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Search Results (1,309)

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30 pages, 5781 KiB  
Article
Enhancing Time Series Anomaly Detection: A Knowledge Distillation Approach with Image Transformation
by Haiwoong Park and Hyeryung Jang
Sensors 2024, 24(24), 8169; https://doi.org/10.3390/s24248169 (registering DOI) - 21 Dec 2024
Viewed by 228
Abstract
Anomaly detection is critical in safety-sensitive fields, but faces challenges from scarce abnormal data and costly expert labeling. Time series anomaly detection is relatively challenging due to its reliance on sequential data, which imposes high computational and memory costs. In particular, it is [...] Read more.
Anomaly detection is critical in safety-sensitive fields, but faces challenges from scarce abnormal data and costly expert labeling. Time series anomaly detection is relatively challenging due to its reliance on sequential data, which imposes high computational and memory costs. In particular, it is often composed of real-time collected data that tends to be noisy, making preprocessing an essential step. In contrast, image anomaly detection has leveraged advancements in technologies for analyzing spatial patterns and visual features, achieving high accuracy and promoting research aimed at improving efficiency. We propose a novel framework that bridges image anomaly detection with time series data. Using Gramian Angular Field (GAF) transformations, we convert time series into images and apply state-of-the-art techniques, Reverse Distillation (RD) and EfficientAD (EAD), for efficient and accurate anomaly detection. Tailored preprocessing and transformations further enhance performance and interoperability. When evaluated on the multivariate time series anomaly detection dataset Secure Water Treatment (SWaT) and the univariate datasets University of California, Riverside (UCR) and Numenta Anomaly Benchmark (NAB), our approach demonstrated high recall overall and achieved approximately 99% F1 scores on some univariate datasets, proving its effectiveness as a novel solution for time series anomaly detection. Full article
(This article belongs to the Section Fault Diagnosis & Sensors)
22 pages, 4278 KiB  
Article
Research on Service-Oriented Sharing and Computing Framework of Geographic Data for Geographic Modeling and Simulation
by Jin Wang, Lingkai Shi, Xuan Zhang, Kai Xu, Zaiyang Ma, Yongning Wen and Min Chen
Appl. Sci. 2024, 14(24), 11983; https://doi.org/10.3390/app142411983 (registering DOI) - 20 Dec 2024
Viewed by 494
Abstract
Geographic data are the foundation of geographic model construction, and any stage of their acquisition, processing, and analysis may have an impact on the efficiency and quality of geographic modeling and simulation. With the advent of the era of big data, a large [...] Read more.
Geographic data are the foundation of geographic model construction, and any stage of their acquisition, processing, and analysis may have an impact on the efficiency and quality of geographic modeling and simulation. With the advent of the era of big data, a large number of data resources are generated in the field of geographic information. However, due to the heterogeneity of geographic data and the security of data usage, massive geographic data resources are difficult to fully explore and utilize, resulting in the formation of data islands. This paper proposes a service-oriented geographic data-sharing and computing framework, which provides users with a complete set of geographic data access and application processes (such as data acquisition, processing, configuration, etc.), so as to reduce the difficulty of using data and improve the efficiency of data sharing. The framework mainly consists of three core components: (1) the “Data service container” can publish data resources as data services to provide a consistent data access interface; (2) the “Workspace” provides a series of methods and tools for users to develop data-computing solutions; and (3) the “Data-computing engine” is responsible for performing computing tasks such as data processing and configuration. Finally, a case of runoff simulation using the SWAT model is designed, in which the whole process of data sharing, acquisition, calculation, and application is realized, so as to verify the validity of the proposed framework. Full article
19 pages, 17870 KiB  
Article
Evolution of Land Use and Its Hydrological Effects in the Fenhe River Basin Under the Production–Living–Ecological Space Perspective
by Junzhe Zhang, Azhar Ali Laghari, Qingxia Guo, Jiyao Liang, Akash Kumar, Zhenghao Liu, Yongheng Shen and Yuehan Wei
Sustainability 2024, 16(24), 11170; https://doi.org/10.3390/su162411170 - 20 Dec 2024
Viewed by 450
Abstract
Analysing the patterns and impacts of land-use changes in the production–living–ecological space (PLES) of the Fenhe River Basin (FRB 39,721 km2), China, is necessary to support sustainable development. Based on remote sensing images from 1990 to 2020, we aimed to analyse [...] Read more.
Analysing the patterns and impacts of land-use changes in the production–living–ecological space (PLES) of the Fenhe River Basin (FRB 39,721 km2), China, is necessary to support sustainable development. Based on remote sensing images from 1990 to 2020, we aimed to analyse the PLES land-use changes. Industrial production and living spaces continuously encroached on the agricultural production and ecological spaces between 1990 and 2022 owing to industrialisation and urbanisation, and the ecological land area decreased by 699.21 km2, while the industrial production land area increased by 521.32 km2. We used the soil and water assessment tool (SWAT) model to quantitatively analyse the impact of PLES changes on runoff in the FRB. With the continuous expansion of production and living spaces, the extensive use of concrete in cities has led to ground hardening, making it difficult for precipitation to infiltrate, with surface runoff increasing by 0.3 mm annually. The reduction in ecological space has led to a reduction in forests and grasslands, weakening the water-holding capacity of the watershed and affecting groundwater storage. This study provides a scientific basis for watershed management and the integrated development of PLES. Full article
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Figure 1
<p>Location of the Fenhe River Basin, Shanxi Province, China.</p>
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<p>Monthly mean temperature and precipitation in the Fenhe River Basin. Data were obtained from eight meteorological stations in the basin (1990−2022), and values were calculated using the Tyson polygon method.</p>
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<p>Soil and water assessment tool (SWAT) model flow chart.</p>
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<p>Observed and SWAT-simulated monthly stream flow for the calibration (January 2014−December 2022) and validation (January 1990–December 2014) periods in the Fenhe River Basin, Shanxi Province, China.</p>
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<p>Development of production–living–ecological space (PLES) over 1990–2020 in Fenhe River Basin.</p>
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<p>Secondary class distribution of PLES in Fenhe River Basin.</p>
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<p>Trajectories of spatial transfer changes of PLES in the Fenhe River Basin. Different coloured trajectory lines show the direction of transfer between land classes, and the thickness of the trajectory lines represents the amount of transformation.</p>
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<p>Spatial transfer of PLES land-use types in Fenhe River Basin.</p>
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<p>Simulated runoff changes in the Fenhe River Basin between 1990 and 2020. (The green dushed line represents the overall trend of precipitation changes).</p>
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<p>Average monthly runoff under different PLES scenarios.</p>
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<p>Average annual surface runoff (SURQ) and groundwater (GWQ) under different PLES scenarios.</p>
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<p>Stacked chart of PLES spatial transfer in sub-basins 42, 43, and 44 from 1990 to 2020.</p>
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<p>Temporal variations of surface runoff and groundwater in sub-basins 42, 43, and 44.</p>
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26 pages, 23421 KiB  
Article
Assessment of Post-Fire Impacts on Vegetation Regeneration and Hydrological Processes in a Mediterranean Peri-Urban Catchment
by Evgenia Koltsida, Nikos Mamassis, Evangelos Baltas, Vassilis Andronis and Andreas Kallioras
Remote Sens. 2024, 16(24), 4745; https://doi.org/10.3390/rs16244745 - 19 Dec 2024
Viewed by 236
Abstract
This study aimed to evaluate the impact of a wildfire on vegetation recovery and hydrological processes in a Mediterranean peri-urban system, using remote sensing and hydrological modeling. NDVI and MSAVI2 time series extracted from burned areas, control plots, and VAR-modeled plots were [...] Read more.
This study aimed to evaluate the impact of a wildfire on vegetation recovery and hydrological processes in a Mediterranean peri-urban system, using remote sensing and hydrological modeling. NDVI and MSAVI2 time series extracted from burned areas, control plots, and VAR-modeled plots were used to analyze vegetation regeneration. The SWAT model, calibrated for pre-fire conditions due to data limitations, was used to evaluate subbasin-scale hydrological impacts. Results showed limited recovery in the first post-fire year, with vegetation indices remaining lower in burned areas compared to control plots. High- and moderate-burn-severity areas presented the most significant NDVI and MSAVI2 increases. The SWAT model showed increased water yield, percolation, and surface runoff with reduced evapotranspiration in post-fire conditions. Peak discharges were notably higher during wet periods. Modified land use and soil properties affected the catchment’s hydrological balance, emphasizing the complexities of post-fire catchment dynamics. Full article
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Figure 1
<p>Elevation of the study area (<b>a</b>), spatial distribution of land use (<b>b</b>), burn severity (<b>c</b>), and soil types (<b>d</b>). Zoomed-out display of Greece and Athens location in red box (<b>upper left</b>) and Athens metropolitan area (<b>lower left</b>). The study area includes 25 subbasins, of which the subbasin numbers 1, 2, 3, 4, 6, 11, 17, 18, 19, and 20 indicate the subbasins inside the burn scar.</p>
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<p><math display="inline"><semantics> <mrow> <mi>N</mi> <mi>D</mi> <mi>V</mi> <mi>I</mi> </mrow> </semantics></math> predictions for the period August 2021 to January 2023 without the influence of fire. (<b>a</b>) AGRL, agriculture. (<b>b</b>) RNGB, shrubland. (<b>c</b>) UCOM, transportation/green areas. (<b>d</b>) FRSD, deciduous forest. (<b>e</b>) FRSE, evergreen forest. (<b>f</b>) FRST, mixed forest.</p>
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<p><math display="inline"><semantics> <mrow> <msub> <mrow> <mi>M</mi> <mi>S</mi> <mi>A</mi> <mi>V</mi> <mi>I</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msub> </mrow> </semantics></math> predictions for the period August 2021 to January 2023 without the influence of fire. (<b>a</b>) AGRL, agriculture. (<b>b</b>) RNGB, shrubland. (<b>c</b>) UCOM, transportation/green areas. (<b>d</b>) FRSD, deciduous forest. (<b>e</b>) FRSE, evergreen forest. (<b>f</b>) FRST, mixed forest.</p>
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<p>Mean <math display="inline"><semantics> <mrow> <mi>N</mi> <mi>D</mi> <mi>V</mi> <mi>I</mi> </mrow> </semantics></math> for the burned and control plots and VAR modeling results from August 2021 to August 2022. (<b>a</b>) AGRL, agriculture. (<b>b</b>) RNGB, shrubland. (<b>c</b>) UCOM, transportation/green areas. (<b>d</b>) FRSD, deciduous forest. (<b>e</b>) FRSE, evergreen forest. (<b>f</b>) FRST, mixed forest.</p>
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<p>Mean <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>M</mi> <mi>S</mi> <mi>A</mi> <mi>V</mi> <mi>I</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msub> </mrow> </semantics></math> for the burned and control plots and VAR modeling results for August 2016–August 2022. (<b>a</b>) AGRL, agriculture. (<b>b</b>) RNGB, shrubland. (<b>c</b>) UCOM, transportation/green areas. (<b>d</b>) FRSD, deciduous forest. (<b>e</b>) FRSE, evergreen forest. (<b>f</b>) FRST, mixed forest.</p>
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<p>Mean <math display="inline"><semantics> <mrow> <mi>N</mi> <mi>D</mi> <mi>V</mi> <mi>I</mi> </mrow> </semantics></math> by burn severity class, August 2016–August 2022. (<b>a</b>) AGRL, agriculture. (<b>b</b>) RNGB, shrubland. (<b>c</b>) UCOM, transportation/green areas. (<b>d</b>) FRSD, deciduous forest. (<b>e</b>) FRSE, evergreen forest. (<b>f</b>) FRST, mixed forest. All classes demonstrated consistently positive post-fire <math display="inline"><semantics> <mrow> <mi>N</mi> <mi>D</mi> <mi>V</mi> <mi>I</mi> </mrow> </semantics></math> gains in the first post-fire year.</p>
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<p>Mean <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>M</mi> <mi>S</mi> <mi>A</mi> <mi>V</mi> <mi>I</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msub> </mrow> </semantics></math> by burn severity class, August 2016–August 2022. (<b>a</b>) AGRL, agriculture. (<b>b</b>) RNGB, shrubland. (<b>c</b>) UCOM, transportation/green areas. (<b>d</b>) FRSD, deciduous forest. (<b>e</b>) FRSE, evergreen forest. (<b>f</b>) FRST, mixed forest. All classes demonstrated consistently positive post-fire <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>M</mi> <mi>S</mi> <mi>A</mi> <mi>V</mi> <mi>I</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msub> </mrow> </semantics></math> gains in the first post-fire year.</p>
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<p>Simulated daily discharge results (<b>a</b>) and flow duration curves (<b>b</b>) (m<sup>3</sup> s<sup>−1</sup>) during the pre-fire and post-fire scenarios.</p>
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<p>Simulated hourly discharge results (<b>a</b>) and flow duration curves (<b>b</b>) (m<sup>3</sup> s<sup>−</sup><sup>1</sup>) during the pre-fire and post-fire scenarios.</p>
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<p>Maximum hourly discharge (m<sup>3</sup>s<sup>−1</sup>) of the rainfall events that occurred in the pre-fire and post-fire periods compared to maximum hourly rainfall intensity (mmh<sup>−1</sup>). The size of the circles is according to the peak discharge for the pre- and post-fire conditions.</p>
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<p>Monthly values of the major hydrological components of the daily (<b>a</b>–<b>d</b>) model during the pre-fire and post-fire scenarios. SURQ: surface runoff (mm), PERC: percolation (mm), AET: actual evapotranspiration (mm), and WYLD: water yield (mm).</p>
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<p>Monthly values of the major hydrological components of hourly (<b>a</b>–<b>d</b>) model during the pre-fire and post-fire scenarios. SURQ: surface runoff (mm), PERC: percolation (mm), AET: actual evapotranspiration (mm), and WYLD: water yield (mm).</p>
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18 pages, 9769 KiB  
Article
A Framework for Integrating an Ecological Environment Process and Ecological Security Pattern in a Prefecture-Level City in China
by Tingshuang Zhang, Sixue Shi, Miao Liu, Chunlin Li, Hongyan Yin and Yan Du
Land 2024, 13(12), 2177; https://doi.org/10.3390/land13122177 - 13 Dec 2024
Viewed by 414
Abstract
Synthetical eco-environmental problems’ treatment is a new stage for certain pollutant control or ecological restoration. Traditional urban planners have focused more on social–economic development but less on eco-environmental considerations. Spatial planning is currently an essential administrative management method for regional development and eco-environmental [...] Read more.
Synthetical eco-environmental problems’ treatment is a new stage for certain pollutant control or ecological restoration. Traditional urban planners have focused more on social–economic development but less on eco-environmental considerations. Spatial planning is currently an essential administrative management method for regional development and eco-environmental protection in China. National and provincial spatial planning designs general strategies, and prefecture-level planning is the most important scale for spatial management. For scientific, spatial governance for eco-environmental protection, we propose a synthetic spatial analysis and planning method framework that involves atmospheric, edaphic, hydrographic, and ecological processes to identify pivotal regions for regional eco-environmental security goals. The synthetic method was conducted using advanced models including the CMAQ and SWAT models and spatial statistical methods. A Chinese prefecture-level city, Anshan City, was chosen to fulfill the method framework due to its various ecosystem types and environmental problems. A total of 67 eco-environmental management units (EMU) were divided based on atmospheric pollution patterns, hydrographic processes, edaphic heavy metal pollution, and ecological spatial analysis. Each unit was identified with ecological or environmental risk and a proposed management regulation. For considering the whole eco-environmental process, the ecological security pattern (ESP) was constructed. The results showed that 166 corridors were identified with an area of 2241.25 km2, with enhanced connectivity among 76 ecological sources (12.27% of Anshan City). By coupling two results, the optimized ecological conservation and restoration pattern was proposed, in which priority protection areas were identified. This synthetic method can provide scientific analysis and guidance to support spatial planning and ecological construction for multi-purpose ecological and environmental protection. Full article
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Figure 1
<p>Location of study area.</p>
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<p>Research methods and analytical framework.</p>
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<p>Spatial patterns of (<b>a</b>) resistance surface and (<b>b</b>) ecological corridors, as well as (<b>c</b>) spatial range of corridors and UTDB.</p>
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<p>Spatial distribution of ecological security pattern.</p>
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<p>The result of the partition control environmental zone. (<b>a</b>) Atmosphere; (<b>b</b>) water; (<b>c</b>) soil; (<b>d</b>) ecological space. PPZ: priority protection zones; GCZ: general control zones; HEZ: high-emission zones; LSZ: layout-sensitive zones; RSZ: receptor-sensitive zones; KPCZA: key pollution control zones for agriculture; KPCZI: key pollution control zones for industry; KPCZU: key pollution control zones for urban areas; KRCZ: key risk control zones.</p>
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<p>Classification map of environmental management units.</p>
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<p>Comprehensive pattern of protection and development in Anshan City. EMU: eco-environmental management unit; ESP: ecological security pattern; NTSP: national territorial spatial planning; UTDB: urban and town development boundary; EPR: ecological protection red line.</p>
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<p>Management policy for each unit.</p>
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<p>NTSP optimiztion route. EMU: eco-environmental management unit; ESP: ecological security pattern; NTSP: national territorial spatial planning; UTDB: urban and town development boundary; EPR: ecological protection red line.</p>
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22 pages, 4414 KiB  
Article
Coupled PLUS and SWAT Model Assessment of Streamflow Response to Climate Change and Human Interventions in Arid Alpine Regions: A Case Study of the Zamu River, China
by Honghua Xia, Linshan Yang, Qi Feng, Wei Liu, Yingqing Su, Minyan Wu, Wanghan He and Xingyi Zou
Land 2024, 13(12), 2166; https://doi.org/10.3390/land13122166 (registering DOI) - 12 Dec 2024
Viewed by 464
Abstract
Climate change and human interventions have exerted a long-term influence on variations in continental streamflow. Despite this, the precise mechanisms by which these factors regulate the change in streamflow remain inadequately understood, especially in arid alpine regions, due to the limited number of [...] Read more.
Climate change and human interventions have exerted a long-term influence on variations in continental streamflow. Despite this, the precise mechanisms by which these factors regulate the change in streamflow remain inadequately understood, especially in arid alpine regions, due to the limited number of observations which exacerbates difficulties in comprehensively assessing streamflow alterations. Consequently, assessing the impacts of climate change and human interventions on streamflow is a challenge in data-scarce regions. Here, using the Zamu River as an example, we analyzed streamflow changes in arid alpine regions using a method that integrates the Patch-generated Land Use Simulation model, the Soil and Water Assessment Tool, and the Coupled Model Intercomparison Project Phase 6. Our analysis highlighted that climate change primarily drove streamflow variations in the Zamu River, accounting for over 80% of the observed contributions. This influence was further amplified by the effects of future climate and changes in land use and land cover, resulting in increased streamflow. Additionally, precipitation emerged as the main factor driving the rise in streamflow. These findings emphasize the significant impact of climate change on water cycles in arid alpine regions and underscore the necessity for tailored water resource management strategies to ensure sustainable regional development and effective climate change adaptation. Full article
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Figure 1
<p>Location of the ZMR basin. (<b>a</b>) describes the location of the ZMR basin in China. (<b>b</b>) illustrates the environmental context of the ZMR basin, where DEM stands for Digital Elevation Model. The abbreviations used in the diagram are provided in <a href="#app1-land-13-02166" class="html-app">Supplementary Materials</a> <a href="#app1-land-13-02166" class="html-app">Table S1</a>.</p>
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<p>Streamflow research method. Note: The abbreviations illustrated in the diagram are defined in <a href="#app1-land-13-02166" class="html-app">Table S1 of the Supplementary Materials</a>.</p>
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<p>Status and simulated LUCC type in 2000, 2010, and 2020. Note: The abbreviations CL, FL, WB, UrL, UnL, HCG, MCG, and LCG represent cultivated land, forest land, water body, urban land, unutilized land, high-cover grassland, medium-coverage grassland, and low-cover grassland, respectively.</p>
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<p>LUCC in the ZMR from 1990 to 2030. (<b>a</b>) represents the spatial distribution of land use in ZMR from 1990 to 2030. (<b>b</b>) represents the land use change in ZMR from 1990 to 2030. Note: Abbreviations have the same meanings as in the caption of <a href="#land-13-02166-f003" class="html-fig">Figure 3</a>.</p>
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<p>Observed and simulated monthly streamflow in the ZMR. (<b>a</b>) illustrates the comparison between SWAT-simulated streamflow and the monthly observational data from the Zamusi Hydrological Station spanning the period 1980–2016. (<b>b</b>) displays a scatter plot of observed versus simulated streamflow during the calibration phase, while (<b>c</b>) shows the same comparison for the validation phase. Note: The green dashed line represents the 1:1 line.</p>
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<p>Taylor diagram of monthly precipitation, with T<sub>max</sub> and T<sub>min</sub> simulation results under different GCM models. (<b>a</b>) Simulation results for monthly precipitation. (<b>b</b>) Simulation results for T<sub>max</sub>. (<b>c</b>) Simulation results for T<sub>min</sub>.</p>
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<p>Annual and monthly change in precipitation (<b>a</b>,<b>b</b>), T<sub>max</sub> (<b>c</b>,<b>d</b>), and T<sub>min</sub> (<b>e</b>,<b>f</b>) from 1985 to 2050 in the ZMR. The 95% uncertainty bands are shown in the shaded region.</p>
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<p>Annual (<b>a</b>) and monthly (<b>b</b>) change in streamflow from 1985 to 2050 in the ZMR. The 95% uncertainty bands are shown in the shaded region.</p>
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<p>Change in monthly streamflow impacted by climate change and LUCC. (<b>a</b>) The impact of historical climate change alone on monthly scale streamflow change. (<b>b</b>) The impact of historical LUCC alone on monthly scale streamflow variations. (<b>c</b>) The impact of future climate change alone on monthly scale streamflow change under different scenarios. (<b>d</b>) The impact of future LUCC alone on monthly scale streamflow change under different scenarios.</p>
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<p>Heat map illustrating the correlation between monthly streamflow and precipitation (<b>a</b>), T<sub>max</sub> (<b>b</b>), and T<sub>min</sub> (<b>c</b>). Note: Single asterisks * represent statistical significance with <span class="html-italic">p</span> &lt; 0.05, whereas double asterisks ** indicate a higher level of significance with <span class="html-italic">p</span> &lt; 0.01.</p>
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<p>Streamflow suitability management in arid alpine regions.</p>
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21 pages, 9144 KiB  
Article
Evaluating the Hydrological Impact of Reservoir Operation on Downstream Flow of Seomjin River Basin: SWAT Model Approach
by Hiyaw Hatiya Ware, Sun Woo Chang, Jeong Eun Lee and Il-Moon Chung
Water 2024, 16(24), 3584; https://doi.org/10.3390/w16243584 (registering DOI) - 12 Dec 2024
Viewed by 372
Abstract
Multi-purpose dams in a river basin frequently result in variations in downstream flow. Precisely assessing the reservoir operation effects can improve management strategies and alleviate extreme hydrological events. This study assesses the impact of reservoir operation scenarios on the downstream flow in the [...] Read more.
Multi-purpose dams in a river basin frequently result in variations in downstream flow. Precisely assessing the reservoir operation effects can improve management strategies and alleviate extreme hydrological events. This study assesses the impact of reservoir operation scenarios on the downstream flow in the Seomjin River basin in South Korea. Four reservoir scenarios were developed utilizing observed daily inflow and outflow data from the reservoirs. A semi-disturbed hydrological model, SWAT (Soil and Water Assessment Tool), was employed to simulate the flow for each reservoir operation scenario in the downstream section of the study basin. Model execution was evaluated by comparing the simulated and measured streamflows using performance metrics, including R2, NSE, and PIBAS, which displayed very good compatibility. The sensitivity of calibration parameters varied across different reservoir operation scenarios. The results of this study indicate that the operation scenarios for the Seomjin and Juam reservoirs led to a maximum downstream flow reduction of 32%. Additionally, the monsoon season exhibited a lower percentage reduction in flow compared to the dry season, which was influenced by the frequency of rainfall in the region. Annual assessment indicated that streamflow reduction varies between 1.35% and 32.9% across all reservoir operation scenarios. Reservoir operations have demonstrated their effect on the alteration of downstream flow in the Seomjin River basin. This study demonstrates that the operation of the Seomjin reservoir has a more significant impact on downstream flow than that of the Juam reservoir in the study region. This study analyzed a substantial basin with various reservoir operation scenarios to assess the influence of flow on the downstream section, yielding important insights for efficient water resource management. Full article
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<p>Seomjin River basin including reservoirs, weather stations, streamflow gauge, and Digital Elevation Model (DEM).</p>
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<p>Study region soil classification: (<b>a</b>) soil code and (<b>b</b>) hydrological group.</p>
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<p>Seomjin watershed: (<b>a</b>) land use and land cover (LULC) classification and (<b>b</b>) slope class.</p>
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<p>Flowchart: overview approach utilized for current study.</p>
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<p>Seomjin and Juam reservoirs: (<b>a</b>) outflow values and (<b>b</b>) inflow values.</p>
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<p>Streamflow: (<b>a</b>) observed and simulated vs. time for calibration and validation periods, (<b>b</b>) observed vs. simulated during calibration, and (<b>c</b>) observed vs. simulated during validation.</p>
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<p>Reservoir operation scenario influence on the downstream flow: (<b>a</b>) monthly average and (<b>b</b>) annual average.</p>
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<p>Percentage of flow reduction due to reservoir operation scenarios vs. non-reservoir operation: (<b>a</b>) monthly average and (<b>b</b>) annual average.</p>
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<p>Box plots for reservoir operation scenarios and their downstream flow impact on the study region: (<b>a</b>) monthly average and (<b>b</b>) annual average.</p>
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<p>The study watershed hydrological water segments: (<b>a</b>) evapotranspiration (ET), (<b>b</b>) surface runoff (SURQ), (<b>c</b>) recharge, and (<b>d</b>) water yield (WYLD) in mm.</p>
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22 pages, 7136 KiB  
Article
Runoff Characteristics and Their Response to Meteorological Condition in the Yarlung Zangbo River Basin: Spatial Heterogeneity Due to the Glacier Coverage Difference
by Lei Zhu, Yun Deng, Ganggang Bai, Yi Tan, Youcai Tuo, Ruidong An, Xingmin Wang and Min Chen
Remote Sens. 2024, 16(24), 4646; https://doi.org/10.3390/rs16244646 - 11 Dec 2024
Viewed by 421
Abstract
The Yarlung Zangbo River (YZR) is a sizeable highland river on the Tibetan Plateau, and its runoff process is crucial for understanding regional water resource features and related ecological patterns. However, the runoff characteristics of the YZR Basin (YZRB) remain unclear, especially how [...] Read more.
The Yarlung Zangbo River (YZR) is a sizeable highland river on the Tibetan Plateau, and its runoff process is crucial for understanding regional water resource features and related ecological patterns. However, the runoff characteristics of the YZR Basin (YZRB) remain unclear, especially how it would react to climate change. This study comprehensively analyzed the runoff characteristics of the entire YZRB based on a validated distributed hydrological model (SWAT) coupled with a glacier module (SWAT-glac), identified the runoff components, and explored the climate–discharge relationship, with a particular focus on the relationships between glacier runoff and changes in precipitation and air temperature. The results indicate that the SWAT-glac model, with localized glacier parameters, accurately simulates the runoff processes due to regional differences in meteorological conditions and uneven glacier distribution. Summer runoff dominates the basin, contributing 46.2% to 57.9% of the total, while spring runoff is notably higher in the downstream sections than in other areas. Runoff components vary significantly across river sections; precipitation is the primary contributor to basin-wide runoff (23.4–59.5%), while glacier runoff contribution can reach up to 54.8% in downstream areas. The study found that underlying surface conditions, particularly glacier coverage, significantly influence runoff responses to meteorological changes. The correlation between runoff and precipitation is stronger at stations where rainfall predominates, whereas runoff shows greater sensitivity to air temperature in glacier-covered areas. These findings enhance the understanding of runoff processes in the YZRB and offer valuable insights for the sustainable management of water resources in similar basins under climate change. Full article
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<p>The distribution of hydrological stations in the Yarlung Zangbo River Basin and the subbasins controlled by each station.</p>
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<p>Schematic diagram of glacier module. P represents precipitation, SF represents snowfall, T<sub>av</sub> is the daily average temperature, SFTMP is the critical temperature at which snowfall occurs. S is the sublimation rate of ice/snow, M is the melt rate of ice/snow, and F represents the turnover rate of snow to ice. f is the refreezing proportion after ice melting and W represents the water equivalent of ice/snow.</p>
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<p>The spatial distributions of soil type (<b>a</b>) and land use (<b>b</b>) over the study area.</p>
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<p>Contribution of seasonal runoff at each station. The four boxes in each row represent the contribution of seasonal runoff at the nine stations in the study area.</p>
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<p>Monthly timestep parameter sensitivity assessment for nine stations in the YZRB. Yellow indicates higher sensitivity of the parameter, green corresponds to lower sensitivity, and black patches denote parameters considered insensitive at that station and not considered in subsequent model tuning processes.</p>
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<p>Monthly observed and simulated runoff trends from 2003 to 2016 for the nine stations in the YZRB. The slope coefficient is provided for both observed runoff (in red) and simulated runoff using the SWAT-glac model (in green). The dashed blue line separates the runoff calibration and validation time periods.</p>
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<p>Monthly average simulated rainfall, snowmelt, glacier, and groundwater runoff at each station in the YZRB from 2003 to 2016, along with their contributions to annual runoff.</p>
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<p>Distribution of simulated average monthly runoff at each station. The solid black line represents the error bars of average monthly runoff.</p>
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<p>Bivariate scatterplot matrix of simulated runoff versus precipitation, maximum and minimum temperatures for the five meteorological stations. The five stations are divided into two graphs to illustrate the content conveyed by the graphs: the left graph compares the Lazi, Rikaze, and Lhasa stations, while the right graph compares the Linzhi and Bomi stations.</p>
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<p>Correlation between monthly average simulated glacier runoff and monthly total precipitation and monthly average air temperature at each station. Black circles represent the correlation between glacier runoff and precipitation, while red circles represent the correlation between glacier runoff and monthly average air temperature.</p>
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14 pages, 432 KiB  
Article
Deep Reinforcement Learning-Based Adversarial Attack and Defense in Industrial Control Systems
by Mun-Suk Kim
Mathematics 2024, 12(24), 3900; https://doi.org/10.3390/math12243900 - 11 Dec 2024
Viewed by 427
Abstract
Adversarial attacks targeting industrial control systems, such as the Maroochy wastewater system attack and the Stuxnet worm attack, have caused significant damage to related facilities. To enhance the security of industrial control systems, recent research has focused on not only improving the accuracy [...] Read more.
Adversarial attacks targeting industrial control systems, such as the Maroochy wastewater system attack and the Stuxnet worm attack, have caused significant damage to related facilities. To enhance the security of industrial control systems, recent research has focused on not only improving the accuracy of intrusion detection systems but also developing techniques to generate adversarial attacks for evaluating the performance of these intrusion detection systems. In this paper, we propose a deep reinforcement learning-based adversarial attack framework designed to perform man-in-the-middle attacks on industrial control systems. Unlike existing adversarial attack methods, our proposed adversarial attack scheme learns to evade detection by the intrusion detection system based on both the impact on the target and the detection results from previous attacks. For performance evaluation, we utilized a dataset collected from the secure water treatment (SWaT) testbed. The simulation results demonstrated that our adversarial attack scheme successfully executed man-in-the-middle attacks while evading detection by the rule-based intrusion detection system, which was defined based on the analysis of the SWaT dataset. Full article
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<p>A simplified scenario of the SWaT system.</p>
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<p>Overview of our deep reinforcement learning process for adversarial attacks.</p>
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<p>Deep neural network-based policy function.</p>
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<p>The actual and manipulated measurements of sensor LIT101 over 100 time steps.</p>
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<p>The actual and manipulated measurements of sensor FIT101 over 100 time steps.</p>
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<p>The actual and manipulated measurements of sensor FIT201 over 100 time steps.</p>
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<p>The actual and manipulated measurements of sensor LIT301 over 100 time steps.</p>
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22 pages, 1542 KiB  
Review
Global Applications of the CE-QUAL-W2 Model in Reservoir Eutrophication: A Systematic Review and Perspectives for Brazil
by Sarah Haysa Mota Benicio, Raviel Eurico Basso and Klebber Teodomiro Martins Formiga
Water 2024, 16(24), 3556; https://doi.org/10.3390/w16243556 - 10 Dec 2024
Viewed by 493
Abstract
The CE-QUAL-W2 model is a significant tool extensively used in lentic environments to analyze eutrophication and water quality. This systematic review of the CE-QUAL-W2 hydrodynamic model revealed its widespread application in analyzing reservoir eutrophication. A total of 151 relevant papers were identified, of [...] Read more.
The CE-QUAL-W2 model is a significant tool extensively used in lentic environments to analyze eutrophication and water quality. This systematic review of the CE-QUAL-W2 hydrodynamic model revealed its widespread application in analyzing reservoir eutrophication. A total of 151 relevant papers were identified, of which 38 were selected after rigorous analysis, showcasing studies in environmental sciences and water resources. In 2021, we saw the highest number of publications, with six papers; 2022 achieved the highest number of citations, with 113. The model has been widely used across countries, with Iran leading in the number of publications, followed by China and Brazil. The standard combination of CE-QUAL-W2 with the SWAT model reflects its effectiveness in complex watershed studies. CE-QUAL-W2 has demonstrated the ability to predict future environmental conditions and diagnose environmental extremes, and it can calculate various hydrodynamic and water quality parameters. Its increasing use in high-impact scientific journals underscores its global relevance and particular promise for Brazilian aquatic environment studies due to its efficiency and accessibility. With its significant potential, this model is poised to enhance the understanding and management of water resources, contributing to environmental sustainability and inspiring optimism for future applications on a global scale. Full article
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<p>Flowchart of the methodology adopted in this systematic review of the CE-QUAL-W2 model. This flowchart illustrates the steps taken to identify, select, and analyze relevant studies on applying the CE-QUAL-W2 hydrodynamic model, focusing on its use in lentic environments for assessing eutrophication and water quality.</p>
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<p>Distribution of journals and categories based on the area of study of the articles analyzed, including the number of citations and publications for the selected works. This figure categorizes the journals that published studies on the CE-QUAL-W2 model. It specifies their thematic areas and provides quantitative data on citations and publications to highlight the model’s impact in different research fields.</p>
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<p>Countries studied in the selected works on the CE-QUAL-W2 model application. This map indicates the geographic distribution of research using the CE-QUAL-W2 model, emphasizing the countries where it has been applied most frequently, including Iran, China, and Brazil. The analysis provides insights into the global adoption of the model in various environmental and water resource studies [<a href="#B12-water-16-03556" class="html-bibr">12</a>,<a href="#B13-water-16-03556" class="html-bibr">13</a>,<a href="#B14-water-16-03556" class="html-bibr">14</a>,<a href="#B18-water-16-03556" class="html-bibr">18</a>,<a href="#B21-water-16-03556" class="html-bibr">21</a>,<a href="#B22-water-16-03556" class="html-bibr">22</a>,<a href="#B23-water-16-03556" class="html-bibr">23</a>,<a href="#B24-water-16-03556" class="html-bibr">24</a>,<a href="#B25-water-16-03556" class="html-bibr">25</a>,<a href="#B26-water-16-03556" class="html-bibr">26</a>,<a href="#B27-water-16-03556" class="html-bibr">27</a>,<a href="#B28-water-16-03556" class="html-bibr">28</a>,<a href="#B29-water-16-03556" class="html-bibr">29</a>,<a href="#B30-water-16-03556" class="html-bibr">30</a>,<a href="#B31-water-16-03556" class="html-bibr">31</a>,<a href="#B32-water-16-03556" class="html-bibr">32</a>,<a href="#B33-water-16-03556" class="html-bibr">33</a>,<a href="#B34-water-16-03556" class="html-bibr">34</a>,<a href="#B35-water-16-03556" class="html-bibr">35</a>,<a href="#B36-water-16-03556" class="html-bibr">36</a>,<a href="#B37-water-16-03556" class="html-bibr">37</a>,<a href="#B38-water-16-03556" class="html-bibr">38</a>,<a href="#B39-water-16-03556" class="html-bibr">39</a>,<a href="#B40-water-16-03556" class="html-bibr">40</a>,<a href="#B41-water-16-03556" class="html-bibr">41</a>,<a href="#B42-water-16-03556" class="html-bibr">42</a>,<a href="#B43-water-16-03556" class="html-bibr">43</a>,<a href="#B44-water-16-03556" class="html-bibr">44</a>,<a href="#B45-water-16-03556" class="html-bibr">45</a>,<a href="#B46-water-16-03556" class="html-bibr">46</a>,<a href="#B47-water-16-03556" class="html-bibr">47</a>,<a href="#B48-water-16-03556" class="html-bibr">48</a>,<a href="#B49-water-16-03556" class="html-bibr">49</a>,<a href="#B50-water-16-03556" class="html-bibr">50</a>,<a href="#B51-water-16-03556" class="html-bibr">51</a>,<a href="#B52-water-16-03556" class="html-bibr">52</a>,<a href="#B53-water-16-03556" class="html-bibr">53</a>,<a href="#B54-water-16-03556" class="html-bibr">54</a>].</p>
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21 pages, 10674 KiB  
Article
Multi-Scale Effect of Land Use Landscape on Basin Streamflow Impacts in Loess Hilly and Gully Region of Loess Plateau: Insights from the Sanchuan River Basin, China
by Zexin Lei, Shifang Zhang, Wenzheng Zhang, Xuqiang Zhao and Jing Gao
Sustainability 2024, 16(23), 10781; https://doi.org/10.3390/su162310781 - 9 Dec 2024
Viewed by 586
Abstract
The gullies and valleys of the Loess Plateau, as key ecological zones for soil erosion control, play a critical role in the region’s sustainable development under increasing urbanization. This study employed the Soil and Water Assessment Tool (SWAT) to analyze the impacts of [...] Read more.
The gullies and valleys of the Loess Plateau, as key ecological zones for soil erosion control, play a critical role in the region’s sustainable development under increasing urbanization. This study employed the Soil and Water Assessment Tool (SWAT) to analyze the impacts of land use/cover changes (LUCC) on runoff at multiple spatial scales and locations within the Sanchuan River Basin (SRB) in the loess hilly and gully region. The methodology integrates SWAT modeling with LUCC scenario analysis, focusing on spatial and scale effects of land use changes on hydrological processes. The results revealed distinct spatial differences, with diminishing LUCC impacts on streamflow from the upper to lower reaches of the basin, regardless of land use type. Scale effects were also evident: grassland effectively controlled runoff within 300 m of riparian zones, while forest land was most effective beyond 750 m. A relatively insensitive range for runoff changes was observed between 300 and 750 m. These findings highlight the critical role of LUCC in influencing runoff patterns and underscore the importance of region-specific and scale-sensitive land use management strategies. This research provides valuable guidance for sustainable land planning, particularly in riparian zones, to enhance runoff control and optimize ecological benefits. Full article
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<p>Location of the SRB. (<b>a</b>) The SRB in the Loess Plateau of northwest China, (<b>b</b>) the digital elevation model of the SRB, (<b>c</b>) rivers and major hydrologic stations of the SRB, and (<b>d</b>) soil classification of the SRB. Readers can refer to the official database (<a href="http://www.fao.org/soils-portal/soil-survey/soil-maps-and-databases/faounesco-soil-map-of-the-world/en/" target="_blank">http://www.fao.org/soils-portal/soil-survey/soil-maps-and-databases/faounesco-soil-map-of-the-world/en/</a>, accessed on 12 October 2024) for a complete list of soil classes and their definitions.</p>
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<p>Setting scenarios at different LUCCs in upper, middle, and lower basins. (<b>a</b>) Upstream, midstream, and downstream zoning of SRB, and (<b>b</b>) 27 scenarios set up for LUCC in the upstream, midstream, and downstream based on 1980 land use/cover.</p>
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<p>Land use/cover change from 1980 to 2020: (<b>a</b>) land use/cover of the SRB in 1980 and 2020, and (<b>b</b>) Sankey diagram of LUCC from 1980 to 2020.</p>
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<p>LUCC at different buffer scales along the stream. (<b>a</b>) Integrated LUCC dynamics at different buffer scales. (<b>b</b>) Spatial transformation of land use/cover at different buffer scales.</p>
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<p>The comparison data of monthly streamflow volume from 1975 to 1984, between the measured value of the Houdacheng Hydrological Station and the simulated value of the SWAT model.</p>
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<p>Model simulation results of multi-year average streamflow in the SRB under 27 scenarios of different LUCCs in the upper, middle, and lower basins.</p>
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<p>Model simulation results under scenarios of LUCC with different buffer widths. (<b>a</b>) Buffer zones of buffer widths from 150 to 1500 m. (<b>b</b>) Model simulation results of multi-year average streamflow in the SRB under 40 scenarios of LUCC with different buffer widths.</p>
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<p>Scenarios of different land uses in the buffer zone along the river based on 1980 land use.</p>
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21 pages, 5674 KiB  
Article
Multi-Scale Spatial Relationship Between Runoff and Landscape Pattern in the Poyang Lake Basin of China
by Panfeng Dou, Yunfeng Tian, Jinfeng Zhang and Yi Fan
Water 2024, 16(23), 3501; https://doi.org/10.3390/w16233501 - 5 Dec 2024
Viewed by 376
Abstract
Runoff research serves as the foundation for watershed management, and the relationship between runoff and landscape pattern represents a crucial basis for decision-making in the context of watershed ecological protection and restoration. However, there is a paucity of research investigating the multi-scale spatial [...] Read more.
Runoff research serves as the foundation for watershed management, and the relationship between runoff and landscape pattern represents a crucial basis for decision-making in the context of watershed ecological protection and restoration. However, there is a paucity of research investigating the multi-scale spatial relationship between runoff and landscape patterns. This study employs the Poyang Lake Basin (PLB) as a case study for illustrative purposes. The construction of the soil and water assessment tool (SWAT) model is the initial step in the process of carrying out runoff simulation, which in turn allows for the analysis of the spatial–temporal characteristics of runoff. Subsequently, Pearson’s correlation analysis, global linear regression and geographically weighted regression (GWR) models are employed to examine the impact of landscape composition on runoff. Finally, the spatial relationship between runoff and landscape pattern is investigated at the landscape and class scales. The results of the study demonstrate the following: (1) runoff in the PLB exhibited considerable spatial–temporal heterogeneity from 2011 to 2020. (2) Forest was the most prevalent landscape type within the PLB. Landscape composition’s impact on runoff exhibited non-linear characteristics, with forest, cropland, barren, and grassland influencing runoff in decreasing order. (3) A spatial relationship between runoff and landscape pattern was observed. At the landscape scale, patch diversity significantly influenced runoff, and reducing patch diversity primarily increased runoff. At the class scale, forest and cropland patch areas had the greatest impact on runoff, potentially enhanced by improving patch edge density. (4) Nine sub-basins needing ecological restoration were identified, with restoration pathways developed based on spatial relationships between runoff and landscape patterns. This study elucidates the impact of landscape composition and pattern on runoff, thereby providing a basis for informed decision-making and technical support for the ecological restoration and management of the watershed. Full article
(This article belongs to the Special Issue Watershed Hydrology and Management under Changing Climate)
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<p>Location of the Poyang Lake Basin.</p>
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<p>Elevation and sub-basin division in the Poyang Lake Basin. Note: The numbers in the right part of this figure represent the sub-basin numbers.</p>
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<p>A comparative analysis of the flow dynamics observed and simulated in the Poyang Lake Basin. Note: 201101 represents January 2011.</p>
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<p>Spatial–temporal pattern of runoff in the Poyang Lake Basin from 2011 to 2020.</p>
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<p>Spatial distribution of landscape types and proportions in the Poyang Lake Basin.</p>
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<p>Spatial distribution of geographically weighted regression coefficients between runoff and landscape type in the Poyang Lake Basin.</p>
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<p>Spatial distribution of key landscape metrics at the landscape and class scales in the Poyang Lake Basin.</p>
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<p>Spatial distribution of geographically weighted regression coefficients between runoff and landscape metrics at landscape and class scales in the Poyang Lake Basin. Note: R<sup>2</sup> = N/A indicates that the GWR model was not successfully constructed.</p>
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<p>Ecological restoration pathways in sub-basins of the Poyang Lake Basin.</p>
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19 pages, 9251 KiB  
Article
Water Balance Analysis in the Majalaya Watershed: Two-Step Calibration and Application of the SWAT+ Model for Low-Flow Conditions
by Hadi Kardhana, Abdul Wahab Insan Lihawa, Faizal Immaddudin Wira Rohmat, Siska Wulandari, Wendi Harjupa, Widyawardana Adiprawita, Edwan Kardena and Muhammad Syahril Badri Kusuma
Water 2024, 16(23), 3498; https://doi.org/10.3390/w16233498 - 5 Dec 2024
Viewed by 595
Abstract
Understanding hydrological processes is crucial for effective watershed management, with SWAT+ being one of the widely adopted models for analyzing water balance at watershed scales. While hydrological components are often assessed through sensitivity analysis, calibration, and validation, parameter sensitivity during dry periods (low-flow [...] Read more.
Understanding hydrological processes is crucial for effective watershed management, with SWAT+ being one of the widely adopted models for analyzing water balance at watershed scales. While hydrological components are often assessed through sensitivity analysis, calibration, and validation, parameter sensitivity during dry periods (low-flow conditions) when baseflow is predominant remains a relevant focus, especially for watersheds like Majalaya, Indonesia, which experience distinct low-flow periods. This study analyzes water balance components in the Majalaya watershed, Indonesia, using SWAT+ across the 2014–2022 period, focusing on low-flow conditions. This study employs a two-step calibration approach using various datasets, including ground rainfall (2014–2022), NASA POWER meteorological data, MODIS land cover, DEMNAS terrain, and DSMW soil types, and the streamflow data for model calibration. The first calibration step optimized the overall performance (R2 = 0.41, NSE = 0.41, and PBIAS = −7.33), and the second step improved the baseflow simulation (R2 = 0.40, NSE = 0.35, and PBIAS = 12.45). A Sobol sensitivity analysis identified six primary parameters, i.e., CN3_SWF, CN2, LATQ_CO, PERCO, SURLAG, and CANMX, as the most influential for streamflow calibration, with CN3_SWF and CN2 being the most critical. This study demonstrates SWAT+’s effectiveness in watershed management and water resource optimization, particularly during low-flow conditions. Full article
(This article belongs to the Special Issue Applications of Remote Sensing and Modeling in Hydrological Systems)
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<p>(<b>a</b>) West Java Province, on the western part of the island. (<b>b</b>) The upper Citarum watershed consists of several sub-watersheds, with the Majalaya watershed as the uppermost sub-watershed. (<b>c</b>) Detailed map of the Majalaya watershed, covering a total area of 207.2 km<sup>2</sup>, with the red dot indicating the outlet point at the AWLR Majalaya stream gauge. (<b>d</b>) Land cover of Majalaya watershed in 2022 based on MODIS data. (<b>e</b>) Soil type of Majalaya watershed based on HWSD data.</p>
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<p>The research workflow utilizes the SWAT+ model to simulate the water balance in the Majalaya watershed. The model requires specific input data to identify the parameters most sensitive to the water balance. Calibration was carried out using observed discharge data from stream gauges, and the model’s performance was evaluated through statistical analysis.</p>
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<p>SWAT+ parameter sensitivity results using a built-in Sobol sensitivity test, ranked from the most sensitive (CN3_SWF) to the least nonzero variable (CANMX). First-order sensitivity (also known as the main effect index) is a dimensionless value, representing the proportion of the total variance in the model output that can be attributed to variations in a single input parameter, without considering interactions with other parameters.</p>
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<p>Calibration results from the first approach indicate that SWAT+ struggles to accurately model field conditions during the dry season, where baseflow continues to contribute to river flow. In contrast, the second approach specifically targets dry season conditions, focusing on periods without rainfall. These periods were divided into three distinct parts (I, II, III) based on rainfall observation data, with an emphasis on improving the model’s performance during dry conditions.</p>
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<p>FDC of the streamflow calibration results for the Majalaya watershed. Shows the differences between the results of the first-step approach (magenta line) and the second-step approach that focuses on the low flow (navy line). The first step approach yielded better NSE but failed to simulate the observed low flow, while the second simulation yielded better results in the low flow area.</p>
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<p>Majalaya SWAT+ modeling results of the monthly streamflow simulation for the 2014–2022 period, which generally show good agreement on a monthly basis. Note that the 2019 observation data were unavailable.</p>
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<p>Annual Majalaya watershed water balance components on the 1st step and 2nd step. The average annual rainfall is 2316.76 mm, with a 1st step water balance of 2320.3 mm and a second-step water balance of 2266.2 mm.</p>
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15 pages, 7252 KiB  
Article
Linking Land Use Change and Hydrological Responses: The Role of Agriculture in the Decline of Urmia Lake
by Amirhossein Mirdarsoltany, Alireza B. Dariane, Mahboobeh Ghasemi, Sepehr Farhoodi, Roza Asadi and Akbar Moghaddam
Hydrology 2024, 11(12), 209; https://doi.org/10.3390/hydrology11120209 - 3 Dec 2024
Viewed by 586
Abstract
The water level and surface area of Urmia Lake, located in the northwest of Iran, has decreased dramatically, presenting significant challenges for hydrological modeling due to complex interactions between surface and groundwater. In this study, the impact of agricultural activities on streamflow within [...] Read more.
The water level and surface area of Urmia Lake, located in the northwest of Iran, has decreased dramatically, presenting significant challenges for hydrological modeling due to complex interactions between surface and groundwater. In this study, the impact of agricultural activities on streamflow within one of the largest sub-basins of Urmia Lake is assessed using the Soil and Water Assessment Tool (SWAT) for hydrological assessments. To have accurate assessments, land use change detections were considered by a novel method, which merges the Normalized Difference Vegetation Index (NDVI) with the Digital Elevation Model (DEM) to create a two-band NDVI-DEM image, effectively differentiating between agricultural and rangeland fields. Our findings reveal that agricultural development and irrigation, escalating between 1977 and 2015, resulted in increased annual evapotranspiration (ET) (ranging from 295 mm to 308 mm) and a decrease in yearly streamflow, from 317 million cubic meters to 300 million cubic meters. Overall, our study highlights the significant role that agricultural development and irrigation may play in contributing to the shrinking of Lake Urmia, underscoring the need for improved regional water management strategies to address these challenges, though further analysis across additional basins would be necessary for broader conclusions. Full article
(This article belongs to the Section Surface Waters and Groundwaters)
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<p>Location of the study area: (<b>a</b>) in Iran, (<b>b</b>) DEM, and (<b>c</b>) stream network along with hydrometric and weather stations.</p>
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<p>Generated land use maps for July (<b>a</b>) 1977 (<b>b</b>) 1993 (<b>c</b>) 2005, and (<b>d</b>) 2015.</p>
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<p>Changes in (<b>a</b>) land area and (<b>b</b>) percentage of agricultural and urban land over time for selected years (1977, 1993, 2005, 2015).</p>
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<p>Monthly averages of simulated and observed streamflow for the calibration and validation periods.</p>
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<p>Comparison of simulated groundwater drawdown with observed values in the Sarab plain.</p>
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<p>Comparison of average annual ET and streamflow for (<b>a</b>) irrigation scenario and (<b>b</b>) no-irrigation scenario.</p>
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<p>Comparison of (<b>a</b>) annual average ET and (<b>b</b>) annual average streamflow for irrigation and no-irrigation scenarios.</p>
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24 pages, 6911 KiB  
Article
The Response of Runoff to Land Use Change in the Northeastern Black Soil Region, China
by Yonggang Hao, Peng Qi and Chong Du
Water 2024, 16(23), 3456; https://doi.org/10.3390/w16233456 - 1 Dec 2024
Viewed by 482
Abstract
With the intensification of climate change and human activities, the impacts of land use shifts on hydrological processes are becoming more pronounced, especially in regions with complex geographic, geological, and climatic conditions such as the Northeast Black Soil Region, China. This study quantitatively [...] Read more.
With the intensification of climate change and human activities, the impacts of land use shifts on hydrological processes are becoming more pronounced, especially in regions with complex geographic, geological, and climatic conditions such as the Northeast Black Soil Region, China. This study quantitatively examines the variations in various land use types from 1980 to 2020 by means of a land use transfer matrix, and it incorporates the multi-year average runoff value to mitigate the interference of short-term climate fluctuations on the runoff trend, thereby enhancing the representativeness and stability of the simulation outcomes. The SWAT (Soil and Water Assessment Tool) model is employed to simulate land use alterations in different periods. The findings indicate that the area of farmland increased by 5.34% and the area of grassland decreased by 5.36% over 40 years. The areas of forest land and wetland have fluctuated significantly due to policy interventions and population growth. This study discovers that LUCC has resulted in a marginal increase in annual water yield. For instance, the water yield of paddy fields in 2020 amounts to 92.26 mm/year, which is 0.52–9.42% higher than the historical scenario and exhibits a notable upward trend in summer. Spatial analysis discloses regional disparities, with substantial changes in the hydrological behavior of northern watersheds (such as the Huma River) and southeastern regions (such as the Toudao River). The augmentation of wetland and forest coverage has effectively mitigated peak runoff, especially during extreme rainfall events. Wetlands have manifested strong water regulation capabilities and alleviated the impact of floods. This study quantitatively discloses the complex response pattern of LUCC to runoff by introducing a multi-scale analysis approach, which furnishes a scientific basis for flood risk assessment, land use optimization, and water resource management, and demonstrates the potential for extensive application in other countries and regions with similar climatic and topographic conditions. Full article
(This article belongs to the Section Soil and Water)
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<p>Location and elevations of the River Basin in Northeast Black Soil Region of China, gauging stations, weather stations, rivers, and the study area.</p>
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<p>Land use in 1980, 1990, 2000, 2010, and 2020 in River Basin in Northeast Black Soil Region, China.</p>
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<p>Land use transfer matrix from 1980 to 2020. The lines illustrate the conversion between different land use types across time periods, highlighting the dynamics of land use change.</p>
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<p>Annual runoff at the downstream outlet of the Songhua River under different scenarios (S0, S1, S2, S3, and S4).</p>
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<p>Monthly distribution of multi-year average water yield in the River Basin of Northeast Black Soil Region, China, under different scenarios (S0, S1, S2, S3, and S4).</p>
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<p>Runoff coefficient distribution in River Basin in Northeast Black Soil Region, China.</p>
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<p>The six hydrological variables expressed as a proportion of the mean annual precipitation are: groundwater contribution to streamflow (GWQ), lateral flow contribution to streamflow (LATQ), percolation beyond the root zone (PERC), surface runoff generated within the watershed (SURQ), and soil water (SW). The six hydrological variables expressed as a proportion of the mean annual precipitation are: groundwater contribution to streamflow (GWQ), lateral flow contribution to streamflow (LATQ), percolation beyond the root zone (PERC), surface runoff generated within the watershed (SURQ), soil water content (SW), and water yield (WYLD).</p>
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<p>Spatial distribution of seasonal water yield under different scenarios (S0, S1, S2, S3, and S4). Each subfigure (<b>a</b>–<b>d</b>) represents the water yield for spring, summer, autumn, and winter.</p>
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<p>Spatial distribution of absolute changes in seasonal water yield under different scenarios (S0, S1, S2, S3, and S4).</p>
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