de.dkrz.wdcc.iso3881144 series storm_tide_1906_DWD_reconstruct Dr. Elke Meyer Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH author Robert Scholz DWD- Niederlassung Leipzig author Birger Tinz Seewetteramt Hamburg author Dr. Elke Meyer Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH pointOfContact Dr. Elke Meyer Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH originator 2022-02-20T04:25:18 ISO 19115 ISO 19139 / DKRZ ISO Simple Profile V1.0 http://doi.org/doi:10.26050/WDCC/storm_tide_1906_DWD_reconstruct storm_tide_1906_DWD_reconstruction storm_tide_1906_DWD_reconstruction 2020-10-27 creation None Reconstruction of the 1906 Storm Tide in the German Bright using TRIM-NP, FES2004, and DWD weather data doi:10.26050/WDCC/storm_tide_1906_DWD_reconstruct Dr. Elke Meyer Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH originator doi:10.26050/WDCC/storm_tide_1906_DWD_reconstruct The hydrodynamic model TRIM-NP in a barotropic mode is used to simulate the strong storm tide in March 1906 forced by reconstructed weather data by the Deutsche Wetterdienst (DWD) and Helmholtz-Zentrum Geesthacht. From georeferenced historical station data, pressure maps are drawn, digitised, and wind speed calculated from them. The model area covers the region of 20W to 30E and 42N to 65N with a spatial resolution of 12.8x12.8 km for grid 1. At the lateral boundaries of grid 1, the water level is calculated with tide model FES2004. TRIM-NP calculates one way nested with higher resolution the North Sea (with 6.4km, grid2), southern North Sea (with 3.2km, grid3) and the German Bight (with 1.6km, grid4). In this data bank, the datasets are available hourly for grid 2 and grid 4. Please contact the authors for grid 1 and grid 3. The datasets are visualised https://doi.org/10.5446/49529 or https://www.dkrz.de/projects-and-partners/projects/focus/stormtide1906. In additional experiments, the tides at the lateral boundaries are shifted backwards (up to minus six hours) or forward (up to plus six hours) in time to calculate the peak of the storm tide. The atmospheric forcing is not changed. Only the water levels from grid4 of this experiment are stored. Dr. Elke Meyer Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH author Robert Scholz DWD- Niederlassung Leipzig author Birger Tinz Seewetteramt Hamburg author Dr. Elke Meyer Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH pointOfContact historical storm tide from station data theme coastal hazard theme water level theme shifting tides theme eng -8.0 17.5 48.1 62.5 1906-03-01 1906-03-15 0 air_pressure_at_sea_level modelResult not filled sea_surface_height_above_sea_level modelResult not filled sea_water_x_velocity modelResult not filled sea_water_y_velocity modelResult not filled x_wind modelResult not filled y_wind modelResult not filled NetCDF network Common Data Format distributor Mb 3050 http://doi.org/doi:10.26050/WDCC/storm_tide_1906_DWD_reconstruct series