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wdc-climate.de:3881135 eng; USA collection storm_tide_1906_20CR Dr. Elke Meyer Helmholtz-Zentrum Hereon www.hereon.de pointOfContact Dr. Elke Meyer Helmholtz-Zentrum Hereon www.hereon.de pointOfContact 2020-10-27T11:07:43 ISO 19115 ISO 19115-2:2009 Reconstruction of the 1906 Storm Tide in the German Bright using TRIM-NP, FES2004, and NOAA-CIRES-DOE Twentieth Century Reanalysis (20CR) version 2c and 3 2021-01-08 publication 1 storm_tide_1906_20CR doi:10.26050/WDCC/storm_tide_1906_20CR Dr. Elke Meyer Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH not filled Email: elke.meyer@hereon.de principalInvestigator Dr. Elke Meyer Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH not filled Email: elke.meyer@hereon.de author WDC Climate at DKRZ publisher The hydrodynamic model TRIM-NP in a barotropic mode is used to simulate the strong storm tide in March 1906 forced by NOAA-CIRES-DOE Twentieth Century Reanalysis (20CR) version 2c and 3. datasets (https://portal.nersc.gov/project/20C_Reanalysis/). 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. Dr. Elke Meyer Helmholtz-Zentrum Hereon www.hereon.de pointOfContact NetCDF 20CR reanalysis coastal hazard historical storm tide water level CC-BY-4.0: Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ eng; USA -8.0 17.5 48.1 62.5 calendrical 1906-03-01 1906-03-31 air_pressure_at_sea_level sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: not filled sea_water_y_velocity A velocity is a vector quantity. "y" indicates a vector component along the grid y-axis, positive with increasing y. [CF-Standard Name]; unit: not filled sea_water_x_velocity A velocity is a vector quantity. "x" indicates a vector component along the grid x-axis, positive with increasing x. [CF-Standard Name]; unit: not filled air_pressure_at_sea_level sea_level means mean sea level, which is close to the geoid in sea areas. Air pressure at sea level is the quantity often abbreviated as MSLP or PMSL.[CF-Standard Name]; unit: not filled y_wind "y" indicates a vector component along the grid y-axis, when this is not true latitude, positive with increasing y. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)[CF-Standard Name]; unit: not filled sea_water_y_velocity A velocity is a vector quantity. "y" indicates a vector component along the grid y-axis, positive with increasing y. [CF-Standard Name]; unit: not filled sea_water_x_velocity A velocity is a vector quantity. "x" indicates a vector component along the grid x-axis, positive with increasing x. [CF-Standard Name]; unit: not filled y_wind "y" indicates a vector component along the grid y-axis, when this is not true latitude, positive with increasing y. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)[CF-Standard Name]; unit: not filled sea_surface_height_above_sea_level sea_surface_height_above_sea_level [CF-Standard Name]; unit: not filled sea_surface_height_above_sea_level sea_surface_height_above_sea_level [CF-Standard Name]; unit: not filled x_wind "x" indicates a vector component along the grid x-axis, when this is not true longitude, positive with increasing x. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)[CF-Standard Name]; unit: not filled x_wind "x" indicates a vector component along the grid x-axis, when this is not true longitude, positive with increasing x. Wind is defined as a two-dimensional (horizontal) air velocity vector, with no vertical component. (Vertical motion in the atmosphere has the standard name upward_air_velocity.)[CF-Standard Name]; unit: not filled NetCDF 261246 https://www.wdc-climate.de/ui/entry?acronym=storm_tide_1906_20CR information collection