The thermal regime of abandoned channels: a preliminary analysis towards a water temperature model for the Allier River, France.
Résumé
The growing recognition of the ecological and water quality significance of river water temperature led to a large
number of studies assessing thermal processes in streams and rivers. Yet, thermal processes in abandoned channels,
which play an important role in maintaining water quality and biological diversity in fluvial corridors, have received
minor attention. This study evaluates water temperature regimes in three abandoned channels of the Allier River,
France, and quantifies the regime sensitivity to climatic (air temperature) and hydrological (surface and subsurface
flow) influence. Analysis was conducted at annual and daily scales, and at two distinct sections of each abandoned
channel: (i) the downstream section, which is well connected to the main stream channel, and (ii) the upstream
section, which is poorly connected to the main stream channel and hence subject to greater influence of subsurface
flow. Annual and daily water temperature regimes for all channels and sections were classified based on relative
differences in the ‘shape’ (timing) and the ‘magnitude’ (size) of the thermographs. The climatic and hydrological
sensitivity of water temperature regimes was quantified using a Sensitivity Index. Analysis at the annual scale
revealed relative similarity in patterns of thermal response over time, with clear differentiation between upstream
and downstream channel sections in all sites. Water temperature regimes in the upstream channel sections were
strongly linked to subsurface water temperature in terms of both timing and size of the annual thermograph; water
temperature regimes in the downstream channel sections were more sensitive to air and river water temperature,
especially regarding the timing of the annual regimes. Although annual regimes of water temperature exhibited
distinct patterns that were similar across sites and over time, analysis of daily water temperature regimes revealed
broad differences within and between sites. Day-to-day sequencing of similar classes of diurnal regime varied
over the year, and between consecutive years. Furthermore, the direction and strength of climatic and hydrological
sensitivity of daily water temperature regimes varied over time, and between sites. Temporal and spatial variability
of diurnal regime class sequencing and sensitivity indicates complex climatic and hydrologic influence on water
temperature variability, strongly related to the morphology of each site. Identifying thresholds of climatic and
hydrologic influence, as well as temporal and spatial variations in the strength of climatic and hydrologic influence,
is the key to further development of predictive models of water temperature in the abandoned channels of the Allier
River.
Domaines
Etudes de l'environnement
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EGU2014-Resume.pdf (41.07 Ko)
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EGU2014_presentation.pdf (6.37 Mo)
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