Long-Term Discharge Records from United States and European Karst Springs: Data Limitations in Trend Analysis

IF 2.6 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Groundwater Pub Date : 2026-09-13 Epub Date: 2026-07-10 DOI:10.1111/gwat.70093
Laura Toran, Teresa Baraza, Kübra Özdemir Çallı, Carly R. Finegan, Elizabeth A. Hasenmueller, Jonathan Nyquist, Shishir K Sarker, Patricia Spellman
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引用次数: 0

Abstract

A cross-site comparison of 49 springs from the United States and Europe with more than a 30-year record of spring discharge was conducted to look for response to climate change (temperature and precipitation). The dataset included both carbonate and non-carbonate springs across urban and rural settings, covering a wide range of discharge (0.001 to 25 m3/s) and discharge variability (45 to 6500% variability index) to encompass aquifers with a variety of hydrologic regimes and degrees of karstification. Relatively small changes in discharge trends (i.e., change in discharge over the long-term time record) and similar responses across the diverse spring dataset were observed, which suggested that groundwater storage buffers hydrologic stresses in these aquifers despite varying degrees of karstification. Although decreases in discharge were associated with an observed increase in air temperature, larger air temperature trends did not lead to larger discharge trends. Spring discharge trends over time could not be categorized by spring behavior as measured by mean discharge, variability in discharge, or rural vs. urban setting. The detection of trends was sensitive to the time period being considered, with selected time periods yielding different and sometimes opposite discharge trends, highlighting the importance of time period selection when making cross-site comparisons. This study benefited from cross-site comparison by finding similarities in spring discharge trends across varied karst regimes.

美国和欧洲喀斯特泉的长期排放记录:趋势分析中的数据局限性。
对美国和欧洲的49个有30多年春季流量记录的泉水进行了跨站点比较,以寻找对气候变化(温度和降水)的响应。该数据集包括城市和农村地区的碳酸盐和非碳酸盐泉,覆盖了大范围的流量(0.001至25 m3/s)和流量变异性(45至6500%变异性指数),涵盖了具有各种水文制度和岩溶程度的含水层。在不同的春季数据集中观察到相对较小的流量趋势变化(即长期时间记录的流量变化)和类似的响应,这表明尽管岩溶程度不同,地下水储存缓冲了这些含水层的水文应力。虽然排放量的减少与观测到的气温升高有关,但较大的气温趋势并没有导致更大的排放量趋势。随着时间的推移,春季流量趋势不能通过平均流量、流量变异性或农村与城市环境测量的春季行为来分类。趋势的检测对所考虑的时间段很敏感,所选时间段产生的流量趋势不同,有时相反,这突出了在进行跨站点比较时选择时间段的重要性。该研究得益于跨站点比较,发现了不同喀斯特体制的泉水流量趋势的相似性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Groundwater
Groundwater 环境科学-地球科学综合
CiteScore
4.80
自引率
3.80%
发文量
0
审稿时长
12-24 weeks
期刊介绍: Ground Water is the leading international journal focused exclusively on ground water. Since 1963, Ground Water has published a dynamic mix of papers on topics related to ground water including ground water flow and well hydraulics, hydrogeochemistry and contaminant hydrogeology, application of geophysics, groundwater management and policy, and history of ground water hydrology. This is the journal you can count on to bring you the practical applications in ground water hydrology.
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