4.6 Article

Using equilibrium temperature to assess thermal disturbances in rivers

Journal

HYDROLOGICAL PROCESSES
Volume 29, Issue 19, Pages 4350-4360

Publisher

WILEY
DOI: 10.1002/hyp.10489

Keywords

water temperature; equilibrium temperature; thermal regime; dams; hydropower; Noguera Pallaresa; Ebro basin

Funding

  1. Biodiversity Conservation Plan of ENDESA S.A., within A3 project 'Analysis of the Effects of Global Change on Water Resources and Potential Ecological Status of Water Bodies in Basins of High Hydroelectrical Activity (Noguera Pallaresa, Lleida, Spain)'
  2. Economy and Knowledge Department of the Catalan Government through Consolidated Research Groups: RIUS-Fluvial Dynamics Research Group [2014 SGR 645]
  3. Economy and Knowledge Department of the Catalan Government through Consolidated Research Groups: Catalan Institute for Water Research [2014 SGR 291]

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Flow regulation is widely known to modify the thermal regime of rivers. Here, we examine the sensitivity of an empirical approach, the Equilibrium Temperature Concept (ETC), to detect both the effects of hydraulic infrastructures on the annual thermal cycle and the recovery of the thermal equilibrium with the atmosphere. Analysis was undertaken in a Pyrenean river (the Noguera Pallaresa, Ebro basin) affected by a series of reservoirs and hydropower plants. Equilibrium temperature (T-e) is defined as the water temperature (T-w) at which the sum of all heat fluxes is zero. Based on the assumption of a linear relationship between T-e and T-w, we identified changes in the T-e-T-w regression slope, used as an indicator of a thermal alteration in river flow. We also assessed the magnitude of the alteration by examining the regression slope and its statistical significance. Variations in the regression parameters were used as indicators of the influence of factors other than atmospheric conditions on water temperature. Observed T-w showed a linear relationship with T-e at all river stations. However, the slopes of the T-e-T-w relationship appeared to be lower in the reaches downstream from hydraulic infrastructures, particularly below large dams. A seasonal analysis indicated that T-e-T-w relationships had higher slopes and lower p-values during autumn, while no significant differences were found at other seasons. Although thermal characteristics did not strongly depend on atmospheric conditions downstream of hydraulic infrastructures, the river recovered to pre-alteration conditions with distance downstream, indicating the natural tendency of water to attain thermal equilibrium with the atmosphere. Accepting associated uncertainties, mostly because of the quality of the data and the lack of consideration of other factors influencing the thermal regime (e.g. discharge), ETC appears to be a simple and effective method to identify thermal alterations in regulated rivers. Copyright (c) 2015 John Wiley & Sons, Ltd.

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