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Quantifying projected changes in runoff variability and flow regimes of the Fraser River Basin, British Columbia

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Figure

Figure 1. (a) Digital elevation model of the FRB with identifica-tion of sub-basins: upper Fraser (UF), Quesnel (QU), Chilko (CH),Thompson–Nicola (TN) and Fraser at Hope (LF)
Table 1. Characteristics of the Water Survey of Canada (WSC) hydrometric stations and three geoclimatic regions within the FRB (Déry etal., 2012)
Table 2. Decomposition of the key drivers affecting cold season runoff changes in the 2080s
Figure 3. Rate of change of mean and interannual variability withwarming for precipitation (a, c, e, g) and runoff (b, d, f, h) duringthe cold season
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