首页 > 最新文献

Journal of Hydrology-Regional Studies最新文献

英文 中文
Season-land-use heterogeneity Bayesian Three-Cornered Hat (SLH-BTCH) for precipitation fusion in ungauged and sparsely gauged regions 降水融合的季节-土地利用异质性贝叶斯三角帽(SLH-BTCH
IF 5 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2026-04-01 Epub Date: 2026-01-13 DOI: 10.1016/j.ejrh.2026.103110
Qiangwei Yu , Xiaohua Dong , Zengchuan Dong , Yaoming Ma , Xiang Cheng , Xue'er Hu , Chengqi Gong , Bob Su , Wenzhuo Wang

Study region

The source region of the Yangtze River, a core part of the “Asian Water Tower,” has sparse gauges, cold high elevation, and complex relief. Together with strong climatic variability, these factors cause large precipitation-estimation errors that undermine hydrological modeling and meteorological assessments.

Study focus

We introduce the Season–Land-Use Heterogeneity Bayesian Three-Cornered Hat (SLH-BTCH), an enhancement of BTCH. Data are grouped by season–land-use strata; within each group we estimate error covariance and then fuse products by weighted averaging, using only multi-source precipitation fields—no in-situ priors. Using CHIRPS, CMFD, TPHiPr, and CHM-PRE, we assess daily performance of the originals, BTCH, and SLH-BTCH against ground observations, and include an equal-weight average (EWA) baseline to gauge the benefit of grouped error modeling.

New hydrological insights for the region

Compared with the original products, BTCH and equal-weight averaging, SLH-BTCH yields event timing and seasonal precipitation more consistent with gauges while reducing storm-intensity bias and day-to-day noise across contrasting land-surface types. Around key headwater stations (Tuotuohe, Wudaoliang, Zhiduo) this sharpens damaging-storm signals and reduces false alarms, providing tighter basin water-balance closure and more reliable flood simulation, routing and dry-season water-availability estimates in ungauged, data-sparse sectors of the Tibetan Plateau.
研究区域长江源区是“亚洲水塔”的核心部分,水位稀疏,海拔寒冷,地形复杂。再加上强烈的气候变率,这些因素造成了很大的降水估计误差,从而破坏了水文模拟和气象评估。研究重点介绍了季节-土地利用异质性贝叶斯三角帽(SLH-BTCH),这是对BTCH的改进。数据按季节土地利用分层分组;在每个组中,我们估计误差协方差,然后通过加权平均融合产物,仅使用多源降水场-没有原位先验。使用CHIRPS、CMFD、TPHiPr和CHM-PRE,我们根据地面观测评估了原始、BTCH和SLH-BTCH的日常性能,并包括等权重平均(EWA)基线来衡量分组误差建模的好处。与原始产品、BTCH和等权平均相比,SLH-BTCH产生的事件时间和季节性降水与测量更加一致,同时减少了不同陆地表面类型的风暴强度偏差和日常噪音。在关键的水源站(沱沱河、五道梁、知多)周围,这一技术使破坏性风暴信号更加清晰,减少了误报,为青藏高原未测量、数据稀疏的地区提供了更严格的流域水平衡封闭和更可靠的洪水模拟、路线和旱季可用水量估算。
{"title":"Season-land-use heterogeneity Bayesian Three-Cornered Hat (SLH-BTCH) for precipitation fusion in ungauged and sparsely gauged regions","authors":"Qiangwei Yu ,&nbsp;Xiaohua Dong ,&nbsp;Zengchuan Dong ,&nbsp;Yaoming Ma ,&nbsp;Xiang Cheng ,&nbsp;Xue'er Hu ,&nbsp;Chengqi Gong ,&nbsp;Bob Su ,&nbsp;Wenzhuo Wang","doi":"10.1016/j.ejrh.2026.103110","DOIUrl":"10.1016/j.ejrh.2026.103110","url":null,"abstract":"<div><h3>Study region</h3><div>The source region of the Yangtze River, a core part of the “Asian Water Tower,” has sparse gauges, cold high elevation, and complex relief. Together with strong climatic variability, these factors cause large precipitation-estimation errors that undermine hydrological modeling and meteorological assessments.</div></div><div><h3>Study focus</h3><div>We introduce the Season–Land-Use Heterogeneity Bayesian Three-Cornered Hat (SLH-BTCH), an enhancement of BTCH. Data are grouped by season–land-use strata; within each group we estimate error covariance and then fuse products by weighted averaging, using only multi-source precipitation fields—no in-situ priors. Using CHIRPS, CMFD, TPHiPr, and CHM-PRE, we assess daily performance of the originals, BTCH, and SLH-BTCH against ground observations, and include an equal-weight average (EWA) baseline to gauge the benefit of grouped error modeling.</div></div><div><h3>New hydrological insights for the region</h3><div>Compared with the original products, BTCH and equal-weight averaging, SLH-BTCH yields event timing and seasonal precipitation more consistent with gauges while reducing storm-intensity bias and day-to-day noise across contrasting land-surface types. Around key headwater stations (Tuotuohe, Wudaoliang, Zhiduo) this sharpens damaging-storm signals and reduces false alarms, providing tighter basin water-balance closure and more reliable flood simulation, routing and dry-season water-availability estimates in ungauged, data-sparse sectors of the Tibetan Plateau.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103110"},"PeriodicalIF":5.0,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145981487","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Spatio – temporal hydrological cycle characteristics in the upper reaches of the Yangtze River: A multi-source remote sensing and machine learning perspective 长江上游水文循环时空特征:多源遥感与机器学习视角
IF 5 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2026-04-01 Epub Date: 2026-01-16 DOI: 10.1016/j.ejrh.2026.103142
Yang Shi , Yousheng Zhang , Minglei Hou , Jiahua Wei

Study region

The upper reaches of the Yangtze River (URYR) of China

Study focus

This study investigates the spatio-temporal variations of hydrological cycle components in the upper reaches of the Yangtze River (URYR) from 1980 to 2030 using multi-source remote sensing data and machine learning. A long short-term memory network with an attention mechanism (LSTM-AT) is initially developed to predict exploitable water resources (EWR) in the URYR.

New hydrological insights for the region

Significant spatial and temporal variations are identified over the past four decades (1980–2015) and projected through 2030. Precipitation ranges from about 230 mm in the arid northwest to over 1600 mm in the humid southeast, with evapotranspiration varying from less than 100 mm at high altitudes to over 800 mm in low-lying areas. Runoff and terrestrial water storage exhibit similar spatial gradients, and runoff shows strong dependence on precipitation, particularly in the Min–Tuo River basin. LSTM-AT predictions suggest that the regional water balance remains dynamically stable, while EWR in the upper Jinsha River shows a fluctuating upward trend of 2.13 ± 0.87 mm/yr, underscoring the need for adaptive water resource management under ongoing environmental change. By leveraging an attention-based deep learning framework and interpretable feature-weight analysis, this work also provides new insight into the dominant hydro-climatic and human-regulation drivers shaping annual water availability in this highly regulated basin.
利用多源遥感数据和机器学习技术,研究了1980 - 2030年长江上游地区水循环成分的时空变化特征。初步建立了一个具有注意机制的长短期记忆网络(LSTM-AT)来预测长江流域的可开发水资源。在过去40年(1980-2015年)中发现了显著的时空变化,并预测了到2030年的变化。降水范围从干旱的西北约230 mm到潮湿的东南1600 mm以上,蒸散量从高海拔小于100 mm到低洼地区超过800 mm不等。径流与陆地储水量表现出相似的空间梯度,径流对降水的依赖性较强,特别是在岷沱河流域。LSTM-AT预测表明,区域水平衡保持动态稳定,而金沙江上游的EWR呈波动上升趋势(2.13 ± 0.87 mm/yr),表明在持续变化的环境下需要进行适应性水资源管理。通过利用基于注意力的深度学习框架和可解释的特征权重分析,这项工作还提供了新的见解,以了解在这个高度调节的盆地中,主要的水文气候和人类调节驱动因素对年可用水量的影响。
{"title":"Spatio – temporal hydrological cycle characteristics in the upper reaches of the Yangtze River: A multi-source remote sensing and machine learning perspective","authors":"Yang Shi ,&nbsp;Yousheng Zhang ,&nbsp;Minglei Hou ,&nbsp;Jiahua Wei","doi":"10.1016/j.ejrh.2026.103142","DOIUrl":"10.1016/j.ejrh.2026.103142","url":null,"abstract":"<div><h3>Study region</h3><div>The upper reaches of the Yangtze River (URYR) of China</div></div><div><h3>Study focus</h3><div>This study investigates the spatio-temporal variations of hydrological cycle components in the upper reaches of the Yangtze River (URYR) from 1980 to 2030 using multi-source remote sensing data and machine learning. A long short-term memory network with an attention mechanism (LSTM-AT) is initially developed to predict exploitable water resources (<em>EWR</em>) in the URYR.</div></div><div><h3>New hydrological insights for the region</h3><div>Significant spatial and temporal variations are identified over the past four decades (1980–2015) and projected through 2030. Precipitation ranges from about 230 mm in the arid northwest to over 1600 mm in the humid southeast, with evapotranspiration varying from less than 100 mm at high altitudes to over 800 mm in low-lying areas. Runoff and terrestrial water storage exhibit similar spatial gradients, and runoff shows strong dependence on precipitation, particularly in the Min–Tuo River basin. LSTM-AT predictions suggest that the regional water balance remains dynamically stable, while <em>EWR</em> in the upper Jinsha River shows a fluctuating upward trend of 2.13 ± 0.87 mm/yr, underscoring the need for adaptive water resource management under ongoing environmental change. By leveraging an attention-based deep learning framework and interpretable feature-weight analysis, this work also provides new insight into the dominant hydro-climatic and human-regulation drivers shaping annual water availability in this highly regulated basin.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103142"},"PeriodicalIF":5.0,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145981835","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Thresholds of bank collapse in the Middle and Lower Yangtze River: A framework for early bank collapse warning using multi-source remote sensing 长江中下游岸塌阈值:多源遥感岸塌预警框架
IF 5 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2026-04-01 Epub Date: 2026-01-31 DOI: 10.1016/j.ejrh.2026.103189
Jing Deng , Kebing Chen , Zhiwei Li , Jing Yuan , Lingling Zhu

Study region

The Middle and Lower Yangtze River, China.

Study focus

This study integrates multi-source remote sensing data (Landsat and Google Earth) and field-measured topographic data to establish a quantitative framework for identifying bank collapse, which progresses from large-scale screening to localized analysis. Using Google Earth Engine (GEE), we automated the extraction of banklines from 2004 to 2024 and employed the Digital Shoreline Analysis System (DSAS) to quantify the erosion rate. After an initial large-scale screening, six high-risk river segments (e.g., Xiangjiazhou, Qigongling) were selected for detailed analysis, where five key bank collapse indicators were quantified: bank slope, toe erosion slope, Bank-Groove Elevation Difference, Main Stream Proximity Distance, and bankline change rate.

New hydrological insights for the region

Spatially varying thresholds were identified: bank slope (0.1–0.5), toe erosion slope (0.1–0.25), Bank-Groove Elevation Difference (>15 m), and Main Stream Proximity Distance (0.3–0.5 times the channel width). Following the implementation of systematic bank protection after 2015, erosion rates were reduced by 20–30 %. Unprotected banks, however, saw an acceleration in collapse rates. The channel incision induced by the Three Gorges Dam increased instability in unprotected areas, while protected segments showed stable morphodynamics. This study provides a quantitative analysis of bank collapse risk indicators for the Middle and Lower Yangtze River, offering scientific methods and evidence for intelligent bank collapse screening.
研究区域:长江中下游地区。本研究将多源遥感数据(Landsat和谷歌Earth)与实测地形数据相结合,建立岸塌定量识别框架,从大规模筛选到局部分析。利用谷歌Earth Engine (GEE)对2004 - 2024年的岸线进行了自动提取,并利用数字海岸线分析系统(DSAS)对侵蚀速率进行了量化。经过初步的大规模筛选,选取了6个高风险河段(如相家洲、气公岭)进行详细分析,量化了河岸坡度、坡脚侵蚀坡度、岸沟高差、干流接近距离、岸线变化率等5个关键塌岸指标。确定了区域空间变化阈值:岸坡(0.1-0.5)、坡脚侵蚀坡(0.1-0.25)、岸沟高差(>15 m)和主流接近距离(0.3-0.5倍河道宽度)。2015年后实施系统的护岸措施后,侵蚀率降低了20 - 30% %。然而,不受保护的银行的倒闭率却在加速上升。三峡大坝造成的河道切割增加了未受保护区域的不稳定性,而受保护区域则表现出稳定的形态动力学特征。本研究为长江中下游地区塌岸风险指标的定量分析提供了依据,为塌岸智能筛选提供了科学的方法和依据。
{"title":"Thresholds of bank collapse in the Middle and Lower Yangtze River: A framework for early bank collapse warning using multi-source remote sensing","authors":"Jing Deng ,&nbsp;Kebing Chen ,&nbsp;Zhiwei Li ,&nbsp;Jing Yuan ,&nbsp;Lingling Zhu","doi":"10.1016/j.ejrh.2026.103189","DOIUrl":"10.1016/j.ejrh.2026.103189","url":null,"abstract":"<div><h3>Study region</h3><div>The Middle and Lower Yangtze River, China.</div></div><div><h3>Study focus</h3><div>This study integrates multi-source remote sensing data (Landsat and Google Earth) and field-measured topographic data to establish a quantitative framework for identifying bank collapse, which progresses from large-scale screening to localized analysis. Using Google Earth Engine (GEE), we automated the extraction of banklines from 2004 to 2024 and employed the Digital Shoreline Analysis System (DSAS) to quantify the erosion rate. After an initial large-scale screening, six high-risk river segments (e.g., Xiangjiazhou, Qigongling) were selected for detailed analysis, where five key bank collapse indicators were quantified: bank slope, toe erosion slope, Bank-Groove Elevation Difference, Main Stream Proximity Distance, and bankline change rate.</div></div><div><h3>New hydrological insights for the region</h3><div>Spatially varying thresholds were identified: bank slope (0.1–0.5), toe erosion slope (0.1–0.25), Bank-Groove Elevation Difference (&gt;15 m), and Main Stream Proximity Distance (0.3–0.5 times the channel width). Following the implementation of systematic bank protection after 2015, erosion rates were reduced by 20–30 %. Unprotected banks, however, saw an acceleration in collapse rates. The channel incision induced by the Three Gorges Dam increased instability in unprotected areas, while protected segments showed stable morphodynamics. This study provides a quantitative analysis of bank collapse risk indicators for the Middle and Lower Yangtze River, offering scientific methods and evidence for intelligent bank collapse screening.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103189"},"PeriodicalIF":5.0,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146079809","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Geological knowledge and land use: Key drivers in determining natural background levels of groundwater contaminants arsenic, radon, and fluoride in the volcanic area of Viterbo (Central Italy) 地质知识和土地利用:确定维特博(意大利中部)火山地区地下水污染物砷、氡和氟化物自然背景水平的主要驱动因素
IF 5 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2026-04-01 Epub Date: 2026-02-02 DOI: 10.1016/j.ejrh.2026.103194
Giulia Felli , Paolo Ciampi , Leonardo Maria Giannini , Ebrahim Ghaderpour , Carlo Esposito , Marco Petrangeli Papini

Study region

The volcanic–sedimentary domain of Viterbo (Central Italy), a region characterized by complex hydrogeology, naturally elevated arsenic, fluoride, and radon concentrations, and intense industrial land-use pressures.

Study focus

Understanding the combined influence of geological and anthropogenic factors on groundwater quality is essential for sustainable water resource management. This study develops an integrated regional screening framework to distinguish geogenic from anthropogenic contributions to groundwater contamination in complex hydrogeological settings, even when data availability is limited. A dataset of 659 groundwater samples was integrated with geological, structural, and land-use information within a geographic information system. Multivariate statistical analysis based on principal component analysis was combined with spatial analysis to identify dominant environmental controls and screen samples potentially influenced by human activities prior to natural background level estimation.

New hydrological insights for the region

Radon concentrations are predominantly controlled by geological factors, particularly ignimbrite formations and fault systems, confirming a geogenic origin. In contrast, arsenic and fluoride exhibit mixed controls, reflecting natural background conditions locally amplified by industrial and agricultural land use. The screening framework enabled the identification and exclusion of anthropogenically influenced samples, as well as the estimation of representative regional natural background levels: 57 µg/L for arsenic, 2.80 mg/L for fluoride, and 187 Bq/L for radon. The proposed workflow provides a robust and reproducible tool for groundwater quality screening and supports informed assessment of natural background levels in hydrogeologically complex and anthropized regions.
研究区域维泰博(意大利中部)的火山-沉积区,该地区水文地质复杂,砷、氟化物和氡浓度自然升高,工业用地压力大。研究重点了解地质和人为因素对地下水水质的综合影响是水资源可持续管理的基础。本研究开发了一个综合的区域筛选框架,以便在复杂的水文地质环境中区分地质和人为对地下水污染的贡献,即使在数据可用性有限的情况下。利用地理信息系统将659个地下水样本数据集与地质、构造和土地利用信息相结合。基于主成分分析的多元统计分析与空间分析相结合,确定了主要的环境控制因素,并在自然背景水平估计之前筛选了可能受人类活动影响的样本。氡浓度主要受地质因素控制,特别是烟灰岩地层和断层系统,这证实了其地质成因。相比之下,砷和氟化物表现出混合控制,反映了当地因工农业土地使用而放大的自然背景条件。筛选框架能够识别和排除受人为影响的样品,并估计具有代表性的区域自然本底水平:砷57 微克/升,氟化物2.80 毫克/升,氡187 Bq/升。所提出的工作流程为地下水质量筛选提供了一个强大且可重复的工具,并支持对水文地质复杂地区和人类活动地区的自然背景水平进行知情评估。
{"title":"Geological knowledge and land use: Key drivers in determining natural background levels of groundwater contaminants arsenic, radon, and fluoride in the volcanic area of Viterbo (Central Italy)","authors":"Giulia Felli ,&nbsp;Paolo Ciampi ,&nbsp;Leonardo Maria Giannini ,&nbsp;Ebrahim Ghaderpour ,&nbsp;Carlo Esposito ,&nbsp;Marco Petrangeli Papini","doi":"10.1016/j.ejrh.2026.103194","DOIUrl":"10.1016/j.ejrh.2026.103194","url":null,"abstract":"<div><h3>Study region</h3><div>The volcanic–sedimentary domain of Viterbo (Central Italy), a region characterized by complex hydrogeology, naturally elevated arsenic, fluoride, and radon concentrations, and intense industrial land-use pressures.</div></div><div><h3>Study focus</h3><div>Understanding the combined influence of geological and anthropogenic factors on groundwater quality is essential for sustainable water resource management. This study develops an integrated regional screening framework to distinguish geogenic from anthropogenic contributions to groundwater contamination in complex hydrogeological settings, even when data availability is limited. A dataset of 659 groundwater samples was integrated with geological, structural, and land-use information within a geographic information system. Multivariate statistical analysis based on principal component analysis was combined with spatial analysis to identify dominant environmental controls and screen samples potentially influenced by human activities prior to natural background level estimation.</div></div><div><h3>New hydrological insights for the region</h3><div>Radon concentrations are predominantly controlled by geological factors, particularly ignimbrite formations and fault systems, confirming a geogenic origin. In contrast, arsenic and fluoride exhibit mixed controls, reflecting natural background conditions locally amplified by industrial and agricultural land use. The screening framework enabled the identification and exclusion of anthropogenically influenced samples, as well as the estimation of representative regional natural background levels: 57 µg/L for arsenic, 2.80 mg/L for fluoride, and 187 Bq/L for radon. The proposed workflow provides a robust and reproducible tool for groundwater quality screening and supports informed assessment of natural background levels in hydrogeologically complex and anthropized regions.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103194"},"PeriodicalIF":5.0,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146173871","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Comparative assessment of environmental water requirements and river flow health in the Ghezel-Ozan River, Iran 伊朗gehezel - ozan河环境用水要求和河流流量健康的比较评估
IF 5 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2026-04-01 Epub Date: 2026-02-03 DOI: 10.1016/j.ejrh.2026.103203
Kazem Sadeghian , Mehdi Vafakhah , Sayed M. Bateni , Mohammad Hasan Naderi , Jaber Aazami , Mohammad Sadegh Alavi-Yeganeh

Study Region

This study examines the Divandarreh-Bijar watershed, which covers an area of 5560.16 km² and through which the 180 km-long Qezlozan River flows, originating from the Chehel Cheshme Mountains.

Study Focus

This study assesses the suitability of the Ghezel-Ozan River for the native fish Capote razii in western Iran by applying conventional hydrological methods, hydraulic techniques, and model-based habitat-suitability approaches, and by evaluating the flow regime using the Flow Health Tool.

New Hydrological Insights for the Region

The main findings of this study are the following: (1) Capoeta razii has been identified as an ecological indicator species occurring in all types of mesohabitats; (2) The greatest fish diversity was found in the habitats of the run and riffle of the river rafts; (3) The deviation of the flow regime has increased considerably after 2012 as a result of the operation of the dams; (4) The EWRs ranged from 0.33 to 43.9 m3/s according to the different methods; (5) The Habitat Suitability model was the most representative of the environmental needs; and (6) To protect 75 % of suitable habitats, a minimum average flow of 10.09 m3/s is required. The best method to estimate environmental flows is to consider river health and the habitat requirements of native species.
本研究考察了Divandarreh-Bijar流域,该流域面积为5560.16平方公里,起源于Chehel Cheshme山脉的180公里长的Qezlozan河流经该流域。本研究通过应用常规水文方法、水力技术和基于模型的栖息地适宜性方法,以及使用流量健康工具评估流量状况,评估了伊朗西部Ghezel-Ozan河对本地鱼类卡波特razii的适宜性。本研究的主要发现如下:(1)在所有类型的中生境中,都可以发现卡波塔(Capoeta razii)是一种生态指示物种;(2)河筏的流水和流水生境鱼类多样性最大;(3) 2012年以后,由于大坝的运行,流型偏差明显增加;(4)不同方法的水冷比在0.33 ~ 43.9 m3/s之间;(5)生境适宜性模型最能反映环境需求;(6)为保护75%的适宜生境,最低平均流量要求为10.09立方米/秒。估计环境流量的最佳方法是考虑河流健康和本地物种的栖息地要求。
{"title":"Comparative assessment of environmental water requirements and river flow health in the Ghezel-Ozan River, Iran","authors":"Kazem Sadeghian ,&nbsp;Mehdi Vafakhah ,&nbsp;Sayed M. Bateni ,&nbsp;Mohammad Hasan Naderi ,&nbsp;Jaber Aazami ,&nbsp;Mohammad Sadegh Alavi-Yeganeh","doi":"10.1016/j.ejrh.2026.103203","DOIUrl":"10.1016/j.ejrh.2026.103203","url":null,"abstract":"<div><h3>Study Region</h3><div>This study examines the Divandarreh-Bijar watershed, which covers an area of 5560.16 km² and through which the 180 km-long Qezlozan River flows, originating from the Chehel Cheshme Mountains.</div></div><div><h3>Study Focus</h3><div>This study assesses the suitability of the Ghezel-Ozan River for the native fish Capote razii in western Iran by applying conventional hydrological methods, hydraulic techniques, and model-based habitat-suitability approaches, and by evaluating the flow regime using the Flow Health Tool.</div></div><div><h3>New Hydrological Insights for the Region</h3><div>The main findings of this study are the following: (1) Capoeta razii has been identified as an ecological indicator species occurring in all types of mesohabitats; (2) The greatest fish diversity was found in the habitats of the run and riffle of the river rafts; (3) The deviation of the flow regime has increased considerably after 2012 as a result of the operation of the dams; (4) The EWRs ranged from 0.33 to 43.9 m3/s according to the different methods; (5) The Habitat Suitability model was the most representative of the environmental needs; and (6) To protect 75 % of suitable habitats, a minimum average flow of 10.09 m3/s is required. The best method to estimate environmental flows is to consider river health and the habitat requirements of native species.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103203"},"PeriodicalIF":5.0,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146173851","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Decoding the hydroclimatic variability in the Minjiang River, Southeast China: The influence of ENSO, PDO, AO, and anthropogenic regulations 解析闽江水文气候变率:ENSO、PDO、AO和人为调节的影响
IF 5 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2026-04-01 Epub Date: 2026-02-03 DOI: 10.1016/j.ejrh.2026.103192
Xiaohe Lai , Xuan Lin , Huangjie Zou , Yan Liu , Qianli Sun , Aijun Wang , Feng Cai

Study region

Minjiang River (MJR), Southeast (SE) China

Study focus

The hydrological response mechanisms of rivers to coupled climatic and anthropogenic influences remain insufficiently understood. To address this gap, we analyzed the hydrological and climatic variations of the MJR using a suite of approaches, including the Bayesian Estimator of Abrupt Change, Seasonality and Trend (BEAST), Double Mass Curve (DMC), Continuous Wavelet Transform (CWT), Wavelet Coherence (WTC), and Multiscale Wavelet-Bayesian Coupled Regression (MWBCR).

New hydrologic Insights

The results revealed that sediment load exhibited an interannual (7-a, ENSO-like) periodicity, with a significant reduction due to damming prior to 1993, whereas its decadal (PDO-like) signal was obscured by intensive human interventions. Precipitation and water discharge fluctuated within a relatively narrow range but showed distinct interannual and decadal periodicities, reflecting the combined influences of the Arctic Oscillation (AO), ENSO, and PDO. Since the 1990s, precipitation variability has been strongly associated with frequent AOI shifts. Moreover, higher precipitation variability was closely linked to in-phase La Niña–cold PDO events, which enhanced typhoon landfalls in SE China. In contrast, out-of-phase ENSO–PDO conditions corresponded to relatively drier and less variable hydroclimatic conditions, characterized by reduced precipitation and fewer typhoon occurrences.
研究区域:中国东南部岷江流域研究重点河流对气候和人为耦合影响的水文响应机制尚不清楚。为了解决这一问题,我们使用贝叶斯突变、季节性和趋势估计器(BEAST)、双质量曲线(DMC)、连续小波变换(CWT)、小波相干(WTC)和多尺度小波-贝叶斯耦合回归(MWBCR)等方法分析了MJR的水文和气候变化。结果表明,泥沙负荷表现出年际(7-a,类似enso)的周期性,1993年以前由于筑坝而显著减少,而其年代际(类似pdo)的信号被密集的人类干预所掩盖。降水和水量波动范围较窄,但年际和年代际变化明显,反映了北极涛动(AO)、ENSO和PDO的综合影响。自20世纪90年代以来,降水变率与AOI的频繁变化密切相关。此外,较高的降水变率与La Niña-cold PDO同相事件密切相关,该事件增强了中国东南部的台风登陆。相反,非相位ENSO-PDO条件对应于相对干燥和变化较少的水文气候条件,其特征是降水减少和台风发生次数减少。
{"title":"Decoding the hydroclimatic variability in the Minjiang River, Southeast China: The influence of ENSO, PDO, AO, and anthropogenic regulations","authors":"Xiaohe Lai ,&nbsp;Xuan Lin ,&nbsp;Huangjie Zou ,&nbsp;Yan Liu ,&nbsp;Qianli Sun ,&nbsp;Aijun Wang ,&nbsp;Feng Cai","doi":"10.1016/j.ejrh.2026.103192","DOIUrl":"10.1016/j.ejrh.2026.103192","url":null,"abstract":"<div><h3>Study region</h3><div>Minjiang River (MJR), Southeast (SE) China</div></div><div><h3>Study focus</h3><div>The hydrological response mechanisms of rivers to coupled climatic and anthropogenic influences remain insufficiently understood. To address this gap, we analyzed the hydrological and climatic variations of the MJR using a suite of approaches, including the Bayesian Estimator of Abrupt Change, Seasonality and Trend (BEAST), Double Mass Curve (DMC), Continuous Wavelet Transform (CWT), Wavelet Coherence (WTC), and Multiscale Wavelet-Bayesian Coupled Regression (MWBCR).</div></div><div><h3>New hydrologic Insights</h3><div>The results revealed that sediment load exhibited an interannual (7-a, ENSO-like) periodicity, with a significant reduction due to damming prior to 1993, whereas its decadal (PDO-like) signal was obscured by intensive human interventions. Precipitation and water discharge fluctuated within a relatively narrow range but showed distinct interannual and decadal periodicities, reflecting the combined influences of the Arctic Oscillation (AO), ENSO, and PDO. Since the 1990s, precipitation variability has been strongly associated with frequent AOI shifts. Moreover, higher precipitation variability was closely linked to in-phase La Niña–cold PDO events, which enhanced typhoon landfalls in SE China. In contrast, out-of-phase ENSO–PDO conditions corresponded to relatively drier and less variable hydroclimatic conditions, characterized by reduced precipitation and fewer typhoon occurrences.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103192"},"PeriodicalIF":5.0,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146173848","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Effective porosity in carbonate rocks from the Betic Cordillera (southern Spain): A regional dataset for reservoir and aquifer characterization Betic Cordillera(西班牙南部)碳酸盐岩有效孔隙度:储层和含水层表征的区域数据集
IF 5 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2026-04-01 Epub Date: 2026-02-05 DOI: 10.1016/j.ejrh.2026.103173
Carlos Marín-Lechado , Antonio Pedrera , Antonio González-Ramón , Ana Ruiz-Constán , Antonio Luis Molina , Antonio Pulido-Bosch , Iñaki Vadillo , Concepción Fernández-Leyva , Mónica Reyes , Nuria Naranjo-Fernández , Antonio Lope Morales , Sergio Martos-Rosillo

Study region

The Betic Cordillera (southern Spain) comprises carbonate formations ranging from Paleozoic to Cenozoic age, distributed across the Internal, Subbetic, and Prebetic domains. These include metamorphic marbles as well as non-metamorphic limestones and dolostones deposited in contrasting tectonostratigraphic settings.

Study focus

This study compiles and statistically characterizes 866 laboratory-measured effective (open) porosity values from carbonate rocks of the Betic Cordillera. Porosity was determined following the UNE-EN 1936:2007 standard. The dataset shows a strongly right-skewed distribution, with porosity values ranging from 0.03 % to 36.8 % and a median of 1.5 %. Porosity magnitude and variability systematically increase toward younger stratigraphic units.

New hydrological insights

The lowest porosity values are associated with Internal Zone metamorphic marbles and the Middle–Late Jurassic Ammonitico Rosso Formation, whereas the highest porosities occur in Upper Cretaceous and Cenozoic carbonates. A statistically significant inverse linear relationship between apparent (bulk) density and effective porosity is observed for both limestones and dolostones, supporting the use of bulk-density data as a first-order regional proxy for porosity estimation. The compiled database provides first-order constraints relevant to the matrix-controlled hydraulic behavior of Betic carbonate aquifers and supports preliminary, screening-level assessments of subsurface storage capacity. The applicability of the dataset is limited to regional-scale analyses and does not account for fracture or conduit permeability. Despite these limitations, the dataset contributes to groundwater-resource assessments, preliminary screening of geological formations for CO₂ and H₂ storage, and evaluations of durability in carbonate dimension stones.
西班牙南部的Betic Cordillera由古生代至新生代的碳酸盐岩地层组成,分布于内部、亚碳酸盐岩和前碳酸盐岩域。这些岩石包括变质大理岩、非变质灰岩和白云岩,它们沉积在不同的构造地层环境中。本研究编制并统计了866个实验室测量的Betic Cordillera碳酸盐岩的有效(开放)孔隙度值。孔隙率的测定遵循UNE-EN 1936:2007标准。数据集呈现强烈的右偏分布,孔隙度值范围为0.03 % ~ 36.8 %,中位数为1.5 %。孔隙度大小和变异性向更年轻的地层单位有系统地增加。孔隙度最低的地层为内变质大理岩和中晚侏罗世菊石组,孔隙度最高的地层为上白垩世和新生代碳酸盐岩。在灰岩和白云岩中,表观(体积)密度与有效孔隙度之间存在统计学上显著的反线性关系,支持将体积密度数据作为孔隙度估算的一级区域代理。编译后的数据库提供了与Betic碳酸盐含水层基质控制的水力行为相关的一级约束条件,并支持初步的筛选级地下储存能力评估。该数据集的适用性仅限于区域尺度分析,并且不考虑裂缝或管道渗透率。尽管存在这些局限性,但该数据集有助于地下水资源评估,对CO₂和H₂储存的地质构造进行初步筛选,以及对碳酸盐尺寸岩石的耐久性进行评估。
{"title":"Effective porosity in carbonate rocks from the Betic Cordillera (southern Spain): A regional dataset for reservoir and aquifer characterization","authors":"Carlos Marín-Lechado ,&nbsp;Antonio Pedrera ,&nbsp;Antonio González-Ramón ,&nbsp;Ana Ruiz-Constán ,&nbsp;Antonio Luis Molina ,&nbsp;Antonio Pulido-Bosch ,&nbsp;Iñaki Vadillo ,&nbsp;Concepción Fernández-Leyva ,&nbsp;Mónica Reyes ,&nbsp;Nuria Naranjo-Fernández ,&nbsp;Antonio Lope Morales ,&nbsp;Sergio Martos-Rosillo","doi":"10.1016/j.ejrh.2026.103173","DOIUrl":"10.1016/j.ejrh.2026.103173","url":null,"abstract":"<div><h3>Study region</h3><div>The Betic Cordillera (southern Spain) comprises carbonate formations ranging from Paleozoic to Cenozoic age, distributed across the Internal, Subbetic, and Prebetic domains. These include metamorphic marbles as well as non-metamorphic limestones and dolostones deposited in contrasting tectonostratigraphic settings.</div></div><div><h3>Study focus</h3><div>This study compiles and statistically characterizes 866 laboratory-measured effective (open) porosity values from carbonate rocks of the Betic Cordillera. Porosity was determined following the UNE-EN 1936:2007 standard. The dataset shows a strongly right-skewed distribution, with porosity values ranging from 0.03 % to 36.8 % and a median of 1.5 %. Porosity magnitude and variability systematically increase toward younger stratigraphic units.</div></div><div><h3>New hydrological insights</h3><div>The lowest porosity values are associated with Internal Zone metamorphic marbles and the Middle–Late Jurassic Ammonitico Rosso Formation, whereas the highest porosities occur in Upper Cretaceous and Cenozoic carbonates. A statistically significant inverse linear relationship between apparent (bulk) density and effective porosity is observed for both limestones and dolostones, supporting the use of bulk-density data as a first-order regional proxy for porosity estimation. The compiled database provides first-order constraints relevant to the matrix-controlled hydraulic behavior of Betic carbonate aquifers and supports preliminary, screening-level assessments of subsurface storage capacity. The applicability of the dataset is limited to regional-scale analyses and does not account for fracture or conduit permeability. Despite these limitations, the dataset contributes to groundwater-resource assessments, preliminary screening of geological formations for CO₂ and H₂ storage, and evaluations of durability in carbonate dimension stones.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103173"},"PeriodicalIF":5.0,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146174225","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Evaluating the three-cornered hat method for hourly satellite precipitation fusion in hydrological forecasting: A case study in a Tropical Andean Basin 评价三角帽方法在水文预报中的逐时卫星降水融合:以热带安第斯盆地为例
IF 5 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2026-04-01 Epub Date: 2026-01-29 DOI: 10.1016/j.ejrh.2026.103163
Patricio Luna Abril , Paul Muñoz , Esteban Samaniego , David F. Muñoz , María José Merizalde , Mario Lillo-Saavedra , Rolando Célleri

Study region

Jubones River Basin, a tropical mountainous basin in the Andes, Ecuador.

Study focus

Satellite precipitation products (SPPs) are essential for hydrological forecasting in data-scarce regions, yet their uncertainties increase at hourly timescales. This study evaluates the applicability of the Three-Cornered Hat (TCH) method for satellite-only precipitation fusion at hourly resolution and its hydrological value for machine learning–based runoff forecasting. TCH was applied to fuse IMERG, PERSIANN, and GSMaP precipitation estimates, and Random Forest runoff forecasts were developed for increasing lead times from 3 to 24 h. Results were benchmarked against a single-source SPP (IMERG-ER) and the multi-source MSWEP dataset, with particular emphasis on numerical issues arising during no-precipitation periods.

New hydrological insight

(1) Frequent dry periods induce strong statistical dependence among SPPs, leading to singular difference covariance matrices that disable the classical TCH formulation. (2) Introducing Tikhonov regularization permits consistent application of the method without altering precipitation magnitudes or temporal variability, enabling continuous satellite-only fusion. (3) Runoff forecasting skill is comparable across precipitation scenarios; MSWEP slightly outperforms others in NSE, KGE, and RMSE, while the TCH-based product consistently reduces bias. Overall, although regularized TCH is technically feasible for hourly precipitation fusion, its added value for operational runoff forecasting is limited under dry-hour-dominated conditions. These findings highlight both the potential and constraints of satellite-only fusion for near-real-time hydrological forecasting in data-scarce regions.
研究区域:jubones河流域,厄瓜多尔安第斯山脉的热带山地盆地。研究重点:卫星降水产品(SPPs)对数据稀缺地区的水文预报至关重要,但其不确定性在每小时时间尺度上增加。本研究评估了三角帽(TCH)方法在逐时分辨率的卫星降水融合中的适用性及其在基于机器学习的径流预测中的水文价值。TCH应用于融合IMERG、persann和GSMaP降水估计,并开发随机森林径流预测,将提前期从3增加到24 h。结果以单源SPP (imergp - er)和多源MSWEP数据集为基准,特别强调了无降水期间出现的数值问题。(1)频繁的干旱期导致spp之间的强统计依赖性,导致奇异差协方差矩阵使经典的TCH公式失效。(2)引入Tikhonov正则化允许在不改变降水强度或时间变率的情况下一致地应用该方法,从而实现连续的仅卫星融合。(3)径流预测技术在不同降水情景下具有可比性;MSWEP在NSE、KGE和RMSE方面的表现略优于其他产品,而基于技术的产品则始终如一地减少了偏差。总的来说,尽管正则化TCH在技术上对逐小时降水融合是可行的,但在干时为主的条件下,其对径流预报的附加价值有限。这些发现突出了在数据稀缺地区,仅用卫星融合进行近实时水文预报的潜力和限制。
{"title":"Evaluating the three-cornered hat method for hourly satellite precipitation fusion in hydrological forecasting: A case study in a Tropical Andean Basin","authors":"Patricio Luna Abril ,&nbsp;Paul Muñoz ,&nbsp;Esteban Samaniego ,&nbsp;David F. Muñoz ,&nbsp;María José Merizalde ,&nbsp;Mario Lillo-Saavedra ,&nbsp;Rolando Célleri","doi":"10.1016/j.ejrh.2026.103163","DOIUrl":"10.1016/j.ejrh.2026.103163","url":null,"abstract":"<div><h3>Study region</h3><div>Jubones River Basin, a tropical mountainous basin in the Andes, Ecuador.</div></div><div><h3>Study focus</h3><div>Satellite precipitation products (SPPs) are essential for hydrological forecasting in data-scarce regions, yet their uncertainties increase at hourly timescales. This study evaluates the applicability of the Three-Cornered Hat (TCH) method for satellite-only precipitation fusion at hourly resolution and its hydrological value for machine learning–based runoff forecasting. TCH was applied to fuse IMERG, PERSIANN, and GSMaP precipitation estimates, and Random Forest runoff forecasts were developed for increasing lead times from 3 to 24 h. Results were benchmarked against a single-source SPP (IMERG-ER) and the multi-source MSWEP dataset, with particular emphasis on numerical issues arising during no-precipitation periods.</div></div><div><h3>New hydrological insight</h3><div>(1) Frequent dry periods induce strong statistical dependence among SPPs, leading to singular difference covariance matrices that disable the classical TCH formulation. (2) Introducing Tikhonov regularization permits consistent application of the method without altering precipitation magnitudes or temporal variability, enabling continuous satellite-only fusion. (3) Runoff forecasting skill is comparable across precipitation scenarios; MSWEP slightly outperforms others in NSE, KGE, and RMSE, while the TCH-based product consistently reduces bias. Overall, although regularized TCH is technically feasible for hourly precipitation fusion, its added value for operational runoff forecasting is limited under dry-hour-dominated conditions. These findings highlight both the potential and constraints of satellite-only fusion for near-real-time hydrological forecasting in data-scarce regions.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103163"},"PeriodicalIF":5.0,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146079718","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Study on regional nonlinear seepage flow combining indoor tests and numerical simulation 室内试验与数值模拟相结合的区域非线性渗流研究
IF 5 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2026-04-01 Epub Date: 2026-01-21 DOI: 10.1016/j.ejrh.2026.103157
Yanrong Zhao , Haonan Wang , Jinguo Wang , Yikai Yang , Xiaosong Dong , Zhiheng Ma

Study region

The Xixiayuan area on the northern bank of the Yellow River in Luoyang, Henan Province, China, is characterized by a typical riverbank dual-structure aquifer system with high permeability. The Yellow River boundary water level is elevated, resulting in strong inward recharge within the region.

Study focus

In seepage analysis and modelling, the influence of non-Darcy effects cannot be neglected. However, most seepage problems are still directly simplified as linear flow, which can lead to substantial errors. In this study, a local-scale physical model test is used to investigate nonlinear seepage behaviour at the local scale, and two parameters are proposed to identify flow regime transitions: the nonlinear hydraulic conductivity KF and the non-Darcy effect parameter δ, which quantifies the degree of nonlinearity. To further assess the impact of nonlinear seepage on regional-scale groundwater level distribution, a nonlinear partial differential governing equation is derived from the Forchheimer equation. A numerical simulation code is then developed to model the nonlinear seepage field at the regional scale; it directly uses parameters obtained from indoor tests without additional adjustment of fluid or medium properties, thereby avoiding secondary parameter tuning. These findings provide a new approach for mechanistic investigation and numerical simulation of similar nonlinear seepage fields.

New hydrological insights for the region

Field sampling were used to investigate the nonlinear seepage behaviour of the sand–gravel medium at the local scale. Analysis of the test data and parameter KF trends shows that, owing to the granular structure of the sand–gravel deposits, seepage within the porous matrix tends to become nonlinear even at relatively low seepage velocities. Building on these results, a regional seepage field was simulated numerically. Using field observations as the benchmark, the independently developed regional-scale nonlinear seepage model reproduces the actual seepage conditions more accurately than a conventional linear model, reducing inflow prediction errors by approximately 40 % and producing maximum hydraulic gradients along the excavation slope that are about 16 % higher. These results have practical implications for hydraulic design in riverbank engineering and for preventing and mitigating seepage-induced failures.
河南洛阳黄河北岸西夏园地区具有典型的高渗河岸双结构含水层体系。黄河边界水位升高,区域内向内补给强烈。在渗流分析和建模中,非达西效应的影响不容忽视。然而,大多数渗流问题仍然直接简化为线性流动,这可能导致很大的误差。在本研究中,采用局部尺度物理模型试验研究了局部尺度下的非线性渗流行为,并提出了两个参数来识别流型转变:非线性水力传导系数KF和非达西效应参数δ,该参数量化了非线性程度。为了进一步评价非线性渗流对区域尺度地下水位分布的影响,从Forchheimer方程推导出非线性偏微分控制方程。在此基础上,建立了区域尺度下非线性渗流场的数值模拟程序;它直接使用室内试验获得的参数,无需对流体或介质特性进行额外调整,从而避免了二次参数调整。这些发现为类似非线性渗流场的力学研究和数值模拟提供了新的途径。新的水文见解为区域现场采样被用来研究非线性渗流行为的砂砾介质在局部尺度。试验数据和参数KF趋势分析表明,由于砂砾层的颗粒状结构,即使在较低的渗流速度下,多孔基质内的渗流也趋于非线性。在此基础上,对区域渗流场进行了数值模拟。独立开发的区域尺度非线性渗流模型以现场观测为基准,比传统的线性模型更准确地再现了实际渗流情况,将入流预测误差降低了约40% %,并使沿开挖边坡的最大水力梯度提高了约16% %。这些结果对堤岸工程的水力设计以及预防和减轻渗漏破坏具有实际意义。
{"title":"Study on regional nonlinear seepage flow combining indoor tests and numerical simulation","authors":"Yanrong Zhao ,&nbsp;Haonan Wang ,&nbsp;Jinguo Wang ,&nbsp;Yikai Yang ,&nbsp;Xiaosong Dong ,&nbsp;Zhiheng Ma","doi":"10.1016/j.ejrh.2026.103157","DOIUrl":"10.1016/j.ejrh.2026.103157","url":null,"abstract":"<div><h3>Study region</h3><div>The Xixiayuan area on the northern bank of the Yellow River in Luoyang, Henan Province, China, is characterized by a typical riverbank dual-structure aquifer system with high permeability. The Yellow River boundary water level is elevated, resulting in strong inward recharge within the region.</div></div><div><h3>Study focus</h3><div>In seepage analysis and modelling, the influence of non-Darcy effects cannot be neglected. However, most seepage problems are still directly simplified as linear flow, which can lead to substantial errors. In this study, a local-scale physical model test is used to investigate nonlinear seepage behaviour at the local scale, and two parameters are proposed to identify flow regime transitions: the nonlinear hydraulic conductivity <em>K</em><sub><em>F</em></sub> and the non-Darcy effect parameter <em>δ</em>, which quantifies the degree of nonlinearity. To further assess the impact of nonlinear seepage on regional-scale groundwater level distribution, a nonlinear partial differential governing equation is derived from the Forchheimer equation. A numerical simulation code is then developed to model the nonlinear seepage field at the regional scale; it directly uses parameters obtained from indoor tests without additional adjustment of fluid or medium properties, thereby avoiding secondary parameter tuning. These findings provide a new approach for mechanistic investigation and numerical simulation of similar nonlinear seepage fields.</div></div><div><h3>New hydrological insights for the region</h3><div>Field sampling were used to investigate the nonlinear seepage behaviour of the sand–gravel medium at the local scale. Analysis of the test data and parameter <em>K</em><sub><em>F</em></sub> trends shows that, owing to the granular structure of the sand–gravel deposits, seepage within the porous matrix tends to become nonlinear even at relatively low seepage velocities. Building on these results, a regional seepage field was simulated numerically. Using field observations as the benchmark, the independently developed regional-scale nonlinear seepage model reproduces the actual seepage conditions more accurately than a conventional linear model, reducing inflow prediction errors by approximately 40 % and producing maximum hydraulic gradients along the excavation slope that are about 16 % higher. These results have practical implications for hydraulic design in riverbank engineering and for preventing and mitigating seepage-induced failures.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103157"},"PeriodicalIF":5.0,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146024547","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Spatiotemporal evolution of permafrost deformation and active layer thickness in the eastern Qilian Mountains based on an enhanced multi-temporal InSAR 基于增强型多时相InSAR的祁连山东部多年冻土变形与活动层厚度时空演化
IF 5 2区 地球科学 Q1 WATER RESOURCES Pub Date : 2026-04-01 Epub Date: 2026-01-24 DOI: 10.1016/j.ejrh.2026.103151
Hongyu Zhou , Guanjun Wei , Yuncong Zhu , Xiying Dou

Study region

The eastern Qilian Mountains, located on the northeastern margin of the Tibetan Plateau, span elevations from ∼2600 to 5300 m around the Menyuan area. It is characterized by cold, alpine climatic conditions and hosts both permafrost and seasonally frozen ground, which are highly sensitive to climate change and have important hydrological and ecological implications.

Study focus

This study develops an enhanced multi-temporal InSAR framework to monitor frozen ground dynamics in the eastern Qilian Mountains using Sentinel-1 data from 2014 to 2024, with a particular focus on the permafrost–seasonally frozen ground transition zone around Menyuan. It addresses key challenges in permafrost monitoring by implementing a co-seismic deformation separation model, a Common Scene Stack (CSS)-based atmospheric correction method, and a time-series decomposition model with linearly varying annual amplitude to capture evolving freeze-thaw behavior under climate change.

New hydrological insights for the region

The results reveal clear hydrological and thermal contrasts between permafrost and seasonally frozen ground. Seasonally frozen ground exhibits higher seasonal deformation amplitudes, more rapid interannual changes, and shorter thermal response lags compared to permafrost, reflecting its more dynamic hydrothermal regime. The estimated freeze-thaw layer thickness ranges from 0 to 5.3 m, with thinning trends in seasonally frozen ground at lower elevations and slight thickening of active layers in high-elevation permafrost. These findings highlight ongoing frozen ground degradation and provide new insights into subsurface water-energy interactions and long-term cryospheric responses to climate warming in alpine environments.
东祁连山位于青藏高原东北缘,以门源地区为中心,海拔高度为~ 2600 ~ 5300 m。它的特点是寒冷的高山气候条件,拥有多年冻土和季节性冻土,对气候变化高度敏感,具有重要的水文和生态意义。本研究利用2014 - 2024年Sentinel-1数据,开发了一个增强型多时相InSAR框架,对祁连山东部冻土动态进行监测,特别关注门源附近的永久冻土-季节性冻土过渡区。通过实施同震形变分离模型、基于公共场景堆栈(CSS)的大气校正方法和具有线性变化年振幅的时间序列分解模型来捕捉气候变化下不断变化的冻融行为,解决了多年冻土监测中的关键挑战。研究结果揭示了永久冻土和季节性冻土之间清晰的水文和热对比。与多年冻土相比,季节性冻土表现出更大的季节变形幅度、更快速的年际变化和更短的热响应滞后,反映了其更动态的热液状态。冻融层厚度在0 ~ 5.3 m之间,低海拔季节冻土有变薄趋势,高海拔多年冻土活动层略有增厚。这些发现强调了正在进行的冻土退化,并为高山环境中地下水-能量相互作用和冰冻圈对气候变暖的长期响应提供了新的见解。
{"title":"Spatiotemporal evolution of permafrost deformation and active layer thickness in the eastern Qilian Mountains based on an enhanced multi-temporal InSAR","authors":"Hongyu Zhou ,&nbsp;Guanjun Wei ,&nbsp;Yuncong Zhu ,&nbsp;Xiying Dou","doi":"10.1016/j.ejrh.2026.103151","DOIUrl":"10.1016/j.ejrh.2026.103151","url":null,"abstract":"<div><h3>Study region</h3><div>The eastern Qilian Mountains, located on the northeastern margin of the Tibetan Plateau, span elevations from ∼2600 to 5300 m around the Menyuan area. It is characterized by cold, alpine climatic conditions and hosts both permafrost and seasonally frozen ground, which are highly sensitive to climate change and have important hydrological and ecological implications.</div></div><div><h3>Study focus</h3><div>This study develops an enhanced multi-temporal InSAR framework to monitor frozen ground dynamics in the eastern Qilian Mountains using Sentinel-1 data from 2014 to 2024, with a particular focus on the permafrost–seasonally frozen ground transition zone around Menyuan. It addresses key challenges in permafrost monitoring by implementing a co-seismic deformation separation model, a Common Scene Stack (CSS)-based atmospheric correction method, and a time-series decomposition model with linearly varying annual amplitude to capture evolving freeze-thaw behavior under climate change.</div></div><div><h3>New hydrological insights for the region</h3><div>The results reveal clear hydrological and thermal contrasts between permafrost and seasonally frozen ground. Seasonally frozen ground exhibits higher seasonal deformation amplitudes, more rapid interannual changes, and shorter thermal response lags compared to permafrost, reflecting its more dynamic hydrothermal regime. The estimated freeze-thaw layer thickness ranges from 0 to 5.3 m, with thinning trends in seasonally frozen ground at lower elevations and slight thickening of active layers in high-elevation permafrost. These findings highlight ongoing frozen ground degradation and provide new insights into subsurface water-energy interactions and long-term cryospheric responses to climate warming in alpine environments.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103151"},"PeriodicalIF":5.0,"publicationDate":"2026-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146024587","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
期刊
Journal of Hydrology-Regional Studies
全部 Acc. Chem. Res. ACS Applied Bio Materials ACS Appl. Electron. Mater. ACS Appl. Energy Mater. ACS Appl. Mater. Interfaces ACS Appl. Nano Mater. ACS Appl. Polym. Mater. ACS BIOMATER-SCI ENG ACS Catal. ACS Cent. Sci. ACS Chem. Biol. ACS Chemical Health & Safety ACS Chem. Neurosci. ACS Comb. Sci. ACS Earth Space Chem. ACS Energy Lett. ACS Infect. Dis. ACS Macro Lett. ACS Mater. Lett. ACS Med. Chem. Lett. ACS Nano ACS Omega ACS Photonics ACS Sens. ACS Sustainable Chem. Eng. ACS Synth. Biol. Anal. Chem. BIOCHEMISTRY-US Bioconjugate Chem. BIOMACROMOLECULES Chem. Res. Toxicol. Chem. Rev. Chem. Mater. CRYST GROWTH DES ENERG FUEL Environ. Sci. Technol. Environ. Sci. Technol. Lett. Eur. J. Inorg. Chem. IND ENG CHEM RES Inorg. Chem. J. Agric. Food. Chem. J. Chem. Eng. Data J. Chem. Educ. J. Chem. Inf. Model. J. Chem. Theory Comput. J. Med. Chem. J. Nat. Prod. J PROTEOME RES J. Am. Chem. Soc. LANGMUIR MACROMOLECULES Mol. Pharmaceutics Nano Lett. Org. Lett. ORG PROCESS RES DEV ORGANOMETALLICS J. Org. Chem. J. Phys. Chem. J. Phys. Chem. A J. Phys. Chem. B J. Phys. Chem. C J. Phys. Chem. Lett. Analyst Anal. Methods Biomater. Sci. Catal. Sci. Technol. Chem. Commun. Chem. Soc. Rev. CHEM EDUC RES PRACT CRYSTENGCOMM Dalton Trans. Energy Environ. Sci. ENVIRON SCI-NANO ENVIRON SCI-PROC IMP ENVIRON SCI-WAT RES Faraday Discuss. Food Funct. Green Chem. Inorg. Chem. Front. Integr. Biol. J. Anal. At. Spectrom. J. Mater. Chem. A J. Mater. Chem. B J. Mater. Chem. C Lab Chip Mater. Chem. Front. Mater. Horiz. MEDCHEMCOMM Metallomics Mol. Biosyst. Mol. Syst. Des. Eng. Nanoscale Nanoscale Horiz. Nat. Prod. Rep. New J. Chem. Org. Biomol. Chem. Org. Chem. Front. PHOTOCH PHOTOBIO SCI PCCP Polym. Chem.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1