Towards reconstruction of the flow duration curve: Development of a conceptual framework with a physical basis

79Citations
Citations of this article
101Readers
Mendeley users who have this article in their library.

Abstract

In this paper we investigate the climatic and landscape controls on the flow duration curve (FDC) with the use of a physically-based rainfall-runoff model. The FDC is a stochastic representation of the variability of runoff, which arises from the transformation, by the catchment, of within-year variability of precipitation that can itself be characterized by a corresponding duration curve for precipitation (PDC). Numerical simulations are carried out with the rainfall-runoff model under a variety of combinations of climatic inputs (i.e. precipitation, potential evaporation, including their within-year variability) and landscape properties (i.e. soil type and depth). The simulations indicated that the FDC can be disaggregated into two components, with sharply differing characteristics and origins: the FDC for surface (fast) runoff (SFDC) and the FDC for subsurface (slow) runoff (SSFDC), which included base flow in our analysis. SFDC closely tracked PDC and can be approximated with the use of a simple, nonlinear (threshold) filter model. On the other hand, SSFDC tracked the FDC that is constructed from the regime curve (i.e. mean monthly runoff), which can be closely approximated by a linear filter model. Sensitivity analyses were carried out to understand the climate and landscape controls on each component, gaining useful physical insights into their respective shapes. In particular the results suggested that evaporation from dynamic saturated areas, especially in the dry season, can contribute to a sharp dip at the lower tail of the FDCs. Based on these results, we develop a conceptual framework for the reconstruction of FDCs in ungauged basins. This framework partitions the FDC into: (1) a fast flow component, governed by a filtered version of PDC, (2) a slow flow component governed by the regime curve, and (3) a correction to SSFDC to capture the effects of high evapotranspiration (ET) at low flows. © 2011 Author(s).

References Powered by Scopus

Low flow hydrology: A review

1299Citations
N/AReaders
Get full text

Time distribution of rainfall in heavy storms

501Citations
N/AReaders
Get full text

A process-based diagnostic approach to model evaluation: Application to the NWS distributed hydrologic model

434Citations
N/AReaders
Get full text

Cited by Powered by Scopus

Runoff prediction in ungauged basins: Synthesis across processes, places and scales

377Citations
N/AReaders
Get full text

Patterns of similarity of seasonal water balances: A window into streamflow variability over a range of time scales

183Citations
N/AReaders
Get full text

Smart low flow signature metrics for an improved overall performance evaluation of hydrological models

153Citations
N/AReaders
Get full text

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Cite

CITATION STYLE

APA

Yokoo, Y., & Sivapalan, M. (2011). Towards reconstruction of the flow duration curve: Development of a conceptual framework with a physical basis. Hydrology and Earth System Sciences, 15(9), 2805–2819. https://doi.org/10.5194/hess-15-2805-2011

Readers' Seniority

Tooltip

PhD / Post grad / Masters / Doc 50

67%

Researcher 15

20%

Professor / Associate Prof. 6

8%

Lecturer / Post doc 4

5%

Readers' Discipline

Tooltip

Environmental Science 25

34%

Earth and Planetary Sciences 22

30%

Engineering 22

30%

Agricultural and Biological Sciences 4

5%

Save time finding and organizing research with Mendeley

Sign up for free