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wdc-climate.de:3889895 eng; USA collection Hagemannetal2020 Dr. Stefan Hagemann Helmholtz-Zentrum Hereon www.hereon.de pointOfContact Dr. Stefan Hagemann Helmholtz-Zentrum Hereon www.hereon.de pointOfContact 2026-02-04T10:21:32 ISO 19115 ISO 19115-2:2009 Forcing for HD Model (JSBACH, MPI-HM) and HD Model discharge from Hagemann et al. (2020) 2021-09-03 publication 1 Hagemannetal2020 doi:10.26050/WDCC/Hagemannetal2020 Dr. Stefan Hagemann Helmholtz-Zentrum Hereon www.hereon.de Email: stefan.hagemann@hereon.de principalInvestigator Dr. Stefan Hagemann Helmholtz-Zentrum Hereon www.hereon.de Email: stefan.hagemann@hereon.de author Dr. Tobias Stacke Helmholtz-Zentrum Hereon www.hereon.de Email: tobias.stacke@mpimt.mpg.de author WDC Climate at DKRZ publisher The data of this experiment have been used in (Hagemann et al., 2020). It comprise daily data of surface runoff and subsurface runoff (drainage) from JSBACH and MPI-HM and simulated daily discharges (river runoff). To generate river runoff, the Hydrological discharge (HD) model (Hagemann et al., 2020; Hagemann and Ho-Hagemann, 2021) was used that was operated at 5 arc minutes horizontal resolution. Different to the published version of HD model parameters (5.0) on Zenodo, an earlier version (4.0) of flow directions and model parameters has been used that is provided as an auxiliary data file. The HD model was set up over the European domain covering the land areas between -11°W to 69°E and 27°N to 72°N. First, the respective forcing data of surface and sub-surface runoff were interpolated to the HD model domain using conservative remapping. Then, daily discharges were simulated with the HD model for the period 1979-2009 (1999-2009 for HD5-MESCAN). In addition, daily discharges were analogously simulated using only JSBACH forcing with the global 0.5° version 1.10 of the HD model. The associated flow directions and model parameters of vs. 1.10 are provided as an auxiliary data file. The HD forcing data are: a) HD5-JSBACH In order to generate daily input fields of surface runoff and drainage, the land surface scheme JSBACH (vs. 3 + frozen soil physics; (Ekici et al., 2014)) was forced globally at 0.5° with daily atmospheric forcing data based on the Interim Re-Analysis of the European Centre for Medium-Range Weather Forecast (ERA-Interim; (Dee et al., 2011)). These forcing data are bias-corrected (see (Beer et al., 2014)) towards the so-called WATCH forcing data (WFD; (Weedon et al., 2011)) that have been generated in the EU project WATCH. b) HD5-MPIHM The MPI-M hydrology model MPI-HM (Stacke and Hagemann, 2012) was driven by daily WATCH forcing data based on ERA-Interim (WFDEI; (Weedon et al., 2014)) from 1979-2009 to generate daily input fields of surface runoff and drainage at global 0.5° resolution. c) HD5-MESCAN Six hourly data of surface runoff and drainage (variable name: percolation) were retrieved from the MESCAN-SURFEX regional surface reanalysis (Bazile et al., 2017) created in the EU project UERRA (Uncertainties in Ensembles of Regional ReAnalysis; www.uerra.eu). SURFEX (Masson et al., 2013) is a land surface platform that was driven by atmospheric forcing at 5.5 km. The forcing comprises 24h-precipitation, near-surface temperature and relative humidity analyzed by the MESCAN surface analysis system as well as radiative fluxes and wind downscaled at 5.5 km from the 3DVar re-analysis conducted with the HARMONIE system at 11 km (Ridal et al., 2017). The latter has been generated using six-hourly fields of the ERA-Interim reanalysis as boundary conditions and covers a domain comprising Europe and parts of the Atlantic, which is similar to the European domain of the Coordinated Downscaling Experiment (CORDEX) at 11 km. Dr. Stefan Hagemann Helmholtz-Zentrum Hereon www.hereon.de pointOfContact NetCDF Discharge Subsurface runoff Surface runoff river runoff CC-BY-4.0: Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ eng; USA -11.0 69.0 27.0 72.0 1979-01-01 2009-12-31 water_volume_transport_in_river_channel The water flux or volume transport in rivers is the amount of water flowing in the river channel and flood plain. "Water" means water in all phases. [CF-Standard Name]; unit: not filled surface_runoff_flux The surface called "surface" means the lower boundary of the atmosphere. Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: not filled water_volume_transport_in_river_channel The water flux or volume transport in rivers is the amount of water flowing in the river channel and flood plain. "Water" means water in all phases. [CF-Standard Name]; unit: not filled subsurface_runoff_flux Runoff is the liquid water which drains from land. If not specified, "runoff" refers to the sum of surface runoff and subsurface drainage. In accordance with common usage in geophysical disciplines, "flux" implies per unit area, called "flux density" in physics. [CF-Standard Name]; unit: not filled NetCDF 32149 https://www.wdc-climate.de/ui/entry?acronym=Hagemannetal2020 information collection n/a None