stream flow prediction than the fixed ratio error propagation, particularly during high
flow, that is, heavy rainfall periods.
13.4 CONCLUSIONS
As satellite-based precipitation estimates are increasingly applied to atmospheric and
hydrological studies at various space–time scales, the quantification of scale-based
FIGURE 13.8 Uncertainty estimation of stream flow prediction corresponding to 95 percentile confidence using rainfall error propagation: (a) fixed rainfall error 50% and (b) scaledependent rainfall error according to Equation (13.1). The red dots are mean of the 100
ensemble streamflow sequences simulated from satellite rainfall estimates.
262
SPATIOTEMPORAL SCALES OF REMOTE SENSING PRECIPITATION
flow, that is, heavy rainfall periods.
13.4 CONCLUSIONS
As satellite-based precipitation estimates are increasingly applied to atmospheric and
hydrological studies at various space–time scales, the quantification of scale-based
FIGURE 13.8 Uncertainty estimation of stream flow prediction corresponding to 95 percentile confidence using rainfall error propagation: (a) fixed rainfall error 50% and (b) scaledependent rainfall error according to Equation (13.1). The red dots are mean of the 100
ensemble streamflow sequences simulated from satellite rainfall estimates.
262
SPATIOTEMPORAL SCALES OF REMOTE SENSING PRECIPITATION