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Dam-induced impacts on the water temperature of the Charef River (North East Algeria)
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The Charef sub-watershed (1735 km
2
, 200000
inhabitants) is part of the large Seybouse basin (North-east of
Algeria). It contains several reservoirs, of which the Charef dam is the
largest (157 10
6
m
3
). The main
objective of this work was to assess downstream thermal responses to the
dam and examine the impacts of the water flow and the water residence
time (WRT) on the variability in water downstream temperature. During
the period January–December 2012, the hydrological parameters of the
Charef dam’s waters varied greatly on a spatiotemporal scale. Salinity,
EC, TDS, and water flow all respond similarly, with larger magnitudes in
waters upstream of the dam than downstream, whatever the season.
Moreover, salinity and EC have a significant positive correlation with
temperature, but flow rate and precipitation have a negative one.
Besides, TDS and temperature do not have a statistically significant
relationship. In terms of flux, the Charef dam retains 59% and 56% of
the incoming water and TDS fluxes, respectively. Furthermore, the
temperature of the upstream waters is on average higher than that of the
downstream in 83% of samples. During the dry season, the thermal
response of the waters downstream of the Charef dam can exceed 2°C
(downstream cooling). Despite being a small dam, the WRT (2.3 years) in
the Charef dam has a significant impact on the downstream water
temperature. These temperature changes downstream of dams may cause
significant physicochemical and biological issues. This research applies
to a critical issue in hydrology: the potential impact of dam-induced
changes to water residence time and flow regimes on thermal dynamics,
which in turn affect downstream ecosystems. Some restoration practices
like increasing discharges during dry seasons could mitigate thermal
impacts and minimize negative impacts. Also, riparian cover restoration
could enhance riparian habitat, stabilize banks, and maintain cooler
stream temperatures.
Title: Dam-induced impacts on the water temperature of the Charef River (North East Algeria)
Description:
The Charef sub-watershed (1735 km
2
, 200000
inhabitants) is part of the large Seybouse basin (North-east of
Algeria).
It contains several reservoirs, of which the Charef dam is the
largest (157 10
6
m
3
).
The main
objective of this work was to assess downstream thermal responses to the
dam and examine the impacts of the water flow and the water residence
time (WRT) on the variability in water downstream temperature.
During
the period January–December 2012, the hydrological parameters of the
Charef dam’s waters varied greatly on a spatiotemporal scale.
Salinity,
EC, TDS, and water flow all respond similarly, with larger magnitudes in
waters upstream of the dam than downstream, whatever the season.
Moreover, salinity and EC have a significant positive correlation with
temperature, but flow rate and precipitation have a negative one.
Besides, TDS and temperature do not have a statistically significant
relationship.
In terms of flux, the Charef dam retains 59% and 56% of
the incoming water and TDS fluxes, respectively.
Furthermore, the
temperature of the upstream waters is on average higher than that of the
downstream in 83% of samples.
During the dry season, the thermal
response of the waters downstream of the Charef dam can exceed 2°C
(downstream cooling).
Despite being a small dam, the WRT (2.
3 years) in
the Charef dam has a significant impact on the downstream water
temperature.
These temperature changes downstream of dams may cause
significant physicochemical and biological issues.
This research applies
to a critical issue in hydrology: the potential impact of dam-induced
changes to water residence time and flow regimes on thermal dynamics,
which in turn affect downstream ecosystems.
Some restoration practices
like increasing discharges during dry seasons could mitigate thermal
impacts and minimize negative impacts.
Also, riparian cover restoration
could enhance riparian habitat, stabilize banks, and maintain cooler
stream temperatures.
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