Gilbert Derek E, Morris Jeremy E, Kaveney Anna R, Déry Stephen J
Department of Geography, Earth and Environmental Sciences, University of Northern British Columbia, 3333 University Way, Prince George, British Columbia, V2N 4Z9, Canada.
Data Brief. 2022 Jun 27;43:108425. doi: 10.1016/j.dib.2022.108425. eCollection 2022 Aug.
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 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 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 (, rainbow trout ( and white sturgeon (, 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.
目前正在对不列颠哥伦比亚省北部(BC)受管制的尼查科河及其一些未受管制的支流的水温进行积极监测,以确定气候变率、气候变化和流量调节如何影响水温。尼查科流域主要位于亚寒带云杉生物地理气候区,面积达47200平方公里[1]。该地区气候在气温和降水方面呈现出显著的季节性循环,冬季气温低于冰点且有积雪。因此,冬季水道的水温/冰温会在接近0°C的水平持续较长时间。在未受管制的支流中,春季洪水期积雪融化会导致流量出现峰值[2]。关于气候的区域研究表明,近期存在变暖趋势,预计这种趋势将持续到21世纪,到2050年代预计平均气温将升高约2°C[3]。随着气温升高,区域水温也在上升,1950年至2015年期间平均升温趋势为0.7°C[4]。了解水温变化对于理解对河流系统的生态和环境影响非常重要,这些影响包括对鱼类(如红大马哈鱼(、虹鳟(和白鲟(,这些都是尼查科流域的特有物种)、无脊椎动物和微生物等水生物种的影响。在鱼类产卵季节管理水温至关重要,因为水温升高会引发压力并影响繁殖成功率[5]。从2019年夏季的一个试点项目开始,我们将水温的现场监测扩展到了29个地点;然而,在本文中,仅纳入了24个地点的数据(一些地点的数据样本有限,或者无法在现场找回记录器)。目前,有25个地点全面投入运行并收集数据,所有这些地点均从整点开始每隔15分钟进行一次数据采样和记录。每个地点的数据收集每年至少进行一次(通常在夏季/初秋),同时进行地点和记录器的维护。记录现场笔记以识别数据收集过程中的任何潜在问题,例如低流量期间记录器脱水、为收集数据而取出记录器的时长,以及在数据分析过程中稍后应考虑的任何其他环境问题。收集到的数据有助于构建尼查科流域观测水温的长期时间序列,并作为未来项目的基线。这些数据还用于确定尼查科水库和斯金斯湖溢洪道夏季温度管理计划的有效性[1]。因此,这些数据未来可用于更好地确定水库的最佳泄流量,以尽量减少对流域的生态影响。