Hydrological Processes最新文献

{"title":"40@40: 40 Key Papers From the First 40 Years of Hydrological Processes","authors":"Doerthe Tetzlaff, Christian Birkel, Sean K. Carey, Tanya Doody, James McNamara, Des E.Walling","doi":"10.1002/hyp.70695","DOIUrl":"https://doi.org/10.1002/hyp.70695","url":null,"abstract":"","PeriodicalId":13189,"journal":{"name":"Hydrological Processes","volume":"40 9","pages":""},"PeriodicalIF":3.1,"publicationDate":"2026-09-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148942858","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Drivers of Runoff Sensitivity in the Rivers of Great Britain","authors":"Pei Xue,&nbsp;Dominick Spracklen,&nbsp;Joseph Holden","doi":"10.1002/hyp.70696","DOIUrl":"https://doi.org/10.1002/hyp.70696","url":null,"abstract":"<p>Runoff sensitivity refers to the magnitude of seasonal or annual river discharge change in response to changes in other driving factors. We analysed the runoff sensitivity of 547 watersheds in Great Britain (GB) using data from 2000 to 2015, considering 14 driving factors, including climate, terrain and soils. Using interquartile ranges of daily discharge at annual and seasonal scales, we applied generalised additive models to quantify the influence of each factor. Partial dependence analysis was used to rank driver importance, and perturbation experiments simulated runoff responses under different change levels. Our results reveal strong spatial and temporal variability in runoff sensitivity across GB. Sensitivity is higher in central-east and southwest Scotland as well as southern England. Relative runoff sensitivity, defined as runoff response normalised by precipitation variability, is especially elevated in northwest Scotland and southwest England. On an annual scale, key drivers include evergreen woodland cover, soil saturated hydraulic conductivity and mean daily potential evapotranspiration (PET). In contrast, seasonal sensitivity is shaped by varying combinations of PET, temperature, precipitation, evergreen woodland cover and terrain slope, with precipitation influence differing most across seasons. For relative sensitivity, PET and evergreen woodland are consistently dominant, while temperature, precipitation and soil permeability also contribute seasonally. Perturbation analysis highlights urban, shrub and evergreen woodland cover as having the greatest effects on runoff sensitivity. These findings provide a basis for identifying which land management practices, catchment properties and climate change factors might be most important influencers of riverflow change in different regional settings in GB, thereby supporting evidence-based catchment management and water resources planning under changing environmental conditions.</p>","PeriodicalId":13189,"journal":{"name":"Hydrological Processes","volume":"40 9","pages":""},"PeriodicalIF":3.1,"publicationDate":"2026-09-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/hyp.70696","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148942859","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Daily Pan Evaporation Reconstruction Reveals a Climate-Gradient-Dependent Evaporation Paradox Across China","authors":"Ruibiao Li,&nbsp;Xi Cheng,&nbsp;Kaikui Cai,&nbsp;Lian Hu,&nbsp;Kai Huang,&nbsp;Jincheng Li,&nbsp;Yong Liu,&nbsp;Qingsong Jiang","doi":"10.1002/hyp.70694","DOIUrl":"https://doi.org/10.1002/hyp.70694","url":null,"abstract":"<div>\u0000 \u0000 <p>Accurate daily pan evaporation (E_pan) records are needed to diagnose changes in atmospheric evaporative demand, but long-term analyses can be confounded by instrument transitions and inconsistent treatment of missing or freezing-period observations. We developed an observation-aware framework that combined instrument homogenisation, sequence-based daily reconstruction and interpretable attribution across China's climate gradients during 2000–2024. Historical D20 observations were converted to E601-equivalent values with a meteorology-dependent random forest model, producing a homogenised daily dataset for 1351 stations. A Transformer driven exclusively by meteorological forcing then reconstructed daily E_pan, and SHAP analysis quantified the contributions of thermal, radiative, aerodynamic and moisture-related variables. The Transformer achieved the highest performance among the evaluated models (NSE = 0.76; RMSE = 0.83 mm day⁻¹). The reconstruction showed that the evaporation paradox was spatially heterogeneous rather than a uniform response to warming. E_pan increased significantly in the Huaihe, Haihe and Yangtze River Basins, whereas it declined significantly in the Songliao River Basin (−0.74 mm a⁻¹, <i>p</i> &lt; 0.01). There, declining shortwave radiation and moisture-related constraints offset the positive contribution of temperature. In contrast with previous studies that variously emphasised land–atmosphere complementarity, declining wind speed, reduced solar input or rising vapour-pressure deficit, the Chinese results showed that the controlling balance changed among hydroclimatic regimes. This workflow separated observing-system discontinuities from climate signals before daily reconstruction and attribution, and can be adapted to other heterogeneous monitoring networks that require local data, recalibration and independent validation.</p>\u0000 </div>","PeriodicalId":13189,"journal":{"name":"Hydrological Processes","volume":"40 9","pages":""},"PeriodicalIF":3.1,"publicationDate":"2026-09-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148942803","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Groundwater Leakage, Resolved—The Hidden Flux Connecting Ridge to Reef in the Hawaiian Islands","authors":"Jasper Oshun,&nbsp;David Dralle,&nbsp;Gregory P. Asner","doi":"10.1002/hyp.70681","DOIUrl":"https://doi.org/10.1002/hyp.70681","url":null,"abstract":"<div>\u0000 \u0000 <p>In Hawaiʻi, groundwater draining from upland areas of high recharge provides virtually all drinking water and delivers freshwater nutrients (as well as contaminants) to ecosystems in the nearshore environment. Despite the importance of groundwater flow, its hidden nature makes it difficult to observe and quantify, which results in a poor understanding of its spatiotemporal dynamics from the uplands to the coast. We combine a storage-discharge approach with a long-term (7+ years) water balance to quantify the relationship between catchment storage and stream discharge in 11 (USGS-gaged) watersheds across the Hawaiian Islands. We then use each watershed's storage-discharge relationship to resolve daily estimates of catchment storage and the ‘groundwater leakage’ flux emanating from the watersheds. The resolved mean specific daily leakage is consistent with compiled measurements of submarine groundwater discharge (SGD) at the coast downstream of the 11 watersheds and upland leakage appears to be hydraulically connected to head responses in a basal aquifer. Example groundwater leakage hydrographs from Hālawa (Oʻahu) and Waiākea (Hawaiʻi) watersheds resolve temporal dynamics of groundwater flowing beneath the urban centres of Honolulu and Hilo, where contaminants enter aquifers, threaten drinking water supply, and degrade coastal environments. Although additional data are needed to validate results across space and time, resolving the groundwater leakage flux reveals a previously hidden portion of the hydrologic cycle that can inform modelling of water resources and water quality in leaky watersheds in Hawaiʻi and beyond.</p>\u0000 </div>","PeriodicalId":13189,"journal":{"name":"Hydrological Processes","volume":"40 9","pages":""},"PeriodicalIF":3.1,"publicationDate":"2026-09-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148942974","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Wildfire Impacts on Hydrology: A Forested Catchment Case Study in Temperate Australia","authors":"Negash Roba,&nbsp;Ketema Zeleke,&nbsp;Andrew Hall,&nbsp;Nigussie Haregeweyn","doi":"10.1002/hyp.70676","DOIUrl":"https://doi.org/10.1002/hyp.70676","url":null,"abstract":"<p>As climate change worsens fire weather and intensifies wildfires, understanding how catchment hydrology and water balance respond post-fire becomes increasingly important. However, the roles of land use/land cover and soil attributes in shaping post-fire hydrological processes under varying wildfire severities remain insufficiently studied. This study applied the Soil and Water Assessment Tool (SWAT) to characterise and quantify wildfire-induced changes in the water balance across different realistic post-fire scenarios. The Gudgenby River catchment in temperate Australia was selected as the case study area. The following scenarios describe catchment hydrologic conditions: (1) baseline (pre-fire) of 2019–20 wildfires, (2) post-fire Scenario 1 (immediately after the event, March 2020), (3) Scenario 2 (1 year after, March 2021), (4) Scenario 3 (2 years after, March 2022), and (5) Scenario 4 (5 years after, March 2025). The SWAT model was calibrated for the baseline (pre-fire) scenario using observed streamflow to enable detailed sub-catchment-level analysis of post-fire changes. The model performed well, with <i>R</i>² values of 0.83 and 0.78 for the calibration and validation periods, respectively, with corresponding NSE values of 0.79 and 0.74. Immediately after a wildfire (Scenario 1), surface runoff increased by an average of 34.7% across the sub-catchment. In Scenarios 2 and 3, runoff increased slightly (0.96%), but in Scenario 4, it increased by 1.04% and then decreased relative to Scenario 1 as vegetation began to resprout. Evapotranspiration showed the opposite response: it decreased by 10.3% immediately after the wildfire, then increased by 1.6%, 0.3%, and 0.8% for Scenarios 2, 3, and 4, respectively, as vegetation recovered. Similarly, groundwater recharge declined by 17.7%, 9.1%, and 1.4% in Scenarios 1, 2, and 3, respectively, but increased significantly (22.2%) in Scenario 4, indicating delayed subsurface recovery. These findings offer valuable insights for developing realistic post-fire water management plans and support the design of adaptation strategies and policies for sustainable water management in Australia's temperate zones.</p>","PeriodicalId":13189,"journal":{"name":"Hydrological Processes","volume":"40 9","pages":""},"PeriodicalIF":3.1,"publicationDate":"2026-09-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/hyp.70676","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148942973","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Threshold Behaviour and Loss Mechanisms of Water and Nitrogen Transport in Karst Soil Columns Regulated by Fracture-Filling Particle Size","authors":"Yang Ya,&nbsp;Liu Dongdong","doi":"10.1002/hyp.70686","DOIUrl":"https://doi.org/10.1002/hyp.70686","url":null,"abstract":"<div>\u0000 \u0000 <p>Karst regions, where extensive fracture networks accelerate water and nitrogen losses, face severe challenges to ecological restoration, yet how fracture-filling particle size regulates coupled water–nitrogen dynamics through nonlinear threshold behaviour remains poorly understood. Here, we conducted field soil column experiments under natural rainfall using three fracture-filling particle size gradations (C0: 3–5 mm; C1: 6–13 mm; C2: 10–30 mm), coupled with PRA and RSS threshold identification. Medium-sized fractures (C1) achieved the most favourable water retention through a hydraulic conductivity–capillary retention balance: although surface runoff increased relative to C0, the combined runoff and deep leakage loss was lowest in C1 (14.49 mm) versus C0 (16.45 mm) and C2 (16.43 mm). Runoff initiation thresholds consistently ranked C0 &gt; C1 &gt; C2 under both precipitation (124.68, 113.60, 103.27 mm) and antecedent soil moisture (14.79, 10.71, 8.70 mm), with precipitation as the stronger predictor, indicating that coarser fillings lower the activation threshold for preferential flow by enhancing network connectivity. A nitrogen transformation paradox emerged in C1: despite the highest leachate nitrate concentrations (18.34 μg mL⁻¹), total nitrogen leaching was ~30% lower than C0, reflecting coupled nitrification–denitrification within its intermediate pore architecture. Runoff thresholds acted as switches for nitrogen loss: leaching increased stepwise only after threshold exceedance, creating nitrogen export hot moments that alternated with safe operating spaces wherein nitrification proceeded without connected leaching pathways. These findings establish fracture-filling particle size as a structural control valve governing water–nitrogen dynamics through threshold-mediated mechanisms, providing a mechanistic foundation for precision water and nitrogen management in karst regions.</p>\u0000 </div>","PeriodicalId":13189,"journal":{"name":"Hydrological Processes","volume":"40 9","pages":""},"PeriodicalIF":3.1,"publicationDate":"2026-09-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148942482","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Delineation of Flow Components in a Tropical Region With Carbonate Rocks of Southeastern Mexico","authors":"Castro-Zarate Martha Edith,&nbsp;Olea-Olea Selene,&nbsp;Morales-Casique Eric,&nbsp;Neri-Flores Iris,&nbsp;Salas-Barrena Citlali,&nbsp;Zamora-Martínez Olivia,&nbsp;Valera Fernández Daisy,&nbsp;Mariño-Tapia Ismael de Jesús,&nbsp;Ramírez-Serrato Nelly,&nbsp;Valencia Morales Yuly Tatiana","doi":"10.1002/hyp.70692","DOIUrl":"https://doi.org/10.1002/hyp.70692","url":null,"abstract":"<p>This study analyses groundwater flow systems in a tropical karst aquifer of the Yucatán Peninsula, Mexico, where population growth and tourism are concerns due to increasing urbanisation. Through multivariate statistical and hydrogeochemical analyses, three flow components were identified: a local component, characterised by HCO₃⁻-Ca type water with recent recharge; an intermediate SO₄²⁻ component associated with gypsum dissolution and flow path modification by the Ticul Fault; and an intermediate Cl⁻ component resulting from mixing with seawater along the coastal zone. The results show that geology—particularly the presence of evaporitic rocks and tectonic structures—controls hydrogeochemical evolution and flow pathways, while the intense precipitation of the tropical climate modulates recharge and promotes the system's rapid response. This work represents the first delineation of groundwater flow system components in a tropical carbonate region of Mexico and constitutes a significant advance for sustainable groundwater management in a complex karst environment that can be extrapolated to other karstic zones in Central America and the Caribbean.</p>","PeriodicalId":13189,"journal":{"name":"Hydrological Processes","volume":"40 9","pages":""},"PeriodicalIF":3.1,"publicationDate":"2026-09-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/hyp.70692","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148942367","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Identifying Groundwater Flow Paths in Mountainous Systems Using Environmental Tracers: Insights From the Matsumoto Intermountain Basin, Japan","authors":"Shinji Nakaya,&nbsp;Ryogo Takada","doi":"10.1002/hyp.70687","DOIUrl":"https://doi.org/10.1002/hyp.70687","url":null,"abstract":"<div>\u0000 \u0000 <p>Groundwater sulphur hexafluoride (SF₆) is widely used as a tracer for groundwater dating. However, because SF₆ concentrations readily equilibrate with the atmosphere upon air contact, the reliability of SF₆-based age estimates can be strongly influenced by groundwater flow pathways. In this study, we identify groundwater flow systems by exploiting the sensitivity of SF₆ to recharge and flow processes. By integrating SF₆ characteristics with stable oxygen isotopes, we delineate two major groundwater flow pathways in the Matsumoto Basin, a large intermontane basin in central Japan. One pathway involves recharge in mountainous catchments followed by direct subsurface flow into the basin aquifer and is characterised by older, chemically evolved groundwater influenced by cation exchange and reducing conditions. The other involves recharge within the basin lowlands by surface water derived from the mountains and is characterised by relatively young, oxygenated groundwater associated with carbonate and sulphate mineral dissolution. Intermediate hydrochemical signatures indicate hydraulic connectivity and mixing between these flow systems, reflecting differences in groundwater residence time, flow dynamics and water–rock interaction histories. These pathways are supported by elevated SF₆ concentrations exceeding atmospheric equilibrium and by the behaviour of fluoride and lithium ions, indicating anthropogenic influences at the land surface. The systematic relationships among hydrochemical parameters, stable isotopes and environmental tracers demonstrate that the contrasting signatures primarily reflect distinct groundwater flow regimes and their mixing processes. Identifying these dominant pathways is critical for developing effective recharge strategies to mitigate long-term groundwater-level declines in the Matsumoto Basin. More broadly, recognition of such flow-path structures is fundamental for designing sustainable recharge practices and supporting water-resource management and environmental protection in intermontane basins with similar geographic, geological and climatic settings.</p>\u0000 </div>","PeriodicalId":13189,"journal":{"name":"Hydrological Processes","volume":"40 9","pages":""},"PeriodicalIF":3.1,"publicationDate":"2026-09-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148942366","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Physics-Informed Simulation of Vadose-Zone Water Flow Linking Surface Forcing and Groundwater Recharge","authors":"Chengzhong Cao,&nbsp;Lin Xiong,&nbsp;Libo Shen,&nbsp;Tianyu Li,&nbsp;Tao Wang,&nbsp;Yulong Gao,&nbsp;Guobo Wu,&nbsp;Huanyu Chang","doi":"10.1002/hyp.70684","DOIUrl":"https://doi.org/10.1002/hyp.70684","url":null,"abstract":"<div>\u0000 \u0000 <p>Climate variability and agricultural water use jointly regulate the transfer of surface inputs through vadose zones towards groundwater, yet this vertical pathway remains difficult to quantify in thick, heterogeneous profiles. We developed a physics-informed neural network (PINN) for the pressure-head form of the Richards equation with van Genuchten hydraulic relationships and evaluated it against an analytical benchmark and observations from a 45.2 m multilayer agricultural profile at the Luancheng Experimental Station. Across six monitoring depths, the PINN achieved a mean Nash–Sutcliffe efficiency of 0.916 ± 0.050, compared with 0.853 ± 0.109 for a finite-difference method. The field simulation reproduced rapid near-surface wetting–drying, delayed and attenuated responses at depth, and the partitioning of 887.5 mm of precipitation and irrigation among evapotranspiration, storage change and 247.32 mm of deep percolation below the 0–2 m root zone. Following a local hydraulic-parameter update, the warm-started PINN re-converged with a mean relative error of 2.43% against paired pressure-head observations. Although conditional on fixed hydraulic parameters, deterministic inputs and a one-dimensional structure, the framework links climate-driven and human-managed surface forcing with vadose-zone buffering and potential groundwater recharge. It also clarifies why deep percolation below the root zone should not be equated with contemporaneous recharge at a deep water table. These findings support process-based interpretation of groundwater–surface water interactions and agricultural water management in irrigated, water-limited regions.</p>\u0000 </div>","PeriodicalId":13189,"journal":{"name":"Hydrological Processes","volume":"40 9","pages":""},"PeriodicalIF":3.1,"publicationDate":"2026-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148942059","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Budyko Curve Conformance Unravelling Hydrological Change in a Semi-Arid Mediterranean-Climate River Basin","authors":"Yonca Cavus,&nbsp;Dilek Eren Akyuz,&nbsp;Ebru Eris,&nbsp;Hafzullah Aksoy","doi":"10.1002/hyp.70657","DOIUrl":"https://doi.org/10.1002/hyp.70657","url":null,"abstract":"<p>This study investigates long-term streamflow changes in the Gediz River Basin, a climatically Mediterranean catchment in western Turkey, by employing a Budyko-based water balance framework. Using multi-decadal observations from 18 streamflow gauging stations and four meteorological stations, we analyse basin behaviour through (i) Budyko and Fu curves fitting, (ii) detection of regime shifts using time-series segmentation and (iii) attribution of streamflow changes via both decomposition and sensitivity methods. A common hydrological regime shift was detected in 1984, after which streamflow consistently declines across most streamflow gauges. Post-change periods exhibit elevated Fu parameters and increased evaporation ratios, indicating reduced runoff and intensified aridity. A high majority of gauging stations align closely with Budyko expectations, while deviations—particularly in high-altitude headwaters—are attributed to karst geomorphology, snowmelt processes and data limitations. Attribution analysis reveals that climate variability, especially declining precipitation, accounts for 50%–75% of the total streamflow change, though local anthropogenic drivers also contribute significantly in specific sub-basins. These findings mirror regional hydroclimatic patterns across the Mediterranean Basin and reinforce the Gediz River Basin's sensitivity to both climate stress and water management practices. The well-established knowledge that humans are the main factor creating the streamflow decrease has been softened with our data-limited results showing that the climate-driven change in Western part of Turkey could be higher than the human effect. The study is a detailed basin-scale understanding, rather than implying a methodological breakthrough or a definitive proof of persistent Budyko conformance. It emphasises that the hydrological character of Gediz River Basin provides an opportunity to develop Budyko-based practical methodologies for the river basin-scale water resources planning and management strategies that could potentially be transferable to data-scarce, semi-arid regions facing escalating water insecurity.</p>","PeriodicalId":13189,"journal":{"name":"Hydrological Processes","volume":"40 9","pages":""},"PeriodicalIF":3.1,"publicationDate":"2026-09-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/hyp.70657","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"148942153","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}