The hydrological cycle does not appear to be that complicated at first sight. Sea water evaporates and then arrives back at the Earth’s surface in the form of precipitation. There, it evaporates again, infiltrates into the ground, and is transported by rivers back into the sea. This cycle is, however, influenced by complex interactions between the atmosphere, the surface of the Earth, soils, vegetation and groundwater. Scientists from Jülich and Bonn have developed a modelling platform, the Terrestrial Systems Modeling Platform (TSMP), which they use to simulate flows of terrestrial water, energy, and nutrients for large areas like parts of Germany or even Europe.
