Detection of Changes in the Hydrological Balance in Seven River Basins Along the Western Carpathians in Slovakia

IF 0.6 Q4 ENGINEERING, CIVIL
KeszeliovÁ Anita, HlavČovÁ Kamila, DanÁČovÁ Michaela, DanÁČovÁ Zuzana, Szolgay Ján
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引用次数: 8

Abstract

Abstract Due to a changing climate, likely changes to a hydrological regime are one of the primary sources of uncertainty to consider in managing water resources. In Slovakia, a decline in the country’s water resources, combined with a change in the seasonality of runoff and an increase in the extremeness of floods and droughts, represents a potential threat. The objective of the paper was to explore trends in the components of the long-term hydrological balance of various river basins to detect the impacts of changing climate conditions along the Western Carpathians. The proposed method is a comparative exploratory analysis of the hydrological balance of the selected river basins. Temporal changes in the catchments’ average air temperatures, precipitation, runoff, and their differences (considered as an index of the actual evapotranspiration), were estimated for 49 years of data; two non-overlapping sub-periods (25 and 24 years) in the seven river basins were also compared. This work also aims at evaluating the applicability of gridded inputs from the CarpatClim database for modelling the hydrological balance over an extended period. The results document the impact of the rising air temperature and, in part, local physiographic factors on the changes in runoff and actual catchment evapotranspiration.
斯洛伐克喀尔巴阡山脉西部七个流域水文平衡变化的探测
摘要由于气候变化,水文状况的可能变化是水资源管理中需要考虑的不确定性的主要来源之一。在斯洛伐克,该国水资源的减少,加上径流季节性的变化以及极端洪水和干旱的增加,构成了一种潜在的威胁。本文的目的是探索不同流域长期水文平衡组成部分的趋势,以检测喀尔巴阡山脉西部气候条件变化的影响。所提出的方法是对选定流域的水文平衡进行比较探索性分析。根据49年的数据估计了集水区平均气温、降水量、径流量的时间变化及其差异(被视为实际蒸散的指标);比较了7个流域的两个非重叠子周期(25年和24年)。这项工作还旨在评估CarpatClim数据库中网格输入在长期水文平衡建模中的适用性。研究结果记录了气温上升以及部分当地地形因素对径流量和实际集水区蒸发蒸腾量变化的影响。
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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