Abstract
We used a calibrated coupled climate-hydrological model to simulate Meuse discharge over the late Holocene (4000-3000 BP and 1000-2000 AD). We then used this model to simulate discharge in the twenty-first century under SRES emission scenarios A2 and B1, with and without future land use change. Mean discharge and medium-sized high-flow (e. g. Q
Original language | English |
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Pages (from-to) | 179-202 |
Journal | Climatic Change |
Volume | 106 |
Issue number | 2 |
DOIs | |
Publication status | Published - 2011 |