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Sub-hourly water temperature data collected across the Nechako Watershed, 2019-2021

Water temperature is actively being monitored along the regulated Nechako River and some of its unregulated tributaries in northern British Columbia (BC) to determine how climate variability, climate change and flow regulation influence water temperatures. The Nechako Watershed, located mainly in th...

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Autores principales: Gilbert, Derek E., Morris, Jeremy E., Kaveney, Anna R., Déry, Stephen J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Elsevier 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9278022/
https://www.ncbi.nlm.nih.gov/pubmed/35845095
http://dx.doi.org/10.1016/j.dib.2022.108425
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author Gilbert, Derek E.
Morris, Jeremy E.
Kaveney, Anna R.
Déry, Stephen J.
author_facet Gilbert, Derek E.
Morris, Jeremy E.
Kaveney, Anna R.
Déry, Stephen J.
author_sort Gilbert, Derek E.
collection PubMed
description Water temperature is actively being monitored along the regulated Nechako River and some of its unregulated tributaries in northern British Columbia (BC) to determine how climate variability, climate change and flow regulation influence water temperatures. The Nechako Watershed, located mainly in the sub-boreal spruce biogeoclimatic zone, spans 47,200 km(2) in area [1]. The regional climate experiences a prominent seasonal cycle in air temperature and precipitation, with subfreezing temperatures and snow accumulating during winter. Waterways therefore experience extended near 0°C water/ice temperatures during the winter season. The accumulation of snow yields snowmelt-generated peaks in discharge during the spring freshet period in unregulated tributaries [2]. Regional studies on climate reveal recent warming trends that are anticipated to persist through the 21(st) century, with a projected mean air temperature increase of ∼2°C by the 2050’s [3]. In response to warming air temperatures, regional water temperatures are also on the rise, with an average warming trend of 0.7°C from 1950 to 2015 [4]. Changing water temperatures are important in understanding ecological and environmental impacts on riverine systems, including aquatic species such as fish (e.g., sockeye salmon (Oncorhynchus nerka), rainbow trout (Oncorhynchus mykiss) and white sturgeon (Acipenser transmontanus), all endemic species to the Nechako Watershed), invertebrates, and micro-organisms. Managing water temperatures during the fish spawning season is crucial as elevated temperatures induce stress and affect reproduction success [5]. Starting with a pilot project in summer of 2019, we expanded in situ monitoring of water temperature to 29 sites; however, for the purposes of this paper, only data from 24 sites are included (some sites have limited data samples or loggers could not be retrieved in the field). Currently, 25 sites are fully operational and collecting data, all deployed to sample and record data at 15-minute intervals starting at the top of the hour. Site data collection occurs at minimum once annually (typically during summer/early fall), along with site and logger maintenance. Field notes are taken to identify any potential issues with data collection, such as loggers dewatering during low flows, duration of logger removal for data collection, and any other environmental concerns that should later be considered during data analysis. The assembled data are useful to build long-term time series of observed water temperatures within the Nechako Watershed and as a baseline for future projects. The data are also used to determine the effectiveness of the Summer Temperature Management Program at the Nechako Reservoir and Skins Lake Spillway [1]. Therefore, these data can be used in the future to better identify the optimal discharge from the reservoir to minimize ecological effects on the watershed.
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spelling pubmed-92780222022-07-14 Sub-hourly water temperature data collected across the Nechako Watershed, 2019-2021 Gilbert, Derek E. Morris, Jeremy E. Kaveney, Anna R. Déry, Stephen J. Data Brief Data Article Water temperature is actively being monitored along the regulated Nechako River and some of its unregulated tributaries in northern British Columbia (BC) to determine how climate variability, climate change and flow regulation influence water temperatures. The Nechako Watershed, located mainly in the sub-boreal spruce biogeoclimatic zone, spans 47,200 km(2) in area [1]. The regional climate experiences a prominent seasonal cycle in air temperature and precipitation, with subfreezing temperatures and snow accumulating during winter. Waterways therefore experience extended near 0°C water/ice temperatures during the winter season. The accumulation of snow yields snowmelt-generated peaks in discharge during the spring freshet period in unregulated tributaries [2]. Regional studies on climate reveal recent warming trends that are anticipated to persist through the 21(st) century, with a projected mean air temperature increase of ∼2°C by the 2050’s [3]. In response to warming air temperatures, regional water temperatures are also on the rise, with an average warming trend of 0.7°C from 1950 to 2015 [4]. Changing water temperatures are important in understanding ecological and environmental impacts on riverine systems, including aquatic species such as fish (e.g., sockeye salmon (Oncorhynchus nerka), rainbow trout (Oncorhynchus mykiss) and white sturgeon (Acipenser transmontanus), all endemic species to the Nechako Watershed), invertebrates, and micro-organisms. Managing water temperatures during the fish spawning season is crucial as elevated temperatures induce stress and affect reproduction success [5]. Starting with a pilot project in summer of 2019, we expanded in situ monitoring of water temperature to 29 sites; however, for the purposes of this paper, only data from 24 sites are included (some sites have limited data samples or loggers could not be retrieved in the field). Currently, 25 sites are fully operational and collecting data, all deployed to sample and record data at 15-minute intervals starting at the top of the hour. Site data collection occurs at minimum once annually (typically during summer/early fall), along with site and logger maintenance. Field notes are taken to identify any potential issues with data collection, such as loggers dewatering during low flows, duration of logger removal for data collection, and any other environmental concerns that should later be considered during data analysis. The assembled data are useful to build long-term time series of observed water temperatures within the Nechako Watershed and as a baseline for future projects. The data are also used to determine the effectiveness of the Summer Temperature Management Program at the Nechako Reservoir and Skins Lake Spillway [1]. Therefore, these data can be used in the future to better identify the optimal discharge from the reservoir to minimize ecological effects on the watershed. Elsevier 2022-06-27 /pmc/articles/PMC9278022/ /pubmed/35845095 http://dx.doi.org/10.1016/j.dib.2022.108425 Text en © 2022 The Author(s) https://creativecommons.org/licenses/by-nc-nd/4.0/This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
spellingShingle Data Article
Gilbert, Derek E.
Morris, Jeremy E.
Kaveney, Anna R.
Déry, Stephen J.
Sub-hourly water temperature data collected across the Nechako Watershed, 2019-2021
title Sub-hourly water temperature data collected across the Nechako Watershed, 2019-2021
title_full Sub-hourly water temperature data collected across the Nechako Watershed, 2019-2021
title_fullStr Sub-hourly water temperature data collected across the Nechako Watershed, 2019-2021
title_full_unstemmed Sub-hourly water temperature data collected across the Nechako Watershed, 2019-2021
title_short Sub-hourly water temperature data collected across the Nechako Watershed, 2019-2021
title_sort sub-hourly water temperature data collected across the nechako watershed, 2019-2021
topic Data Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9278022/
https://www.ncbi.nlm.nih.gov/pubmed/35845095
http://dx.doi.org/10.1016/j.dib.2022.108425
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