2021
DOI: 10.1029/2021gh000438
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Comparative Study on Temperature Response of Hydropower Development in the Dry‐Hot Valley

Abstract:  The difference of surface temperature affected by reservoirs was compared in dry-hot and non-dry-hot valleys. To facilitate comparison of the different downstream river temperature changes, downstream river temperature change index was established. The reservoir effect change intensity was established to explore how reservoirs regulate the surface temperature in the surrounding areas.

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Cited by 3 publications
(3 citation statements)
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“…This led to notable changes in the water temperature rhythms at the PZH hydrological station, the first downstream control station of these reservoirs. According to this study, these changes, characterized by phase shifts in water temperature curves and a consistent increase in water temperature homogenization, underscore the significant role of cascade hydropower development in altering the thermal regime of the Jinsha River's middle reaches [67,70]. Additionally, the correlation between water and air temperatures downstream of cascade reservoirs in the middle reaches of the Jinsha River weakened significantly post-construction, indicating the potential for cascade reservoirs to disrupt the downstream air-water temperature synchronization [32,56].…”
Section: The Phase Offset Time Indexmentioning
confidence: 57%
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“…This led to notable changes in the water temperature rhythms at the PZH hydrological station, the first downstream control station of these reservoirs. According to this study, these changes, characterized by phase shifts in water temperature curves and a consistent increase in water temperature homogenization, underscore the significant role of cascade hydropower development in altering the thermal regime of the Jinsha River's middle reaches [67,70]. Additionally, the correlation between water and air temperatures downstream of cascade reservoirs in the middle reaches of the Jinsha River weakened significantly post-construction, indicating the potential for cascade reservoirs to disrupt the downstream air-water temperature synchronization [32,56].…”
Section: The Phase Offset Time Indexmentioning
confidence: 57%
“…Topography and geomorphology impact the meteorological and hydrological conditions of rivers, which in turn affect water temperature. In the Jinsha River basin, for example, the upper reaches are marked by high terrain and colder climate, while the middle reaches feature a dry-warm valley climate with higher temperatures [67,68], which explains that the value of ∆T in the middle and upper reaches of the Jinsha River is consistently greater than 0 • C/100 km, indicating a longitudinal warming trend in water temperature.…”
Section: The Phase Offset Time Indexmentioning
confidence: 99%
“…Laxiwa hydropower station is 8.6 km away from the downstream Nina hydropower station, and is the second largest cascade hydropower station in the upper reaches of the Yellow River, with a total storage capacity of 10.79 Â 10 8 m 3 . The annual power generation of 102.23 Â 10 8 kW•h is about five times that of the Longyangxia hydropower station (Wang et al 2021).…”
Section: Study Area and Datamentioning
confidence: 98%