Fig. 3: Dissolved oxygen (DO) and its percent saturation (DO%sat) variability between the flood and non-flood periods and the occurrence of hypoxia and anoxia. | Nature Communications

Fig. 3: Dissolved oxygen (DO) and its percent saturation (DO%sat) variability between the flood and non-flood periods and the occurrence of hypoxia and anoxia.

From: Episodic flooding causes sudden deoxygenation shocks in human-dominated rivers

Fig. 3

A, B Ratios of DO and DO%sat between the flood period (discharge ranked above the 95th percentile threshold) and the non-flood period, i.e., DOflood:DOnon-flood and DO%sat flood:DO%sat non-flood calculated from nationwide 1156 rivers monitored daily from November 8, 2020, to December 31, 2023. C, D Boxplots showing different categories of DOflood:DOnon-flood and DO%sat flood:DO%sat non-flood in rivers with different Strahler orders. EG Locations of sites with at least one occurrence of hypoxia (DO ≤2 mg L−1) or anoxia (DO ≤0.5 mg L−1) during flood events, and these sites were categorized into different rivers with different Strahler orders. Each box shown in panels C, D and F, G represents the interquartile range, the horizontal line is the median and the whiskers are 1.5× the interquartile range. HK Relationships between DOflood:DOnon-flood and NH4+-Nflood: NH4+-Nnon-flood, and between DOflood:DOnon-flood and agricultural and urban land use (within 30 km radius of each site); Relationships between DO%sat flood:DO%sat non-flood and NH4+-Nflood: NH4+-Nnon-flood, and between DO%sat flood:DO%sat non-flood and agricultural and urban land use. These relationships were categorized for rivers with different Strahler orders.

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