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Enhancing flood forecasting accuracy in Data-Scarce regions through advanced modeling approaches 通过先进的建模方法提高数据匮乏地区洪水预报的准确性
IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Pub Date : 2024-11-10 DOI: 10.1016/j.jhydrol.2024.132283
Abdelmonaim Okacha , Adil Salhi , Mounir Bouchouou , Hamid Fattasse
Flood forecasting in data-scarce regions poses significant challenges due to irregular rainfall patterns and limited hydrological monitoring networks, particularly in semi-arid regions in Africa, South America, and Asia. However, despite significant efforts and advancements, there remains a substantial gap in the accurate prediction of flood events necessary for effective risk management and mitigation, evidenced by the recurrence of devastating floods in middle to low-income countries in recent years. Here, we address this problem by testing advanced modeling techniques in a local African case, using a combination of statistical methods for extreme event prediction, hydrodynamic modeling, and remote sensing data, to recommend the most adapted and accurate approach under a variety of settings. Our case study is an emerging urban area in Northern Morocco, situated in a triangular plain interposed between adverse geomorphological and precipitation settings, and unregulated expansion flow, creating an exceptionally overwhelming context for disastrous floods. In the absence of previous studies, we integrate frequency distribution analysis to predict extreme rainfall events and flood flow modeling to simulate floodplain inundation. Data sources included high-resolution remote sensing, local hydrological measurements, fine topographical data, and interviews with stakeholders. We found the Pearson Type 3 distribution to be the most suitable for modeling extreme precipitation in coastal areas, whereas the Generalized Extreme Value (GEV) distribution better fits inland areas. For flood flow assessment, the Gradex method proved to be the most accurate, while other empirical methods outlined critical limitations. Findings reveal that advanced hydrodynamic models significantly enhance flood hazard assessments, even in regions with limited data, showing outstanding correlations with previous flood records and stakeholder feedback. The outcomes carry critical implications for highlighting the importance of selecting appropriate models based on geographical and climatic conditions to inform more resilient urban planning and disaster management practices. We anticipate that these insights will support local decision-makers and urban planners in developing strategies that enhance community resilience and reduce the adverse impacts of flooding. Our work contributes to the broader field of flood risk management, providing a foundation for future developments and practical applications in similar regions worldwide.
由于降雨模式不规则和水文监测网络有限,特别是在非洲、南美洲和亚洲的半干旱地区,数据稀缺地区的洪水预报工作面临巨大挑战。然而,尽管做出了巨大努力并取得了巨大进步,但在有效风险管理和减灾所需的洪水事件准确预测方面仍存在巨大差距,近年来中低收入国家不断发生的毁灭性洪水就是证明。为解决这一问题,我们在非洲当地案例中测试了先进的建模技术,结合使用了极端事件预测统计方法、水动力建模和遥感数据,以推荐在各种环境下最合适、最准确的方法。我们的案例研究是摩洛哥北部的一个新兴城市地区,该地区位于一个三角平原上,地貌和降水环境恶劣,水流扩张不受控制,这为灾难性洪水的发生创造了一个异常恶劣的环境。由于缺乏相关研究,我们将频率分布分析与洪水流量建模相结合,预测极端降雨事件,模拟洪泛区淹没情况。数据来源包括高分辨率遥感、当地水文测量、精细地形数据以及对利益相关者的访谈。我们发现皮尔逊 3 型分布最适合沿海地区的极端降水建模,而广义极值分布(GEV)更适合内陆地区。在洪水流量评估方面,Gradex 方法被证明是最准确的,而其他经验方法则存在严重的局限性。研究结果表明,即使在数据有限的地区,先进的流体力学模型也能显著提高洪水灾害评估的效率,并显示出与以往洪水记录和利益相关者反馈的出色相关性。这些成果具有重要意义,强调了根据地理和气候条件选择适当模型的重要性,从而为更具抗灾能力的城市规划和灾害管理实践提供信息。我们预计,这些见解将有助于当地决策者和城市规划者制定战略,增强社区的抗灾能力,减少洪灾的不利影响。我们的工作为更广泛的洪水风险管理领域做出了贡献,为全球类似地区的未来发展和实际应用奠定了基础。
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引用次数: 0
Water and carbon fluxes from a supra-permafrost aquifer to a stream across hydrologic states 不同水文状态下从超冻土含水层流向溪流的水和碳通量
IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Pub Date : 2024-11-09 DOI: 10.1016/j.jhydrol.2024.132285
Neelarun Mukherjee , Jingyi Chen , Bethany T. Neilson , George W. Kling , M. Bayani Cardenas
Supra-permafrost aquifers within the active layer are present in the Arctic during summer. Permafrost thawing due to Arctic warming can liberate previously frozen particulate organic matter (POM) in soils to leach into groundwater as dissolved organic carbon (DOC). DOC transport from groundwater to surface water is poorly understood because of the unquantified variability in subsurface properties and hydrological environments. These dynamics must be better characterized because DOC transport to surface waters is critical to predict the long-term fate of recently thawed carbon in permafrost environments. Here, we used distributed Darcy’s Law calculations to quantify groundwater and DOC fluxes into Imnavait Creek, Alaska, a representative headwater stream in a continuous permafrost watershed. We developed a statistical ensemble approach to model the parameter variability and range of potential contributions of steady-state groundwater flow to the creek. We quantified the model prediction uncertainty using statistical sampling of in-situ, active-layer soil hydro-stratigraphy (water table, ice table, and soil stratigraphy), high-resolution topography data, and DOC data. Moreover, the predicted groundwater discharge values representing all possible hydrologic conditions towards the end of the thawing season were also considered given the potential variability in saturation. The model predictions were similar to and span most of the observed range of Imnavait Creek streamflow, especially during recession periods, and also during saturation excess overland flow. As the Arctic warms and supra-permafrost aquifers deepen, groundwater flow is expected to increase. This increase is expected to impact stream, river, and lake biogeochemical processes by dissolving and mobilizing more soil constituents in continuous permafrost regions. This study highlights how quantifying the uncertainty of hydro-stratigraphical input parameters helps understand and predict supra-permafrost aquifer dynamics and connectivity to aquatic systems using a simple, but scalable, modeling approach.
北极地区夏季存在活动层内的超永久冻土含水层。北极变暖导致的永久冻土融化可使土壤中先前冻结的颗粒有机物(POM)以溶解有机碳(DOC)的形式渗入地下水。由于地下特性和水文环境的变化无法量化,人们对 DOC 从地下水向地表水的迁移知之甚少。必须更好地描述这些动力学特征,因为 DOC 向地表水的迁移对于预测永久冻土环境中最近解冻的碳的长期命运至关重要。在这里,我们使用分布式达西定律计算来量化进入阿拉斯加 Imnavait 溪的地下水和 DOC 通量,该溪流是连续永冻土流域中具有代表性的上游溪流。我们开发了一种统计集合方法来模拟稳定状态地下水流的参数变化和潜在贡献范围。我们利用对原位活动层土壤水文地层(地下水位、冰层和土壤地层)、高分辨率地形数据和 DOC 数据的统计采样,量化了模型预测的不确定性。此外,考虑到饱和度的潜在变化,还考虑了解冻季节末期代表所有可能水文条件的预测地下水排放值。模型预测值与观测到的 Imnavait 溪流量范围相似,并跨越了大部分范围,尤其是在衰退期和饱和过量陆地流期间。随着北极变暖和超冻土含水层的加深,地下水流量预计会增加。预计地下水流量的增加会溶解和调动更多连续永冻土区的土壤成分,从而影响溪流、河流和湖泊的生物地球化学过程。本研究强调了水文地层输入参数的不确定性量化如何通过一种简单但可扩展的建模方法帮助理解和预测超永久冻土含水层的动态以及与水生系统的连通性。
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引用次数: 0
Effects of human and tectonic activities on groundwater in the upper Yellow River terraces of the loess Plateau 人类活动和构造活动对黄土高原黄河上游阶地地下水的影响
IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Pub Date : 2024-11-07 DOI: 10.1016/j.jhydrol.2024.132279
Runqiang Zeng , Zonglin Zhang , Shufen Zhao , Ruihuan Su , Ziran Wei , Xiaorui Wang , Zhao Long , Jianhua Ma , Guan Chen , Xingmin Meng
Terraces of the Yellow River are among the most crucial geomorphological landforms pertaining to human survival on the Loess Plateau. After more than half a century of surface flood irrigation, rapid rises in groundwater levels have led to frequent geological disasters, causing a rapid short-term evolution of Yellow River terraces, and an increasingly serious contradiction between this rapid evolution and human survival. However, the process by which water transfers through the thick loess vadose zone and causes a rapid groundwater response within months or years remains controversial. Using the Heitai platform of Yellow River terrace IV as an example, we found, on the basis of regional geological surveys, that at least 112 tectonically-induced cracks have developed in this area. We contend that the superimposed effects of earthquake ground motions from historical and ancient earthquakes since the Late Pleistocene have driven the development of such densely distributed cracks in the loess layer. These cracks, together with a series of fault planes generated by NE-directed extrusive stress at the regional scale, constitute a potential network of preferential channels for water transport within the Heitai platform. Combined with the results of a large-scale in situ ponding test and electrical resistivity tomography, we found that this network of cracks helps to establish catchment areas within the loess layer, thereby increasing soil saturation at a more extensive spatial scale, which may then increase the overall movement velocity of the wetting front. We semi-quantified the efficiency of the crack network in enhancing the recharge of surface water to groundwater, and suggested that the impact of human and tectonic activities substantially shortens the response time of groundwater to surface water, with the reduced time far exceeding one order of magnitude. The results of a field investigation of structural traces and terrace groundwater after the Ms 6.2 Jishishan earthquake on 18 December 2023 further emphasize that a causal mechanism of human and tectonic activities leading to the rapid short-term evolution of groundwater distribution patterns may be universally applicable to all Yellow River terraces on the Loess Plateau. This study mitigates the long-standing controversy concerning the mode of surface water infiltration, including piston flow and preferential flow, and the infiltration medium by which rapid surface water recharge to groundwater occurs in loess areas over short time periods.
黄河梯田是黄土高原上关系到人类生存的最重要的地貌景观之一。经过半个多世纪的地表漫灌,地下水位急剧上升,地质灾害频发,造成黄河梯田短期内急剧演变,急剧演变与人类生存之间的矛盾日益突出。然而,水流通过厚厚的黄土黏滞带并在数月或数年内引起地下水快速反应的过程仍存在争议。以黄河第四阶地的黑台地台为例,我们根据区域地质调查发现,该地区至少发育了 112 条构造引起的裂缝。我们认为,晚更新世以来的历史地震和古地震所产生的地震地动叠加效应促使黄土层中出现了这种密集分布的裂缝。这些裂缝与区域范围内东北向挤压应力产生的一系列断层面共同构成了黑土台地内部潜在的水运优先通道网络。结合大规模原地积水试验和电阻率层析成像的结果,我们发现这种裂缝网络有助于在黄土层内建立集水区,从而在更大的空间尺度上提高土壤饱和度,进而提高湿润前沿的整体移动速度。我们对裂缝网络提高地表水向地下水补给的效率进行了半定量分析,认为人类活动和构造活动的影响大大缩短了地下水对地表水的响应时间,缩短的时间远远超过一个数量级。2023 年 12 月 18 日积石山 6.2 级地震后构造痕迹和阶地地下水的实地调查结果进一步强调,人类和构造活动导致地下水分布格局短期快速演变的因果机制可能普遍适用于黄土高原的所有黄河阶地。该研究缓解了长期以来关于黄土地区地表水入渗方式(包括活塞流和优先流)以及地表水短时快速补给地下水的入渗介质的争议。
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引用次数: 0
A two-source non-parametric method for estimating terrestrial evapotranspiration: Validation at eddy covariance sites 估算陆地蒸散量的双源非参数方法:涡度协方差站点验证
IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Pub Date : 2024-11-07 DOI: 10.1016/j.jhydrol.2024.132278
Xin Pan , Zi Yang , Jie Yuan , Rufat Guluzade , Zhanchuan Wang , Suyi Liu , Yulong Zhou , Wenqing Ma , Yingbao Yang , Yuanbo Liu
Developing a two-source evapotranspiration (ET) method is a major challenge of the accurate ET estimation. As a single source ET method, the performance of Non-Parametric (NP) approach is limited by the unavailability of conventional equation of equilibrium ET in the water-limited situation. To solve this problem, a two-source equilibrium ET equation derived from Penman–Monteith equation expressed using relative humidity (RH-PM) is introduced into the NP method, then a Two-Source Non-Parametric (TS-NP) method is proposed regarding vegetation and soil as individual source. The accuracy of equilibrium ET derived from two-source method has significantly improved in the bare-soil surface (relative error: 31.26 %; RMSE: 13.18 W/m2) compared with that of conventional equilibrium ET equation and surface flux equilibrium (SFE) theory. Validated by eddy covariance tower sites, the performance of TS-NP method on bare soil surfaces is satisfactory, involving a significant reduction (near to 1/2) in the ET estimation error (relative error: 49.45 %; RMSE: 16.15 W/m2) compared with that of NP, SFE-NP and RH-PM method. On the dense vegetation surface, the performance of TS-NP method (relative error: 8.44 %; RMSE: 17.44 W/m2) is also slightly better than that of the NP method, SFE-NP and RH-PM method. In addition, air temperature and surface temperature are the most sensitive input variables in the TS-NP method, particularly in bare soil surface. The ET derived from the combined TS-NP method shows the best performance in arid areas (relative error: 22.20 %; RMSE: 16.52 W/m2) and non-arid areas (relative error: 8.12 %; RMSE: 17.61 W/m2), and the combined TS-NP method has satisfactory accuracy on the heterogeneity of underlying. Therefore, the TS-NP method provides a simple but efficient two-source method for high-precision ET estimation.
开发双源蒸散(ET)方法是精确估算蒸散发的一大挑战。作为一种单源蒸散发方法,非参数(NP)方法的性能受限于限水情况下传统蒸散发平衡方程的不可用性。为解决这一问题,在 NP 方法中引入了由相对湿度(RH-PM)表示的彭曼-蒙蒂斯方程导出的双源平衡蒸散发方程,然后提出了将植被和土壤作为单独来源的双源非参数(TS-NP)方法。与传统的平衡蒸散发方程和地表通量平衡理论相比,双源法得出的裸土地表平衡蒸散发精度有了显著提高(相对误差:31.26%;均方根误差:13.18 W/m2)。经涡度协方差塔站点验证,TS-NP 方法在裸露土壤表面的性能令人满意,与 NP、SFE-NP 和 RH-PM 方法相比,其蒸散发估算误差显著减少(接近 1/2)(相对误差:49.45%;有效值误差:16.15 W/m2)。在茂密植被地表,TS-NP 方法的性能(相对误差:8.44 %;有效值:17.44 W/m2)也略好于 NP 方法、SFE-NP 方法和 RH-PM 方法。此外,气温和地表温度是 TS-NP 方法中最敏感的输入变量,尤其是在裸露土壤表面。由 TS-NP 组合方法得出的蒸散发在干旱地区(相对误差:22.20%;均方根误差:16.52 W/m2)和非干旱地区(相对误差:8.12%;均方根误差:17.61 W/m2)表现最佳,并且 TS-NP 组合方法在底层异质性方面具有令人满意的精度。因此,TS-NP 方法为高精度蒸散发估算提供了一种简单而高效的双源方法。
{"title":"A two-source non-parametric method for estimating terrestrial evapotranspiration: Validation at eddy covariance sites","authors":"Xin Pan ,&nbsp;Zi Yang ,&nbsp;Jie Yuan ,&nbsp;Rufat Guluzade ,&nbsp;Zhanchuan Wang ,&nbsp;Suyi Liu ,&nbsp;Yulong Zhou ,&nbsp;Wenqing Ma ,&nbsp;Yingbao Yang ,&nbsp;Yuanbo Liu","doi":"10.1016/j.jhydrol.2024.132278","DOIUrl":"10.1016/j.jhydrol.2024.132278","url":null,"abstract":"<div><div>Developing a two-source evapotranspiration (ET) method is a major challenge of the accurate ET estimation. As a single source ET method, the performance of Non-Parametric (NP) approach is limited by the unavailability of conventional equation of equilibrium ET in the water-limited situation. To solve this problem, a two-source equilibrium ET equation derived from Penman–Monteith equation expressed using relative humidity (RH-PM) is introduced into the NP method, then a Two-Source Non-Parametric (TS-NP) method is proposed regarding vegetation and soil as individual source. The accuracy of equilibrium ET derived from two-source method has significantly improved in the bare-soil surface (relative error: 31.26 %; RMSE: 13.18 W/m<sup>2</sup>) compared with that of conventional equilibrium ET equation and surface flux equilibrium (SFE) theory. Validated by eddy covariance tower sites, the performance of TS-NP method on bare soil surfaces is satisfactory, involving a significant reduction (near to 1/2) in the ET estimation error (relative error: 49.45 %; RMSE: 16.15 W/m<sup>2</sup>) compared with that of NP, SFE-NP and RH-PM method. On the dense vegetation surface, the performance of TS-NP method (relative error: 8.44 %; RMSE: 17.44 W/m<sup>2</sup>) is also slightly better than that of the NP method, SFE-NP and RH-PM method. In addition, air temperature and surface temperature are the most sensitive input variables in the TS-NP method, particularly in bare soil surface. The ET derived from the combined TS-NP method shows the best performance in arid areas (relative error: 22.20 %; RMSE: 16.52 W/m<sup>2</sup>) and non-arid areas (relative error: 8.12 %; RMSE: 17.61 W/m<sup>2</sup>), and the combined TS-NP method has satisfactory accuracy on the heterogeneity of underlying. Therefore, the TS-NP method provides a simple but efficient two-source method for high-precision ET estimation.</div></div>","PeriodicalId":362,"journal":{"name":"Journal of Hydrology","volume":"645 ","pages":"Article 132278"},"PeriodicalIF":5.9,"publicationDate":"2024-11-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142663524","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"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
Reconstructing MODIS normalized difference snow index product on Greenland ice sheet using spatiotemporal extreme gradient boosting model 利用时空极端梯度提升模型重建格陵兰冰盖上的 MODIS 归一化差异积雪指数产品
IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Pub Date : 2024-11-07 DOI: 10.1016/j.jhydrol.2024.132277
Fan Ye , Qing Cheng , Weifeng Hao , Dayu Yu
The spatiotemporally continuous data of normalized difference snow index (NDSI) are key to understanding the mechanisms of snow occurrence and development as well as the patterns of snow distribution changes. However, the presence of clouds, particularly prevalent in polar regions such as the Greenland Ice Sheet (GrIS), introduces a significant number of missing pixels in the MODIS NDSI daily data. To address this issue, this study proposes the utilization of a spatiotemporal extreme gradient boosting (STXGBoost) model generate a comprehensive NDSI dataset. In the proposed model, various input variables are carefully selected, encompassing terrain features, geometry-related parameters, and surface property variables. Moreover, the model incorporates spatiotemporal variation information, enhancing its capacity for reconstructing the NDSI dataset. Verification results demonstrate the efficacy of the STXGBoost model, with a coefficient of determination of 0.962, root mean square error of 0.030, mean absolute error of 0.011, and negligible bias (0.0001). Furthermore, simulation comparisons involving missing data and cross-validation with Landsat NDSI data illustrate the model’s capability to accurately reconstruct the spatial distribution of NDSI data. Notably, the proposed model surpasses the performance of traditional machine learning models, showcasing superior NDSI predictive capabilities. This study highlights the potential of leveraging auxiliary data to reconstruct NDSI in GrIS, with implications for broader applications in other regions. The findings offer valuable insights for the reconstruction of NDSI remote sensing data, contributing to the further understanding of spatiotemporal dynamics in snow-covered regions.
归一化差异积雪指数(NDSI)的时空连续数据是了解积雪发生和发展机制以及积雪分布变化规律的关键。然而,由于云层的存在,尤其是在格陵兰冰原等极地地区,MODIS NDSI 每日数据中会出现大量缺失像素。为解决这一问题,本研究提出利用时空极端梯度提升(STXGBoost)模型生成一个全面的 NDSI 数据集。在提议的模型中,各种输入变量都经过精心挑选,包括地形特征、几何相关参数和地表属性变量。此外,该模型还纳入了时空变化信息,增强了重建 NDSI 数据集的能力。验证结果证明了 STXGBoost 模型的有效性,其判定系数为 0.962,均方根误差为 0.030,平均绝对误差为 0.011,偏差可忽略不计(0.0001)。此外,涉及缺失数据的模拟比较和与大地遥感卫星 NDSI 数据的交叉验证也说明了该模型准确重建 NDSI 数据空间分布的能力。值得注意的是,所提出的模型超越了传统机器学习模型的性能,展示了卓越的 NDSI 预测能力。这项研究强调了利用辅助数据重建 GrIS 中 NDSI 的潜力,并对其他地区的更广泛应用产生了影响。研究结果为重建 NDSI 遥感数据提供了宝贵的见解,有助于进一步了解积雪地区的时空动态。
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引用次数: 0
Synthesis of research findings and general criteria for sustainable groundwater recharge and recovery in saline aquifers 含盐含水层可持续地下水补给和恢复的研究成果和一般标准综述
IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Pub Date : 2024-11-06 DOI: 10.1016/j.jhydrol.2024.132280
Shubham Tiwari , Brijesh Kumar Yadav , Maurizio Polemio
Managed Aquifer Recharge (MAR), a reliable technique for groundwater restoration in arid regions, struggles with the limited recovery of stored water in salt-affected areas due to fresh-saline water mixing. Groundwater recharge and recovery project performance in saline aquifers is primarily controlled by operational factors because it influences fresh-saline water mixing significantly. Understanding the impact of operational factors is thus crucial for optimizing MAR performance, particularly in saline groundwater regions. This study conducted a comprehensive literature review of literature studies related to MAR in Salt-affected groundwater regions (MARS), along with statistical analysis to discuss each operational factor’s common positive or negative effects on aquifer recharge and recovery performance. The Recovery Efficiency (RE) values in each MARS study analyzed in this article are influenced by unique hydrogeological and operational settings, resulting in significant variations. However, a similar influencing trend of each operational factor on the observed RE variation is found. To validate the results of this analysis, a variable density groundwater flow model was developed from the data of a MAR field application project given in Reese (2002) and simulated for similar variations in operational factors. The simulation results corroborated the general trends observed in the review analysis. This study provides a comprehensive analysis of how operational factors influence the RE of MARS. The results demonstrate that a higher recharge rate, larger freshwater volume, smaller storage durations, and a minimum of four subsequent recharge-recovery cycles may lead to higher RE. The trends obtained for each operational factor can be utilized to optimize the operation of MARS projects for achieving higher RE in the salt-affected regions of the world.
含盐蓄水层管理补给(MAR)是干旱地区地下水恢复的一项可靠技术,但由于淡盐水混合,受盐影响地区的储水恢复有限。含盐含水层的地下水补给和恢复项目的绩效主要受运行因素控制,因为它对淡盐水混合有很大影响。因此,了解运行因素的影响对于优化地下水补给与恢复工程的性能至关重要,尤其是在盐碱地下水区域。本研究对受盐分影响的地下水区域(MARS)有关 MAR 的文献研究进行了全面的文献综述,并进行了统计分析,以讨论每个运行因素对含水层补给和恢复性能的常见积极或消极影响。本文分析的每项 MARS 研究中的回收效率(RE)值都受到独特的水文地质和运行环境的影响,因此差异很大。不过,每个运行因素对观测到的 RE 变化都有类似的影响趋势。为了验证这一分析结果,根据 Reese(2002 年)提供的一个 MAR 实地应用项目的数据开发了一个可变密度地下水流模型,并对类似的运行因素变化进行了模拟。模拟结果证实了审查分析中观察到的总体趋势。这项研究全面分析了运行因素如何影响 MARS 的可再生能源。结果表明,较高的补给率、较大的淡水量、较短的贮存时间以及至少四个后续补给-恢复周期可导致较高的可再生能源利用率。可以利用每个运行因素的趋势来优化 MARS 项目的运行,从而在世界受盐影响地区实现更高的可再生能源。
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引用次数: 0
Characterizing interactive compound flood drivers in the Pearl River Estuary: A case study of Typhoon Hato (2017) 珠江口互动复合洪水驱动因素的特征:台风 "哈托"(2017 年)案例研究
IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Pub Date : 2024-11-06 DOI: 10.1016/j.jhydrol.2024.132270
Qianru Lin , Luming Shi , Bingchen Liang , Guoxiang Wu , Zhenlu Wang , Xuecheng Zhang , Yi Wu
Tropical cyclone (TC) induced compound floods involve dynamic interactions among astronomical tides, storm surges, precipitation, and associated river pulses. This study employs a one-way coupled WRF, Delft3D, and HEC-RAS model to investigate the impacts of oceanic, pluvial, and fluvial processes on compound flood dynamics during Typhoon Hato (2017) in the Pearl River Estuary (PRE), South China. Total water levels driven by different combinations of flood drivers are modeled and analyzed. Relative contributions of each type of flood driver are quantified and used to categorize flood zones. This study highlights the persistent impacts of storm surges and their nonlinear interactions with other flood drivers. They can modify both the timing and magnitude of maximum water levels, thereby distorting tidal signals and contributing to post-TC landfall water level peaks. Along coastal regions, water levels exhibit three successive peaks, predominantly driven by storm surge, rainfall, and the combined actions of both factors, respectively. In upstream regions and coastal areas sheltered from islands, a singular water level peak arises exclusively from rainfall-runoff processes. Moreover, nonlinear interactions between surge and rainfall-runoff have non-negligible impacts on the relative contribution of individual flood drivers, which underscores the necessity of considering both rainfall and storm surge in modeling compound flood water levels. During the flooding period, peak storm surge and the following peak rainfall resulted in a time-varying distribution of flood zones. Alternating feedback between compounded and ocean-dominant areas manifests in the midsections of the upper PRE. Maximum flooding depth, extent, and duration are mainly influenced by rainfall. Storm surges play a secondary role, causing intense but short-lived flooding in coastal regions. These findings aid in understanding the generation mechanism of compound floods and provide references for hazard mitigation strategies.
热带气旋(TC)诱发的复合洪水涉及天文潮汐、风暴潮、降水和相关河流脉冲之间的动态相互作用。本研究采用单向耦合 WRF、Delft3D 和 HEC-RAS 模型,研究台风 "哈托"(2017 年)期间华南珠江口(PRE)的海洋、冲积和河流过程对复合洪水动力学的影响。模拟并分析了由不同洪水驱动因素组合驱动的总水位。对各类洪水驱动因素的相对贡献进行了量化,并用于洪水区域的划分。这项研究强调了风暴潮的持续影响及其与其他洪水驱动因素的非线性相互作用。它们可以改变最高水位的时间和幅度,从而扭曲潮汐信号,并导致热带风暴登陆后的水位峰值。在沿岸地区,水位会出现三个连续的峰值,主要分别由风暴潮、降雨和这两个因素的共同 作用引起。在上游地区和岛屿遮蔽的沿海地区,水位峰值只由降雨-径流过程产生。此外,风暴潮和降雨-径流之间的非线性相互作用对单个洪水驱动因素的相对作用有不可忽视的影响,这就强调了在模拟复合洪水水位时同时考虑降雨和风暴潮的必要性。在洪水泛滥期间,风暴潮峰值和随后的降雨峰值导致洪泛区的时变分布。复合区和海洋主导区之间的交替反馈表现在 PRE 上游中段。最大洪水深度、范围和持续时间主要受降雨影响。风暴潮起次要作用,在沿海地区造成强烈但短暂的洪水。这些发现有助于了解复合洪水的生成机制,并为减轻灾害战略提供参考。
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引用次数: 0
Reconstructed centennial precipitation-driven water storage anomalies in the Nile River Basin using RecNet and their suitability for studying ENSO and IOD impacts 利用 RecNet 重建的尼罗河流域百年降水驱动的蓄水异常及其对研究厄尔尼诺/南方涛动和国际大 旱影响的适用性
IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Pub Date : 2024-11-04 DOI: 10.1016/j.jhydrol.2024.132272
Jielong Wang , Joseph Awange , Yunzhong Shen , Ling Yang , Tengfei Feng , Yongze Song
While the Gravity Recovery And Climate Experiment (GRACE) and its Follow-On (GFO) missions have offered valuable observations for monitoring total water storage anomalies (TWSA), their short record constrains our ability to study the complete range and long-term variability of TWSA in the Nile River Basin (NRB). Previous studies reconstructing TWSA in this region either relied on specific hydrological models or did not consider spatial correlations among the TWSA grids. Here, we employ RecNet, a deep learning model capable of providing independent TWSA observations without relying on hydrological models while considering spatial correlations, to reconstruct precipitation-driven TWSA in the NRB from 1923 to 2022. The reconstructed data are validated by comparisons with the Global Land Data Assimilation System (GLDAS), the WaterGAP Global Hydrology Model (WGHM), the water balance budget, long-term runoff data, and GRACE-REC (i.e., a global reconstruction dataset freely available online). Subsequently, the suitability of the reconstructed data for studying El Niño Southern Oscillation (ENSO) and Indian Ocean Dipole (IOD) impacts within the NRB is assessed. Dividing the NRB into four sub-regions, i.e., the Lake Victoria Basin (LVB), the Bahr el Jebel and Bahr el Ghazal basins (BJBG), Ethiopian Highlands region (EH), and the Lower Nile River Basin (LNRB), it is shown that RecNet successfully reconstructs precipitation-driven TWSA over BJBG and EH, achieving correlation coefficient (CC), normalized root mean square error (NRMSE), and Nash–Sutcliffeefficiency (NSE) of 0.94/0.11/0.88 and 0.96/0.09/0.91 during the testing period, respectively. Additionally, RecNet’s reconstruction shows better agreement with GLDAS and WGHM than GRACE-REC, correlating well with runoff and the water balance budget in these regions. The relatively poor performance in the LVB and LNRB regions could be attributed to the substantial influence of Lake Victoria and the arid climate, respectively. Correlation analysis and wavelet coherence analysis identify significant coherence between ENSO/IOD and the reconstructed TWSA in BJBG and EH, with CC values of −0.68/0.34 and −0.82/0.56, respectively. This study provides centennial reconstructed TWSA data that could be useful in climate change/variability studies and water resource management within the NRB.
虽然重力恢复和气候实验(GRACE)及其后续(GFO)任务为监测总蓄水异常(TWSA)提供了宝贵的观测数据,但其较短的记录限制了我们研究尼罗河流域(NRB)总蓄水异常的完整范围和长期变化的能力。以前在该地区重建 TWSA 的研究要么依赖于特定的水文模型,要么没有考虑 TWSA 网格之间的空间相关性。在此,我们采用 RecNet(一种能够提供独立 TWSA 观测数据的深度学习模型,无需依赖水文模型,同时考虑空间相关性)来重建 1923 年至 2022 年 NRB 地区降水驱动的 TWSA。通过与全球陆地数据同化系统(GLDAS)、WaterGAP 全球水文模型(WGHM)、水平衡预算、长期径流数据和 GRACE-REC(即可在线免费获取的全球重建数据集)进行比较,对重建数据进行了验证。随后,评估了重建数据是否适合用于研究厄尔尼诺南方涛动(ENSO)和印度洋偶极子(IOD)对 NRB 的影响。将 NRB 划分为四个子区域,即结果表明,RecNet 成功地重建了维多利亚湖流域(LVB)、杰贝勒河流域和加扎勒河流域(BJBG)、埃塞俄比亚高原地区(EH)和尼罗河下游流域(LNRB)降水驱动的 TWSA,相关系数(CC)、归一化均方根误差(NRMSE)和纳什-苏特克里夫效率(NSE)分别为 0.94/0.11/0.88 和 0.96/0.09/0.91。此外,与 GRACE-REC 相比,RecNet 的重建结果与 GLDAS 和 WGHM 的一致性更好,与这些区域的径流和水平衡预算相关性也很好。LVB 和 LNRB 区域的表现相对较差,这可能分别是由于维多利亚湖和干旱气候的巨大影响。相关性分析和小波相干性分析确定了 ENSO/IOD 与 BJBG 和 EH 重建的 TWSA 之间的显著相干性,CC 值分别为 -0.68/0.34 和 -0.82/0.56。该研究提供的百年重建 TWSA 数据可用于北大西洋区域局内的气候变化/变率研究和水资源管理。
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引用次数: 0
A case study of canal seepage quantification using gain/loss method and electrical resistivity tomography in an intensively managed water resource system in the Treasure Valley, Idaho, United States 在美国爱达荷州金银谷一个密集管理的水资源系统中使用增益/损耗法和电阻率层析成像法对运河渗流进行量化的案例研究
IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Pub Date : 2024-11-02 DOI: 10.1016/j.jhydrol.2024.132251
Dina Ragab , Kendra E. Kaiser , Qifei Niu , Mohamed Attwa , Alejandro N. Flores
Monitoring groundwater-surface water (GW-SW) interactions is essential for effectively managing the available water resources in semi-arid and arid environments. The focus of this study was to quantify how much SW is being exchanged with the shallow GW aquifer in the Treasure Valley (TV), Idaho, USA. Previous water budgets estimated regional canal seepage without incorporating canal variability and flow measurement uncertainty. To address this, we applied both direct (gain/loss) and indirect (electrical resistivity tomography (ERT)) techniques. Direct seepage measurements were taken on canals capturing a range of different characteristics in the TV. The discrete measurements were then used to estimate the total seepage anticipated to be lost from these canals during the irrigation season. Our findings showed high seepage variability across the canals. The ERT inversion approach was utilized before and after the irrigation season by applying an advanced inversion scheme to better constrain the canal seepage spatial variability and uncertainty by quantifying changes in the saturated zone with 2D-ERT results. Temporal changes in the subsurface resistivity were observed due to the lateral flow from the nearby surface canal during the irrigation season. The combination of these approaches improves our understanding of SW-GW interactions in intensively managed irrigation systems.
监测地下水与地表水(GW-SW)之间的相互作用对于有效管理半干旱和干旱环境中的可用水资源至关重要。本研究的重点是量化与美国爱达荷州金银谷(Treasure Valley,TV)浅层地下水含水层进行交换的地下水量。以前的水量预算在估算区域运河渗漏量时没有考虑运河的变化和流量测量的不确定性。为了解决这个问题,我们采用了直接(增/减)和间接(电阻率层析成像 (ERT))技术。直接渗流测量是在电视中捕捉一系列不同特征的运河上进行的。然后,利用离散测量结果估算出灌溉季节预计从这些渠道流失的总渗水量。我们的研究结果表明,各条渠道的渗流变化很大。在灌溉季节前后,我们采用了 ERT 反演方法,应用先进的反演方案,通过二维反演结果量化饱和带的变化,更好地限制了渠道渗流的空间变化和不确定性。在灌溉季节,由于附近地表运河的横向流动,地下电阻率发生了时间变化。这些方法的结合提高了我们对集约化管理灌溉系统中地下水-地面水相互作用的理解。
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引用次数: 0
Groundwater sustainability assessment and the research-practice nexus 地下水可持续性评估以及研究与实践之间的关系
IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Pub Date : 2024-11-01 DOI: 10.1016/j.jhydrol.2024.132166
Behzad Ataie Ashtiani , Craig T. Simmons , Leila Farhadi , Shuo Zhang
This special issue on “Groundwater Sustainability Assessment and the Research-Practice Nexus” presents 18 papers aimed at addressing the widening gap between scientific research and practical groundwater management. Despite recent advancements in data and modeling technologies, many studies lack lasting academic and practical impact, raising concerns about their value. To counter this, the issue brings together research that emphasizes practical application in four key areas: groundwater management and policy, dynamics and modeling, quality and pollution, and sustainability assessment, aiming to ensure that hydrological research leads to tangible, long-term benefits.
本期特刊的主题是 "地下水可持续性评估与研究与实践之间的联系",共收录了 18 篇论文,旨在解决科学研究与实际地下水管理之间日益扩大的差距。尽管最近在数据和建模技术方面取得了进步,但许多研究缺乏持久的学术和实际影响,从而引起了人们对其价值的担忧。为解决这一问题,本期杂志汇集了强调实际应用的四个关键领域的研究成果:地下水管理与政策、动力学与建模、水质与污染以及可持续性评估,旨在确保水文研究带来切实的长期效益。
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引用次数: 0
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Journal of Hydrology
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