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Does nonstationarity in rainfall require nonstationary intensity–duration–frequency curves?

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Figure

Table 1. Selected station locations, population distribution, and hourly and daily data availability.
Figure 2. Schematics of the process flow (blue – input steps, orange – process steps, and green – decision steps)
Figure 3. Spatial distribution of trends, change points, and nonstationarities in rainfall extremes of several durations in nine urbanizedlocations, Southern Ontario (a–g)
Figure 4. DSI estimates of the median (horizontal line within the box plot) and 95 % credible intervals for 100-year return periods ofstationary vs
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