baltic Sea (horizontal resolution ca. 5 km). The model (HBM, HIROMB-BOOS-Model) is run four times each day in a configuration with a fine grid in the German Bight and western Baltic Sea (900 m resolution, separate dataset) and a coarser grid which covers the North and Baltic Sea (5 km resolution, this dataset). The model is forced by the weather forecast of the German Weather Service (DWD). More detailed information about the model configuration can be found in Brüning et al. (2021); https://doi.org/10.23784/HN118-01.

Modelled temperature and salinity forecast of the operational circulation model of the Federal Maritime and Hydrographic Agency of Germany (BSH), in the North and Baltic Sea (horizontal resolution ca. 5 km). The model (HBM, HIROMB-BOOS-Model) is run four times each day in a configuration with a fine grid in the German Bight and western Baltic Sea (900 m resolution, separate dataset) and a coarser grid which covers the North and Baltic Sea (5 km resolution, this dataset). The model is forced by the weather forecast of the German Weather Service (DWD). More detailed information about the model configuration can be found in Brüning et al. (2021); https://doi.org/10.23784/HN118-01.

Modelled forecast of the sea surface height above mean sea level of the operational circulation model of the Federal Maritime and Hydrographic Agency of Germany (BSH), in the North and Baltic Sea (horizontal resolution ca. 5 km). The model (HBM, HIROMB-BOOS-Model) is run four times each day in a configuration with a fine grid in the German Bight and western Baltic Sea (900 m resolution, separate dataset) and a coarser grid which covers the North and Baltic Sea (5 km resolution, this dataset). The model is forced by the weather forecast of the German Weather Service (DWD). More detailed information about the model configuration can be found in Brüning et al. (2021); https://doi.org/10.23784/HN118-01.

Modelled forecast of sea surface height above mean sea level of the operational circulation model of the Federal Maritime and Hydrographic Agency of Germany (BSH), in the German Bight and the western Baltic Sea (horizontal resolution ca. 900 m). The model (HBM, HIROMB-BOOS-Model) is run four times each day in a configuration with a fine grid in the German Bight and western Baltic Sea (900 m resolution, this dataset) and a coarser grid which covers the North and Baltic Sea (5 km resolution, separate dataset). The model is forced by the weather forecast of the German Weather Service (DWD). More detailed information about the model configuration can be found in Brüning et al. (2021); https://doi.org/10.23784/HN118-01.

Layer thickness of the operational circulation model of the Federal Maritime and Hydrographic Agency of Germany (BSH), in the North and Baltic Sea (horizontal resolution ca. 5 km). The model (HBM, HIROMB-BOOS-Model) is run four times each day in a configuration with a fine grid in the German Bight and western Baltic Sea (900 m resolution, separate dataset) and a coarser grid which covers the North and Baltic Sea (5 km resolution, this dataset). The model is forced by the weather forecast of the German Weather Service (DWD). More detailed information about the model configuration can be found in Brüning et al. (2021); https://doi.org/10.23784/HN118-01.

Modelled current forecast of the operational circulation model of the Federal Maritime and Hydrographic Agency of Germany (BSH), in the North and Baltic Sea (horizontal resolution ca. 5 km). The model (HBM, HIROMB-BOOS-Model) is run four times each day in a configuration with a fine grid in the German Bight and western Baltic Sea (900 m resolution, separate dataset) and a coarser grid which covers the North and Baltic Sea (5 km resolution, this dataset). The model is forced by the weather forecast of the German Weather Service (DWD). More detailed information about the model configuration can be found in Brüning et al. (2021); https://doi.org/10.23784/HN118-01.

Layer thickness of the operational circulation model of the Federal Maritime and Hydrographic Agency of Germany (BSH), in the German Bight and the western Baltic Sea (horizontal resolution ca. 900 m). The model (HBM, HIROMB-BOOS-Model) is run four times each day in a configuration with a fine grid in the German Bight and western Baltic Sea (900 m resolution, this dataset) and a coarser grid which covers the North and Baltic Sea (5 km resolution, separate dataset). The model is forced by the weather forecast of the German Weather Service (DWD). More detailed information about the model configuration can be found in Brüning et al. (2021); https://doi.org/10.23784/HN118-01.