缺水地区气候和人为压力下气象和水文干旱的动态演变

IF 3.2 3区 地球科学 Q1 Environmental Science Hydrological Processes Pub Date : 2024-10-01 DOI:10.1002/hyp.15290
Achala Singh, Harshvardhan Solanki, Priyank J. Sharma
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引用次数: 0

摘要

气候变化和人为影响扩大了干旱的复杂性,使非稳态性(NS)纠缠在一起,进一步挑战了对干旱的理解。本研究旨在通过评估水文变量与干旱特征之间的非稳态联系,了解气候和人为压力导致的干旱传播模式的动态演变。研究采用了四个标准化干旱指标,全面考察了气象(MD)和水文(HD)干旱特征的时空演变。研究分析了印度半岛 6 个流域 29 个半干旱集水区的数据,揭示了不同的干旱传播模式。这项研究采用了一种新颖的非重叠块分层随机抽样(NBRS)方法来检测干旱特征和水文变量中的 NS,从而揭示了这种动态行为的潜在驱动因素。结果表明,与戈达瓦里流域、克里希纳流域和彭纳尔流域(GKP)相比,萨巴尔马蒂流域、马希流域和塔皮流域(SMT)的干旱行为具有相似性,SMT(GKP)流域的干旱传播时间更短(更长)。随着时间的推移,SMT 盆地的干旱严重程度有所减轻,而 GKP 盆地的干旱严重程度则有所加剧,这与人类活动的密集干预(如河流调节和水库运行)有关,从而导致干旱的延长和加剧。降雨量主要表现为时变性,而所有流域的潜在蒸散量(尤其是克里希纳和佩纳尔流域)、溪流和基流则表现为显著的非时变性。研究还确定了这些流域三种不同的干旱传播模式,突出显示了 MD 未过渡到 HD 的情况、在 MD 之前未发生 HD 的情况以及 MD 同步传播到 HD 的情况。研究成果为了解气候和人为压力下干旱动态的演变提供了深刻见解,有助于政策制定者和利益相关者制定干旱防备和应对战略。
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Dynamic evolution of meteorological and hydrological droughts under climatic and anthropogenic pressures in water-scarce regions

Climate change and anthropogenic influences amplify drought complexity, entangle non-stationarity (NS) and further challenge drought comprehension. This study aims to understand the dynamic evolution of drought propagation patterns due to climatic and anthropogenic pressures by assessing the non-stationary linkages between hydrological variables and drought characteristics. It employs four standardized drought indicators to comprehensively examine the spatio-temporal evolution of meteorological (MD) and hydrological (HD) drought characteristics. Data from 29 semi-arid catchments from six river basins in Peninsular India, are analyzed to uncover distinct drought propagation patterns. This study utilizes a novel Non-overlapping Block-stratified Random Sampling (NBRS) approach to detect NS in drought characteristics and hydrological variables, shedding light on the underlying drivers of this dynamic behavior. The results indicate similarities in drought behavior for the Sabarmati, Mahi and Tapi (SMT) basins compared with the Godavari, Krishna and Pennar (GKP) basins, with shorter (longer) propagation times noted for SMT (GKP) basins. While HD severity decreases over time in SMT basins, it intensifies in GKP basins, which are linked to intensive anthropogenic interventions such as river regulation and reservoir operations, thus resulting in prolonged and intensified droughts. Rainfall primarily exhibits time-invariance, while significant NS is observed in potential evapotranspiration (particularly in the Krishna and Pennar basins), streamflow and baseflow across all basins. The study also identified three distinct drought propagation patterns in these basins, highlighting cases where MD did not transition to HD, instances of HD occurring without preceding MD and synchronous propagation of MD to HD. The study outcomes provide profound insights into the evolution of drought dynamics under climatic and anthropogenic pressures, which will aid policymakers and stakeholders in formulating strategies for drought preparedness and response.

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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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