wdc-climate.de:2477267 eng; USA collection coastDat-2_TRIM-NP-2d Dr. Lidia Gaslikova Helmholtz-Zentrum Hereon www.hereon.de pointOfContact Dr. Lidia Gaslikova Helmholtz-Zentrum Hereon www.hereon.de pointOfContact 2013-04-03T14:41:05 ISO 19115 ISO 19115-2:2009 coastDat-2 TRIM-NP-2d Tide-Surge North Sea 2013-09-16 publication 1 coastDat-2_TRIM-NP-2d doi:10.1594/WDCC/coastDat-2_TRIM-NP-2d Dr. Lidia Gaslikova Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH not filled Email: lidia.gaslikova@hereon.de principalInvestigator Dr. Lidia Gaslikova Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH not filled Email: lidia.gaslikova@hereon.de author Dr. Ralf Weisse Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH not filled Email: ralf.weisse@hzg.de author WDC Climate at DKRZ publisher This is a hydrodynamic hindcast for the North Sea and the Northeast Atlantic over the period 1948-2015. The simulation has been performed with the hydrodynamic model TRIM-NP V2.1.22 in barotropic 2D mode. Water level and current component fields are stored hourly. The model is set up on an equidistant Cartesian grid cascade with the center near Helgoland (7.88 E, 54.18 N). The coarsest grid with 12.8 km resolution covers the area from 20 W to 30 E and from 42 N to 65 N. Further 3 nested grids better resolve the North Sea (with 6.4km), southern North Sea (with 3.2km) and the German Bight (with 1.6km). Model data from grid 1 and grid 4 are available in this data bank. Please contact the authors for data from grid 2 and grid 3. Time supplement procedure: data over period 2013-2015 appended 04-05-2016 Dr. Lidia Gaslikova Helmholtz-Zentrum Hereon www.hereon.de pointOfContact NetCDF climate simulation coastdat hindcasting regional modelling scientific use: For scientific use only eng; USA -20.0 30.0 42.0 65.0 calendrical 1948-01-01 2015-08-31 latitude latitude [CF-Standard Name]; unit: degrees_north 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: m s-1 longitude longitude [CF-Standard Name]; unit: degrees_east northward_sea_water_velocity sea_water_y_velocity [CF-Standard Name]; unit: m s-1 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: hPa eastward_sea_water_velocity sea_water_x_velocity [CF-Standard Name]; unit: m s-1 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: m s-1 sea_surface_height_above_sea_level sea_surface_height_above_sea_level [CF-Standard Name]; unit: m NetCDF 2068689 https://www.wdc-climate.de/ui/entry?acronym=coastDat-2_TRIM-NP-2d information collection n/a None n/a None