ANALYSIS OF MULTI-DECADAL (1960-2010) DYNAMICS IN SEDIMENT AND WATER DISCHARGES FROM GLOBAL RIVERS: TEMPORAL VARIABILITY AND INTRA-BASIN CONTROLS
Considerable intra-basin variability in both water and sediment discharge is observed in different regions of the world. A correlation analysis between continental-averaged suspended sediment and water discharge shows that yearly changes in intra-basin precipitation dynamics explain most of the discrepancies between water discharge and suspended sediment. The mechanism proposed and demonstrated here (for the Ganges, Danube and Amazon Rivers) is that regions with high relief and soft lithology will amplify the effect of higher than average precipitation by producing an increase in sediment yield that greatly exceeds increase in water discharge. Preliminary analysis of the effect of sediment variability on large tropical deltas and a new bedload module are also presented.