Impacts of small dams on stream temperature

Small, surface-release dams are ubiquitous features of the landscape that typically slow water flow and decrease canopy cover through impounded reaches, potentially increasing stream temperatures. However, reported effects of small dams on water temperature are variable, likely due to differences in...

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Autores principales: Peter A. Zaidel, Allison H. Roy, Kristopher M. Houle, Beth Lambert, Benjamin H. Letcher, Keith H. Nislow, Christopher Smith
Formato: article
Lenguaje:EN
Publicado: Elsevier 2021
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Acceso en línea:https://doaj.org/article/4093dd8f53174d9db8e3a74b13f0fe0e
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spelling oai:doaj.org-article:4093dd8f53174d9db8e3a74b13f0fe0e2021-12-01T04:28:13ZImpacts of small dams on stream temperature1470-160X10.1016/j.ecolind.2020.106878https://doaj.org/article/4093dd8f53174d9db8e3a74b13f0fe0e2021-01-01T00:00:00Zhttp://www.sciencedirect.com/science/article/pii/S1470160X20308165https://doaj.org/toc/1470-160XSmall, surface-release dams are ubiquitous features of the landscape that typically slow water flow and decrease canopy cover through impounded reaches, potentially increasing stream temperatures. However, reported effects of small dams on water temperature are variable, likely due to differences in landscape and dam characteristics. To quantify the range of thermal effects of small dams, we deployed continuous temperature loggers for one to four years at 30 dam sites across a range of environmental settings throughout Massachusetts (USA). Most dams (67%) warmed downstream waters, with August mean temperatures 0.20–5.25 °C higher than upstream. Downstream temperatures cooled with increased distance from the dam at 68% of sites, such that the warmest temperatures were observed closest to the dam. Where there was both a significant downstream warming effect and cooling pattern (seven sites), elevated temperatures persisted for an average of 1.31 km downstream of the dam. Dams with impoundments that caused the greatest relative widening of the stream channel and those on coldwater streams had the most warming, while streams with short dams in forested watersheds cooled most quickly downstream of the dam. Flow had a homogenizing effect on water temperatures at over half of the sites, whereby summer thermal impacts were more pronounced (e.g., more warming, faster cooling rates) under periods of lower flows. Downstream warming may reduce habitat for coldwater fishes and invertebrates, particularly where dams shift coldwater/coolwater habitat to warmwater. These results suggest that dam removal may mitigate elevated stream temperatures and increase ecosystem resilience in the face of a changing climate via restoration of critical coldwater habitats.Peter A. ZaidelAllison H. RoyKristopher M. HouleBeth LambertBenjamin H. LetcherKeith H. NislowChristopher SmithElsevierarticleThermal regimeColdwater habitatDam removalRiver restorationWater qualityEcologyQH540-549.5ENEcological Indicators, Vol 120, Iss , Pp 106878- (2021)
institution DOAJ
collection DOAJ
language EN
topic Thermal regime
Coldwater habitat
Dam removal
River restoration
Water quality
Ecology
QH540-549.5
spellingShingle Thermal regime
Coldwater habitat
Dam removal
River restoration
Water quality
Ecology
QH540-549.5
Peter A. Zaidel
Allison H. Roy
Kristopher M. Houle
Beth Lambert
Benjamin H. Letcher
Keith H. Nislow
Christopher Smith
Impacts of small dams on stream temperature
description Small, surface-release dams are ubiquitous features of the landscape that typically slow water flow and decrease canopy cover through impounded reaches, potentially increasing stream temperatures. However, reported effects of small dams on water temperature are variable, likely due to differences in landscape and dam characteristics. To quantify the range of thermal effects of small dams, we deployed continuous temperature loggers for one to four years at 30 dam sites across a range of environmental settings throughout Massachusetts (USA). Most dams (67%) warmed downstream waters, with August mean temperatures 0.20–5.25 °C higher than upstream. Downstream temperatures cooled with increased distance from the dam at 68% of sites, such that the warmest temperatures were observed closest to the dam. Where there was both a significant downstream warming effect and cooling pattern (seven sites), elevated temperatures persisted for an average of 1.31 km downstream of the dam. Dams with impoundments that caused the greatest relative widening of the stream channel and those on coldwater streams had the most warming, while streams with short dams in forested watersheds cooled most quickly downstream of the dam. Flow had a homogenizing effect on water temperatures at over half of the sites, whereby summer thermal impacts were more pronounced (e.g., more warming, faster cooling rates) under periods of lower flows. Downstream warming may reduce habitat for coldwater fishes and invertebrates, particularly where dams shift coldwater/coolwater habitat to warmwater. These results suggest that dam removal may mitigate elevated stream temperatures and increase ecosystem resilience in the face of a changing climate via restoration of critical coldwater habitats.
format article
author Peter A. Zaidel
Allison H. Roy
Kristopher M. Houle
Beth Lambert
Benjamin H. Letcher
Keith H. Nislow
Christopher Smith
author_facet Peter A. Zaidel
Allison H. Roy
Kristopher M. Houle
Beth Lambert
Benjamin H. Letcher
Keith H. Nislow
Christopher Smith
author_sort Peter A. Zaidel
title Impacts of small dams on stream temperature
title_short Impacts of small dams on stream temperature
title_full Impacts of small dams on stream temperature
title_fullStr Impacts of small dams on stream temperature
title_full_unstemmed Impacts of small dams on stream temperature
title_sort impacts of small dams on stream temperature
publisher Elsevier
publishDate 2021
url https://doaj.org/article/4093dd8f53174d9db8e3a74b13f0fe0e
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AT allisonhroy impactsofsmalldamsonstreamtemperature
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AT benjaminhletcher impactsofsmalldamsonstreamtemperature
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