Document Type

Article

Language

eng

Publication Date

11-8-2015

Publisher

The Royal Society

Source Publication

Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences

Source ISSN

1471-2946

Abstract

Stream runoff is perhaps the most poorly represented process in ecohydrological stochastic soil moisture models. Here we present a rainfall-runoff model with a new stochastic description of runoff linked to soil moisture dynamics. We describe the rainfall-runoff system as the joint probability density function (PDF) of rainfall, soil moisture and runoff forced by random, instantaneous jumps of rainfall. We develop a master equation for the soil moisture PDF that accounts explicitly for a general state-dependent rainfall-runoff transformation. This framework is then used to derive the joint rainfall-runoff and soil moisture-runoff PDFs. Runoff is initiated by a soil moisture threshold and a linear progressive partitioning of rainfall based on the soil moisture status. We explore the dependence of the PDFs on the rainfall occurrence PDF (homogeneous or state-dependent Poisson process) and the rainfall magnitude PDF (exponential or mixed-exponential distribution). We calibrate the model to 63 years of rainfall and runoff data from the Upper Little Tennessee watershed (USA) and show how the new model can reproduce the measured runoff PDF.

Comments

Accepted version. Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, Vol. 471, No. 2183 (November 8, 2015). DOI. © 2015 The Royal Society. Used with permission.

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