DK model 2019 - Calibration statistics

Land-covering hydrostratigraphic model is used by GEUS to perform model calculations with DK model HIP.

Model calculations are a dataset that includes modelled depth for ground-level groundwater, ground-level groundwater, water content in the root zone and water flow in streams. The model calculations have been produced by GEUS using DK model HIP in 100 meters grid for the period since 1990. The model calculations are suitable for screening in connection with water management, climate adaptation, urban planning and more.

Model uncertainty is a data product that includes modelled depth for ground water and water flow in the period 1990-2019. The calculations were performed by GEUS using DK model HIP to show the suitability of HIP model calculations for screening.

Machine learning and uncertainty is a data set that shows nationwide depth to ground-level groundwater in high spatial resolution (10 m-grid) for a typical summer and winter situation as well as associated uncertainties in the period 1991-2025. The calculations have been carried out by GEUS using the DK model HIP and machine learning in order to provide screening data that can support the work on water management, climate adaptation, urban planning and more.

Randterms is a data product containing nationwide model calculations of hydrological conditions in the period 1990-2019, prepared by GEUS using the DK model HIP in the 100 m grid. These boundary conditions are suitable for defining and delimiting local hydrological submodels, as well as for further development of more detailed analyses and mappings for use in detailed planning.

Climate change includes nationwide modelled depth for ground water, water content in the root zone and water flow in streams as well as associated uncertainties in the periods 1991-2020, 2041-2070 and 2071-2100. Calculations for the future are based on the reference period 1991-2020. The calculations were carried out by GEUS using the DK model HIP in a grid with a resolution of 500 m for climate adaptation. Climate change for the depth to ground water can also be found in a grid with a resolution of 100 m.