Pub Date : 2026-01-31DOI: 10.1016/j.ejrh.2026.103127
Aylar Azizi , Amir Asadi Vaighan , Sina Sadeghfam , Rahman Khatibi
Study region
Aerosol dispersion is investigated in this study at the basin of Lake Urmia in Iran following its disappearance in 2023, a disaster triggered by mismanagement and the absence of effective planning.
Study focus
The study introduces the STOP-SaltWind framework composed of six consensually-selected data layers processed by a scoring system of rates and weights, including: Temperature, Precipitation, Salt (Normalised Difference Salinity Index) and Wind speed. Their information content is assessed through correlations; although the scores are subjective, their quality can be enhanced by methods similar to deep neural networks (DNN) using aerosol absorption index as a label dataset.
New hydrological insights
Basic framework results show that correlation in the data layers are non-random signal, achieving 41–60 % ‘overall accuracy’ in confusion matrix across three major salt-wind events (2021/2022/2023), and hence proof-of-concept for STOP-SaltWind. A supervised clustering DNN further enhanced overall accuracy to 80 % with consistently high Area Under Curve (AUC) values exceeding 0.9. These findings confirm that the information content of the framework is significant and inherent subjectivity reducible by advanced techniques, making it applicable to similar study areas. The desiccated lakebed exposes the basin to chronic aerosol dispersion risks, particularly at five hotspots, impacting health, the environment, agriculture, flora and fauna. Basin-wide risk exposures can be reduced by effective planning and governance, including measures to restore inflows and cover the exposed saltpan.
{"title":"Introducing the STOP-SaltWind framework enhanced by deep neural networks to investigate aerosol dispersion in Lake Urmia Basin","authors":"Aylar Azizi , Amir Asadi Vaighan , Sina Sadeghfam , Rahman Khatibi","doi":"10.1016/j.ejrh.2026.103127","DOIUrl":"10.1016/j.ejrh.2026.103127","url":null,"abstract":"<div><h3>Study region</h3><div>Aerosol dispersion is investigated in this study at the basin of Lake Urmia in Iran following its disappearance in 2023, a disaster triggered by mismanagement and the absence of effective planning.</div></div><div><h3>Study focus</h3><div>The study introduces the STOP-SaltWind framework composed of six consensually-selected data layers processed by a scoring system of rates and weights, including: Temperature, Precipitation, Salt (Normalised Difference Salinity Index) and Wind speed. Their information content is assessed through correlations; although the scores are subjective, their quality can be enhanced by methods similar to deep neural networks (DNN) using aerosol absorption index as a label dataset.</div></div><div><h3>New hydrological insights</h3><div>Basic framework results show that correlation in the data layers are non-random signal, achieving 41–60 % ‘overall accuracy’ in confusion matrix across three major salt-wind events (2021/2022/2023), and hence proof-of-concept for STOP-SaltWind. A supervised clustering DNN further enhanced overall accuracy to 80 % with consistently high Area Under Curve (AUC) values exceeding 0.9. These findings confirm that the information content of the framework is significant and inherent subjectivity reducible by advanced techniques, making it applicable to similar study areas. The desiccated lakebed exposes the basin to chronic aerosol dispersion risks, particularly at five hotspots, impacting health, the environment, agriculture, flora and fauna. Basin-wide risk exposures can be reduced by effective planning and governance, including measures to restore inflows and cover the exposed saltpan.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103127"},"PeriodicalIF":5.0,"publicationDate":"2026-01-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146079721","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}
Pub Date : 2026-01-31DOI: 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.
{"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 , Kebing Chen , Zhiwei Li , Jing Yuan , 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 (>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":"2026-01-31","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}
Pub Date : 2026-01-31DOI: 10.1016/j.ejrh.2026.103197
Dekang Zhao , Fan Miao , Guorui Feng , Xiang Li , Jiaying Cai , Shuning Dong , Yujiang Zhang , Yongqi Chen , Ruoyu Niu , Ziqing Yang
Study region
Liulin County, located on the eastern bank of the Yellow River (YR) in Shanxi Province, China, is characterized by complex terrain including mountains and loess plateaus under a semi-arid climate.
Study focus
To mitigate seasonal water supply instability and identify reliable groundwater sources, this study proposes a novel machine-learning framework integrating the Sparrow Search Algorithm (SSA) with Extreme Gradient Boosting (XGBoost). Utilizing Geographic Information System (GIS) and field surveys, a comprehensive hydrogeological dataset was constructed. The Boruta Algorithm (BA) was employed to eliminate redundant variables, while Random Forest (RF) evaluated feature importance. The proposed model was rigorously benchmarked against five alternative methods, including hybrids optimized by the Grey Wolf Optimizer (GWO). Furthermore, SHapley Additive exPlanations (SHAP) were applied to decipher the "black-box" nature of the models, quantifying feature contributions and non-linear interactions.
New hydrological insights for the region
The results demonstrate that the SSA-XGBoost model achieved superior predictive accuracy, yielding a maximum Area Under the Curve (AUC) of 0.8812. Consensus from RF and SHAP analyses identified lithology and altitude as the dominant controlling factors, while the Normalized Difference Vegetation Index (NDVI) and rainfall provided essential spatial variability. GIS-based zonation revealed that approximately 22.06 % of the study area possesses high groundwater potential. This framework effectively balances high predictive accuracy with transparency, providing a scientifically robust tool for sustainable groundwater management in complex terrain regions.
{"title":"Interpretable groundwater spring potential mapping in complex terrain of Liulin County, China, using SSA-XGBoost with GIS-based validation","authors":"Dekang Zhao , Fan Miao , Guorui Feng , Xiang Li , Jiaying Cai , Shuning Dong , Yujiang Zhang , Yongqi Chen , Ruoyu Niu , Ziqing Yang","doi":"10.1016/j.ejrh.2026.103197","DOIUrl":"10.1016/j.ejrh.2026.103197","url":null,"abstract":"<div><h3>Study region</h3><div>Liulin County, located on the eastern bank of the Yellow River (YR) in Shanxi Province, China, is characterized by complex terrain including mountains and loess plateaus under a semi-arid climate.</div></div><div><h3>Study focus</h3><div>To mitigate seasonal water supply instability and identify reliable groundwater sources, this study proposes a novel machine-learning framework integrating the Sparrow Search Algorithm (SSA) with Extreme Gradient Boosting (XGBoost). Utilizing Geographic Information System (GIS) and field surveys, a comprehensive hydrogeological dataset was constructed. The Boruta Algorithm (BA) was employed to eliminate redundant variables, while Random Forest (RF) evaluated feature importance. The proposed model was rigorously benchmarked against five alternative methods, including hybrids optimized by the Grey Wolf Optimizer (GWO). Furthermore, SHapley Additive exPlanations (SHAP) were applied to decipher the \"black-box\" nature of the models, quantifying feature contributions and non-linear interactions.</div></div><div><h3>New hydrological insights for the region</h3><div>The results demonstrate that the SSA-XGBoost model achieved superior predictive accuracy, yielding a maximum Area Under the Curve (AUC) of 0.8812. Consensus from RF and SHAP analyses identified lithology and altitude as the dominant controlling factors, while the Normalized Difference Vegetation Index (NDVI) and rainfall provided essential spatial variability. GIS-based zonation revealed that approximately 22.06 % of the study area possesses high groundwater potential. This framework effectively balances high predictive accuracy with transparency, providing a scientifically robust tool for sustainable groundwater management in complex terrain regions.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103197"},"PeriodicalIF":5.0,"publicationDate":"2026-01-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146079717","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}
The Wadi Djendjen alluvial plain, located within a Mediterranean coastal aquifer in northeastern Algeria.
Study focus
In April 2021, thirty-one groundwater samples were collected to assess the hydrogeochemical characteristics and overall quality of the aquifer. An integrated methodological approach was employed, combining multivariate statistical analyses (Principal Component Analysis and Hierarchical Cluster Analysis), hydrochemical diagrams, and water quality indices. Electrical conductivity (EC) ranged from 325 to 1896 µS/cm, while total dissolved solids (TDS) ranged from 208 to 1213 mg/L, indicating slightly to moderately mineralized water. Two dominant hydrochemical facies were identified: Ca2⁺-Mg2⁺-Cl⁻ and Ca2⁺-HCO3⁻ (84 % and 16 % of samples, respectively), reflecting the combined effects of freshwater recharge and seawater intrusion. Principal Component Analysis revealed that groundwater chemistry is primarily controlled by geogenic processes (mineral dissolution, dedolomitization, and ion exchange) together with anthropogenic inputs from agricultural return flows and domestic effluents.
New hydrological insights
Drinking water quality assessment based on the water quality index (WQI) revealed pronounced spatial variability. Approximately 50 % of samples were classified as excellent to good quality (WQI ≤ 50), while the remaining samples ranged from poor to unsuitable for human consumption (50 < WQI < 100), with one sample (P8) deemed non-potable (WQI = 138). Similarly, the Irrigation Water Quality Index (IWQI) delineated three distinct irrigation suitability zones, including a high-restriction zone associated with industrial and port-related activities. These findings pinpoint critical zones of groundwater degradation and provide a robust scientific basis for targeted groundwater management strategies aimed at protecting public health and ensuring agricultural sustainability.
{"title":"Integrating water quality indices and multivariate statistics for groundwater assessment in a Mediterranean coastal aquifer, Northeast Algeria","authors":"Faouzi Zahi , Abdelmalek Drouiche , Fethi Medjani , Azzeddine Reghais , Mohamed A.E. Abdel Rahman , Ilyes Mecibah , Antonio Scopa , Shao Bing Fong , Ahmed Refaee","doi":"10.1016/j.ejrh.2026.103200","DOIUrl":"10.1016/j.ejrh.2026.103200","url":null,"abstract":"<div><h3>Study region</h3><div>The Wadi Djendjen alluvial plain, located within a Mediterranean coastal aquifer in northeastern Algeria.</div></div><div><h3>Study focus</h3><div>In April 2021, thirty-one groundwater samples were collected to assess the hydrogeochemical characteristics and overall quality of the aquifer. An integrated methodological approach was employed, combining multivariate statistical analyses (Principal Component Analysis and Hierarchical Cluster Analysis), hydrochemical diagrams, and water quality indices. Electrical conductivity (EC) ranged from 325 to 1896 µS/cm, while total dissolved solids (TDS) ranged from 208 to 1213 mg/L, indicating slightly to moderately mineralized water. Two dominant hydrochemical facies were identified: Ca<sup>2</sup>⁺-Mg<sup>2</sup>⁺-Cl⁻ and Ca<sup>2</sup>⁺-HCO<sub>3</sub>⁻ (84 % and 16 % of samples, respectively), reflecting the combined effects of freshwater recharge and seawater intrusion. Principal Component Analysis revealed that groundwater chemistry is primarily controlled by geogenic processes (mineral dissolution, dedolomitization, and ion exchange) together with anthropogenic inputs from agricultural return flows and domestic effluents.</div></div><div><h3>New hydrological insights</h3><div>Drinking water quality assessment based on the water quality index (WQI) revealed pronounced spatial variability. Approximately 50 % of samples were classified as excellent to good quality (WQI ≤ 50), while the remaining samples ranged from poor to unsuitable for human consumption (50 < WQI < 100), with one sample (P8) deemed non-potable (WQI = 138). Similarly, the Irrigation Water Quality Index (IWQI) delineated three distinct irrigation suitability zones, including a high-restriction zone associated with industrial and port-related activities. These findings pinpoint critical zones of groundwater degradation and provide a robust scientific basis for targeted groundwater management strategies aimed at protecting public health and ensuring agricultural sustainability.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103200"},"PeriodicalIF":5.0,"publicationDate":"2026-01-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146079811","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}
Pub Date : 2026-01-31DOI: 10.1016/j.ejrh.2026.103186
Kaize Zhang , Leyi Zhang , Zengchuan Dong , Li Guo , Carlos R. Mello , Xiangyang Sun , Bihang Fan
Study region
Yiluo River Basin, China.
Study focus
Under the influence of climate change, China has seen an increase in flood frequency, resulting in substantial flood damage. However, current flood drainage rights (FDR) allocation methods are hindered by incomplete assessments of driving factors and methodological limitations.
To address these challenges, this study first adopts a resilience strategy as a guiding framework, incorporating the dynamic regional flood response to climate change as a key hydrological driver, and establishes a comprehensive qualitative indicator system. Second, a β-Variational Autoencoder (β-VAE) is introduced to address the high-dimensional, non-linear, and non-normal characteristics of FDR data. Subsequently, applying this model to the Yiluo River Basin using 2004–2023 data yields the following FDR allocation among five cities, aiming to develop a scientifically sound and efficient FDR allocation scheme.
New hydrological insights for the region
The results indicate that the FDR allocation ratios for the five cities in the Yiluo River Basin should be: Zhengzhou (29.60 %), Luoyang (23.67 %), Shangluo (16.31 %), Sanmenxia (15.61 %), and Weinan (14.81 %). Comparative analysis shows that the β-VAE model achieves faster data convergence and lower fluctuations, thereby improving the computational efficiency of the allocation scheme. Moreover, incorporating the dynamic regional flood response under climate change enhances the rationality and scientific rigor of the allocation scheme. This approach offers a viable pathway to support more effective flood management in China.
{"title":"Research on the flood drainage rights allocation method incorporating the dynamic response of floods to climate change","authors":"Kaize Zhang , Leyi Zhang , Zengchuan Dong , Li Guo , Carlos R. Mello , Xiangyang Sun , Bihang Fan","doi":"10.1016/j.ejrh.2026.103186","DOIUrl":"10.1016/j.ejrh.2026.103186","url":null,"abstract":"<div><h3>Study region</h3><div>Yiluo River Basin, China.</div></div><div><h3>Study focus</h3><div>Under the influence of climate change, China has seen an increase in flood frequency, resulting in substantial flood damage. However, current flood drainage rights (FDR) allocation methods are hindered by incomplete assessments of driving factors and methodological limitations.</div><div>To address these challenges, this study first adopts a resilience strategy as a guiding framework, incorporating the dynamic regional flood response to climate change as a key hydrological driver, and establishes a comprehensive qualitative indicator system. Second, a β-Variational Autoencoder (β-VAE) is introduced to address the high-dimensional, non-linear, and non-normal characteristics of FDR data. Subsequently, applying this model to the Yiluo River Basin using 2004–2023 data yields the following FDR allocation among five cities, aiming to develop a scientifically sound and efficient FDR allocation scheme.</div></div><div><h3>New hydrological insights for the region</h3><div>The results indicate that the FDR allocation ratios for the five cities in the Yiluo River Basin should be: Zhengzhou (29.60 %), Luoyang (23.67 %), Shangluo (16.31 %), Sanmenxia (15.61 %), and Weinan (14.81 %). Comparative analysis shows that the β-VAE model achieves faster data convergence and lower fluctuations, thereby improving the computational efficiency of the allocation scheme. Moreover, incorporating the dynamic regional flood response under climate change enhances the rationality and scientific rigor of the allocation scheme. This approach offers a viable pathway to support more effective flood management in China.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103186"},"PeriodicalIF":5.0,"publicationDate":"2026-01-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146079806","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}
Pub Date : 2026-01-30DOI: 10.1016/j.ejrh.2026.103183
Sheng Wang , Xingyu Wang , Yuzhe Wang , Tandong Yao , Jianchen Pu , Jinfeng Wang
Study region
Qiyi Glacier in the Qilian Mountains, China.
Study focus
Glacier flow is one of the important processes in the glacier development and evolution. It provides a scientific basis for assessing glacial disaster risks, and is of great significance for formulating adaptive strategies in response to glacial environmental variations. In this study, a two-dimensional higher-order flow-band glacier flow model (PoLIM) was constructed to analyze the spatio-temporal patterns of surface flow velocity on Qiyi Glacier, and the future dynamics and dominant influencing factors of flow velocity under various climate scenarios were investigated.
New hydrological insights for the region
Impacted by glacier (ice) volume and thickness, the annual variation in surface flow velocity of Qiyi Glacier exhibits a decreasing trend, declining from 16 m a−1 in 1958–5.97 m a−1 in 2021, with significantly higher flow velocity during the ablation season compared to the non-ablation season. The mean glacier surface flow velocity along the main flowline was 6.92 ± 0.13 m a−1 from 2017 to 2021. Under three future scenarios, this velocity is projected to decrease to 0.71 ± 0.13 m a−1, 0.73 ± 0.12 m a−1 and 0.47 ± 0.09 m a−1 by 2050, respectively. The spatio-temporal patterns of glacier flow velocity are primarily related to glacier scale (ice thickness) and its variation, with climate warming-induced basal sliding serving as a principal driver of velocity changes in certain part of the glacier.
祁连山七一冰川研究区冰川流动是冰川发育演化的重要过程之一。这为评估冰川灾害风险提供了科学依据,对制定应对冰川环境变化的适应策略具有重要意义。本文通过构建二维高阶流带冰川流动模型(PoLIM),分析了七一冰川地表流速的时空格局,探讨了不同气候情景下地表流速的未来动态及其主导影响因素。受冰川(冰)体积和厚度的影响,七宜冰川地表流速年际变化呈减小趋势,从1958年的16 m a−1下降至2021年的5.97 m a−1,消融期流速明显高于非消融期。2017 - 2021年冰川地表流速平均值为6.92 ± 0.13 m a−1。三个未来情景下,这个速度预计将下降到0.71 ±0.13 m−1, 0.73±0.12 m −1和0.47±0.09 m−1到2050年,分别。冰川流速的时空格局主要与冰川尺度(冰厚)及其变化有关,气候变暖引起的基底滑动是部分冰川流速变化的主要驱动因素。
{"title":"Diagnostic and prognostic modeling of glacier dynamics and the driving factors in the Qilian Mountains, China","authors":"Sheng Wang , Xingyu Wang , Yuzhe Wang , Tandong Yao , Jianchen Pu , Jinfeng Wang","doi":"10.1016/j.ejrh.2026.103183","DOIUrl":"10.1016/j.ejrh.2026.103183","url":null,"abstract":"<div><h3>Study region</h3><div>Qiyi Glacier in the Qilian Mountains, China.</div></div><div><h3>Study focus</h3><div>Glacier flow is one of the important processes in the glacier development and evolution. It provides a scientific basis for assessing glacial disaster risks, and is of great significance for formulating adaptive strategies in response to glacial environmental variations. In this study, a two-dimensional higher-order flow-band glacier flow model (PoLIM) was constructed to analyze the spatio-temporal patterns of surface flow velocity on Qiyi Glacier, and the future dynamics and dominant influencing factors of flow velocity under various climate scenarios were investigated.</div></div><div><h3>New hydrological insights for the region</h3><div>Impacted by glacier (ice) volume and thickness, the annual variation in surface flow velocity of Qiyi Glacier exhibits a decreasing trend, declining from 16 m a<sup>−1</sup> in 1958–5.97 m a<sup>−1</sup> in 2021, with significantly higher flow velocity during the ablation season compared to the non-ablation season. The mean glacier surface flow velocity along the main flowline was 6.92 ± 0.13 m a<sup>−1</sup> from 2017 to 2021. Under three future scenarios, this velocity is projected to decrease to 0.71 ± 0.13 m a<sup>−1</sup>, 0.73 ± 0.12 m a<sup>−1</sup> and 0.47 ± 0.09 m a<sup>−1</sup> by 2050, respectively. The spatio-temporal patterns of glacier flow velocity are primarily related to glacier scale (ice thickness) and its variation, with climate warming-induced basal sliding serving as a principal driver of velocity changes in certain part of the glacier.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103183"},"PeriodicalIF":5.0,"publicationDate":"2026-01-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146079719","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}
Pub Date : 2026-01-30DOI: 10.1016/j.ejrh.2026.103175
Peng Wang , Xizhen Wu , Haowen Tan , Hongyu Zhi , Zhangli Chen , Lei Huang
Study region
Gulou district, Nanjing, China.
Study focus
Facing escalating extreme precipitation and urbanization, urban infrastructure resilience is critical. While previous recovery strategies often used optimization models, they largely overlooked the underlying mechanisms driving efficient recovery. This study addresses this gap by developing an optimal strategy for post-extreme precipitation infrastructure recovery. We establish a multi-objective optimization model and a novel recovery efficiency index to evaluate recovery combinations, specifically focusing on Gulou District. The analysis considers recovery objectives, infrastructure categories, and spatial distribution to identify efficient recovery methods.
New hydrological insights for the region
Findings reveal significant spatial and categorical disparities in recovery efficiency, emphasizing the need for context-specific strategies. Optimal recovery methods depend on the interplay between infrastructure type and their geographic clustering. Strategic prioritization of spatially interconnected infrastructure and category-specific recovery sequences can enhance overall efficiency by 15–20 %. These insights provide actionable guidance for policymakers to design resilient recovery plans under climate change pressures. Future refinements will incorporate dynamic interactions between adjacent infrastructure systems to further optimize recovery outcomes.
{"title":"Urban infrastructure recovery strategy under extreme precipitation based on multi-objective optimization algorithm","authors":"Peng Wang , Xizhen Wu , Haowen Tan , Hongyu Zhi , Zhangli Chen , Lei Huang","doi":"10.1016/j.ejrh.2026.103175","DOIUrl":"10.1016/j.ejrh.2026.103175","url":null,"abstract":"<div><h3>Study region</h3><div>Gulou district, Nanjing, China.</div></div><div><h3>Study focus</h3><div>Facing escalating extreme precipitation and urbanization, urban infrastructure resilience is critical. While previous recovery strategies often used optimization models, they largely overlooked the underlying mechanisms driving efficient recovery. This study addresses this gap by developing an optimal strategy for post-extreme precipitation infrastructure recovery. We establish a multi-objective optimization model and a novel recovery efficiency index to evaluate recovery combinations, specifically focusing on Gulou District. The analysis considers recovery objectives, infrastructure categories, and spatial distribution to identify efficient recovery methods.</div></div><div><h3>New hydrological insights for the region</h3><div>Findings reveal significant spatial and categorical disparities in recovery efficiency, emphasizing the need for context-specific strategies. Optimal recovery methods depend on the interplay between infrastructure type and their geographic clustering. Strategic prioritization of spatially interconnected infrastructure and category-specific recovery sequences can enhance overall efficiency by 15–20 %. These insights provide actionable guidance for policymakers to design resilient recovery plans under climate change pressures. Future refinements will incorporate dynamic interactions between adjacent infrastructure systems to further optimize recovery outcomes.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103175"},"PeriodicalIF":5.0,"publicationDate":"2026-01-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146079829","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}
Pub Date : 2026-01-30DOI: 10.1016/j.ejrh.2026.103178
Bartholomew Hill , Qiuhua Liang , Huili Chen , Lee Bosher
Study region
Cocker River catchment (145 km²), Lake District, Cumbria, United Kingdom.
Study focus
This study investigates the influence that Natural Flood Management (NFM) features have on flood behaviour at the catchment scale using a high-resolution, two-dimensional hydrodynamic modelling approach. A high-performance computing framework, based on the High-Performance Integrated hydrodynamic Modelling System (HiPIMS), was applied to simulate two events; 1) pre-NFM implementation - Storm Desmond flood in 2015, and 2) post-NFM implementation – High rainfall event in 2021. Leaky wooden barriers and other NFM features were explicitly represented using UAV-derived digital terrain data at 2 m and 4 m spatial resolutions.
Hydrological insights
The simulations indicate that the hydrological response to NFM within the Cocker catchment is strongly event dependent. Clearer flow attenuation and hydrograph smoothing were observed during the smaller 2021 event, while impacts during the extreme 2015 event were modest and spatially variable. Localised water retention within the Whinlatter sub-catchment translated into small but measurable downstream changes in flood levels, alongside indications that delayed flows may interact with contributions from other tributaries. These findings highlight the importance of event magnitude, spatial configuration, and flow timing when assessing the role of NFM in catchment-scale flood risk management.
{"title":"From reach to catchment-scale impacts: High-resolution hydrodynamic modelling of Nature-based solutions in the Cocker Catchment, UK","authors":"Bartholomew Hill , Qiuhua Liang , Huili Chen , Lee Bosher","doi":"10.1016/j.ejrh.2026.103178","DOIUrl":"10.1016/j.ejrh.2026.103178","url":null,"abstract":"<div><h3>Study region</h3><div>Cocker River catchment (145 km²), Lake District, Cumbria, United Kingdom.</div></div><div><h3>Study focus</h3><div>This study investigates the influence that Natural Flood Management (NFM) features have on flood behaviour at the catchment scale using a high-resolution, two-dimensional hydrodynamic modelling approach. A high-performance computing framework, based on the High-Performance Integrated hydrodynamic Modelling System (HiPIMS), was applied to simulate two events; 1) pre-NFM implementation - Storm Desmond flood in 2015, and 2) post-NFM implementation – High rainfall event in 2021. Leaky wooden barriers and other NFM features were explicitly represented using UAV-derived digital terrain data at 2 m and 4 m spatial resolutions.</div></div><div><h3>Hydrological insights</h3><div>The simulations indicate that the hydrological response to NFM within the Cocker catchment is strongly event dependent. Clearer flow attenuation and hydrograph smoothing were observed during the smaller 2021 event, while impacts during the extreme 2015 event were modest and spatially variable. Localised water retention within the Whinlatter sub-catchment translated into small but measurable downstream changes in flood levels, alongside indications that delayed flows may interact with contributions from other tributaries. These findings highlight the importance of event magnitude, spatial configuration, and flow timing when assessing the role of NFM in catchment-scale flood risk management.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103178"},"PeriodicalIF":5.0,"publicationDate":"2026-01-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146079807","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}
Pub Date : 2026-01-29DOI: 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.
{"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 , Paul Muñoz , Esteban Samaniego , David F. Muñoz , María José Merizalde , Mario Lillo-Saavedra , 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":"2026-01-29","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}
Pub Date : 2026-01-29DOI: 10.1016/j.ejrh.2026.103177
Paul Xavier Flanagan
Study region
Central Oklahoma, USA
Study focus
Research shows that the timing of regional growing season maxima in daily temperature and precipitation is related to the sub-seasonal to seasonal variability of precipitation. However, it is uncertain if these results will translate to the local scale. The studies goal is to extend asynchronous difference index (ADI) research to the Fort Reno location within the United States Department of Agriculture (USDA)-Agricultural Research Service (ARS) Oklahoma and Central Plains Agricultural Research Center. Numerous datasets were combined to investigate ADI and its impacts on meteorological, hydrological, and agricultural facets of the environment. Analysis shows that ADI impacts the environment similarly to regional results, namely that April to June precipitation is enhanced (reduced) for positive (negative) ADI growing seasons and July to October precipitation is reduced (enhanced). These regimes of precipitation variability impacted local hydrology and agricultural yields. Overall, this study shows that the regional aspects of ADI translate to the local scale, and that the regimes of ADI relate to distinct hydrologic and agricultural outcomes.
New hydrological insights for the region
This research shows that ADI relates to not only meteorological features of the environment, but also to local hydrological and agricultural conditions. Knowledge of ADI can potentially be used to infer the impact of heavy precipitation events later in the year and water requirements for future growing seasons.
{"title":"Investigating Fort Reno, Oklahoma, growing season temperature and precipitation maxima temporal variability and corresponding impacts to hydrological and agricultural observations","authors":"Paul Xavier Flanagan","doi":"10.1016/j.ejrh.2026.103177","DOIUrl":"10.1016/j.ejrh.2026.103177","url":null,"abstract":"<div><h3>Study region</h3><div>Central Oklahoma, USA</div></div><div><h3>Study focus</h3><div>Research shows that the timing of regional growing season maxima in daily temperature and precipitation is related to the sub-seasonal to seasonal variability of precipitation. However, it is uncertain if these results will translate to the local scale. The studies goal is to extend asynchronous difference index (ADI) research to the Fort Reno location within the United States Department of Agriculture (USDA)-Agricultural Research Service (ARS) Oklahoma and Central Plains Agricultural Research Center. Numerous datasets were combined to investigate ADI and its impacts on meteorological, hydrological, and agricultural facets of the environment. Analysis shows that ADI impacts the environment similarly to regional results, namely that April to June precipitation is enhanced (reduced) for positive (negative) ADI growing seasons and July to October precipitation is reduced (enhanced). These regimes of precipitation variability impacted local hydrology and agricultural yields. Overall, this study shows that the regional aspects of ADI translate to the local scale, and that the regimes of ADI relate to distinct hydrologic and agricultural outcomes.</div></div><div><h3>New hydrological insights for the region</h3><div>This research shows that ADI relates to not only meteorological features of the environment, but also to local hydrological and agricultural conditions. Knowledge of ADI can potentially be used to infer the impact of heavy precipitation events later in the year and water requirements for future growing seasons.</div></div>","PeriodicalId":48620,"journal":{"name":"Journal of Hydrology-Regional Studies","volume":"64 ","pages":"Article 103177"},"PeriodicalIF":5.0,"publicationDate":"2026-01-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146079703","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}