Rasmus Vest Nielsen

Malmö experiment 3 demo

This demo visualizes the ongoing work with improving flood forecasting in urban areas by coupling high-resolution hydrological models and hydrodynamic models. River discharge is predicted from HYPE is propergated into MIKE as a boundary conditions. HYPE is using weather forecast X as forcing data, and MIKE is using a perfect forecast from the observed rain intensity according to a rain gauge.
Precipitation data and forecast_mapbox
The data used in the figure above is generated for the sole purpose of showing the general idea.