Abstract

This paper describes a new application of the Fourier series for a detailed simulation of runoff in a small catchment in dry periods, when the streamflow is significantly impacted by evapotranspiration, particularly during daytime hours. The catchment was considered as a dynamic system, in which evapotranspiration has an impact on the day–night fluctuation of discharges. Measurements of these discharges were accomplished by a high-resolution water-level sensor attached to a V-notch. In parallel, the free water evaporation and also the soil moisture content have been measured nearby. The paper describes three runoff recession episodes in dry periods. Using short time step measurements and calculations, it was not difficult to analyze the diurnal streamflow fluctuations as harmonic waves. An application of the finite Fourier series model (FSM) to a quasi-periodic hydrologic data series clearly shows how the actual evapotranspiration influences surface runoff from small catchments. The method was verified by direct numerical evaluation of the convolution integral. The Fourier transformation works better if the number of discharge points (n) is large. The method allows computing the missing discharges in order to bridge accidental data gaps. The automatic measurement of free water evaporation multiplied by the measured soil water content compared semiquantitatively with the Fourier transformation function derived backward from the discharge hydrograph. Hence, this measurement can, to some extent, substitute the actual evapotranspiration on the catchment scale. The observation has been carried out with a time delay of the stream discharges behind the water evaporation, caused by the unsaturated zone processes and the hydraulic resistance to water flow, both in the saturated zone and in the streambed.

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Acknowledgments

This study was supported within Czech Technological Agency Project TA02020402 Water Regime Optimisation to Mitigate Impacts on Hydrological Extremes. We express our gratitude for this financial support.

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Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 22Issue 8August 2017

History

Received: Oct 16, 2016
Accepted: Mar 9, 2017
Published online: Jun 12, 2017
Published in print: Aug 1, 2017
Discussion open until: Nov 12, 2017

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Full Professor, Dept. of Land Use and Improvement, Faculty of Environmental Sciences, Czech Univ. of Life Sciences Prague, Kamycka 129, 165 00 Prague, Czech Republic (corresponding author). ORCID: https://orcid.org/0000-0003-0221-1031. E-mail: [email protected]
Jitka Peskova [email protected]
Assistant Professor, Dept. of Land Use and Improvement, Faculty of Environmental Sciences, Czech Univ. of Life Sciences Prague, Kamycka 129, 165 00 Prague, Czech Republic. E-mail: [email protected]
Frantisek Dolezal [email protected]
Scientist and Lecturer, Dept. of Water Resources, Faculty of Agrobiology, Food and Natural Resources, Czech Univ. of Life Sciences Prague, Kamycka 129, 165 00 Prague, Czech Republic. E-mail: [email protected]
Hana Bacinova [email protected]
Assistant Professor, Dept. of Land Use and Improvement, Faculty of Environmental Sciences, Czech Univ. of Life Sciences Prague, Kamycka 129, 165 00 Prague, Czech Republic. E-mail: [email protected]
Frantisek Krovak [email protected]
Assistant Professor, Dept. of Land Use and Improvement, Faculty of Environmental Sciences, Czech Univ. of Life Sciences Prague, Kamycka 129, 165 00 Prague, Czech Republic. E-mail: [email protected]
Marketa Mihalikova [email protected]
Assistant Professor, Dept. of Water Resources, Faculty of Agrobiology, Food and Natural Resources, Czech Univ. of Life Sciences Prague, Kamycka 129, 165 00 Prague, Czech Republic. E-mail: [email protected]

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