Investigating meteorological wet and dry transitions in the Dutch Meuse River basin

IF 2.6 Q2 WATER RESOURCES Frontiers in Water Pub Date : 2024-05-15 DOI:10.3389/frwa.2024.1394563
Srividya Hariharan Sudha, Elisa Ragno, Oswaldo Morales-Nápoles, Matthijs Kok
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Abstract

The Netherlands has traditionally focused on managing flood risk. However, the frequent occurrence of droughts in recent years has brought attention to managing both extremes. Transitions between these opposite extremes pose additional challenges to water management, requiring a trade-off between water storage during dry periods and flood control during wet periods. In this study, we develop a framework to define wet and dry meteorological events and study their transitions using timeseries of meteorological data namely, precipitation, temperature and potential evapotranspiration. The magnitudes of event characteristics are retained, which presents a different approach to the normalized climate indices (like the Standardized Precipitation Index) commonly used in literature. We apply this framework to the Dutch part of the Meuse River basin in northwestern Europe using climate observations between 1951 and 2022. Our analysis shows a statistically significant increase in the amount of water lost from potential evapotranspiration compared to water gained from precipitation between April and September of the water year and an increase in the length of this drying period over the past decades. Such trends in the drying period are related to variability in potential evapotranspiration caused by rising temperatures in the region, indicating the potential for increased water shortage in Spring and Summer due to future temperature increases. We also identify abrupt transitions between opposite extreme events where there is a lack of water at the end of the second event as meteorological situations that challenge water management due to overlapping impacts like flash flooding, less time for water storage, and reduced water availability. We see such conditions occur in 6% of the wet-dry transitions and 20% of the dry-wet transitions, highlighting meteorological scenarios to which the hydrological response of the catchment can be simulated to increase our understanding of the combined risk of floods and droughts.
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荷兰默兹河流域干湿转换气象调查
荷兰历来注重洪水风险的管理。然而,近年来频繁发生的干旱使人们开始关注两种极端情况的管理。在这两个极端之间的过渡给水管理带来了额外的挑战,需要在干旱时期的蓄水和潮湿时期的防洪之间进行权衡。在这项研究中,我们建立了一个框架来定义干湿气象事件,并利用气象数据的时间序列(即降水、温度和潜在蒸散量)来研究它们之间的过渡。我们保留了事件特征的大小,这与文献中常用的归一化气候指数(如标准化降水指数)不同。我们利用 1951 年至 2022 年期间的气候观测数据,将这一框架应用于欧洲西北部默兹河流域的荷兰部分。我们的分析表明,在过去几十年中,潜在蒸散损失的水量与水年 4 月至 9 月期间从降水中获得的水量相比有显著的统计学增长,而且这一干燥期的长度也在增加。干燥期的这种趋势与该地区气温升高导致的潜在蒸散量变化有关,表明未来气温升高有可能导致春夏季缺水加剧。我们还发现,由于山洪暴发、蓄水时间减少和可用水量减少等叠加影响,在相反的极端事件之间会出现突然过渡,即在第二个极端事件结束时出现缺水,这也是对水资源管理构成挑战的气象状况。我们发现,在 6% 的干湿转换和 20% 的干湿转换中都出现了这种情况,这突出说明了可以模拟集水区水文响应的气象情景,以增加我们对洪水和干旱综合风险的了解。
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来源期刊
Frontiers in Water
Frontiers in Water WATER RESOURCES-
CiteScore
4.00
自引率
6.90%
发文量
224
审稿时长
13 weeks
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