Most of western China is prone to large precipitation variability (>5), particularly in the Tarim River basin in northwest China (>10).
All scenarios predict larger precipitation amount averaged over the entire domain with the exception of GSE scenario.
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.
There is typically a time lag following a large precipitation event and resultant change in the discharge concentration of sulfate and chloride.
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.
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.
The generation of large raindrops leads to the fast terminal velocity of the hydrometeors and a large precipitation flux in the one-moment bulk scheme (Fig. 5e), which, in turn, leads to the large precipitation flux at the surface and the fast onset of surface precipitation.
We used eight large precipitation datasets (more than 30 years) as input for a large scale hydrological and hydrodynamic model (MGB-IPH).
Water level responses that occur within hours of the larger precipitation events are attributed to focused groundwater recharge in near field braided stream channels.
