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oai:wdcc.dkrz.de:iso_3580496 2026-04-05T23:08:04Z iso-wdcc-doi

wdc-climate.de:3580496 eng; USA collection coastDat_COSMO-CLM_GB0028 Benjamin Schaaf Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH not filled pointOfContact Benjamin Schaaf Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH not filled pointOfContact 2017-11-20T16:36:17 ISO 19115 ISO 19115-2:2009 coastDat_COSMO-CLM German Bight 0028 2018-06-08 publication 1 coastDat_COSMO-CLM_GB0028 doi:10.1594/WDCC/coastDat_COSMO-CLM_GB0028 Benjamin Schaaf Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH not filled Email: benjamin.schaaf@hzg.de principalInvestigator Benjamin Schaaf Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH not filled Email: benjamin.schaaf@hzg.de author WDC Climate at DKRZ publisher This is an atmospheric hourly hindcast for the German Bight using COSMO-CLM version 5.00_clm2 from 1948-August 2015 (http://www.cosmo-model.org/content/model/documentation/core/default.htm). The model uses a rotated grid with 250 x 180 grid points and a grid point distance of 0.025 degrees, the rotated North pole is located at 172.97 W, 34.925 N. The forcing is coastDat2 doi:10.1594/WDCC/coastDat-2_COSMO-CLM . In rotated coordinates the model area extends from 2.25 W to 2.25 E, 3.125 S to 3.125 N, in geographical coordinates this corresponds to about 1.3 E to 12.8 E, 52.7 N to 57.3 N. Benjamin Schaaf Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH not filled pointOfContact NetCDF COSMO-CLM coastdat convection-permitting hindcasting regional modelling CC-BY-4.0: Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ eng; USA 1.3 12.8 52.7 57.3 calendrical 1948-01-01 2015-08-31 convective_rainfall_amount "Amount" means mass per unit area.[CF-Standard Name]; unit: kg m-2 large_scale_snowfall_amount "Amount" means mass per unit area.[CF-Standard Name]; unit: kg m-2 cloud_area_fraction "X_area_fraction" means the fraction of horizontal area occupied by X. "X_area" means the horizontal area occupied by X within the grid cell. Cloud area fraction is also called "cloud amount" and "cloud cover". The cloud area fraction is for the whole atmosphere column, as seen from the surface or the top of the atmosphere. The cloud area fraction in a layer of the atmosphere has the standard name cloud_area_fraction_in_atmosphere_layer. [CF-Standard Name]; unit: 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: Pa surface_air_pressure The surface called "surface" means the lower boundary of the atmosphere.[CF-Standard Name]; unit: Pa wind_speed-at10m (maximum) wind_speed-at10m (maximum) [CF-Standard Name-vertical_coordinate]; unit: m s-1 wind_speed-at10m Speed is the magnitude of velocity. 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.) The wind speed is the magnitude of the wind velocity. [CF-Standard Name-vertical_coordinate]; unit: m s-1 eastward_wind-at10m "Eastward" indicates a vector component which is positive when directed eastward (negative westward). 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-vertical_coordinate]; unit: m s-1 air_temperature Air temperature is the bulk temperature of the air, not the surface (skin) temperature. [CF-Standard Name]; unit: K eastward_wind "Eastward" indicates a vector component which is positive when directed eastward (negative westward). 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 northward_wind-at10m "Northward" indicates a vector component which is positive when directed northward (negative southward). 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-vertical_coordinate]; unit: m s-1 wind_speed Speed is the magnitude of velocity. 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.) The wind speed is the magnitude of the wind velocity.[CF-Standard Name]; unit: m s-1 soil_temperature Soil temperature is the bulk temperature of the soil, not the surface (skin) temperature. [CF-Standard Name]; unit: K wind_speed_of_gust-at10m Speed is the magnitude of velocity. 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.) The wind speed is the magnitude of the wind velocity. A gust is a sudden brief period of high wind speed. In an observed timeseries of wind speed, the gust wind speed can be indicated by a cell_methods of maximum for the time-interval. In an atmospheric model which has a parametrised calculation of gustiness, the gust wind speed may be separately diagnosed from the wind speed. [CF-Standard Name-vertical_coordinate]; unit: m s-1 northward_wind "Northward" indicates a vector component which is positive when directed northward (negative southward). 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 large_scale_rainfall_amount "Amount" means mass per unit area.[CF-Standard Name]; unit: kg m-2 atmosphere_convective_available_potential_energy Convective(ly) available potential energy (often abbreviated CAPE) is a stability measure calculated by integrating the positive temperature difference between the surrounding atmosphere and a parcel of air lifted adiabatically from a given starting height to its equilibrium level. A coordinate variable of original_air_pressure_of_lifted_parcel should be specified to indicate the starting height of the lifted parcel. CAPE exists under conditions of potential instability, and measures the potential energy per unit mass that would be released by the unstable parcel if it were able to convect upwards to equilibrium. [CF-Standard Name]; unit: J kg-1 wind_speed_without_gust-at10m not filled; unit: m s-1 precipitation_amount "Amount" means mass per unit area. "Precipitation" in the earths atmosphere means precipitation of water in all phases. [CF-Standard Name]; unit: kg m-2 dew_point_temperature Dew point temperature is the temperature at which a parcel of air reaches saturation upon being cooled at constant pressure and specific humidity. [CF-Standard Name]; unit: K convective_snowfall_amount "Amount" means mass per unit area.[CF-Standard Name]; unit: kg m-2 NetCDF 8063522 https://www.wdc-climate.de/ui/entry?acronym=coastDat_COSMO-CLM_GB0028 information collection n/a None