Sentence examples for runoff duration from inspiring English sources

An exponential model was derived to mirror the relationship between instantaneous sediment trapping efficiency and runoff duration, with findings that STC is closely related to the initial efficiency and attenuation coefficients.

Increasing urban land cover increased runoff duration and the likelihood that a rainfall event would result in runoff, but did not increase the time to peak discharge of episodic runoff.

In general, the studied variables explained 50 90% of the EMLs but only 30 60% of the EMCs, with runoff duration having an important role in most of the SMLR models.

Hydrological data was obtained for each event from which includes antecedent dry day, event rainfall, runoff duration, rainfall intensity and runoff rate.

Such response characteristics are often indicative of a specific watershed and how its response differs from others; examples include common descriptors of the hydrograph shape such as the runoff duration curve and the time to peak flow (Shamir et al., [2005]).

For all PM loadings, k0 (3.1 × 10−1 mm/s) was reduced to 10−4 mm/s for runoff loading durations from 100 to 250 h, respectively.

Our observations indicate that biochar-amended biofilters are able to treat (to comply with recreational water quality standard for FIB) urban stormwater runoff for the duration of the experiment.

It is assumed that the amount of runoff represents certain duration of water contact.

Calculations of coefficients were made on 5-year average-outs both for runoff and for duration (total days) of ECM.

Study of dynamic schemes of additional types of 4, 5, 8, 12 revealed that these types of ECM cause the direct inflow of moist air to the territory of Central Asia and, therefore, influence precipitation and runoff; moreover the duration of effects of these types in days increases in the last decade.

Results are analyzed for changes in mean annual flow, peak runoff timing, and duration of low flow conditions to highlight which watersheds are most resilient to climate warming within a region, and how individual watersheds may be affected by changes to runoff quantity and timing.