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A framework to nowcast soil moisture with NASA SMAP level 4 data using in-situ measurements and deep learning 利用现场测量和深度学习对 NASA SMAP 第 4 级数据进行土壤湿度预报的框架
IF 4.7 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2024-11-01 DOI: 10.1016/j.ejrh.2024.102020
Hassan Dashtian , Michael H. Young , Bissett E. Young , Tyson McKinney , Ashraf M. Rateb , Dev Niyogi , Sujay V. Kumar

Study Region

Southeast Texas, USA.

Study Focus

NASA's Soil Moisture Active Passive (SMAP) product, particularly the Level 4 (SMAPL4) data, provides high-resolution and extensive coverage of surface and root zone soil moisture (SM), essential for weather and climate research. However, a latency of 2.5–4.0 days in SMAPL4 data limits its real-time hydrologic and weather prediction applications. To address this, we developed a model integrating deep learning (DL) techniques (Long Short-Term Memory, Fully Connected Neural Network) with Principal Component Analysis (PCA) to nowcast SM data in real-time. The model is trained on multi-source SM observations, including near real-time in-situ and satellite data, and deployed over a 56,000+ km² area in southeast Texas.

New Hydrological Insights for the Region

Our DL methodology nowcasts SM accurately in both time and space through real-time assimilation of multi-source data, mitigating SMAP's latency and offering near real-time soil moisture estimates. The nowcasted SM aligns closely with actual SMAPL4 data, capturing spatial and temporal variations. SMAP underestimates the spatio-temporal variability of soil moisture compared to in-situ data, highlighting the necessity for diverse data integration. The proposed framework can improve the real-time flood and drought monitoring and offers insights for various hydrological applications. Nowcasting error mapping identifies regions with higher uncertainties, guiding future model improvements.
研究地区美国得克萨斯州东南部。研究重点美国国家航空航天局的土壤水分主动被动(SMAP)产品,特别是第 4 级(SMAPL4)数据,提供了高分辨率和广泛覆盖的地表和根区土壤水分(SM),对天气和气候研究至关重要。然而,SMAPL4 数据 2.5-4.0 天的延迟限制了其实时水文和天气预报应用。为解决这一问题,我们开发了一种将深度学习(DL)技术(长短期记忆、全连接神经网络)与主成分分析(PCA)相结合的模型,用于实时预报 SM 数据。我们的深度学习方法通过对多源数据的实时同化,在时间和空间上对土壤水分进行了准确的预报,减轻了 SMAP 的延迟,并提供了接近实时的土壤水分估算。现在预测的土壤水分与实际的 SMAPL4 数据密切吻合,捕捉到了空间和时间上的变化。与原位数据相比,SMAP 低估了土壤水分的时空变化,这凸显了多样化数据整合的必要性。所提出的框架可改善实时洪水和干旱监测,并为各种水文应用提供见解。预报误差绘图可确定不确定性较高的区域,从而指导未来模型的改进。
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引用次数: 0
Disentangling hydrodynamic drivers of the Southern Venice (Italy) coastal aquifer via frequency decomposition analysis: Insights, challenges, and limitations 通过频率分解分析解密意大利威尼斯南部沿海含水层的水动力驱动因素:见解、挑战和局限性
IF 4.7 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2024-10-31 DOI: 10.1016/j.ejrh.2024.102039
Mattia Gaiolini , Fabrizio Rama , Micòl Mastrocicco , Marta Cosma , Sandra Donnici , Luigi Tosi , Nicolò Colombani

Study region

Shallow coastal aquifer located in the southern part of the Venice lagoon (Italy).

Study focus

This study aims to improve the understanding of coastal aquifers’ hydrodynamics by implementing systematic time-series analyses of data. A collection of non-intrinsically consistent time series from hydrological (surface water and groundwater) and meteo-mareographic monitoring networks was obtained from different institutions. Each signal was broken down through a frequency decomposition analysis, isolating the main driving forces to focus on phenomena that occur at different time and spatial scales.

New hydrological insights for the region

Results highlighted that the aquifer is highly connected with the Venice lagoon, with a clear fluctuation of piezometric heads induced by tidal major constituents, decreasing landward. Besides, the effects exerted by reclamation canals and pumping stations were also determined and found to increase landward. Despite the relatively simple behaviour of piezometric heads, the groundwater salinity is influenced by additional local factors, like probe depth, wells’ screen length, and vertical salinity distribution along the aquifer. These findings suggested how to make use of limited and sparse data to enhance the conceptual model of coastal aquifer hydrodynamics, while highlighting the limitations of existing monitoring networks. This outcome justified the need for an intrinsically-consistent network of dedicated multi-level samplers to avoid intra-borehole mixing and reliably characterize the groundwater salinity distribution.
研究重点 这项研究旨在通过对数据进行系统的时间序列分析,加深对沿海含水层水动力的了解。从不同机构获得了来自水文(地表水和地下水)和气象监测网络的非内在一致的时间序列。结果表明,含水层与威尼斯泻湖高度相连,潮汐主要成分引起的压水头波动明显,并向陆地方向递减。此外,还测定了填海运河和抽水站的影响,发现其向陆地方向增大。尽管压水头的行为相对简单,但地下水盐度还受到其他局部因素的影响,如探头深度、水井滤网长度和含水层沿线的垂直盐度分布。这些发现提出了如何利用有限和稀少的数据来改进沿岸含水层水动力概念模型,同时也突 出了现有监测网络的局限性。这一结果证明,有必要建立一个内在一致的多层次专用采样器网络,以避免钻孔内混 合,可靠地描述地下水盐度分布特征。
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引用次数: 0
Advanced long-term actual evapotranspiration estimation in humid climates for 1958–2021 based on machine learning models enhanced by the RReliefF algorithm 基于RReliefF算法增强的机器学习模型的1958-2021年湿润气候长期实际蒸散量高级估算方法
IF 4.7 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2024-10-31 DOI: 10.1016/j.ejrh.2024.102043
Ahmed Elbeltagi , Salim Heddam , Okan Mert Katipoğlu , Abdullah A. Alsumaiei , Mustafa Al-Mukhtar

Study region

Chengdu, Wuhan, Chongqing, and Kunming regions in China.

Study focus

Accurate estimation of crop water use or actual evapotranspiration (AET) remains a key obstacle in the effective design of irrigation schedules, plans, and design. This is due to the non-linear nature of this phenomenon. To address this issue and guarantee more accurate ET predictions, this study attempts the following: i) to assess the performance of five machine learning (ML) models optimized by the RReliefF algorithm in estimating actual ET values for each month in four Chinese provinces under various agroclimatic conditions; and ii) to select the optimal model based on statistical metrics while minimizing discrepancies between the estimated and actual ET values. AET was estimated using support vector machine (SVM), ensemble bagged and boosted trees, robust linear regression (RLR), and Matern 5/2 Gaussian process regression (M-GPR) models.

New hydrological insights for the region

The M-GPR model outperformed the other models and generated the best values for all statistical measures for training and testing stages: R2 (0.979, 0.982), RMSE (5.56, 5.09), MAE (3.29,3.16). In comparison, the RLR model exhibited the lowest training and testing performances metrics. The results of this study demonstrate the capacity of the M-GPR model to accurately predict long-term AET values. This model is best suited for further research on AET prediction at the stations under investigation, which could improve irrigation and boost agricultural productivity.
研究地区中国成都、武汉、重庆和昆明地区。研究重点准确估算作物用水量或实际蒸散量(AET)仍然是有效设计灌溉计划、规划和设计的关键障碍。这是由于这种现象的非线性性质造成的。为解决这一问题并保证更准确的蒸散发预测,本研究尝试进行以下工作:i) 评估经 RReliefF 算法优化的五个机器学习(ML)模型在估算中国四个省份不同农业气候条件下每月实际蒸散发值时的性能;ii) 根据统计指标选择最优模型,同时最大限度地减少估算值与实际蒸散发值之间的差异。使用支持向量机 (SVM)、集合袋装树和提升树、鲁棒性线性回归 (RLR) 和 Matern 5/2 高斯过程回归 (M-GPR) 模型估算了蒸散发量:R2(0.979,0.982)、RMSE(5.56,5.09)、MAE(3.29,3.16)。相比之下,RLR 模型的训练和测试性能指标最低。研究结果表明,M-GPR 模型能够准确预测长期 AET 值。该模型最适合用于对所调查站点的 AET 预测进行进一步研究,从而改善灌溉条件,提高农业生产率。
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引用次数: 0
A diagnostic framework to reveal future clean water scarcity in a changing climate 揭示不断变化的气候条件下未来清洁水稀缺状况的诊断框架
IF 4.7 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2024-10-31 DOI: 10.1016/j.ejrh.2024.102040
Shanlin Tong , Rui Xia , Jie Chen , Wenpan Li , Yan Chen , Chong-Yu Xu

Study region

The Yangtze River basin.

Study focus

Clean water scarcity is one of the major constraints for human sustainable development. Previous diagnosis of water scarcity has focus on fluctuations in the amount of water needed by humans, while ignoring the imbalance between water supply and demand that is exacerbated by changes in water quality under the context of climate change. This study proposes a diagnosis framework for clean water scarcity analysis under future climate projections by combining climate and socioeconomic projections, hydrological system, environmental requirement and human water withdrawal simulations, and water quality projections. This framework is demonstrated in analyzing the clean water scarcity for near (2031–2060) and far (2070–2099) futures.

New hydrological insights for the region

The results show that by the end of this century, the clean water stress index will decrease substantially, and the number of people potentially threatened by clean water scarcity is expected to decrease from 294.8 million to 159.1 million. Clean water scarcity is expected to ease as freshwater resources increase in the future. Based on scenario simulations, the results further reveal that mitigation measures for clean water scarcity are mainly affected by natural factors in near and far futures. These findings support that the proposed framework can provide a new perspective for assessing and explaining the multifaceted influences of climate change on clean water scarcity.
研究区域长江流域。研究重点清洁水短缺是人类可持续发展的主要制约因素之一。以往的缺水诊断主要关注人类需水量的波动,而忽视了气候变化背景下水质变化加剧的水资源供需失衡。本研究结合气候和社会经济预测、水文系统、环境要求和人类取水模拟以及水质预测,提出了未来气候预测下清洁水稀缺性分析的诊断框架。结果表明,到本世纪末,洁净水压力指数将大幅下降,可能受到洁净水短缺威胁的人口数量预计将从 2.948 亿减少到 1.591 亿。随着未来淡水资源的增加,清洁水稀缺的情况预计会有所缓解。根据情景模拟,结果进一步显示,在近期和远期,清洁水稀缺的缓解措施主要受自然因素的影响。这些结果证明,所提出的框架可以为评估和解释气候变化对清洁水稀缺的多方面影响提供一个新的视角。
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引用次数: 0
Multi-objective synergy and competition relationship of water and sediment regulation of the Heishanxia reservoir in upstream of the Yellow River Basin 黄河流域上游黑山峡水库水沙调控的多目标协同与竞争关系
IF 4.7 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2024-10-31 DOI: 10.1016/j.ejrh.2024.102045
Jieyu Li , Hang Li , Yuanjian Wang , Gang Liu , Fei Yang , Qiang Wang , Donglin Li

Study region

Heishanxia Reservoir, upstream of the Yellow River Basin.

Study focus

The complicated management of the Yellow River Basin stems primarily from an uncoordinated relationship between water and sediment. The un-built Heishanxia Reservoir has been designated as one of seven pivotal projects, and its regulating effect remains to be thoroughly studied. First, nine typical inflow water and sediment scenarios were constructed based on probability inference. Then, a multi-objective water and sediment regulation model of Heishanxia Reservoir was established with the objectives of maximum erosion quantity (EQ) of the channel, maximum ecological satisfaction rate (ESR), and maximum power generation (PG). Finally, the multi-dimensional regulating effect was revealed, and the synergy-competition relationships among EQ, ESR and PG were analyzed.

New hydrological insights for the region

The operation of Heishanxia can increase the discharge during the flood season in the downstream Ning-Meng Channel, and the average annual EQ is 0.19×108 t more than the current condition. Further, the ESR decreases slightly during the high-flow and normal-flow years and increases slightly during the low-flow years. The PG in the upper reaches of the Yellow River has increased by approximately 10 %. Among the three objectives, EQ and ESR, as well as EQ and PG, demonstrate a competitive relationship, whereas ESR and PG exhibit a synergistic relationship. Reservoir inflow plays a major role in the changes of synergy-competition relationship.
研究区域黄河流域上游的黑山峡水库。研究重点黄河流域的复杂管理主要源于水与泥沙之间不协调的关系。尚未建成的黑山峡水库被列为七大枢纽工程之一,其调节作用仍有待深入研究。首先,基于概率推理构建了九种典型的入库水沙情景。然后,以河道侵蚀量(EQ)最大、生态满足率(ESR)最大和发电量(PG)最大为目标,建立了黑山峡水库多目标水沙调节模型。黑山峡的运行可增加下游宁蒙河道汛期下泄流量,年平均侵蚀量比现状增加 0.19×108 t。此外,ESR 在丰水年和常丰水年略有减少,在枯水年略有增加。黄河上游的 PG 增加了约 10%。在这三个目标中,EQ 和 ESR 以及 EQ 和 PG 呈现竞争关系,而 ESR 和 PG 则呈现协同关系。在协同与竞争关系的变化中,水库流入量起着重要作用。
{"title":"Multi-objective synergy and competition relationship of water and sediment regulation of the Heishanxia reservoir in upstream of the Yellow River Basin","authors":"Jieyu Li ,&nbsp;Hang Li ,&nbsp;Yuanjian Wang ,&nbsp;Gang Liu ,&nbsp;Fei Yang ,&nbsp;Qiang Wang ,&nbsp;Donglin Li","doi":"10.1016/j.ejrh.2024.102045","DOIUrl":"10.1016/j.ejrh.2024.102045","url":null,"abstract":"<div><h3>Study region</h3><div>Heishanxia Reservoir, upstream of the Yellow River Basin.</div></div><div><h3>Study focus</h3><div>The complicated management of the Yellow River Basin stems primarily from an uncoordinated relationship between water and sediment. The un-built Heishanxia Reservoir has been designated as one of seven pivotal projects, and its regulating effect remains to be thoroughly studied. First, nine typical inflow water and sediment scenarios were constructed based on probability inference. Then, a multi-objective water and sediment regulation model of Heishanxia Reservoir was established with the objectives of maximum erosion quantity (EQ) of the channel, maximum ecological satisfaction rate (ESR), and maximum power generation (PG). Finally, the multi-dimensional regulating effect was revealed, and the synergy-competition relationships among EQ, ESR and PG were analyzed.</div></div><div><h3>New hydrological insights for the region</h3><div>The operation of Heishanxia can increase the discharge during the flood season in the downstream Ning-Meng Channel, and the average annual EQ is 0.19×10<sup>8</sup> t more than the current condition. Further, the ESR decreases slightly during the high-flow and normal-flow years and increases slightly during the low-flow years. The PG in the upper reaches of the Yellow River has increased by approximately 10 %. Among the three objectives, EQ and ESR, as well as EQ and PG, demonstrate a competitive relationship, whereas ESR and PG exhibit a synergistic relationship. Reservoir inflow plays a major role in the changes of synergy-competition relationship.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"56 ","pages":"Article 102045"},"PeriodicalIF":4.7,"publicationDate":"2024-10-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142561254","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Hydro-chemical tracers and hydro-chemical modeling assessing groundwater leakage for a karst aquifer in Yarkon-Taninim basin, Israel 水化学示踪剂和水化学模型评估以色列亚尔康-塔尼尼姆盆地岩溶含水层的地下水渗漏情况
IF 4.7 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2024-10-29 DOI: 10.1016/j.ejrh.2024.102033
Michael Zilberbrand , Vladimir Mirlas , Alexander Gimburg , Yaakov Anker

Study region

Yarkon-Taninim groundwater basin, Israel.

Study focus

A Paleocene-Eocene thermal episode caused an anomaly of barium and silica concentrations in the Eocene aquitard that were used as natural tracers for identifying and quantifying leakage into the Turonian – Upper Cenomanian aquifer through the Senonian-Paleocene (Mount-Scopus Group) strata. Increased concentrations of both Ba2+ and SiO2 in Turonian – Upper Cenomanian aquifer groundwater were supposed to be a sign of downward leakage from the Eocene aquitard. Within the Menashe syncline where these tracers pointed to the leakage, it was estimated by the balance method. Using this estimate, the area-averaged hydraulic conductivity of the intermedium layer was assessed from the Darcy’s law by using this layer thickness and a hydraulic gradient between the Avdat-Group aquitard and the Turonian – Upper Cenomanian aquifer. The calculation and integration of its results over the balance area by a grid with 1×1 km2 cells was performed by using the GIS-based ARGUS ONE software. Cl- and SO42- concentrations in the leakage have been estimated by using the mixing model considering the assessed leakage. PHREEQC software was used for solubility calculation of amorphous silica, quartz and barite at different temperatures, pH and salinities and for calculation of saturation indices of Ba-bearing minerals.

New hydrological insights for the region

Previously the Senonian layers within synclines in the Yarkon-Taninim basin, which is the primary source of the groundwater supply in Israel, were supposed to be impermeable. This study has shown that the main leakage is concentrated in the Menashe syncline vicinity north of the Yarkon-Taninim basin. The two tracers first provided a possibility of the leakage assessment within the Menashe syncline: more than 2.3*106 – 11.4*106 m3 yr−1 (leakage rate of 5.4*10−5 – 2.6*10−4 m day−1 at the Eocene outcrops of the syncline). The average regional permeability of the Senonian aquiclude within the Menashe syncline was estimated in the range 7.7*10−5 – 3.8*10−4 m day−1, essentially higher as compared to the values for the Bet-Govrin syncline. The salinity of the slow leakage was assessed to be low; therefore, it will not damage the high-quality groundwater in the Turonian – Upper Cenomanian aquifer that is exploited for the potable water supply.
研究重点 古新世-始新世的热事件导致始新世含水层中的钡和二氧化硅浓度异常,这些钡和二氧化硅被用作天然示踪剂,用于确定和量化通过塞诺尼-古新世(斯科普斯山组)地层渗漏到图伦纪-上新世含水层的情况。都龙纪-上新统含水层地下水中 Ba2+ 和 SiO2 浓度的增加,被认为是始新世含水层向下渗漏的迹象。在这些示踪剂表明存在渗漏的梅纳谢突岩中,用平衡法对渗漏进行了估算。根据这一估算结果,利用中间层厚度和阿夫达特组含水层与都伦-上新统含水层之间的水力梯度,根据达西定律评估了中间层的区域平均水力传导率。利用基于地理信息系统的 ARGUS ONE 软件,通过 1×1 平方公里的网格对平衡区进行了计算和整合。考虑到评估的泄漏量,使用混合模型估算了泄漏中的 Cl- 和 SO42- 浓度。PHREEQC 软件用于计算无定形二氧化硅、石英和重晶石在不同温度、pH 值和盐度下的溶解度,以及计算含钡矿物的饱和指数。这项研究表明,主要的渗漏集中在亚尔康-塔尼尼姆盆地北部的梅纳谢突岩附近。两种示踪剂首先提供了对梅纳谢突岩内部渗漏评估的可能性:超过 2.3*106 - 11.4*106 立方米/年-1(在突岩的始新世露头处,渗漏率为 5.4*10-5 - 2.6*10-4 米/天-1)。据估计,梅纳谢向斜内的塞诺尼安含水层的平均区域渗透率为 7.7*10-5 - 3.8*10-4 米/天-1,基本上高于 Bet-Govrin 向斜的数值。经评估,缓慢渗漏的盐度较低;因此,它不会对用于饮用水供应的图伦纪--上塞努曼纪含水层中的优质地下水造成损害。
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引用次数: 0
Machine learning modeling reveals the spatial variations of lake water salinity on the endorheic Tibetan Plateau 机器学习建模揭示青藏高原内流湖湖水盐度的空间变化
IF 4.7 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2024-10-29 DOI: 10.1016/j.ejrh.2024.102042
Pengju Xu , Kai Liu , Lan Shi , Chunqiao Song

Study region

The endorheic Tibetan Plateau (TP).

Study focus

Water salinity is sensitive indicator for variations of lake hydrologic and physicochemical characteristics. Due to the heterogeneous influences from geographical and climatic factors, lake water salinity is highly sensitive to environmental diversity and changes. The TP hosts a wide distribution of lakes, the majority of which belong to endorheic drainage type and are saline or salty lakes. However, the harsh environment on the TP poses great challenges for the insite measurements at large scales, impeding the comprehension of the pattern and variations of lake water salinity across the TP.

New hydrological insights for the region

Benefiting extensive field surveys and a meta–analysis, this study establishes machine learning models based on measurements from 100 terminal lakes (>1 km2) and related physical variables. The optimal model (R2 = 0.90, MAE = 8.11 g/L, MAPE = 36.40 %, RMSE = 12.51 g/L, RRMSE = 36.96 g/L) is then applied to predict the water salinity of the other 214 unmeasured terminal lakes. The modeling results reveal a spatial variation pattern of increasing water salinity of these terminal lakes from south to north across the endorheic basins. Further classification of water salinity levels indicated that more than half (213) of the terminal lakes are in an oligosaline state. This study contributes to a spatially–explicit understanding of the distribution variations in water salinity of terminal TP lakes and provides a feasible approach for estimating water salinity of unmeasured lakes at large scales.
研究区域青藏高原(TP)。研究重点湖水盐度是反映湖泊水文和物理化学特征变化的敏感指标。由于受到地理和气候因素的不同影响,湖水盐度对环境的多样性和变化高度敏感。大洋洲的湖泊分布广泛,其中大部分属于内流式排水类型,属于盐湖或咸水湖。通过广泛的实地调查和荟萃分析,本研究基于 100 个终端湖泊(1 平方公里)的测量数据和相关物理变量建立了机器学习模型。最佳模型(R2 = 0.90、MAE = 8.11 g/L、MAPE = 36.40 %、RMSE = 12.51 g/L、RRMSE = 36.96 g/L)随后被用于预测其他 214 个未测量终端湖泊的水盐度。建模结果显示,这些终端湖泊的水体盐度在整个内流河流域呈现出由南向北递增的空间变化规律。水盐度的进一步分类表明,半数以上(213 个)的终端湖泊处于低盐状态。这项研究有助于从空间上明确了解终极热量湖泊水盐度的分布变化,并为在大尺度上估算未测量湖泊的水盐度提供了一种可行的方法。
{"title":"Machine learning modeling reveals the spatial variations of lake water salinity on the endorheic Tibetan Plateau","authors":"Pengju Xu ,&nbsp;Kai Liu ,&nbsp;Lan Shi ,&nbsp;Chunqiao Song","doi":"10.1016/j.ejrh.2024.102042","DOIUrl":"10.1016/j.ejrh.2024.102042","url":null,"abstract":"<div><h3>Study region</h3><div>The endorheic Tibetan Plateau (TP).</div></div><div><h3>Study focus</h3><div>Water salinity is sensitive indicator for variations of lake hydrologic and physicochemical characteristics. Due to the heterogeneous influences from geographical and climatic factors, lake water salinity is highly sensitive to environmental diversity and changes. The TP hosts a wide distribution of lakes, the majority of which belong to endorheic drainage type and are saline or salty lakes. However, the harsh environment on the TP poses great challenges for the in<strong>–</strong>site measurements at large scales, impeding the comprehension of the pattern and variations of lake water salinity across the TP.</div></div><div><h3>New hydrological insights for the region</h3><div>Benefiting extensive field surveys and a meta–analysis, this study establishes machine learning models based on measurements from 100 terminal lakes (&gt;1 km<sup>2</sup>) and related physical variables. The optimal model (R<sup>2</sup> = 0.90, MAE = 8.11 g/L, MAPE = 36.40 %, RMSE = 12.51 g/L, RRMSE = 36.96 g/L) is then applied to predict the water salinity of the other 214 unmeasured terminal lakes. The modeling results reveal a spatial variation pattern of increasing water salinity of these terminal lakes from south to north across the endorheic basins. Further classification of water salinity levels indicated that more than half (213) of the terminal lakes are in an oligosaline state. This study contributes to a spatially–explicit understanding of the distribution variations in water salinity of terminal TP lakes and provides a feasible approach for estimating water salinity of unmeasured lakes at large scales.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"56 ","pages":"Article 102042"},"PeriodicalIF":4.7,"publicationDate":"2024-10-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142538713","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
The role of automated surface water distribution systems in energy-saving agriculture: A case study from central Iran’s Arid Plateau 自动化地表水分配系统在节能农业中的作用:伊朗中部干旱高原案例研究
IF 4.7 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2024-10-29 DOI: 10.1016/j.ejrh.2024.102036
Dorsa Rahparast , Seied Mehdy Hashemy Shahdany , Ronny Berndtsson

Study region

The NekooAbad Irrigation District in central Iran faces challenges due to inefficient surface water distribution. 82 million m3 of groundwater is extracted annually from 15,000 tube-wells, leading to decreased groundwater levels and increased energy consumption of 234 million kWh per year.

Study focus

This study explores implementing automation in surface water distribution to reduce groundwater extraction and conserve energy. A hydraulic simulation model and a centralized Model Predictive Control approach were used to analyze the existing system and propose a recovery plan. The potential impact of automated surface water distribution on reducing groundwater extraction and energy conservation was evaluated through spatial assessment in GIS.

New hydrological insights for the region

The results demonstrate that the introduction of automation can significantly improve surface water distribution and, accordingly, groundwater overexploitation and, consequently, energy conservation, particularly during water scarcity. Energy conservation increased by 42.3 %, 54.8 %, 56.2 %, and 57.7 % under normal conditions, with water shortages of less than 10 %, 10–15 %, and 15–20 %, respectively. However, as the surface water shortages intensified, the energy conservation rates decreased to 57.7 %, 43.7 %, 25.4 %, and 18.9 % for normal conditions, water shortages of 15–20 %, 20–30 %, 30–40 %, and over 40 %, respectively. The automation introduction effectively provided reliable surface water resources, prompting farmers to shut down pumping stations or reduce working hours. Even in extreme scenarios, the project achieved up to 18.9 % energy savings.
研究区域伊朗中部的内库阿巴德灌区因地表水分配效率低下而面临挑战。每年从 15,000 口管井中抽取 8,200 万立方米地下水,导致地下水位下降,能源消耗每年增加 2.34 亿千瓦时。采用水力模拟模型和集中模型预测控制方法对现有系统进行分析,并提出恢复计划。结果表明,引入自动化可显著改善地表水分配,从而减少地下水的过度开采,进而节约能源,尤其是在缺水时期。在正常情况下,缺水量低于 10%、10-15% 和 15-20% 时,节能率分别提高了 42.3%、54.8%、56.2% 和 57.7%。然而,随着地表水短缺的加剧,正常情况下的节能率分别下降到 57.7 %、43.7 %、25.4 % 和 18.9 %,缺水率分别为 15-20 %、20-30 %、30-40 % 和 40 % 以上。自动化的引入有效地提供了可靠的地表水资源,促使农民关闭泵站或减少工作时间。即使在极端情况下,该项目也实现了高达 18.9% 的能源节约。
{"title":"The role of automated surface water distribution systems in energy-saving agriculture: A case study from central Iran’s Arid Plateau","authors":"Dorsa Rahparast ,&nbsp;Seied Mehdy Hashemy Shahdany ,&nbsp;Ronny Berndtsson","doi":"10.1016/j.ejrh.2024.102036","DOIUrl":"10.1016/j.ejrh.2024.102036","url":null,"abstract":"<div><h3>Study region</h3><div>The NekooAbad Irrigation District in central Iran faces challenges due to inefficient surface water distribution. 82 million m<sup>3</sup> of groundwater is extracted annually from 15,000 tube-wells, leading to decreased groundwater levels and increased energy consumption of 234 million kWh per year.</div></div><div><h3>Study focus</h3><div>This study explores implementing automation in surface water distribution to reduce groundwater extraction and conserve energy. A hydraulic simulation model and a centralized Model Predictive Control approach were used to analyze the existing system and propose a recovery plan. The potential impact of automated surface water distribution on reducing groundwater extraction and energy conservation was evaluated through spatial assessment in GIS.</div></div><div><h3>New hydrological insights for the region</h3><div>The results demonstrate that the introduction of automation can significantly improve surface water distribution and, accordingly, groundwater overexploitation and, consequently, energy conservation, particularly during water scarcity. Energy conservation increased by 42.3 %, 54.8 %, 56.2 %, and 57.7 % under normal conditions, with water shortages of less than 10 %, 10–15 %, and 15–20 %, respectively. However, as the surface water shortages intensified, the energy conservation rates decreased to 57.7 %, 43.7 %, 25.4 %, and 18.9 % for normal conditions, water shortages of 15–20 %, 20–30 %, 30–40 %, and over 40 %, respectively. The automation introduction effectively provided reliable surface water resources, prompting farmers to shut down pumping stations or reduce working hours. Even in extreme scenarios, the project achieved up to 18.9 % energy savings.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"56 ","pages":"Article 102036"},"PeriodicalIF":4.7,"publicationDate":"2024-10-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142538714","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Simplified spatially distributed, coupled soil moisture–groundwater model, evaluated for Flanders (Belgium) 简化的空间分布式土壤水分-地下水耦合模型,在比利时佛兰德斯进行评估
IF 4.7 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2024-10-26 DOI: 10.1016/j.ejrh.2024.102006
Sotirios Moustakas, Patrick Willems

Study region

Flanders region of Belgium.

Study focus

In hydrological studies, there is a need for computationally fast, spatially distributed models involving the unsaturated zone soil moisture, groundwater and their interactions, while maintaining good accuracy. This study builds on an approach based on the AquaCrop model for the unsaturated zone and a 2D explicit groundwater flow model. The model’s speed stems from its simplicity, while AquaCrop’s wide use provides a basic database for parameterization.
Capillary rise, often not (explicitly) assessed in distributed models, is considered. For coupling the unsaturated and saturated zones better, the capillary rise algorithm by AquaCrop was modified. Groundwater flow to the rivers is represented combining Darcy’s law and the linear reservoir concept. Surface runoff modelling is modified to better incorporate the effects of urban environments. The model was parameterized using publicly available data (involving minimal calibration) and tested for Flanders.

New hydrological insights for the region

Despite its simplicity, the model often performed acceptably. Its accuracy was generally higher for the degree of saturation in the upper 70 cm of the soil (R=0.90, RMSE=0.14) than the first 10 cm (R=0.68, RMSE=0.17). The groundwater levels for wells with observed depths less than 5 m were simulated better (R=0.82, RMSE=0.72 m) than the deeper ones (R=0.63, RMSE=4.59 m). Capillary rise was found to be a potentially substantial source of water to the crops.
研究地区比利时佛兰德斯地区。研究重点在水文研究中,需要计算速度快、空间分布式的模型,涉及非饱和带土壤水分、地下水及其相互作用,同时保持良好的精度。本研究采用的方法基于 AquaCrop 非饱和带模型和二维显式地下水流模型。该模型的速度源于其简单性,而 AquaCrop 的广泛使用则为参数化提供了基本数据库。为了更好地耦合非饱和区和饱和区,对 AquaCrop 的毛细管上升算法进行了修改。结合达西定律和线性水库概念来表示流向河流的地下水。对地表径流模型进行了修改,以更好地结合城市环境的影响。该模型使用公开数据进行参数化(涉及最少的校准),并在佛兰德斯进行了测试。对于土壤上部 70 厘米的饱和度(R=0.90,RMSE=0.14),其准确性普遍高于前 10 厘米(R=0.68,RMSE=0.17)。观测深度小于 5 米的水井的地下水位模拟结果(R=0.82,RMSE=0.72 米)优于更深的水井(R=0.63,RMSE=4.59 米)。毛细管上升可能是农作物的一个重要水源。
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引用次数: 0
Compound effects of sea level and flow on river-induced flooding in coastal areas of southern Sweden 海平面和流量对瑞典南部沿海地区河流引发的洪水的复合影响
IF 4.7 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2024-10-26 DOI: 10.1016/j.ejrh.2024.102032
Fainaz Inamdeen, Magnus Larson

Study region

Rönne River, Säve River, and Höje River, Sweden.

Study focus

River-induced flooding in coastal areas results from a multitude of drivers interacting in complex ways. The primary drivers are sea level (SL) and river flow (Q) that often exhibit coherent behavior to be considered in flood risk management. To describe and quantify the compound effects of SL and Q on flooding, a methodology was developed involving hydraulic simulations with long time series of data yielding statistical properties of output quantities such as river water level and flooded areas. Dominance analysis was conducted to quantify the relative influence of SL and Q on river water level along reaches. Also, simplified, empirically based equations were derived to predict the river water level at any location based on SL and Q.

New hydrological insights for the region

The long-term simulations revealed that the relative influence of SL and Q on the river water level changes significantly from the coast to upstream. For example, at the Rönne River, influence of SL decreases from 90 % to 20 % between 1 km and 11 km from the coast. Meanwhile, influence of Q increases from 10 % to 80 % over the same distance. The simplified equations derived to predict the water level can be used by stakeholders to forecast flood events or in risk assessment where many alternatives need to be considered.
研究重点沿岸地区由河流引发的洪水是多种驱动因素以复杂方式相互作用的结果。主要的驱动因素是海平面 (SL) 和河流流量 (Q),它们通常表现出一致的行为,需要在洪水风险管理中加以考虑。为了描述和量化 SL 和 Q 对洪水的复合影响,我们开发了一种方法,其中包括利用长时间序列数据进行水力模拟,得出河水水位和洪水淹没面积等输出量的统计特性。进行了优势分析,以量化 SL 和 Q 对河道水位的相对影响。对该地区水文情况的新认识 长期模拟显示,SL 和 Q 对河流水位的相对影响从沿岸到上游变化很大。例如,在 Rönne 河,SL 的影响在距海岸 1 至 11 公里处从 90% 下降到 20%。同时,在相同距离内,Q 值的影响从 10% 增加到 80%。得出的预测水位的简化方程可用于利益相关者预测洪水事件,或用于需要考虑多种备选方案的风险评估。
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引用次数: 0
期刊
Journal of Hydrology-Regional Studies
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