Articles | Volume 15, issue 6
Hydrol. Earth Syst. Sci., 15, 1945–1957, 2011
https://doi.org/10.5194/hess-15-1945-2011
Hydrol. Earth Syst. Sci., 15, 1945–1957, 2011
https://doi.org/10.5194/hess-15-1945-2011

Research article 24 Jun 2011

Research article | 24 Jun 2011

Quantifying spatial and temporal discharge dynamics of an event in a first order stream, using distributed temperature sensing

M. C. Westhoff1, T. A. Bogaard1,2, and H. H. G. Savenije1 M. C. Westhoff et al.
  • 1Water Resources Section, Faculty of Civil Engineering and Geosciences, Delft University of Technology, P.O. Box 5048, 2600 GA Delft, The Netherlands
  • 2Centre de Recherche Public Gabriel Lippmann, Department Environment and Agro-Biotechnologies, 4422 Belvaux, Grand-Duchy of Luxembourg

Abstract. Understanding the spatial distribution of discharge can be important for water quality and quantity modeling. Non-steady flood waves can, particularly as a result of short high intensity summer rainstorms, influence small headwater streams significantly. The aim of this paper is to quantify the spatial and temporal dynamics of stream flow in a headwater stream during a summer rainstorm. These dynamics include gains and losses of stream water, the effect of bypasses that become active and hyporheic exchange fluxes that may vary over time as a function of discharge. We use an advection-dispersion model coupled with an energy balance model to simulate in-stream water temperature, which we compare with high resolution temperature observations obtained with Distributed Temperature Sensing. This model was used as a learning tool to stepwise unravel the complex puzzle of in-stream processes subject to varying discharge. Hypotheses were tested and rejected, which led to more insight in the spatial and temporal dynamics in discharge and hyporheic exchange processes. We showed that, for the studied stream infiltration losses increase during a small rain event, while gains of water remained constant over time. We conclude that, eventually, part of the stream water bypassed the main channel during peak discharge. It also seems that hyporheic exchange varies with varying discharge in the first 250 m of the stream; while further downstream it remains constant. Because we relied on solar radiation as the main energy input, we were only able to apply this method during a small summer storm and low flow conditions. However, when additional (artificial) energy is available, the presented method is also applicable in larger streams, during higher flow conditions or longer storms.