It is about an automated derived coastline of the North Sea and Baltic Sea from different scale ranges of the Electronic Navigational Chart (ENC) corresponding to the relative coverage area – see nautical product catalogue. The ENCs are produced in accordance with the valid international standard S-57. It consists of generalised lines in the different ENC scale ranges Approach, Harbour and Berthing. None of these scale ranges provides a continuous coastline. The derived coastline consists of natural and man-made (e. g. piers) elements. As an alternative, there is a further coastline available. Information on this high-precision coastline is available via customer@bsh.de.

It is about an automated derived coastline of the North Sea and Baltic Sea from different scale ranges of the Electronic Navigational Chart (ENC) corresponding to the relative coverage area – see nautical product catalogue. The ENCs are produced in accordance with the valid international standard S-57. It consists of generalised lines in the different ENC scale ranges Approach, Harbour and Berthing. None of these scale ranges provides a continuous coastline. The derived coastline consists of natural and man-made (e. g. piers) elements. As an alternative, there is a further coastline available. Information on this high-precision coastline is available via customer@bsh.de.

It is about an automated derived coastline of the North Sea and Baltic Sea from different scale ranges of the Electronic Navigational Chart (ENC) corresponding to the relative coverage area – see nautical product catalogue. The ENCs are produced in accordance with the valid international standard S-57. It consists of generalised lines in the different ENC scale ranges Approach, Harbour and Berthing. None of these scale ranges provides a continuous coastline. The derived coastline consists of natural and man-made (e. g. piers) elements. As an alternative, there is a further coastline available. Information on this high-precision coastline is available via customer@bsh.de.

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.

Modelled temperature and salinity forecast 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.

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.

Modelled current forecast 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 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.

Hourly tidal currents (related to high water Helgoland) of the German coastal waters and neighbouring regions (inner German Bight and Western Baltic) in a horizontal resolution of 900 meters. The information is based on a tidal current simulation using the BSH circulation model BSHcmod.

Grid map showing the spatial distribution of boulders (>50 cm) on the seabed