Jihun Ryu , Shih-Yu Wang , Jee-Hoon Jeong , Hyungjun Kim , Jin-Ho Yoon
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引用次数: 0
Abstract
Quantifying the timing of hydroclimatic changes due to global warming is crucial for water resources management. This study investigates the hydroclimatic changes based on the Time of Emergence (TOE) analysis in the western United States, with a focus on the impacts of climate change and aridification. Utilizing the Community Earth System Model Version 2 Large Ensemble (CESM2-LE), we investigate projected changes in temperature, precipitation, evapotranspiration, runoff, snow, and Total Water Storage (TWS). Despite precipitation increases in the future, our results project a robust decrease in TWS by the end of the 21st century, mainly driven by higher evapotranspiration and reduced snow. Total Water Storage, which is an integrated measure of all terrestrial hydrological processes, exhibits a more pronounced climate change signal compared to precipitation. Significant regional variations also emerge in the TOE of TWS, with states around the interior and high-elevation regions experiencing changes faster, as early as in the 2030 s, than those on the Pacific Coast or in southern regions. The study highlights the Upper Colorado River Basin as an emerging aridification hotspot, emphasizing the need for targeted research and adaptive water resource management strategies. This research underscores the importance of jointly considering TWS and the aridity index to comprehensively assess hydrologic regime shifts under global warming.
Plain Language Summary
Climate change is leading to shifts in temperature, rainfall, evapotranspiration, river flow, snow, and other factors. These changes collectively affect what we call the ’hydroclimate,’ which includes changes in groundwater and aridity. Our study finds that as climate change progresses, there will be a noticeable decrease in groundwater, particularly in the interior states. Additionally, we observe an expansion of dry areas, especially in the Upper Colorado River Basin due to reduced snow. This information is crucial for policymakers who need to plan and prepare for future water resource management in the face of a warming climate.
量化全球变暖引起的水文气候变化的时间对水资源管理至关重要。本文以美国西部为研究对象,基于出现时间(Time of Emergence, TOE)分析,探讨了气候变化和干旱化对西部水文气候的影响。利用社区地球系统模型第2版大集合(CESM2-LE),我们研究了温度、降水、蒸散发、径流、雪和总储水量(TWS)的预估变化。尽管未来降水会增加,但我们的研究结果预测,到21世纪末,TWS将大幅减少,主要是由于蒸散发增加和积雪减少。总储水量是所有陆地水文过程的综合度量,与降水相比,它表现出更明显的气候变化信号。TWS的TOE也出现了显著的区域差异,内陆和高海拔地区周边各州的变化速度更快,早在2030年代就比太平洋沿岸或南部地区快。该研究强调了科罗拉多河上游流域是一个新兴的干旱化热点,强调了有针对性的研究和适应性水资源管理策略的必要性。该研究强调了联合考虑TWS和干旱指数对综合评估全球变暖下水文情势变化的重要性。气候变化正在导致温度、降雨、蒸散、河流流量、积雪和其他因素的变化。这些变化共同影响我们所说的“水文气候”,包括地下水和干旱的变化。我们的研究发现,随着气候变化的进展,地下水将显著减少,尤其是在内陆各州。此外,我们观察到干旱地区的扩大,特别是在科罗拉多河上游盆地,由于降雪减少。这一信息对于决策者来说至关重要,因为他们需要在气候变暖的情况下为未来的水资源管理进行规划和准备。
期刊介绍:
The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.