high-flow periods and is lower in low-flow regions. However, the 95% uncertainty
bound of the simulated runoff as shown in Figure 13.8b is lower than the one
generated from the fixed error ratio case pictured in Figure 13.8a. The first scenario,
scale-dependent error propagation, offers more realistic uncertainty assessment of
FIGURE 13.5 Same as Figure 13.3, expect the error is expressed as percentage (%) of rain
rates.
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SPATIOTEMPORAL SCALES OF REMOTE SENSING PRECIPITATION