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Responses of natural runoff to recent climatic variations in the Yellow River basin, China

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Academic year: 2020

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Figure

Fig. 1. The study area and sub-basins.
Fig.4.SWAT-simulatedannualnaturalstreamflowattheHuayuankou station from 1960 to 2011. The horizontal lines showthe SWAT-simulated mean annual streamflow in the baseline (1960–1990), low-flow (1991–2002), and recent (2003–2011) periods.
Table 2. Performance of the SWAT model in the calibration (1960–1979) and validation (1980–2000) periods.
Table 3. Mean annual streamflows estimated from the SWAT model and derived from the runoff elasticities in the baseline (1960–1990),low-flow (1991–2002), and recent (2003–2011) periods.

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