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Search Results (3,693)

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Keywords = spatial-temporal dynamic

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17 pages, 5497 KiB  
Article
High Spatiotemporal Resolution Monitoring of Water Body Dynamics in the Tibetan Plateau: An Innovative Method Based on Mixed Pixel Decomposition
by Yuhang Jing and Zhenguo Niu
Sensors 2025, 25(4), 1246; https://doi.org/10.3390/s25041246 - 18 Feb 2025
Abstract
The Tibetan Plateau, known as the “Third Pole” and the “Water Tower of Asia”, has experienced significant changes in its surface water due to global warming. Accurately understanding and monitoring the spatiotemporal distribution of surface water is crucial for ecological conservation and the [...] Read more.
The Tibetan Plateau, known as the “Third Pole” and the “Water Tower of Asia”, has experienced significant changes in its surface water due to global warming. Accurately understanding and monitoring the spatiotemporal distribution of surface water is crucial for ecological conservation and the sustainable use of water resources. Among existing satellite data, the MODIS sensor stands out for its long time series and high temporal resolution, which make it advantageous for large-scale water body monitoring. However, its spatial resolution limitations hinder detailed monitoring. To address this, the present study proposes a dynamic endmember selection method based on phenological features, combined with mixed pixel decomposition techniques, to generate monthly water abundance maps of the Tibetan Plateau from 2000 to 2023. These maps precisely depict the interannual and seasonal variations in surface water, with an average accuracy of 95.3%. Compared to existing data products, the water abundance maps developed in this study provide better detail of surface water, while also benefiting from higher temporal resolution, enabling effective capture of dynamic water information. The dynamic monitoring of surface water on the Tibetan Plateau shows a year-on-year increase in water area, with an increasing fluctuation range. The surface water abundance products presented in this study not only provide more detailed information for the fine characterization of surface water but also offer a new technical approach and scientific basis for timely and accurate monitoring of surface water changes on the Tibetan Plateau. Full article
(This article belongs to the Special Issue Feature Papers in Remote Sensors 2024)
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<p>Study Area Overview.</p>
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<p>Workflow of Water Body Abundance Inversion on the Tibetan Plateau.</p>
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<p>Abundance maps and validation results: (<b>a</b>) Abundance results for July 2017; (<b>b</b>) Distribution of classification accuracy, commission rate, and omission rate; (<b>c</b>) Scatter plot of RMSE and ME distribution.</p>
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<p>Analysis of Area Trend Over the Year.</p>
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<p>Comparison with Other Datasets: (<b>a</b>) Comparison of Area with Other Datasets; (<b>b</b>) Correlation of Abundance Map with Other Datasets.</p>
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<p>Interannual Area Change Diagram.</p>
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<p>Correlation Analysis with JRC and GSWED Datasets.</p>
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<p>Identification Results of Small Water Bodies.</p>
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<p>Identification of Linear Water Bodies.</p>
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<p>Potential of Abundance Maps in Wetland Classification.</p>
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20 pages, 25931 KiB  
Article
Evaluation of In-Situ Low-Cost Sensor Network in a Tropical Valley, Colombia
by Laura Rojas González and Elena Montilla-Rosero
Sensors 2025, 25(4), 1236; https://doi.org/10.3390/s25041236 - 18 Feb 2025
Abstract
The increase in yearly particulate matter concentrations has been a constant issue since 2017 in the Aburrá Valley, located in Antioquia, Colombia. Although local certified air quality monitors provide high accuracy, they are limited in spatial coverage, limiting chemical transport and pollution dynamic [...] Read more.
The increase in yearly particulate matter concentrations has been a constant issue since 2017 in the Aburrá Valley, located in Antioquia, Colombia. Although local certified air quality monitors provide high accuracy, they are limited in spatial coverage, limiting chemical transport and pollution dynamic studies in this mountainous environment. In this work, a local, Low-Cost Sensor network is proposed as an alternative and has been installed around the valley in representative locations and heights. To calibrate PM2.5 and O3 sensors used by the network, temporal delays were analyzed with Dynamic Time Warping and the linear scale was corrected with a Single Linear Regression model. As a result, the correlation coefficient R2 of the sensor reached values of 0.8 and 0.9 after calibration. For all network stations, rescaled data agrees with official historical reports on the behavior of pollutant concentrations and meteorological variables. The ability to compare the network results with certified data confirms the success of the calibration/validation method employed and contributes to the growing field of low-cost air quality sensors in Latin America. Full article
(This article belongs to the Section Environmental Sensing)
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<p>Simple LCS unit and cross section, labeled main parts.</p>
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<p>4DAir in-situ Monitoring Network in Aburrá Valley.</p>
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<p>Temporal delay identification between SIATA and Simple unit signals using the DTW-AROW method. For (<b>a</b>) PM<sub>2.5</sub> and (<b>b</b>) O<sub>3</sub> raw signals.</p>
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<p>Simple unit data corrected compared with SIATA reference values and Simple unit raw signals. (<b>a</b>) PM<sub>2.5</sub>, (<b>b</b>) O<sub>3</sub>.</p>
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<p>Corrected measurements for the Simple LCS signals compared to the reference values (SIATA). (<b>a</b>) PM<sub>2.5</sub>, (<b>b</b>) O<sub>3</sub>.</p>
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<p>Scatter plots of the correlation between Simple unit data and reference data: (<b>a</b>) PM<sub>2.5</sub> concentration comparison with reference sampler; (<b>b</b>) O<sub>3</sub> concentration comparison with reference analyzer.</p>
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<p>Monthly average concentration reported by the 4DAir network for PM<sub>2.5</sub> and O<sub>3</sub>.</p>
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<p>Monthly average of meteorological variables in the 4DAir network according to classified areas.</p>
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<p>PM<sub>2.5</sub> daily averages reported by the network.</p>
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<p>Air Quality Index (AQI) for PM<sub>2.5</sub> from 4DAir network information.</p>
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17 pages, 6293 KiB  
Article
Exploiting Enhanced Altimetry for Constraining Mesoscale Variability in the Nordic Seas and Arctic Ocean
by Antonio Bonaduce, Andrea Storto, Andrea Cipollone, Roshin P. Raj and Chunxue Yang
Remote Sens. 2025, 17(4), 684; https://doi.org/10.3390/rs17040684 - 17 Feb 2025
Viewed by 120
Abstract
Recent advances in Arctic observational capabilities have revealed that the Arctic Ocean is highly turbulent in all seasons and have improved temporal and spatial sampling of sea level retrievals from remote sensing, even above 80°N. Such data are expected to be increasingly valuable [...] Read more.
Recent advances in Arctic observational capabilities have revealed that the Arctic Ocean is highly turbulent in all seasons and have improved temporal and spatial sampling of sea level retrievals from remote sensing, even above 80°N. Such data are expected to be increasingly valuable in the future when the extent of sea ice in the Arctic Ocean is reduced. Assimilating this new data into ocean models, together with in situ observations, provides an enriched representation of the mesoscale population that induces new eddy-driven contributions to local dynamics and thermodynamics. To quantify the content of the new information, we compare three-year-long assimilative experiments at ¼° resolution incorporating in situ-only data, in situ and standard altimetry, and in situ and high-latitude-enhanced altimetry, respectively. The enhanced altimetry data lead to an increase in three-dimensional eddy kinetic energy, generated by coherent vortexes, of up to 20% in several areas. Robust ocean warming is generated in the Arctic sector down to 800 m. Via heat budget analysis, this warming can be ascribed to a local enhancement of vertical mixing, as well as an increase in meridional heat transport. The assimilation of enhanced altimetry amplifies the transport, compared to standard altimetry, especially north of 70°N. Full article
(This article belongs to the Special Issue Recent Advances on Oceanic Mesoscale Eddies II)
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<p><b>Top</b>: Variance of the sea-level anomaly (SLA) field (cm<sup>2</sup>) obtained considering conventional (<b>left</b>) and enhanced satellite altimetry gridded maps (L4) over the period 2017–2019. The letters in the (<b>right</b>) panel depict the areas of the Lofoten Basin (LB), Barents Sea (BS), Fram Strait (FS), Nansen Basin (NB), Kara Sea (KS), Laptev Sea (LS), Beaufort Gyre (BG), Greenland Sea (GS) and Labrador Sea (LBS). <b>Bottom</b>: SLA variance differences (cm<sup>2</sup>) between enhanced and conventional altimetry data: positive values show a larger variability in the enhanced altimetry signals.</p>
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<p>Extension and bathymetry of the CREG025 regional configuration of the NEMO model used in this study as a model component of the analysis system. The black rectangle identifies the region where the heat budget analysis was performed (<a href="#sec3-remotesensing-17-00684" class="html-sec">Section 3</a>).</p>
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<p>REKE obtained considering eddy lifetime &gt;14 days in each experiment during 2017–2019 at the surface (<b>top panels</b>). Focusing on summer months only (JJA), surface REKE is shown in the <b>central panels</b> while 3D REKE is shown in the <b>bottom panels</b>. Values are expressed as the fraction of ocean kinetic energy carried by eddies.</p>
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<p>Meridional heat transport (MHT). The panels show the MHT in the experiments, obtained considering a latitudinal range between 61°N and 82°N during 2017–2019 (<b>top left</b>), as a difference with respect to EXP0 (<b>bottom left</b>) and as a percent difference between EXP2 and EXP1 during winter (DJF), spring (MAM), summer (JJA) and autumn (SON) over the period 2017–2019.</p>
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<p>Eddy component of the MHT (<b>left panel</b>) and percent contribution of the eddy and mean components (<b>middle</b> and <b>right panels</b>) for the three experiments presented in the text, as a function of latitude.</p>
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<p>Time-averaged difference of ocean heat content (full column, <b>left panel</b>, in J m<sup>−2</sup>), sea-ice concentration (<b>middle panel</b>, dimensionless), and net downward heat flux (<b>right panel</b>, in W m<sup>−2</sup>) between experiments EXP2 and EXP1. The black rectangle identifies the region where the heat budget analysis was performed.</p>
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<p>Heat budget component analysis as a time series of different heat components for the study region (<b>left panel</b>) and vertical profiles of mean temperature, mean cumulated analysis increments, and their differences between EXP2 and EXP1 (<b>right panels</b>). OHC: Ocean heat content (total warming); NHF: net downward heat flux at the sea interface with atmosphere or ice; ANI: data assimilation analysis of increments’ contribution; TRA: lateral transport. In the rightmost panel, TEM refers to the total temperature differences, and ANI refers to those induced by the data assimilation analysis increments.</p>
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29 pages, 6598 KiB  
Article
Relationships and Spatiotemporal Variations of Ecosystem Services and Land Use in Alpine Ecosystems: A Case Study of the Daxing’anling Forest Area, Inner Mongolia
by Laixian Xu, Youjun He, Liang Zhang, Chunwei Tang and Hui Xu
Forests 2025, 16(2), 359; https://doi.org/10.3390/f16020359 - 17 Feb 2025
Viewed by 106
Abstract
Quantifying the dynamic changes and relationships between ecosystem services (ESs) and land use change is critical for sustainable ecosystem management and land use optimization. However, comprehensive discussions on the spatiotemporal variations of ESs and their relationships with land use intensity (LUI) are lacking, [...] Read more.
Quantifying the dynamic changes and relationships between ecosystem services (ESs) and land use change is critical for sustainable ecosystem management and land use optimization. However, comprehensive discussions on the spatiotemporal variations of ESs and their relationships with land use intensity (LUI) are lacking, particularly in the context of significant climate warming. Systematic analyses of the forestry management unit scale are limited, leading to considerable uncertainty in sustainable ecosystem management, especially in alpine ecosystems of the Northern Hemisphere, where ESs have significantly degraded. The study focuses on the Daxing’anling forest area, Inner Mongolia (DFIAM), a representative sensitive alpine ecosystem and crucial ecological security barrier in Northern China. Utilizing the InVEST model, we analyzed the spatiotemporal variations in land use and four essential ESs, water yield (WY), carbon storage (CS), soil conservation (SC), and habitat quality (HQ), from 2013 to 2018. We also assessed the dynamic relationships between LUI and these ESs using a four-quadrant model. Our findings indicate the following: (1) Land use types in DFIAM remained relatively stable between 2013 and 2018, with forest being the dominant type (approximately 93%). During this period, areas of forest, cropland, impervious surfaces, and bare land increased, while areas of grassland, water, and wetland decreased. Although the overall change of LUI was gentle, a spatial pattern of “high in the southeast and low in the northwest” emerged, with low LUI areas showing slight expansion. (2) WY, SC, and HQ decreased, while CS increased from 2013 to 2018. The spatial distributions of these ESs showed higher values in the center and lower values at the edges, with forests demonstrating a strong capacity to provide multiple ESs. (3) The relationship between LUI and the four ESs from 2013 to 2018 was predominantly negative, primarily situated in Quadrant II, indicating that increased LUI inhibited ES supply capacity. Within Quadrant II, the distribution range of LUI, WY, and HQ decreased, while CS remained stable and SC increased. Furthermore, Quadrant III (positive correlation) accounted for a large proportion (19.23%~42.31%), highlighting the important role of non-anthropogenic factors in ES changes. Overall, most ESs in the DFAIM showed a decline while LUI remained relatively stable, with predominantly negative correlations between LUI and ESs. The increased LUI driven by human activities, and other non-human factors, may have contributed significantly to ES degradation. To improve ESs, we proposed implementing differentiated land use planning and management, systematic ecological protection and restoration strategies, a multi-level ecological early-warning monitoring and evaluation network, ecological corridors and buffer zones, and a collaborative management system with multiple participation. These results provide scientific guidance for the sustainable management of alpine ecosystems, enhancement of ESs, and formulation of land resource protection policies. Full article
(This article belongs to the Section Forest Ecology and Management)
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<p>Map of the study area.</p>
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<p>Spatial distribution of DFAIM land use in 2013 (<b>a</b>) and 2018 (<b>b</b>), and land use transfer change (<b>c</b>) from 2013 to 2018.</p>
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<p>LUI and changes in DFAIM from 2013 to 2018.</p>
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<p>Supply capacity of individual ESs for different land use types in DFAIM from 2013 to 2018. WY, CS, SC, and HQ are short for water yield, carbon storage, soil conservation, and habitat quality, respectively. Same below.</p>
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<p>ESCI of different land use types in DFAIM. ESCI stands for ecosystem service change index.</p>
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<p>Spatial distribution of ESs in DFAIM for the years 2013 (<b>a</b>,<b>d</b>,<b>g</b>,<b>j</b>) and 2018 (<b>b</b>,<b>e</b>,<b>h</b>,<b>k</b>) and the difference between the two years (<b>c</b>,<b>f</b>,<b>i</b>,<b>l</b>).</p>
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<p>The supply capacity levels of various ESs of DFAIM in 2013 and 2018.</p>
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<p>Relationship between LUI and individual ESs in 2013 and 2018. I represents Quadrant I; II represents Quadrant II; III represents Quadrant III; and IV represents Quadrant IV.</p>
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20 pages, 3955 KiB  
Article
Deep Learning Extraction of Tidal Creeks in the Yellow River Delta Using GF-2 Imagery
by Bojie Chen, Qianran Zhang, Na Yang, Xiukun Wang, Xiaobo Zhang, Yilan Chen and Shengli Wang
Remote Sens. 2025, 17(4), 676; https://doi.org/10.3390/rs17040676 - 16 Feb 2025
Viewed by 276
Abstract
Tidal creeks are vital geomorphological features of tidal flats, and their spatial and temporal variations contribute significantly to the preservation of ecological diversity and the spatial evolution of coastal wetlands. Traditional methods, such as manual annotation and machine learning, remain common for tidal [...] Read more.
Tidal creeks are vital geomorphological features of tidal flats, and their spatial and temporal variations contribute significantly to the preservation of ecological diversity and the spatial evolution of coastal wetlands. Traditional methods, such as manual annotation and machine learning, remain common for tidal creek extraction, but they are slow and inefficient. With increasing data volumes, accurately analyzing tidal creeks over large spatial and temporal scales has become a significant challenge. This study proposes a residual U-Net model that utilizes full-dimensional dynamic convolution to segment tidal creeks in the Yellow River Delta, employing Gaofen-2 satellite images with a resolution of 4 m. The model replaces the traditional convolutions in the residual blocks of the encoder with Omni-dimensional Dynamic Convolution (ODConv), mitigating the loss of fine details and improving segmentation for small targets. Adding coordinate attention (CA) to the Atrous Spatial Pyramid Pooling (ASPP) module improves target classification and localization in remote sensing images. Including dice coefficients in the focal loss function improves the model’s gradient and tackles class imbalance within the dataset. Furthermore, the inclusion of dice coefficients in the focal loss function improves the gradient of the model and tackles the dataset’s class inequality. The study results indicate that the model attains an F1 score and kappa coefficient exceeding 80% for both mud and salt marsh regions. Comparisons with several semantic segmentation models on the mud marsh tidal creek dataset show that ODU-Net significantly enhances tidal creek segmentation, resolves class imbalance issues, and delivers superior extraction accuracy and stability. Full article
(This article belongs to the Special Issue Remote Sensing of Coastal, Wetland, and Intertidal Zones)
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<p>Location of the study area: GF-2 images of the Yellow River Delta (RGB: 3, 2, 1 bands) (<b>a</b>), (<b>b</b>) mudflat creek area, and (<b>c</b>) salt marsh creek area.</p>
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<p>The ODU-Net model structure.</p>
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<p>CA-ASPP module structure.</p>
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<p>Coordinate attention module structure.</p>
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<p>Comparison of results of ablation experiments on the mudflat creek test set.</p>
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<p>Comparison of results of ablation experiments on the salt marsh creek test set.</p>
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<p>(<b>a</b>) Larger spatial mudflat area; (<b>b</b>) prediction results for mudflat creeks; (<b>c</b>) larger spatial mudflat area; (<b>d</b>) prediction results for salt marsh creeks.</p>
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<p>Comparison of the edge detection results (1–3 for mudflat regions, 4–6 for salt marsh regions).</p>
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<p>Semantic segmentation results of different models on the mudflat creek test set.</p>
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<p>Semantic segmentation results of different models on the salt marsh creek test set.</p>
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24 pages, 7997 KiB  
Article
A Spatial–Temporal Adaptive Graph Convolutional Network with Multi-Sensor Signals for Tool Wear Prediction
by Yu Xia, Guangji Zheng, Ye Li and Hui Liu
Appl. Sci. 2025, 15(4), 2058; https://doi.org/10.3390/app15042058 - 16 Feb 2025
Viewed by 226
Abstract
Tool wear monitoring is crucial for optimizing cutting performance, reducing costs, and improving production efficiency. Existing tool wear prediction models usually design integrated models based on a convolutional neural network (CNN) and recurrent neural network (RNN) to extract spatial and temporal features separately. [...] Read more.
Tool wear monitoring is crucial for optimizing cutting performance, reducing costs, and improving production efficiency. Existing tool wear prediction models usually design integrated models based on a convolutional neural network (CNN) and recurrent neural network (RNN) to extract spatial and temporal features separately. However, the topological structures between multi-sensor networks are ignored, and the ability to extract spatial features is limited. To overcome these limitations, a novel spatial–temporal adaptive graph convolutional network (STAGCN) is proposed to capture spatial–temporal dependencies with multi-sensor signals. First, a simple linear model is used to capture temporal patterns in individual time-series data. Second, a spatial–temporal layer composed of a bidirectional Mamba and an adaptive graph convolution is established to extract degradation features and reflect the dynamic degradation trend using an adaptive graph. Third, multi-scale triple linear attention (MTLA) is used to fuse the extracted multi-scale features across spatial, temporal, and channel dimensions, which can assign different weights adaptively to retain important information and weaken the influence of redundant features. Finally, the fused features are fed into a linear regression layer to estimate the tool wear. Experimental results conducted on the PHM2010 dataset demonstrate the effectiveness of the proposed STAGCN model, achieving a mean absolute error (MAE) of 3.40 μm and a root mean square error (RMSE) of 4.32 μm in the average results across three datasets. Full article
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<p>The overall framework of the STAGCN. FC layer: fully connected layer; AGCN: adaptive graph convolutional network; MTLA: multi-scale triple linear attention.</p>
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<p>The architecture of (<b>a</b>) the proposed bidirectional Mamba module and (<b>b</b>) the Mamba block.</p>
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<p>The architecture of (<b>a</b>) the MTLA module and (<b>b</b>) the linear attention mechanism.</p>
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<p>The process of the tool wear prediction framework based on the STAGCN.</p>
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<p>The experiment equipment and configuration.</p>
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<p>The tool wear value of three datasets: (<b>a</b>) C1; (<b>b</b>) C4; and (<b>c</b>) C6.</p>
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<p>The effect of signal denoising: (<b>a</b>) original signal; (<b>b</b>) the spectral analysis of (<b>a</b>); (<b>c</b>) denoised signal; (<b>d</b>) the spectral analysis of (<b>c</b>).</p>
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<p>The schematic diagram of data processing: (<b>a</b>) steady-state cutting segmentation; (<b>b</b>) time-domain feature extraction after signal denoising.</p>
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<p>The data processing results of the cutting force signal in the <span class="html-italic">x</span> direction of the C1 dataset: (<b>a</b>) variance; (<b>b</b>) maximum; and (<b>c</b>) minimum.</p>
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<p>The tool wear prediction on the dataset: (<b>a</b>) C1; (<b>b</b>) C4; and (<b>c</b>) C6.</p>
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<p>The results of the ablation experiment: (<b>a</b>) MAE; (<b>b</b>)RMSE.</p>
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<p>Impact of the number of subsequences on metrics: (<b>a</b>) MAE; (<b>b</b>) RMSE.</p>
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<p>Impact of node embedding dimension on metrics: (<b>a</b>) MAE; (<b>b</b>) RMSE.</p>
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<p>Impacts of value and channel embedding dimensions on metrics: (<b>a</b>) and (<b>b</b>) are the MAE and RMSE of the value embedding dimension, respectively; (<b>c</b>) and (<b>d</b>) are the MAE and RMSE of the channel embedding dimension, respectively.</p>
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<p>Impact of state expansion factor on metrics: (<b>a</b>) MAE; (<b>b</b>) RMSE.</p>
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<p>Impact of the number of spatial–temporal layers on metrics: (<b>a</b>) MAE; (<b>b</b>) RMSE.</p>
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<p>Impact of different optimizers on metrics: (<b>a</b>) MAE; (<b>b</b>) RMSE.</p>
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3122 KiB  
Proceeding Paper
A Computational Multiphysics Study of a Satellite Thruster
by Marcello A. Lepore, Marzio Piller, Mario Guagliano and Angelo R. Maligno
Eng. Proc. 2025, 85(1), 14; https://doi.org/10.3390/engproc2025085014 - 14 Feb 2025
Abstract
This work concerns a study of the thermomechanical behaviour of a commercial thruster for aerospace use. The thruster, operated using a bipropellant liquid mixture, is used for the motion and in-orbit altitude control of small telecommunications satellites. The mixture used in the combustion [...] Read more.
This work concerns a study of the thermomechanical behaviour of a commercial thruster for aerospace use. The thruster, operated using a bipropellant liquid mixture, is used for the motion and in-orbit altitude control of small telecommunications satellites. The mixture used in the combustion process is composed of propylene and nitrous oxide, while the wall of the thruster is made of PH15-5 stainless steel. A computational fluid dynamics analysis of conjugate heat transfer determines the spatial–temporal distribution of temperature within the thruster wall. This information is passed to a finite element mechanical model that simulates the stress and the equivalent plastic strain distribution within the thruster wall. Full article
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<p>Three-dimensional geometry model of B20 thruster with main components highlighted.</p>
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<p>Geometry and dimensions (m) of B20 thruster.</p>
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<p>The boundary and load conditions applied in the mechanical model of the thruster.</p>
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<p>Operating cycle.</p>
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<p>Each dot (green) represents a heat flow value over time, calculated in the nozzle throat. The interpolation curve (red) highlights a decay law of the heat flux.</p>
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<p>Temperature distribution at the start of combustion (50 ms).</p>
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<p>Temperature distribution at the beginning of combustion (2 s).</p>
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<p>Temperature distribution at the end of combustion (10 s).</p>
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<p>A comparison of temperature profiles over time on the inner surface of the thruster and along the <span class="html-italic">X</span>-axis.</p>
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<p>An image highlighting the most damaged region in the nozzle throat of the thruster at 2 s.</p>
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21 pages, 9146 KiB  
Article
Land Use and Carbon Storage Evolution Under Multiple Scenarios: A Spatiotemporal Analysis of Beijing Using the PLUS-InVEST Model
by Jiaqi Kang, Linlin Zhang, Qingyan Meng, Hantian Wu, Junyan Hou, Jing Pan and Jiahao Wu
Sustainability 2025, 17(4), 1589; https://doi.org/10.3390/su17041589 - 14 Feb 2025
Viewed by 348
Abstract
The carbon stock in terrestrial ecosystems is closely linked to changes in land use. Understanding how land use alterations affect regional carbon stocks is essential for maintaining the carbon balance of ecosystems. This research leverages land use and driving factor data spanning from [...] Read more.
The carbon stock in terrestrial ecosystems is closely linked to changes in land use. Understanding how land use alterations affect regional carbon stocks is essential for maintaining the carbon balance of ecosystems. This research leverages land use and driving factor data spanning from 2000 to 2020, utilizing the Patch-generating Land Use Simulation (PLUS) model alongside the InVEST ecosystem services model to examine the temporal and spatial changes in carbon storage across Beijing. Additionally, four future scenes for 2030—urban development, natural development, cropland protection, as well as eco-protection—are explored, with the PLUS and InVEST models employed to emulate dynamic land use changes and the corresponding carbon stock variations. The results show that the following: (1) Between 2000 and 2020, changes in land use resulted in a significant decline in carbon storage, with a total reduction of 1.04 × 107 tons. (2) From 2000 to 2020, agricultural, forest, and grassland areas in Beijing all declined to varying extents, while built-up land expanded by 1292.04 km2 (7.88%), with minimal changes observed in water bodies or barren lands. (3) Compared to the carbon storage distribution in 2020, carbon storage in the 2030 urban development scenario decreased by 6.99 × 106 tons, highlighting the impact of rapid urbanization and the expansion of built-up areas on the decline in carbon storage. (4) In the ecological protection scenario, the optimization of land use structure resulted in an increase of 6.01 × 105 tons in carbon storage, indicating that the land use allocation in this scenario contributes to the restoration of carbon storage and enhances the carbon sink capacity of the urban ecosystem. This study provides valuable insights for policymakers in optimizing ecosystem carbon storage from a land use perspective and offers essential guidance for the achievement of the “dual carbon” strategic objectives. Full article
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<p>Spatial location and topography of the study area.</p>
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<p>Major factors driving land use change in Beijing: (<b>a</b>) population; (<b>b</b>) distance to trunk; (<b>c</b>) distance to tertiary; (<b>d</b>) distance to water; (<b>e</b>) distance to secondary roads; (<b>f</b>) distance to railway; (<b>g</b>) distance to primary; (<b>h</b>) distance to government; (<b>i</b>) distance to motorway; (<b>j</b>) slope; (<b>k</b>) temperature; (<b>l</b>) DEM; (<b>m</b>) GDP; (<b>n</b>) precipitation; and (<b>o</b>) soil type.</p>
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<p>Diagram of the correlation analysis process.</p>
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<p>Land use transition matrices from 2000 to 2020 for each period.</p>
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<p>Land use type distribution in 2030 under four scenarios.</p>
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<p>2030 land use fluctuation patterns across four scenarios.</p>
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<p>Contribution of factors affecting land use.</p>
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<p>Spatial pattern of carbon storage in Beijing.</p>
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<p>Predicted carbon storage patterns in 2030 across four scenarios.</p>
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22 pages, 6176 KiB  
Article
The Distribution of Microplastic Pollution and Ecological Risk Assessment of Jingpo Lake—The World’s Second Largest High-Mountain Barrier Lake
by Haitao Wang, Chen Zhao and Tangbin Huo
Biology 2025, 14(2), 201; https://doi.org/10.3390/biology14020201 - 14 Feb 2025
Viewed by 334
Abstract
To investigate the influence of factors such as tourism, agriculture, and population density on the presence of microplastic (MP) content in aquatic environments and their associated ecological risks, Jingpo Lake, a remote high-mountain lake situated away from urban areas, was selected as the [...] Read more.
To investigate the influence of factors such as tourism, agriculture, and population density on the presence of microplastic (MP) content in aquatic environments and their associated ecological risks, Jingpo Lake, a remote high-mountain lake situated away from urban areas, was selected as the research subject. This study examined the abundance, types, sizes, colors, and polymer compositions of MPs within the water body, fish, and sediments. By considering variables, including fishing practices, agricultural activities, population dynamics, and vegetation cover, an analysis was conducted to unravel the spatial and temporal distribution of MPs concerning human activities, ultimately leading to an assessment of the ecological risks posed by MP pollution. The findings revealed that the average abundance of MPs in the lake’s surface water was recorded as (304.8 ± 170.5) n/m3, while in the sediments, it averaged (162.0 ± 57.45) n/kg. Inside the digestive tracts of fish, the MP abundance was measured at 11.4 ± 5.4 n/ind. The contamination of MPs within the aquatic environment of Jingpo Lake was found to be relatively minimal. Variations in MP loads across time and space were observed, with MPs predominantly falling within the size range of small planktonic organisms (50–1000 μm). Additionally, the prevalent colors of MPs in the water samples were white or transparent, constituting approximately 55.65% of the entire MP composition. Subsequently, they were black, red, and blue. This colors distribution were consistent across MPs extracted from fish and sediment samples. The chemical compositions of the MPs predominantly comprised PE (31.83%) and PS (25.48%), followed by PP (17.56%), PA (11.84%), PET (6.71%), EVA (4.56%), and PC (2.03%). Regarding the seasonal aspect, MP concentrations were highest during summer (46.68%), followed by spring (36.75%) and autumn (16.56%). The spatial distribution of MPs within Jingpo Lake’s water body, fish, and sediments was notably influenced by human activities, as confirmed by Pearson correlation coefficients. A strong association was observed between MP levels and water quality indicators such as ammonium nitrogen (NH4-N), total phosphorus (TP), and chlorophyll-a (Chla), suggesting that human-related pollution contributed significantly to MP contamination. The diversity assessment of MP pollutants exhibited the highest variability in chemical composition (1.23 to 1.79) using the Shannon–Wiener Index. Subsequently, the diversity of colors ranged from 0.59 to 1.54, shape diversity from 0.78 to 1.30, seasonal diversity from 0.83 to 1.10, and size diversity from 0.44 to 1.01. The assessment results of ecological risk highlighted that the risk categories for MPs within the surface water, fish, and sediments of Jingpo Lake were categorized as I for the PHI and PLI and as “Minor” for the PERI. These relatively low-risk values were attributed to the predominantly low toxicity of the distributed MPs within the Jingpo Lake basin. Moreover, the results of the risk assessment were found to be interconnected with the distribution of the local population and agricultural activities around the sampling sections. Usage patterns of coastal land and population density were recognized as influential factors affecting MP loads within the water body, sediments, fish, and other components of the lake ecosystem. Full article
(This article belongs to the Special Issue Global Fisheries Resources, Fisheries, and Carbon-Sink Fisheries)
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<p>Sampling sections in the Jingpo Lake reservoir. S1–S4 locations are close to settlements including densely populated areas, tourist ports, hotels, and related reception infrastructure, while S2, S3, S10, S11, and S12 are closer to farmland, and other sampling sections are areas with less human activity.</p>
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<p>Profile images of typical MPs and occurrence characteristics of MPs in different sampling sections. (<b>A</b>): Fragment(PS); (<b>B</b>): Film(PVC); (<b>C</b>): Fiber(PVC); (<b>D</b>): Microsphere(PS). The outline of microplastic properties is surrounded by yellow lines.</p>
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<p>MP types and temporal–spatial distribution in Jingpo Lake. S1W–S12W: MPs in water; S1S–S12S: MPs in sediments; S1F–S12F: MPs in fish digestive tracts.</p>
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<p>Factors affecting MPs in Jingpo Lake. (<b>a</b>): Correlation between MP content and other environmental physicochemical factors, MPs W−MP content in water, MPs S−MP content in sediments, MPs F−MP content in fish digestive tracts; (<b>b</b>): relationship between MP content and population density; (<b>c</b>): relationship between MP content and land use; (<b>d</b>): relationship between MP content and vegetation type.</p>
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<p>Diversity of MP pollution in Jingpo Lake. S1W–S12W: MPs in water; S1S–S12S: MPs in sediments; S1F–S12F: MPs in fish digestive tracts.</p>
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<p>Risk assessment of MPs in Jingpo Lake. S1W–S12W—MPs in water; S1S–S12S—MPs in sediment; S1F–S12F—MPs in fish digestive tracts.</p>
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34 pages, 1568 KiB  
Review
Biophysical Modeling of Cardiac Cells: From Ion Channels to Tissue
by Sergio Alonso, Enrique Alvarez-Lacalle, Jean Bragard and Blas Echebarria
Biophysica 2025, 5(1), 5; https://doi.org/10.3390/biophysica5010005 - 14 Feb 2025
Viewed by 197
Abstract
Cardiovascular diseases have become the leading cause of death in developed countries. Among these, some are related to disruptions in the electrical synchronization of cardiac tissue leading to arrhythmias such as atrial flutter, ventricular tachycardia, or ventricular fibrillation. Their origin is diverse and [...] Read more.
Cardiovascular diseases have become the leading cause of death in developed countries. Among these, some are related to disruptions in the electrical synchronization of cardiac tissue leading to arrhythmias such as atrial flutter, ventricular tachycardia, or ventricular fibrillation. Their origin is diverse and involves several spatial and temporal scales, ranging from nanoscale ion channel dysfunctions to tissue-level fibrosis and ischemia. Mathematical models play a crucial role in elucidating the mechanisms underlying cardiac arrhythmias by simulating the electrical and physiological properties of cardiac tissue across different spatial scales. These models investigate the effects of genetic mutations, pathological conditions, and anti-arrhythmic interventions on heart dynamics. Despite their varying levels of complexity, they have proven to be important in understanding the triggers of arrhythmia, optimizing defibrillation protocols, and exploring the nonlinear dynamics of cardiac electrophysiology. In this work, we present diverse modeling approaches to the electrophysiology of cardiac cells and share examples from our own research where these approaches have significantly contributed to understanding cardiac arrhythmias. Although computational modeling of the electrical properties of cardiac tissue faces challenges in integrating data across multiple spatial and temporal scales, it remains an indispensable tool for advancing knowledge in cardiac biophysics and improving therapeutic strategies. Full article
(This article belongs to the Special Issue State-of-the-Art Biophysics in Spain 2.0)
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<p>Equivalent electric circuit model for the cellular membrane. The difference in the transmembrane potential between the extracellular and the intracellular spaces is determined by the ion current through the ion channels, the Nernst potential associated with each ion, and the capacitance of the membrane.</p>
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<p>Sketch of a typical action potential in a ventricular myocyte. Phases and ion currents responsible for the action potential: sharp increase due to sodium influx (0), rapid decrease due to potassium outflux (1), balance currents and plateau phase (2), end of calcium influx (3) and return to the resting potential (4) where the pumps and the exchangers keep the resting potential fix.</p>
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<p>Sketch of the different spatial scales discussed along this work. (<b>A</b>) Ion channels dynamics, (<b>B</b>) intracellular organization, (<b>C</b>) whole cell models for the action potential and the average ion channel dynamics, (<b>D</b>) properties of the gap junction connecting neighboring cardiac cells, and (<b>E</b>) cell organization along the cardiac tissue.</p>
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<p>Different types of Markov models of ion channels. (<b>A</b>) Two-state ion channel. (<b>B</b>) Markov model of the Na<sup>+</sup> channel with different conformations, from [<a href="#B51-biophysica-05-00005" class="html-bibr">51</a>]. (<b>C</b>) Markov model of the L-type calcium channel (LCC) with different configurations and with the pathways of calcium-dependent inhibition (CDI) in red and voltage-dependent inhibition (VDI) in black from [<a href="#B53-biophysica-05-00005" class="html-bibr">53</a>].</p>
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<p>(<b>A</b>) Schematics of the micron subdivision of the cell in calcium release units (CaRUs). Each CaRU is associated with a RyR2 cluster. (<b>B</b>) Schematics of the different fluxes and concentrations taken into consideration in each CaRU; dyadic, subsarcolemma, cytosolic, network SR, and junctional SR. (<b>C</b>) The distribution of these CaRU in the tubulated structure of ventricles is drawn on the lower right. In a non-tubulated atrial cell, CaRU in the interior of the cell might not have LCC nor NCX available.</p>
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<p>Schematics of a whole-cell model where all ionic concentrations are taken as averages, but calcium has five different compartments in the cell. Sodium and potassium concentration and fluxes from different ionic channels are represented. The calcium ionic concentration is different in the cytosol, in the nSR, in the junction SR and close to the membrane or close to the volume between RyR2 and LCC. In these models, however, there is no spatial information in the ionic concentration other than for calcium, which has a different average concentration in each compartment. Inside the NSR (network SR), for example, the calcium concentration is taken as the average in all the SR.</p>
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<p>Schematic view of the structure and functionality of a gap junction (GJ) connecting electrically two cardiac myocytes. The thickness of the bi-lipidic layer is of the order of a few nanometers. The ions can flow in both directions through the GJ.</p>
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<p>Steady-state values of the normalized gap junction <math display="inline"><semantics> <msub> <mi>g</mi> <mrow> <mi>i</mi> <mo>,</mo> <mi>s</mi> <mi>s</mi> </mrow> </msub> </semantics></math> as a function of the transjunctional voltage <math display="inline"><semantics> <msub> <mi>V</mi> <mi>i</mi> </msub> </semantics></math> for the different connexin types (homotypic and heterotypic). The horizontal line (green) represents the case where the conductance is assumed to be constant.</p>
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<p>Space–time plot showing the conductance <span class="html-italic">g</span> of the symmetrical GJ <math display="inline"><semantics> <mrow> <mrow> <mi>Cx</mi> <mn>43</mn> </mrow> <mo>_</mo> <mn>43</mn> </mrow> </semantics></math> taken at stroboscopic time intervals (<math display="inline"><semantics> <mrow> <mi>T</mi> <mo>=</mo> <mn>480</mn> </mrow> </semantics></math> ms). The initial condition is uniformly set to <math display="inline"><semantics> <mrow> <msub> <mi>g</mi> <mrow> <mi>i</mi> <mi>n</mi> <mi>i</mi> </mrow> </msub> <mo>=</mo> <mn>0.4</mn> </mrow> </semantics></math> for all the GJ. The color code represents the local values of the conductance (a.u.) ranging from 0.1 to 0.4. The shrinking factor is set to <math display="inline"><semantics> <mrow> <mi>F</mi> <mi>S</mi> <mo>=</mo> <mn>2</mn> </mrow> </semantics></math>.</p>
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<p>Modeling approaches to cardiac tissue: (<b>A</b>) heterogeneous model where discretization is smaller than single cells and discrete gap junctions are considered for cell-to-cell coupling. (<b>B</b>) Discrete model where the cardiac cell is approximated as a single element which is electrically connected to the rest of the cells in the tissue. (<b>C</b>) Monodomain model where the transmembrane voltage is considered in a continuous model; therefore, the the numerical discretization of space is typically larger than the cell size. (<b>D</b>) Bidomain model where intracellular (blue) and extracellular (yellow) potentials are explicitly considered as two interconnected continuous models.</p>
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<p>Two-dimensional snapshots at six different times, corresponding to simulations of the action potential propagation through the tissue and entering in a region with small (<b>A</b>) close to percolation (<b>B</b>) and large (<b>C</b>) fraction of heterogeneities.</p>
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<p>Two-dimensional snapshots at six different times, corresponding to simulations of the regular action potential propagation through the tissue (<b>A</b>), a spiral wave corresponding to a periodic rapid re-entrant wave related with tachycardia (<b>B</b>), and spiral breakup corresponding to irregular dynamics related to fibrillation (<b>C</b>).</p>
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17 pages, 4266 KiB  
Article
Hyperspectral Image Change Detection Method Based on the Balanced Metric
by Xintao Liang, Xinling Li, Qingyan Wang, Jiadong Qian and Yujing Wang
Sensors 2025, 25(4), 1158; https://doi.org/10.3390/s25041158 - 13 Feb 2025
Viewed by 307
Abstract
Change detection, as a popular research direction for dynamic monitoring of land cover change, usually uses hyperspectral remote-sensing images as data sources. Hyperspectral images have rich spatial–spectral information, but traditional change detection methods have limited ability to express the features of hyperspectral images, [...] Read more.
Change detection, as a popular research direction for dynamic monitoring of land cover change, usually uses hyperspectral remote-sensing images as data sources. Hyperspectral images have rich spatial–spectral information, but traditional change detection methods have limited ability to express the features of hyperspectral images, and it is difficult to identify the complex detailed features, semantic features, and spatial–temporal correlation features in two-phase hyperspectral images. Effectively using the abundant spatial and spectral information in hyperspectral images to complete change detection is a challenging task. This paper proposes a hyperspectral image change detection method based on the balanced metric, which uses the spatiotemporal attention module to translate bi-temporal hyperspectral images to the same eigenspace, uses the deep Siamese network structure to extract deep semantic features and shallow spatial features, and measures sample features according to the Euclidean distance. In the training phase, the model is optimized by minimizing the loss of distance maps and label maps. In the testing phase, the prediction map is generated by simple thresholding of distance maps. Experiments show that on the four datasets, the proposed method can achieve a good change detection effect. Full article
(This article belongs to the Section Sensing and Imaging)
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<p>Flow block diagram.</p>
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<p>Attention module of the change detection model.</p>
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<p>Feature extractor of the change detection model.</p>
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<p>The datasets used in this paper: (<b>a</b>) Farm dataset; (<b>b</b>) River dataset; (<b>c</b>) Babara dataset; (<b>d</b>) Bayarea dataset.</p>
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<p>Comparison of change detection effects on Farm dataset, the red box highlights the differences in the detection results. (<b>a</b>) Change detection result of CNN model; (<b>b</b>) change detection result of Siam-Resnet model; (<b>c</b>) change detection result of CSA-net model; (<b>d</b>) change detection result of the method in this paper; (<b>e</b>) ground-truth map.</p>
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<p>Feature visualization comparison diagram of the three methods. (<b>a</b>) t-SNE feature extracted by CNN method; (<b>b</b>) t-SNE feature extracted by Siam-Resnet method; (<b>c</b>) t-SNE feature extracted by the method in this paper.</p>
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<p>Measurement feature comparison diagram of the two methods. (<b>a</b>) Measurement feature of Siam-Resnet method; (<b>b</b>) measurement feature of the method in this paper; (<b>c</b>) measurement feature of the label map.</p>
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<p>Change detection results on different datasets. (<b>a</b>) CNN result on River dataset; (<b>b</b>) Siam-Resnet result on River dataset; (<b>c</b>) this paper’s method’s result on River dataset; (<b>d</b>) ground truth of River dataset; (<b>e</b>) CNN result on Bayarea dataset; (<b>f</b>) Siam-Resnet result on Bayarea dataset; (<b>g</b>) this paper’s method’s result on Bayarea dataset; (<b>h</b>) ground truth of Bayarea dataset; (<b>i</b>) CNN result on Babara dataset; (<b>j</b>) Siam-Resnet result on Babara dataset; (<b>k</b>) this paper’s method’s result on Babara dataset; (<b>l</b>) ground truth of Babara dataset.</p>
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<p>Change detection performance comparison on three datasets.</p>
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29 pages, 26219 KiB  
Article
Construction of a Desertification Composite Index and Its Application in the Spatiotemporal Analysis of Land Desertification in the Ring-Tarim Basin over 30 Years
by Lei Xi, Zhao Qi, Yiming Feng, Xiaoming Cao, Mengcun Cui, Jiaxiu Zou and Shiang Feng
Remote Sens. 2025, 17(4), 644; https://doi.org/10.3390/rs17040644 - 13 Feb 2025
Viewed by 272
Abstract
Desertification is one of the most severe environmental issues facing the world today, and effective desertification monitoring is critical for understanding its dynamics and developing prevention and control strategies. Although numerous studies on desertification monitoring using remote sensing have been conducted, there remain [...] Read more.
Desertification is one of the most severe environmental issues facing the world today, and effective desertification monitoring is critical for understanding its dynamics and developing prevention and control strategies. Although numerous studies on desertification monitoring using remote sensing have been conducted, there remain differences in indicator selection, and a unified monitoring system has yet to be established. In this study, we constructed the Desertification Composite Index (DCI) using Landsat satellite images, integrating six remote sensing indicators reflecting the natural and ecological characteristics of desertified areas. We also incorporated 383 UAV imagery datasets to accurately identify and analyze the spatial and temporal distributions of desertification in the Ring-Tarim Basin from 1990 to 2020 and subsequently assess its spatiotemporal trends. The results show the following: (1) The constructed DCI was used to identify desertification in 2020, achieving an overall accuracy of 0.86 and a Kappa coefficient of 0.8, indicating that the DCI is suitable for extracting regional desertification information. (2) From 1990 to 2020, the area of desertification decreased significantly, with an average annual reduction rate of −0.0022 ha/a, indicating continuous ecological improvement. Despite localized deterioration, the overall trend was one of “general improvement and local containment.” (3) GeoDetector-based analysis showed that cultivated land area and land use type were the primary single-factor drivers of desertification. The interaction between cultivated land and vegetation type exhibited a synergistic effect as a two-factor driver. (4) Desertification in the Ring-Tarim Basin is primarily influenced by human activities. Appropriate management and intervention measures, efficient and intensive cropland management, and rational land use planning can help develop effective strategies to combat desertification. Full article
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<p>Location of the study area.</p>
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<p>UAV sample plot location diagram.</p>
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<p>Research framework.</p>
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<p>The inversion result diagram of index based on GEE in 2020: (<b>a</b>) FVC. (<b>b</b>) TVDI. (<b>c</b>) Albedo. (<b>d</b>) LST. (<b>e</b>) TGSI. (<b>f</b>) MSAVI.</p>
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<p>Monitoring schematic diagram of desertification degree in the Ring-Tarim Basin in 2020.</p>
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<p>Heat map of confusion matrices for identification of different levels of accuracy of non-desertification and desertification (where 1 indicates non-desertified land, while 2 to 5 represent land with varying degrees of desertification, corresponding to slight, moderate, severe, and extremely severe desertification, respectively).</p>
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<p>Ring-Tarim Basin spatiotemporal dynamics of desertification area and mutation point test: (<b>a</b>) Desertification area share. (<b>b</b>) MK mutation point detection.</p>
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<p>Characteristics of the spatial distribution of desertification levels in the Ring-Tarim Basin.</p>
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<p>Ring-Tarim Basin area share by year for different levels of desertification.</p>
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<p>Characterization of the distribution of transformations between degrees of desertification for the Ring-Tarim Basin (where 1990_1 represents the area of non-desertified land in 1990; 1990_5 represents the area of desertified land in extremely severe in 1990). (<b>a</b>) From 1990 to 1995. (<b>b</b>) From 1995 to 2000. (<b>c</b>) From 2000 to 2005. (<b>d</b>) From 2005 to 2010. (<b>e</b>) From 2010 to 2015. (<b>f</b>) From 2015 to 2020.</p>
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<p>Percentage of different degrees of desertification before and after the Ring-Tarim Basin mutation year ([<a href="#B48-remotesensing-17-00644" class="html-bibr">48</a>,<a href="#B49-remotesensing-17-00644" class="html-bibr">49</a>] and our study): (<b>a</b>) 2000. (<b>b</b>) 2005.</p>
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<p>Ring-Tarim Basin desertification driver explanatory power statistics: (<b>a</b>) Single-factor detection explanatory power. (<b>b</b>) Multi-factor interaction explanatory power.</p>
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<p>Trend map of center of gravity shift for desertified land in the Ring-Tarim Basin.</p>
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23 pages, 3329 KiB  
Article
Dynamic Evolution and Trend Forecasting of New Quality Productive Forces Development Levels in Chinese Urban Agglomerations
by Yufang Shi, Xin Wang and Tianlun Zhang
Sustainability 2025, 17(4), 1559; https://doi.org/10.3390/su17041559 - 13 Feb 2025
Viewed by 362
Abstract
New quality productive forces serve as a catalyst for high-quality development and act as a critical driver of Chinese-style modernization. This study evaluated the degree of new quality productive force in China’s five major urban agglomerations between 2013 and 2022 using the entropy [...] Read more.
New quality productive forces serve as a catalyst for high-quality development and act as a critical driver of Chinese-style modernization. This study evaluated the degree of new quality productive force in China’s five major urban agglomerations between 2013 and 2022 using the entropy approach. Additionally, it utilized kernel density estimation, the Dagum Gini coefficient, and Markov chain analysis to explore the spatial and temporal dynamics of these forces and their evolutionary trends. The findings revealed the following: (1) Overall, the new quality productive forces in China’s five major urban agglomerations have exhibited a steady upward trend, although the overall level remains relatively low. Among these regions, the Pearl River Delta ranks the highest, followed by the Yangtze River Delta, Beijing–Tianjin–Hebei, Chengdu–Chongqing, and the Urban Cluster in the Middle Reaches of the Yangtze River. Nevertheless, significant potential for improvement persists. (2) The traditional Markov probability transfer matrix suggests that the new quality productive forces in these urban agglomerations are relatively stable, with evidence of “club convergence”. Meanwhile, the spatial Markov transfer probability matrix indicates that transfer probabilities are influenced by neighborhood contexts. (3) Over time, the new quality productive forces in Chinese urban agglomerations show a tendency to concentrate at higher levels, reflecting gradual improvement. The developmental state and evolutionary patterns of new quality productive forces in Chinese urban agglomerations are thoroughly evaluated in this paper, along with advice for accelerating their growth to promote Chinese-style modernization. Full article
(This article belongs to the Special Issue Advances in Economic Development and Business Management)
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<p>The trend of new quality productive forces in the five major urban agglomerations.</p>
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<p>Spatial distribution of the new quality productive forces levels in the five major urban agglomerations.</p>
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<p>The trend of regional differences in the five major urban agglomerations.</p>
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<p>Sources of regional differences and their contribution rates in the five major urban agglomerations.</p>
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<p>Trends of regional differences among the five major urban agglomerations.</p>
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<p>Kernel density estimation of the overall and individual five major urban agglomerations. (<b>a</b>) Five urban agglomerations overall. (<b>b</b>) Beijing–Tianjin–Hebei. (<b>c</b>) Yangtze River Delta. (<b>d</b>) Pearl River Delta. (<b>e</b>) Middle reaches of the Yangtze River. (<b>f</b>) Chengdu–Chongqing.</p>
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29 pages, 12829 KiB  
Article
Evaluating the Relationship Between Vegetation Status and Soil Moisture in Semi-Arid Woodlands, Central Australia, Using Daily Thermal, Vegetation Index, and Reflectance Data
by Mauro Holzman, Ankur Srivastava, Raúl Rivas and Alfredo Huete
Remote Sens. 2025, 17(4), 635; https://doi.org/10.3390/rs17040635 - 13 Feb 2025
Viewed by 400
Abstract
Wet rainfall pulses control vegetation growth through evapotranspiration in most dryland areas. This topic has not been extensively analyzed with respect to the vast semi-arid ecosystems of Central Australia. In this study, we investigated vegetation water responses to in situ root zone soil [...] Read more.
Wet rainfall pulses control vegetation growth through evapotranspiration in most dryland areas. This topic has not been extensively analyzed with respect to the vast semi-arid ecosystems of Central Australia. In this study, we investigated vegetation water responses to in situ root zone soil moisture (SM) variations in savanna woodlands (Mulga) in Central Australia using satellite-based optical and thermal data. Specifically, we used the Land Surface Water Index (LSWI) derived from the Advanced Himawari Imager on board the Himawari 8 (AHI) satellite, alongside Land Surface Temperature (LST) from MODIS Terra and Aqua (MOD/MYD11A1), as indicators of vegetation water status and surface energy balance, respectively. The analysis covered the period from 2016 to 2021. The LSWI increased with the magnitude of wet pulses and showed significant lags in the temporal response to SM, with behavior similar to that of the Enhanced Vegetation Index (EVI). By contrast, LST temporal responses were quicker and correlated with daily in situ SM at different depths. These results were consistent with in situ relationships between LST and SM, with the decreases in LST being coherent with wet pulse magnitude. Daily LSWI and EVI scores were best related to subsurface SM through quadratic relationships that accounted for the lag in vegetation response. Tower flux measures of gross primary production (GPP) were also related to the magnitude of wet pulses, being more correlated with the LSWI and EVI than LST. The results indicated that the vegetation response varied with SM depths. We propose a conceptual model for the relationship between LST and SM in the soil profile, which is useful for the monitoring/forecasting of wet pulse impacts on vegetation. Understanding the temporal changes in rainfall-driven vegetation in the thermal/optical spectra associated with increases in SM can allow us to predict the spatial impact of wet pulses on vegetation dynamics in extensive drylands. Full article
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<p>Map of major vegetation groups showing the location of Alice Springs Mulga (ASM) and Ti Tree Ozflux sites (data source: Dynamic Land Cover Dataset Version 2.1).</p>
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<p>Workflow diagram of satellite data (AHI and MODIS) and field data. Both data sources were considered to obtain LST and spectral indices and analyze vegetation response to SM during rainfall wet pulses.</p>
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<p>Study periods, data from the ASM OzFlux station. (<b>a</b>) Daily SM at different depths and GPP; (<b>b</b>) rainfall; (<b>c</b>) in situ SM, EVI, and LSWI values from the AHI; (<b>d</b>) maximum GPP and LSWI values in function of magnitude of wet pulses expressed as m<sup>3</sup>/m<sup>3</sup>. Vertical lines show the 5 analyzed wet pulses during late spring and summer: 2016–2017 and 2020–2021, the wettest seasons, and 2018–2019, the driest season.</p>
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<p>Study periods, data from the ASM OzFlux station. (<b>a</b>) Daily SM at different depths and GPP; (<b>b</b>) rainfall; (<b>c</b>) in situ SM, EVI, and LSWI values from the AHI; (<b>d</b>) maximum GPP and LSWI values in function of magnitude of wet pulses expressed as m<sup>3</sup>/m<sup>3</sup>. Vertical lines show the 5 analyzed wet pulses during late spring and summer: 2016–2017 and 2020–2021, the wettest seasons, and 2018–2019, the driest season.</p>
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<p>Detailed temporal series of the EVI and LSW from the AHI and SM in ASM for each analyzed season: (<b>a</b>) 2017–2018 (normal), (<b>b</b>) 2018–2019 (moderately dry), (<b>c</b>) 2019–2020 (normal), (<b>d</b>) 2020–2021 (extremely wet). Lags between peaks in SM and spectral indices are included.</p>
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<p>MYD/MOD11A1, in situ daily LST and actual evapotranspiration during the study period in ASM. In situ LST was calculated from upwelling longwave radiances measured by the pyrgeometer CNR1.</p>
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<p>Detailed temporal series of MODIS LST, daily in situ LST and SM in ASM during the 5 analyzed seasons: (<b>a</b>) 2016–2017 (extremely wet), (<b>b</b>) 2017–2018 (normal), (<b>c</b>) 2018–2019 (moderately dry), (<b>d</b>) 2019–2020 (normal), and (<b>e</b>) 2020–2021 (extremely wet).</p>
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<p>Relationship between daily in situ SM at different depths, LSWI (<b>left</b>) and EVI (<b>right</b>) from AHI in ASM (<span class="html-italic">n</span> = 356).</p>
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<p>Relationship between average in situ LST and SM at different depths (the best correlation up to 4 days is included) in ASM (<span class="html-italic">n</span> = 475). Although correlation at 100 cm depth is included, most of the time LST fluctuates according to shallower SM.</p>
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<p>Relationship between daily in situ SM at different depths, MOD11A1 (<span class="html-italic">n</span> = 287) and MYD11A1 (n = 274).</p>
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<p>Relationship between daily in situ GPP (gC/m<sup>2</sup>), LSWI (<b>left</b>), and EVI (<b>right</b>) values from the AHI in ASM (n = 145). Note that 2018–2019 was not included, as there was no evident growing season.</p>
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<p>Relationship between daily in situ GPP (gC/m<sup>2</sup>), MOD LST (<b>left</b>), and MYD LST (<b>right</b>) in ASM (n = 232).</p>
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<p>Conceptual model of satellite-derived LST from MODIS (<b>left</b>) and daily in situ GPP (<b>right</b>) as a function of daily SM for the Mulga woodland area. For the GPP plot, the maximum GPP values and average of the maximum values of SM in the soil profile for each analyzed pulse were considered. GPP versus maximum LSWI from the AHI is included. Note that on the left plot, SM values correspond to ASM data (a similar pattern was observed in Ti Tree).</p>
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<p>Study periods: data from the Ti Tree OzFlux station. (<b>a</b>) Daily SM at different depths and GPP; (<b>b</b>) rainfall; (<b>c</b>) in situ SM, EVI, and LSWI values from the AHI; (<b>d</b>) maximum GPP and LSWI values in function of magnitude of wet pulses expressed as m<sup>3</sup>/m<sup>3</sup>. Vertical lines show the analyzed wet pulses during late spring and summer. SM at a 60 cm depth was considered under spinifex, given the lack of data under Mulga.</p>
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<p>MYD/MOD11A1, in situ daily LST and actual evapotranspiration during the study period in the Ti Tree station. In situ LST was calculated from upwelling longwave radiances measured by the pyrgeometer CNR1.</p>
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<p>Relationship between daily in situ SM at different depths: the LSWI (<b>left</b>) and EVI (<b>right</b>) from the AHI in the Ti Tree station (n = 236).</p>
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<p>Relationship between average in situ LST and SM at different depths (the best correlation up to 4 days is included) in the Ti Tree station (n = 377).</p>
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<p>Relationship between daily in situ SM at different depths: MOD11A1 (<b>left</b>, n = 251) and MYD11A1 (<b>right</b>, n = 239) in the Ti Tree station.</p>
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<p>Relationship between daily in situ GPP (gC/m<sup>2</sup>), LSWI (<b>left</b>), and EVI (<b>right</b>) values from the AHI in the Ti Tree station (n = 51). Note that 2018–2019 was not included, as there was no evident growing season.</p>
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<p>Relationship between daily in situ GPP (gC/m<sup>2</sup>), MOD LST (<b>left</b>, n = 177), and MYD LST (<b>right</b>, n = 169) in the Ti Tree station.</p>
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22 pages, 4714 KiB  
Article
Spatiotemporal Evolution and Driving Mechanisms of Ecological Risk in the Yuncheng Salt Lake Wetland, China
by Qicheng He, Zhihao Zhang, Yuan Zhang, Tianyue Sun, Weipeng Wang and Zhifeng Zhang
Water 2025, 17(4), 524; https://doi.org/10.3390/w17040524 - 12 Feb 2025
Viewed by 363
Abstract
As the only large sulfate-type salt lake in the global warm temperate deciduous forest zone, Yuncheng Salt Lake plays a crucial role in maintaining ecosystem stability and establishing a regional ecological barrier due to its unique ecological characteristics. Currently, there is a lack [...] Read more.
As the only large sulfate-type salt lake in the global warm temperate deciduous forest zone, Yuncheng Salt Lake plays a crucial role in maintaining ecosystem stability and establishing a regional ecological barrier due to its unique ecological characteristics. Currently, there is a lack of research on the spatial and temporal differentiation of ecological risks in inland lakes, particularly salt lake wetland ecosystems, under current and future scenarios. Moreover, studies using optimal parameter-based geographical detectors to identify the influencing factors of landscape ecological risks—while avoiding subjective bias—remain limited. This study utilizes land use/land cover data of Yuncheng Salt Lake from 1990 to 2022 to construct a landscape ecological risk assessment model. By employing spatial autocorrelation analysis, the optimal geographical detector, and the Patch-level Land Use Simulation (PLUS) model, the study explores the dynamic evolution of ecological risks in Yuncheng Salt Lake wetlands under different current and future scenarios. Furthermore, it analyzes the influence of various natural and socio-economic factors on ecological risk, aiming to provide valuable insights for targeted ecological risk warning and management measures in inland salt lake regions. The results indicate that: (1) Between 1990 and 2022, the area of built-up land in Yuncheng Salt Lake wetlands increased significantly, primarily due to the continuous decline in farmland area, while the water area initially decreased and then increased. (2) The landscape ecological risk index declined over the study period, indicating an improvement in the ecological risk status of Yuncheng Salt Lake wetlands in recent years, with the overall ecosystem security trending positively. (3) Topographical conditions are the primary factors influencing landscape ecological risk in Yuncheng Salt Lake wetlands, followed by mean annual temperature and population density. The synergistic effect of elevation with annual precipitation and NDVI (Normalized Difference Vegetation Index) exhibits the strongest explanatory power for the landscape ecological risk in the region. (4) Under different future scenarios, the proportion of high ecological risk areas in Yuncheng Salt Lake wetlands is projected to decrease to varying extents, with the ecological protection scenario contributing more effectively to the sustainable development of the salt lake wetland ecosystem. Full article
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Figure 1

Figure 1
<p>Map of the Yuncheng Salt Lake Wetland (<b>a</b>) Indicates the location of the study area in China, highlighting the close hydrological connection between the Yellow River and the salt lake. (<b>b</b>) Shows the location of the study area within the province, situated in Yanhu District, Yuncheng City, in the southern part of Shanxi Province. (<b>c</b>) Displays the specific location of the study area, along with its topographic and hydrological features.</p>
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<p>Land use/cover types in the study area at different time periods.</p>
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<p>Area of different land use/land cover types in the study area across various years.</p>
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<p>Sankey diagram of land use/land cover changes in the salt lake wetland from 1990 to 2022.</p>
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<p>Spatial distribution of ecological risk in the salt lake wetland landscape from 1990 to 2022.</p>
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<p>The interannual change rate of landscape ecological risk in Yuncheng Salt Lake (<b>a</b>) and significantly changed areas (<b>b</b>) from 1990 to 2022.</p>
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<p>Moran’s I scatter plot of the ecological risk of salt lake wetland landscapes from 1990 to 2022.</p>
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<p>Local spatial autocorrelation clustering characteristics of ecological risk in the salt lake wetland landscape from 1990 to 2022.</p>
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<p>Impact of interaction between two factors on ecological risk in the salt lake wetland based on dual-factor interaction detection. Note: X1: GDP; X2: Population density; X3: Annual average precipitation; X4: Annual average temperature; X5: Nighttime lights; X6: NDVI (Normalized Difference Vegetation Index); X7: Elevation; X8: Slope; X9: Distance to urban main roads; X10: Distance to highways.</p>
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<p>Contrast in 2020 and 2030 land use/land cover areas in the salt lake wetland under different scenarios (Unit: km<sup>2</sup>). Note: ND: natural development scenario; UD: urban development scenario; CP: cultivated land protection scenario; EP: ecological protection scenario; ERI: ecological risk index.</p>
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