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Characterising runoff generation processes in a lake-rich thermokarst landscape (Old Crow Flats, Yukon, Canada) using δ18 O, δ2 H and d-excess measurements
(supprimer)
the recession limb of the spring freshet hydrograph provided characteristic patterns of deuterium excess (d-excess) along the Old Crow River. It is shown that river isotope sampling could be used to monitor spatial and temporal variability in runoff generation