In order to better understand the global coastal systems and the dangers and risks associated with them, it is important to examine the atmosphere, the land, hydrology, the ocean and especially their interactions
For the Helsinki Commission (HELCOM), annual waterborne basin inflows of total nitrogen (N) and total phosphorus (P) were compiled for the seven main Baltic Sea sub-basins (Sect. 1.1). In order to allow
1 Dataset description
In ocean model or Earth System model applications, the riverine freshwater inflow is an important flux affecting salinity and marine stratification in coastal areas. However, in
For the Helsinki Commission (HELCOM), annual waterborne basin inflows of total nitrogen (N) and total phosphorus (P) were compiled for the seven main Baltic Sea sub-basins (Sect. 1.1). In order to allow
Under the heading of the OSPAR convention (Sect. 1.1), the IGC-EMO database of daily freshwater inflows and nutrient loads was compiled by van Leeuwen and Lenhart (2021), which covers the major rivers
1 Dataset description In ocean model or Earth System model applications, the riverine freshwater inflow is an important flux affecting salinity and marine stratification in coastal areas. However, in climate
Model runs over Europe were conducted within the ESM project (www.esm-project.net/) for the Frontier Simulations supporting the water and matter fluxes from the European landmass to receiving water bodies
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
This experiment comprises data that have been used in Hagemann et al. (submitted). It comprises daily data of surface runoff and subsurface runoff from HydroPy and simulated daily discharges (river runoff)
This datasets contains simulation output for the global hydrological models HydroPy and MPI-HM. Both used meteorological forcing from the GSWP3 dataset for the period 1979-2014 and a 50 years spinup period.
We bias-corrected the original discharge time series simulated by the Hydrological Discharge (HD) model (see respective dataset of Version 1.0 of this experiment) to generate daily bias-corrected discharges
Redistributed annual HELCOM direct nutrient loads of nitrogen (N) and phosphorus (P) into the Baltic Sea at 1/12° resolution from 1901-2019. For the spatial redistribution we used a dataset of bias corrected
Redistributed daily HELCOM riverine nutrient loads of nitrogen (N) and phosphorus (P) into the Baltic Sea at 1/12° resolution from 1901-2019. For the spatial and temporal redistribution we used a dataset
Short description of how the datasets of the experiment are generated. In addition, the changes for the bias corrected discharges in version 1.1 are shortly described.