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There is typically a time lag following a large precipitation event and resultant change in the discharge concentration of sulfate and chloride.
Most of western China is prone to large precipitation variability (>5), particularly in the Tarim River basin in northwest China (>10).
Most of the discharge occurs soon after placement and must consider using water management practices of retention ponds, dilution, and discharge after large precipitation events.
This indicates that the large precipitation volume and large cloud size in the one-moment bulk scheme restrain the cloud particles from reaching the upper layer.
At low θv, large precipitation events (>20 mm) did not result in increased daily simulated runoff + drainage or measured stream flow.
At high or saturating θv, large precipitation events resulted in increased daily simulated runoff + drainage followed by increased measured stream flow within two days.
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The sudden failures which could be dangerous to humans and the environment usually follow extreme events such as large precipitations, earthquakes or volcanic activity.
All scenarios predict larger precipitation amount averaged over the entire domain with the exception of GSE scenario.
Water level responses that occur within hours of the larger precipitation events are attributed to focused groundwater recharge in near field braided stream channels.
Many laboratory experiments (Baker et al. 1987; Williams et al. 1991; Caranti et al. 1991) suggest that dominant positive charge will appear on larger precipitation particles in the lower portion of the mixed-phase region if ice saturation is maintained.
Given the significant amount of riverine DOC exported from agricultural landscapes during severe weather events, our results suggest that changes in climate promote larger precipitation events that would likely enhance the export of terrestrial DOC to receiving water bodies.
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