Sentence examples for recession coefficient from inspiring English sources

The late exponential recession coefficient decreases with the conduit diameter and conduit storage.

K2, the recession coefficient of the lower groundwater box, is moderately sensitive to most objective functions and plays a lesser role for the objective functions focusing on runoff peaks (S PQ, S PT ).

This phenomenon also often leads to a non-standard recession behaviour, a so called "convex recession", i.e. an increase in the recession coefficient during flow recession, which in turn might be used as an indicator for conduit restricted aquifers.

This study concerns the relationship between the power law recession coefficient k (in −dQ/dt = kQα, Q being discharge at the basin outlet) and past average discharge QN (where N is the temporal distance from the center of the selected time span in the past to the recession peak), which serves as a proxy for past storage state of the basin.

We noticed that the Logarithmic transformation of the HBV recession coefficients leads to 20% improvement of the convergence speed.

The analytical formulae provided in this study link aquifer properties with hydrograph recession coefficients, and provide quantitative characterisation of the spatial and temporal variations of the water table.

The system consists of two conceptual groundwater boxes: an upper box with two outflows (fast runoff Q0 and delayed runoff Q1) with different recession coefficients, and a lower box with one outflow (slow baseflow Q 2 ).

Numerous different recession coefficients α were observed: ∼0.2 to 0.8 d−1 (presumably main conduit system), 0.004 d−1 (fractured matrix), 0.0009 d−1 (plateau caused by flow threshold being exceeded), plus many intermediate values.

The spring displays complex recession behaviour, exhibiting exponential (coefficient α) and linear (coefficient β) recession periods.

The results presented provide in-depth insights on the reasons behind the divergence in Okun's coefficient during the recession and across countries.

The analytical pdfs are defined by four key dimensionless parameters which characterize temporal variability of wetland hydrologic conditions: scaled aridity index, mean daily stage jump (r), relative rate constants for the two recession processes, and wetland shape coefficient.