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Fig. 4 Sedimentological versus hydrological parameters before and after the 2008 Wenchuan earthquake. Sedimentological versus hydrological parameters before.

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Presentation on theme: "Fig. 4 Sedimentological versus hydrological parameters before and after the 2008 Wenchuan earthquake. Sedimentological versus hydrological parameters before."— Presentation transcript:

1 Fig. 4 Sedimentological versus hydrological parameters before and after the 2008 Wenchuan earthquake. Sedimentological versus hydrological parameters before and after the 2008 Wenchuan earthquake. Relationships between (A) annual water discharge and annual depositional thickness and (B) the proportion of total runoff of >3 mm/day and the percentage of coarse grains (>32 μm). Black lines show the best-fit relationship from linear least-squares regression, and the yellow-shaded regions show 95% confidence intervals, excluding the data from 2012 in (A). The outlier from 2012 may result from high Qw dominated by heavy rainfall in the upstream portions of the Min Jiang River catchment with limited earthquake-triggered landslides (fig. S9). In (B), the relationship may reflect a shift from a supply-limited regime (gray-shaded region) to a transport-limited regime (yellow-shaded region) after the Wenchuan earthquake. Fei Zhang et al. Sci Adv 2019;5:eaav7110 Copyright © 2019 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).

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