Learning From Multiyear Meteorological Drought Impacts on Stream Water Quality—Implications for Water Quality Changes Under a Changing Climate

IF 2.9 3区 地球科学 Q1 Environmental Science
Anna Lintern, Robert Sargent, Serene Tan, Danlu Guo, Andrew W. Western, Xixi Shi, Cami Plum
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Abstract

The frequency and intensity of multiyear drought are expected to increase in the future with climate change. This study aims to investigate the impact of multiyear meteorological drought on the behaviour of five water quality constituents (dissolved oxygen, total nitrogen, total phosphorus, electrical conductivity, and turbidity) at 134 sites across Victoria, Australia. A 27-year period (1995–2021) of observed water quality data that spans the Millennium Drought (~1997–2009) was subdivided into meteorological multiyear drought and non-drought conditions. Statistical analysis of these observed data indicates that under multiyear drought, EC increases, while turbidity, TN, TP, and DO decrease in concentration. The magnitude of change in constituent concentrations may be driven by climate characteristics and drought intensity, as inferred from the spatial variability in change in water quality. For salts, TN, and TP, we also identified that constituent loads decrease during multiyear drought periods, regardless of the direction of change of constituent concentrations during drought, highlighting the dominant role of streamflow in driving the trends in constituent loads. Analysis of concentration-streamflow relationships during drought and non-drought periods suggests that parameter values within the concentration-discharge relationship (intercept and slope) shift during multiyear drought, especially in warmer and drier catchments. This indicates that water quality during multiyear drought cannot necessarily be predicted using concentration-discharge relationships calibrated using water quality data from non-drought periods. This investigation can help inform approaches to managing water quality in the future under a changing climate, given persistently drier conditions are expected in this region.

Abstract Image

多年气象干旱对河流水质的影响——气候变化下水质变化的启示
随着气候变化,预计未来多年干旱的频率和强度将增加。本研究旨在调查多年气象干旱对澳大利亚维多利亚州134个地点的五种水质成分(溶解氧、总氮、总磷、电导率和浊度)行为的影响。将跨越千年干旱(~ 1997-2009)的27年(1995-2021)观测水质数据细分为气象多年干旱和非干旱条件。对这些观测数据的统计分析表明,在多年干旱条件下,EC浓度增加,浑浊度、TN、TP和DO浓度降低。从水质变化的空间变异性推断,组分浓度的变化幅度可能受到气候特征和干旱强度的驱动。对于盐、全氮和全磷,我们还发现,在多年干旱期,无论组分浓度的变化方向如何,组分负荷都在减少,这突出了径流在驱动组分负荷变化趋势中的主导作用。干旱期和非干旱期的浓度-流量关系分析表明,在多年干旱期间,浓度-流量关系(截距和坡度)的参数值发生了变化,特别是在温暖和干燥的流域。这表明多年干旱期间的水质不一定能通过使用非干旱时期的水质数据校准的浓度-流量关系来预测。鉴于该地区预计将持续干旱,这项调查有助于为未来在气候变化下管理水质的方法提供信息。
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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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