Climate-analogy mapping as a tool to develop a temporally-adaptive hydrological model of the Meuse basin for more reliable predictions under change

The future hydrological response of a river system is often predicted using hydrological models that are calibrated on past observations. By using static model parameters it is assumed that hydrological systems do not change in time. For long-term predictions, this is in clear contrast with the notion that vegetation actively adapts its root...