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15 pages, 20002 KiB  
Article
Study on the CSES Electric Field VLF Electromagnetic Pulse Sequences Triggered by Volcanic Eruptions
by Siyu Liu, Ying Han, Qingjie Liu, Jianping Huang, Zhong Li and Xuhui Shen
Atmosphere 2025, 16(2), 208; https://doi.org/10.3390/atmos16020208 - 12 Feb 2025
Abstract
Volcanic eruptions, as a natural phenomenon, can generate electric field disturbances that may interfere with the ionosphere, potentially impacting communication systems and electronic devices. This paper conducts identification and classification analyses of the electromagnetic pulse (EMP) disturbances in the very low frequency (VLF) [...] Read more.
Volcanic eruptions, as a natural phenomenon, can generate electric field disturbances that may interfere with the ionosphere, potentially impacting communication systems and electronic devices. This paper conducts identification and classification analyses of the electromagnetic pulse (EMP) disturbances in the very low frequency (VLF) electric field data observed by the China Seismo-Electromagnetic Satellite (CSES) and finds that volcanic eruption events can trigger EMP sequences. This paper first applies Fourier transform to the VLF electric field waveform data to convert it into 4 s spectrograms. Then, a series of operations such as grayscale conversion, edge feature enhancement, and binarization are performed on the spectrograms. Subsequently, a K-means clustering algorithm is applied to the binarized results to identify EMP events on the spectrograms. Finally, a classification analysis is performed on the identified results, revealing that multiple volcanic eruption events generate EMP sequences. The results of this paper not only provide new insights into the impact of volcanic eruptions on the electromagnetic environment but also have significant implications for enhancing the anti-interference capability of communication systems and optimizing electromagnetic environment monitoring technologies. Full article
(This article belongs to the Section Upper Atmosphere)
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<p>Four-second (4 s) spectrogram with orbit number 219320.</p>
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<p>Flowchart of the EMP identification algorithm.</p>
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<p>The result of cropping the image in <a href="#atmosphere-16-00208-f001" class="html-fig">Figure 1</a>.</p>
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<p>The result of converting the image in <a href="#atmosphere-16-00208-f003" class="html-fig">Figure 3</a> to grayscale.</p>
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<p>The result of applying edge feature enhancement to the image in <a href="#atmosphere-16-00208-f004" class="html-fig">Figure 4</a>.</p>
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<p>The result of binarizing the image in <a href="#atmosphere-16-00208-f005" class="html-fig">Figure 5</a>.</p>
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<p>The result of applying KMeans unsupervised clustering to the image in <a href="#atmosphere-16-00208-f006" class="html-fig">Figure 6</a>.</p>
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<p>The result of marking the line classes on the grayscale image.</p>
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<p>Elbow method for determining the optimal K value.</p>
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<p>Non-EMP sequences. (<b>a</b>) Four-second (4 s) spectrograms; (<b>b</b>) Line recognition results.</p>
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<p>EMP sequence. (<b>a</b>) Four-second (4 s) spectrograms; (<b>b</b>) Line recognition results.</p>
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<p>EMP sequence. (<b>a</b>) Four-second (4 s) spectrograms; (<b>b</b>) Line recognition results.</p>
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<p>Monitoring results of the Tonga volcanic eruption. (<b>a</b>) Four-second (4 s) spectrograms; (<b>b</b>) Line identification results.</p>
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<p>Monitoring results of the Tonga volcanic eruption. (<b>a</b>) Four-second (4 s) spectrograms; (<b>b</b>) Line identification results.</p>
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<p>Volcanic eruptions and CSES satellite trajectories.</p>
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29 pages, 7931 KiB  
Article
Spatial Autocorrelation Analysis of CO and NO2 Related to Forest Fire Dynamics
by Hatice Atalay, Ayse Filiz Sunar and Adalet Dervisoglu
ISPRS Int. J. Geo-Inf. 2025, 14(2), 65; https://doi.org/10.3390/ijgi14020065 - 6 Feb 2025
Abstract
The increasing frequency and severity of forest fires globally highlight the critical need to understand their environmental impacts. This study applies spatial autocorrelation techniques to analyze the dispersion patterns of carbon monoxide (CO) and nitrogen dioxide (NO2) emissions during the 2021 [...] Read more.
The increasing frequency and severity of forest fires globally highlight the critical need to understand their environmental impacts. This study applies spatial autocorrelation techniques to analyze the dispersion patterns of carbon monoxide (CO) and nitrogen dioxide (NO2) emissions during the 2021 Manavgat forest fires in Türkiye, using Sentinel-5P satellite data. Univariate (UV) Global Moran’s I values indicated strong spatial autocorrelation for CO (0.84–0.93) and NO2 (0.90–0.94), while Bivariate (BV) Global Moran’s I (0.69–0.84) demonstrated significant spatial correlations between the two gases. UV Local Moran’s I analysis identified distinct UV High-High (UV-HH) and UV Low-Low (UV-LL) clusters, with CO concentrations exceeding 0.10000 mol/m2 and exhibiting wide dispersion, while NO2 concentrations, above 0.00020 mol/m2, remained localized near intense fire zones due to its shorter atmospheric lifetime. BV Local Moran’s I analysis revealed overlapping BV-HH (high CO, high NO2) and BV-LL (low CO, low NO2) clusters, influenced by topography and meteorological factors. These findings enhance the understanding of gas emission dynamics during forest fires and provide critical insights into the influence of environmental and combustion processes on pollutant dispersion. Full article
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<p>Study area. (<b>a</b>) Map of Türkiye and Antalya, created using ArcGIS Pro (version 3.1, Esri, Redlands, CA, USA). (<b>b</b>) Map of the Manavgat fire zone. (<b>c</b>) Sentinel-2 MSI 20 July 2021 false color composite image (RGB: B12, B8, B4) (before fire). (<b>d</b>) Sentinel-2 MSI 4 August 2021 false color composite image (RGB: B12, B8, B4) (during fire).</p>
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<p>Daily fire information, including burned area and daytime and nighttime ignition points (numbered 1–7) reported by the General Directorate of Forestry, was generated using ArcGIS Pro (version 3.1, Esri, Redlands, CA, USA).</p>
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<p>Flowchart of the study.</p>
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<p>Temporal changes in CO and NO<sub>2</sub> concentrations and FRP values during the observed period.</p>
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<p>UV Global Moran’s I values for CO and NO<sub>2</sub> from 28 July to 4 August 2021.</p>
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<p>Parameters considered in the UV Local Moran’s I analysis. (<b>a</b>) DEM of the study area. (<b>b</b>) Daily fire propagation recorded by the Antalya Regional Directorate of Forestry. (<b>c</b>) Daily CO concentrations derived from Sentinel-5P satellite data. (<b>d</b>) Daily CO cluster patterns calculated using UV Local Moran’s I.</p>
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<p>Daily distribution of UV Local Moran’s I UV-HH and UV-LL clusters across different elevation ranes, as determined by UV Local Moran’s I analysis. (<b>a</b>) CO-based clusters. (<b>b</b>) NO<sub>2</sub>-based clusters.</p>
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<p>Daily areas affected CO concentration levels within UV-HH and UV-LL clusters, as determined by UV Local Moran’s I analysis.</p>
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<p>Parameters considered in the UV Local Moran’s I analysis. (<b>a</b>) Daily NO<sub>2</sub> concentrations derived from Sentinel-5P satellite data. (<b>b</b>) Daily NO<sub>2</sub> cluster patterns calculated using UV Local Moran’s I.</p>
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<p>Daily areas affected by NO<sub>2</sub> concentration levels within UV-HH and UV-LL clusters, as determined by UV Local Moran’s I analysis.</p>
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<p>Daily BV Global Moran’s I values for CO-NO<sub>2</sub>.</p>
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<p>BV Local Moran’s I analysis. (<b>a</b>) Daily CO-NO<sub>2</sub> clusters derived from the BV Local Moran’s I and (<b>b</b>) corresponding areal extents of the clusters.</p>
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<p>Meteorological factors influencing fire behavior and smoke dispersion on 30 July 2021. (<b>a</b>) Hourly meteorological parameters recorded at the 17954-Manavgat Station [<a href="#B100-ijgi-14-00065" class="html-bibr">100</a>]. (<b>b</b>) Wind directions adapted from [<a href="#B101-ijgi-14-00065" class="html-bibr">101</a>]. (<b>c</b>) Smoke plume direction on 30 July 2021, observed from wind patterns in the Harmonized Sentinel-2 MSI Level-2A imagery captured between 08:35 and 08:39 UTC.</p>
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<p>Co-occurrence of flaming and smoldering combustion phases observed near Manavgat, east of Antalya, on 31 July 2021 [<a href="#B113-ijgi-14-00065" class="html-bibr">113</a>].</p>
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<p>CORINE (2018) LC types and percentages in the study area [<a href="#B59-ijgi-14-00065" class="html-bibr">59</a>,<a href="#B60-ijgi-14-00065" class="html-bibr">60</a>].</p>
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<p>Moran’s I quadrants and scatterplots illustrating spatial autocorrelation patterns, adapted from [<a href="#B116-ijgi-14-00065" class="html-bibr">116</a>].</p>
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<p>CO-NO<sub>2</sub> clusters and quadrants for 31 July. (<b>a</b>) BV LISA cluster map. (<b>b</b>) BV Local scatterplot with quadrants, generated in Python.</p>
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22 pages, 8396 KiB  
Article
A New Algorithm for the Global-Scale Quantification of Volcanic SO2 Exploiting the Sentinel-5P TROPOMI and Google Earth Engine
by Maddalena Dozzo, Alessandro Aiuppa, Giuseppe Bilotta, Annalisa Cappello and Gaetana Ganci
Remote Sens. 2025, 17(3), 534; https://doi.org/10.3390/rs17030534 - 5 Feb 2025
Abstract
Sulfur dioxide (SO2) is sourced by degassing magma in the shallow crust; hence its monitoring provides information on the rates of magma ascent in the feeding conduit and the style and intensity of eruption, ultimately contributing to volcano monitoring and hazard [...] Read more.
Sulfur dioxide (SO2) is sourced by degassing magma in the shallow crust; hence its monitoring provides information on the rates of magma ascent in the feeding conduit and the style and intensity of eruption, ultimately contributing to volcano monitoring and hazard assessment. Here, we present a new algorithm to extract SO2 data from the TROPOMI imaging spectrometer aboard the Sentinel-5 Precursor satellite, which delivers atmospheric column measurements of sulfur dioxide and other gases with an unprecedented spatial resolution and daily revisit time. Specifically, we automatically extract the volcanic clouds by introducing a two-step approach. Firstly, we used the Simple Non-Iterative Clustering segmentation method, which is an object-based image analysis approach; secondly, the K-means unsupervised machine learning technique is applied to the segmented images, allowing a further and better clustering to distinguish the SO2. We implemented this algorithm in the open-source Google Earth Engine computing platform, which provides TROPOMI imagery collection adjusted in terms of quality parameters. As case studies, we chose three volcanoes: Mount Etna (Italy), Taal (Philippines) and Sangay (Ecuador); we calculated sulfur dioxide mass values from 2018 to date, focusing on a few paroxysmal events. Our results are compared with data available in the literature and with Level 2 TROPOMI imagery, where a mask is provided to identify SO2, finding an optimal agreement. This work paves the way to the release of SO2 flux time series with reduced delay and improved calculation time, hence contributing to a rapid response to volcanic unrest/eruption at volcanoes worldwide. Full article
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<p>Flowchart with the main steps of the methodology: Sentinel-5P Offline/Level 3 Product PS imagery and the geometry outlined around the volcano represent the data input; dark green rectangles report the main processing steps (where GEE stands for Google Earth Engine and SNIC for Simple Non-Iterative Clustering), while the red parallelogram represents the output to highlight the pixels contaminated by SO<sub>2</sub> within those classes with a density higher than the selected threshold, Th.</p>
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<p>Example of the Simple Non-Iterative Clustering algorithm applied on the Sentinel-5P Offline SO<sub>2</sub> product of 2 June 2021 for Mt. Etna (Italy).</p>
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<p>(<b>a</b>) Sentinel-5P TROPOMI product available on the Copernicus browser for Mt. Etna for 2 June 2021. (<b>b</b>) The same product after the application of the SNIC and k-means techniques, reporting in the legend the 10 classes (with the relative density values in brackets). In the top right inset the resulting plume is highlighted, while in the bottom right inset the map of Italy with the area considered for the calculation framed in white is reported.</p>
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<p>SO<sub>2</sub> total mass time series calculated for Mt. Etna, expressed in kton. The red arrows indicate the events analyzed in more detail.</p>
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<p>Volcanic SO<sub>2</sub> plume calculated around Mt. Etna during the paroxysmal events of (<b>a</b>) 19 April 2020 (started at 06:30 UTC), (<b>b</b>) 1 April 2021 (started at 07:40 UTC), (<b>c</b>) 2 June 2021 (started at 8:00 UTC) and (<b>d</b>) 20 July 2021 (started at 07:20 UTC). Shown in red is the plume derived from the Level 2 product, where a detection flag &gt; 0 is applied, and in green is reported the result we obtained on GEE, exploiting the Level 3 product.</p>
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<p>SO<sub>2</sub> total mass time series calculated for Sangay volcano, expressed in kton. The red arrows indicate the events analyzed in more detail.</p>
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<p>Volcanic SO<sub>2</sub> plume calculated for Sangay during the eruptive events of (<b>a</b>) 20 September 2020 (started at 10:15 UTC), (<b>b</b>) 11 March 2021 (started at 11:20 UTC), (<b>c</b>) 7 May 2021 (started at 08:20 UTC) and (<b>d</b>) 16 May 2021 (started at 10:20 UTC). In red, the plume derived from the Level 2 product, where a detection flag &gt; 0 is applied; in green, the result we obtained on GEE, exploiting the Level 3 product.</p>
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<p>SO<sub>2</sub> total mass time series calculated on Taal volcano, expressed in kton. The red arrows indicate two of the four eruptive events analyzed in more detail, which are included in the selected time window.</p>
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<p>Volcanic SO<sub>2</sub> plume calculated on Taal volcano during the eruptions of (<b>a</b>) 12–13 January 2020 (started on 12 January at 06:30 UTC), (<b>b</b>) 1 July 2021 (started at 07:16 UTC), (<b>c</b>) 25–26 March 2022 (started on 25 March at 23:22 UTC) and (<b>d</b>) 11–12 April 2024 (started on 11 April at 21:30 UTC). In red, the plume derived from the Level 2 product, where a detection flag &gt; 0 is applied: in green, the result we obtained on GEE, exploiting the Level 3 product.</p>
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<p>Histograms representing the difference between SO<sub>2</sub> total mass (expressed in kton) calculated on GEE and data from the “SO<sub>2</sub> Flux Calculator” application for Mt. Etna (<b>a</b>), Sangay (<b>b</b>) and Taal volcano (<b>c</b>).</p>
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24 pages, 2886 KiB  
Article
Forest Stem Extraction and Modeling (FoSEM): A LiDAR-Based Framework for Accurate Tree Stem Extraction and Modeling in Radiata Pine Plantations
by Muhammad Ibrahim, Haitian Wang, Irfan A. Iqbal, Yumeng Miao, Hezam Albaqami, Hans Blom and Ajmal Mian
Remote Sens. 2025, 17(3), 445; https://doi.org/10.3390/rs17030445 - 28 Jan 2025
Abstract
Accurate characterization of tree stems is critical for assessing commercial forest health, estimating merchantable timber volume, and informing sustainable value management strategies. Conventional ground-based manual measurements, although precise, are labor-intensive and impractical at large scales, while remote sensing approaches using satellite or UAV [...] Read more.
Accurate characterization of tree stems is critical for assessing commercial forest health, estimating merchantable timber volume, and informing sustainable value management strategies. Conventional ground-based manual measurements, although precise, are labor-intensive and impractical at large scales, while remote sensing approaches using satellite or UAV imagery often lack the spatial resolution needed to capture individual tree attributes in complex forest environments. To address these challenges, this study provides a significant contribution by introducing a large-scale dataset encompassing 40 plots in Western Australia (WA) with varying tree densities, derived from Hovermap LiDAR acquisitions and destructive sampling. The dataset includes parameters such as plot and tree identifiers, DBH, tree height, stem length, section lengths, and detailed diameter measurements (e.g., DiaMin, DiaMax, DiaMean) across various heights, enabling precise ground-truth calibration and validation. Based on this dataset, we present the Forest Stem Extraction and Modeling (FoSEM) framework, a LiDAR-driven methodology that efficiently and reliably models individual tree stems from dense 3D point clouds. FoSEM integrates ground segmentation, height normalization, and K-means clustering at a predefined elevation to isolate stem cores. It then applies circle fitting to capture cross-sectional geometry and employs MLESAC-based cylinder fitting for robust stem delineation. Experimental evaluations conducted across various radiata pine plots of varying complexity demonstrate that FoSEM consistently achieves high accuracy, with a DBH RMSE of 1.19 cm (rRMSE = 4.67%) and a height RMSE of 1.00 m (rRMSE = 4.24%). These results surpass those of existing methods and highlight FoSEM’s adaptability to heterogeneous stand conditions. By providing both a robust method and an extensive dataset, this work advances the state of the art in LiDAR-based forest inventory, enabling more efficient and accurate tree-level assessments in support of sustainable forest management. Full article
(This article belongs to the Special Issue New Insight into Point Cloud Data Processing)
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<p>Overview of the stem segmentation framework for efficient tree stem modeling in complex forest environments using MLS-derived 3D point cloud data. The process begins with data collection using the Hovermap LiDAR scanner, followed by the FoSEM processing method to extract tree stems. The final step involves feature extraction to calculate key parameters, including diameter at breast height (DBH), tree height, and stem deviations.</p>
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<p>Overview of experimental plots and data collection methodology: (<b>a</b>) spatial distribution of 40 circular plots across two sites, representing diverse forest conditions; (<b>b</b>) data acquisition paths and trajectories within the plots, ensuring consistent and uniform LiDAR coverage; (<b>c</b>) top-view of Plot ID 25, showcasing the chopped trees and prominently highlighting the ground control point (GCP) located at the center of the plot.</p>
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<p>Ground-truth generation process for tree stem measurements: (<b>a</b>) a researcher performing destructive sampling, measuring stem diameters at multiple heights; (<b>b</b>) the overall dimensions of a standing tree, with emphasis on the diameter measurement at breast height (1.3 m); (<b>c</b>) The cross-sectional geometry of the stem and segmentation of the felled tree, detailing section lengths and recorded diameters along the trunk.</p>
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<p>Field operations using the Hovermap LiDAR scanner for data collection in Western Australia’s forest plots: (<b>a</b>) the modular design of the Hovermap device; (<b>b</b>) a trained operator conducting data acquisition in a forest plot; (<b>c</b>) the principle of 3D point cloud generation, showcasing the vertical and horizontal spatial data captured for tree structure and stem modeling.</p>
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<p>Forest Stem Extraction and Modeling Method (FoSEM) for efficient tree stem modeling: This framework illustrates the proposed framework for tree stem modeling from LiDAR-derived 3D point cloud data. The framework comprises five sequential phases: (<b>a</b>) preprocessing, including voxelization, SMRF-based ground segmentation, and height normalization to refine raw data; (<b>b</b>) tree extraction and segmentation employing height band segmentation, K-means clustering, BEV height compression, and circle fitting; (<b>c</b>) classification and stem point extraction leveraging MLESAC cylinder fitting for precise tree stem modeling; and (<b>d</b>) feature extraction and results validation for accurate DBH, tree height, and stem inclination computations.</p>
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<p>Visualization of stem extraction and flexure for three representative <span class="html-italic">Pinus radiata</span> samples: (<b>a</b>) Plot 25, Tree 6, (<b>b</b>) Plot 31, Tree 4, and (<b>c</b>) Plot 42, Tree 35. In each subfigure, the original point cloud (blue) is shown alongside the extracted stem (brown), comparing both the trunk geometry and flexure patterns between them. The vertical axis (Z) indicates tree height, while the horizontal axis (Cx) highlights changes in trunk position, thereby depicting the degree of bending or curvature. These visualizations reveal contrasting stem flexure characteristics across plots of differing complexity.</p>
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15 pages, 3578 KiB  
Article
Investigation of the Earliest Ozone Pollution Events in Hangzhou Bay, China Based on Observations and ERA5 Reanalysis Data
by Tianen Yao, Xinhao Li, Zhi Li, Xinyu Yang, Jinjia Zhang, Yaqi Wang, Jianhui Guo and Jing Li
Toxics 2025, 13(2), 99; https://doi.org/10.3390/toxics13020099 - 27 Jan 2025
Abstract
Ozone pollution in Hangzhou Bay, one of the seven petrochemical clusters in China, is severe. Early ozone pollution has been detected recently, such as the maximum daily 8 h average (MDA8) ozone concentration in Jiaxing achieving 171.0 μg/m3 on 7 March 2023. [...] Read more.
Ozone pollution in Hangzhou Bay, one of the seven petrochemical clusters in China, is severe. Early ozone pollution has been detected recently, such as the maximum daily 8 h average (MDA8) ozone concentration in Jiaxing achieving 171.0 μg/m3 on 7 March 2023. Satellites have observed tropospheric column concentrations of ozone precursors formaldehyde (HCHO) and nitrogen dioxide (NOx), and quantitative models are proposed to reveal the causes of the early onset of ozone pollution. VOC-limited and transitional regimes dominate most areas in Hangzhou Bay, and NOx-limited regimes dominate the region around Hangzhou Bay, such as northeastern Jiangsu Province. Results show that HCHO column concentrations are increasing in VOC-limited regions, and NOx column concentrations are increasing more rapidly than HCHO in NOx-limited regions. According to multivariate linear regression (MLR), early spring ozone pollution in Hangzhou Bay is mainly caused by meteorological drivers. Hangzhou Bay has formed an atmospheric meteorological environment with high temperature and low humidity. The richer solar radiation intensifies the photochemical reactions associated with tropospheric ozone formation, producing more tropospheric ozone. Based on the Shapley Additive Explanation (SHAP) algorithm, ozone pollution increases when solar radiation exceeds 12 million J/m2 and is accompanied by high temperatures. Overall, reducing VOC emissions helps to mitigate ozone growth in Shanghai and northern Hangzhou Bay, while reducing NOx emissions is more effective in northeastern Jiangsu Province. Full article
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<p>The location of the Hangzhou Bay and Yangtze River Delta (YRD) region in China.</p>
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<p>Average of MDA8 ozone concentrations between 1 March and 10 March (2019–2023) at sites in the Hangzhou Bay region and their varying trends. (<b>a</b>) shows ozone concentrations and (<b>b</b>) shows ozone trends.</p>
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<p>(<b>a</b>) The mean MDA8 ozone concentrations over the period from 1 to 10 March averaged for sites in the Hangzhou Bay region during 2019–2023. (<b>b</b>) Diurnal cycles of mean MDA8 ozone concentrations over the period from1 March to 10 March averaged for sites in the Hangzhou Bay region during 2019–2023.</p>
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<p>The difference in (<b>a</b>) HCHO average, (<b>b</b>) NO<sub>2</sub> average, and (<b>c</b>) HCHO average/NO<sub>2</sub> average during 1–10 March between 2023 and 2019. (<b>d</b>) The distribution of the ozone–NO<sub>x</sub>–VOC sensitivity classification in the Hangzhou Bay region during April–September 2022 was categorized by three ranges of HCHO average/NO<sub>2</sub> average thresholds (&lt;2.2, 2.2–3.3, &gt;3.3).</p>
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<p>The difference in (<b>a</b>) HCHO average, (<b>b</b>) NO<sub>2</sub> average, and (<b>c</b>) HCHO average/NO<sub>2</sub> average during 1–10 March between 2023 and 2019. (<b>d</b>) The distribution of the ozone–NO<sub>x</sub>–VOC sensitivity classification in the Hangzhou Bay region during April–September 2022 was categorized by three ranges of HCHO average/NO<sub>2</sub> average thresholds (&lt;2.2, 2.2–3.3, &gt;3.3).</p>
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<p>The average of (<b>a</b>) surface downward shortwave radiation flux, (<b>b</b>) air temperature (at 1000 hPa), and (<b>c</b>) relative humidity over the period from 1 to 10 March during 2019–2023 in Hangzhou Bay.</p>
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<p>SHAP summary plot of feature importance (<b>A</b>). The SHAP dependent plot between temperature and radiation (<b>B</b>). The purple vertical line in (<b>B</b>) indicates radiation of 12 million J/m<sup>2</sup>.</p>
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19 pages, 9637 KiB  
Article
Analyzing Travel and Emission Characteristics of Hazardous Material Transportation Trucks Using BeiDou Satellite Navigation System Data
by Yajie Zou, Qirui Hu, Wanbing Han, Siyang Zhang and Yubin Chen
Remote Sens. 2025, 17(3), 423; https://doi.org/10.3390/rs17030423 - 26 Jan 2025
Abstract
Road hazardous material transportation plays a critical role in road traffic management. Due to the dangerous nature of the cargo, hazardous material transportation trucks (HMTTs) have different route selection and driving characteristics compared to traditional freight trucks. These differences lead to unique travel [...] Read more.
Road hazardous material transportation plays a critical role in road traffic management. Due to the dangerous nature of the cargo, hazardous material transportation trucks (HMTTs) have different route selection and driving characteristics compared to traditional freight trucks. These differences lead to unique travel and emission patterns, which in turn affect traffic management strategies and emission control measures. However, existing research predominantly focuses on safety aspects related to individual vehicle behavior, with limited exploration of the broader travel and emission characteristics of HMTTs. To bridge this gap, this study develops a comprehensive framework for analyzing the travel patterns and emissions of HMTTs. The methodology begins by applying a Gaussian mixture distribution model to identify vehicle stop points, eliminating biases associated with subjective settings. Origin–destination (OD) pairs are then determined through stop time clustering, followed by the extraction of travel characteristics using non-negative matrix factorization. Emissions are subsequently calculated based on the identified trip data. The relationship between emissions and land use characteristics is further analyzed using geographically weighted regression (GWR). Crucially, this study leverages data from the BeiDou Satellite Navigation System, focusing on HMTTs operating within Shanghai. The processed data reveal three distinct travel modes of HMTTs, categorized by spatiotemporal patterns: Daytime—Surrounding cities, Early morning—In-city, and Midnight—Scattered. Moreover, unlike other road vehicles, HMTT emissions are heavily influenced by industrial and company-related points of interest (POIs). These findings highlight the significant role of BeiDou Satellite Navigation System data in optimizing HMTT management strategies to reduce emissions and improve overall safety. Full article
(This article belongs to the Special Issue Application of Photogrammetry and Remote Sensing in Urban Areas)
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<p>Overall methodological framework.</p>
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<p>Vehicle speed distribution and fitted curve (<b>a</b>); comparison of static drift points and moving points direction change (<b>b</b>).</p>
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<p>Trip generation results (OD distribution) of HMTTs in Shanghai.</p>
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<p>Travel distance distribution (<b>a</b>) and time distribution (<b>b</b>) of HMTTs.</p>
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<p>Distribution of Vehicle Departure and Arrival Times.</p>
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<p>Daytime—Surrounding cities travel mode of HMTTs. Spatial distribution of travel mode 1 is shown as sub-figure (<b>a</b>), and temporal distribution of travel mode 1 is shown as sub-figure (<b>b</b>).</p>
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<p>Early morning—In-city travel mode of HMTTs. Spatial distribution of travel mode 2 is shown as sub-figure (<b>a</b>), and temporal distribution of travel mode 2 is shown as sub-figure (<b>b</b>).</p>
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<p>Midnight—scattered travel mode of HMTTs. Spatial distribution of travel mode 3 is shown as sub-figure (<b>a</b>), and temporal distribution of travel mode 3 is shown as sub-figure (<b>b</b>).</p>
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<p>Temporal (<b>a</b>) and spatial (<b>b</b>) emission characteristics of HMTTs.</p>
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<p>Comparison of road traffic flow (<b>a</b>), average speed (<b>b</b>), and emission level (<b>c</b>).</p>
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<p>Coefficients of GWR for different land use types: (<b>a</b>) Industrial-related POIs; (<b>b</b>) Company-related POIs; (<b>c</b>) Entertainment-related POIs; (<b>d</b>) Education-related POIs.</p>
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21 pages, 9547 KiB  
Article
Spatial Patterns and Characteristics of Urban–Rural Agricultural Landscapes: A Case Study of Bengaluru, India
by Jayan Wijesingha, Thomas Astor, Sunil Nautiyal and Michael Wachendorf
Land 2025, 14(2), 208; https://doi.org/10.3390/land14020208 - 21 Jan 2025
Viewed by 460
Abstract
Globally, the agricultural landscape is the most exposed due to urbanisation. Therefore, finding the spatial and temporal patterns of changes in agricultural landscapes is essential for sustainable development. This study developed a workflow to address this information gap and determine the spatial patterns [...] Read more.
Globally, the agricultural landscape is the most exposed due to urbanisation. Therefore, finding the spatial and temporal patterns of changes in agricultural landscapes is essential for sustainable development. This study developed a workflow to address this information gap and determine the spatial patterns and characteristics of agricultural landscapes along an urban–rural gradient. The workflow comprised three steps. First, remote sensing data were classified to map crop types. Second, landscape metrics were used to examine the spatial patterns of agricultural land cover concerning urbanisation levels. Finally, unsupervised clustering was applied to categorise agricultural landscape types along the urban–rural interface. The workflow was tested using WorldView-3 satellite data in Bengaluru, India. It identified four major herbaceous crop types (millet, maize, pulses, and cash crops) and woody plantations as agricultural land cover. An analysis revealed that agricultural land cover increased from urban to rural areas, with diverse patterns in transition zones. The cluster analysis characterised four agricultural landscapes. The findings imply that changes in an agricultural landscape along an urban–rural gradient are not linear. The newly developed integrated workflow empowers stakeholders to make informed and well-reasoned decisions, and it can be periodically implemented to maintain the ongoing monitoring of urbanisation’s effect on food systems. Full article
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<p>Map of the study area: (<b>a</b>) India and Karnataka state (in blue), (<b>b</b>) Bengaluru rural and urban districts and selected northern transect (in red), (<b>c</b>) WorldView-3 satellite image in the true-colour composite. “Vidhana Soudha” (lit. Legislative House) is the seat of the state legislature of Karnataka, which is considered the city centre.</p>
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<p>(<b>a</b>) Selected one-square-kilometre plots along the transect and their corresponding survey stratification index (SSI) values. (<b>b</b>) Relationships between the SSI and the distance to the city centre (blue), as well as between the SSI and the percentage of built-up areas (orange) in the selected one–square–kilometre plots.</p>
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<p>The hexagonal grid used in this study.</p>
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<p>The developed ALC (agricultural land cover) map along the northern transect with magnified views of exemplary areas.</p>
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<p>Landscape-level metric patterns against the degree of urbanisation (expressed as the survey stratification index (SSI)). (<b>a</b>) Shannon diversity index (SHDI). (<b>b</b>) Share of agricultural area (TA).</p>
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<p>Class-level landscape metric patterns against the degree of urbanisation (expressed as the survey stratification index (SSI)). (<b>a</b>) Class area (CA). (<b>b</b>) Proportion of class area to total agricultural area (PLAND).</p>
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<p>Exemplary hexagons for the identified four clusters (<b>a</b>–<b>h</b>). True-colour composite satellite images of four hexagons (<b>a</b>–<b>d</b>). Corresponding land-cover information for each hexagon (<b>e</b>–<b>h</b>). In the example hexagons, from top to bottom, each column represents one cluster: Cluster A (<b>a</b>,<b>e</b>), Cluster B (<b>b</b>,<b>f</b>), Cluster C (<b>c</b>,<b>g</b>), and Cluster D (<b>d</b>,<b>h</b>). The distribution of the cluster mean values of the Shannon diversity index (SHDI) in blue, total agricultural area (TA) in yellow, field crop area (FCA) in grey, and woody plantation area (WPA) in red are plotted in the latter part of the.</p>
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<p>Distribution of derived agricultural landscape types.</p>
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<p>The hexagonal grid with (<b>a</b>) distance to city centre in kilometres, (<b>b</b>) share of non-built-up area (%), (<b>c</b>) survey stratification index (SSI), (<b>d</b>) categories of urbanization based on SSI values.</p>
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<p>The hexagonal grid with (<b>a</b>) Shannon diversity index (unit-less), (<b>b</b>) total agricultural area (%), (<b>c</b>) share of total field crop area (%), (<b>d</b>) share of total area for woody plantation crops (%).</p>
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10 pages, 2010 KiB  
Proceeding Paper
Learnable Weight Graph Neural Network for River Ice Classification
by Yifan Qu, Armina Soleymani, Denise Sudom and Katharine Andrea Scott
Proceedings 2024, 110(1), 30; https://doi.org/10.3390/proceedings2024110030 - 13 Jan 2025
Viewed by 284
Abstract
Monitoring river ice is crucial for planning safe navigation routes, with ice–water classification being one of the most important tasks in ice mapping. While high-resolutions satellite imagery, such as synthetic aperture radar (SAR), is well-suited to this task, manual interpretation of these data [...] Read more.
Monitoring river ice is crucial for planning safe navigation routes, with ice–water classification being one of the most important tasks in ice mapping. While high-resolutions satellite imagery, such as synthetic aperture radar (SAR), is well-suited to this task, manual interpretation of these data is challenging due to the large data volume. Machine learning approaches are suitable methods to overcome this; however, training the models might not be time-effective when the desired result is a narrow structure, such as a river, within a large image. To address this issue, we proposed a model incorporating a graph neural network (GNN), called learnable weights graph convolution network (LWGCN). Focusing on the winters of 2017–2021 with emphasis on the Beauharnois Canal and Lake St Lawrence regions of the Saint Lawrence River. The model first converts the SAR image into graph-structured data using simple linear iterative clustering (SLIC) to segment the SAR image, then connecting the centers of each superpixel to form graph-structured data. For the training model, the LWGCN learns the weights on each edge to determine the relationship between ice and water. By using the graph-structured data as input, the proposed model training time is eight times faster, compared to a convolution neural network (CNN) model. Our findings also indicate that the LWGCN model can significantly enhance the accuracy of ice and water classification in SAR imagery. Full article
(This article belongs to the Proceedings of The 31st International Conference on Geoinformatics)
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<p>The study region consists of the Beauharnois Canal and Lake Saint Lawrence. The central coordinates for the Beauharnois Canal are approximately 45.26° N and 73.94° W. The central coordinates for Lake Saint Lawrence are approximately 44.99° N and 74.88° W.</p>
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<p>The process of generating graphs from SAR imagery for an arbitrary chosen date (2017-01-12) in the Beauharnois Canal. (<b>a</b>) Sentinel-1 SAR image. (<b>b</b>) Use simple linear iterative clustering (SLIC) to segment the image into superpixels. (<b>c</b>) Connect the centers of each superpixel. (<b>d</b>) Remove the land area (this is the graph structure used in the LWGCN model).</p>
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<p>(<b>a</b>) Sentinel-1 VV SAR image of Lake Saint Lawrence (see <a href="#proceedings-110-00030-f001" class="html-fig">Figure 1</a> for location within larger study region), (<b>b</b>) ground truth from manually labeled shapefile, where blue indicates water and red indicates ice, and (<b>c</b>) LWGCN model output, where the colors are represented in <a href="#proceedings-110-00030-t005" class="html-table">Table 5</a>. The arbitrary chosen date is 2018-01-07.</p>
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21 pages, 4440 KiB  
Article
Automatic Grape Cluster Detection Combining YOLO Model and Remote Sensing Imagery
by Ana María Codes-Alcaraz, Nicola Furnitto, Giuseppe Sottosanti, Sabina Failla, Herminia Puerto, Carmen Rocamora-Osorio, Pedro Freire-García and Juan Miguel Ramírez-Cuesta
Remote Sens. 2025, 17(2), 243; https://doi.org/10.3390/rs17020243 - 11 Jan 2025
Viewed by 491
Abstract
Precision agriculture has recently experienced significant advancements through the use of technologies such as unmanned aerial vehicles (UAVs) and satellite imagery, enabling more efficient and precise agricultural management. Yield estimation from these technologies is essential for optimizing resource allocation, improving harvest logistics, and [...] Read more.
Precision agriculture has recently experienced significant advancements through the use of technologies such as unmanned aerial vehicles (UAVs) and satellite imagery, enabling more efficient and precise agricultural management. Yield estimation from these technologies is essential for optimizing resource allocation, improving harvest logistics, and supporting decision-making for sustainable vineyard management. This study aimed to evaluate grape cluster numbers estimated by using YOLOv7x in combination with images obtained by UAVs from a vineyard. Additionally, the capability of several vegetation indices calculated from Sentinel-2 and PlanetScope satellites to estimate grape clusters was evaluated. The results showed that the application of the YOLOv7x model to RGB images acquired from UAVs was able to accurately predict grape cluster numbers (R2 value and RMSE value of 0.64 and 0.78 clusters vine−1). On the contrary, vegetation indexes derived from Sentinel-2 and PlanetScope satellites were found not able to predict grape cluster numbers (R2 lower than 0.23), probably due to the fact that these indexes are more related to vegetation vigor, which is not always related to yield parameters (e.g., cluster number). This study suggests that the combination of high-resolution UAV images, multispectral satellite images, and advanced detection models like YOLOv7x can significantly improve the accuracy of vineyard management, resulting in more efficient and sustainable agriculture. Full article
(This article belongs to the Special Issue Cropland and Yield Mapping with Multi-source Remote Sensing)
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<p>Study site location at Alicante, Spain (38°25′5.46″N; 0°38′22.56″W); an example of RGB image acquired with the UAV at a height (h) of 17 m and a sensor tilt (θ) of 45° (green rectangle).</p>
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<p>Example of cluster detection using YOLOv7x with RGB images acquired from UAV. Numbers in the bounding boxes represent the model’s confidence in detecting the objects, expressed as a value between 0 and 1.</p>
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<p>Conceptual framework of the object detection methodology.</p>
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<p>(<b>a</b>) Mean Average Precision at an IoU threshold of 0.5, reflecting the model’s detection accuracy, and (<b>b</b>) Precision-Recall Graph indicating the model’s effectiveness in detecting objects.</p>
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<p>Comparison between the number of grape clusters per vine estimated using the YOLOv7x model and the actual measurements observed from the UAV images. The red dashed line represents the trend line regression, while the black dashed line indicates the 1:1 relationship. For comparison purposes, the trend lines obtained by using YOLOv7-E6 (blue dashed line) and YOLOv8 versions (yellow dashed line) have been included (adapted from [<a href="#B46-remotesensing-17-00243" class="html-bibr">46</a>]).</p>
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<p>Comparison of the reflectance values from PlanetScope (ρ<sub>PS</sub>) and Sentinel-2 (ρ<sub>S2</sub>) satellites obtained in the visible (blue, green, and red) and near-infrared (NIR) spectral bands. The black dashed line represents the general trend line regression, while the black continuous line indicates the 1:1 relationship.</p>
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<p>Example of NDVI calculated from Sentinel2 (<b>a</b>) and PlanetScope (<b>b</b>) images acquired on 29 June 2022.</p>
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<p>Temporal evolution of the different vegetation indexes calculated from PlanetScope and Sentinel-2 satellites (DOY: Day Of Year).</p>
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17 pages, 7144 KiB  
Article
Fine-Grained Building Classification in Rural Areas Based on GF-7 Data
by Mingbo Liu, Ping Wang, Peng Han, Longfei Liu and Baotian Li
Sensors 2025, 25(2), 392; https://doi.org/10.3390/s25020392 - 10 Jan 2025
Viewed by 312
Abstract
Building type information is widely used in various fields, such as disaster management, urbanization studies, and population modelling. Few studies have been conducted on fine-grained building classification in rural areas using China’s Gaofen-7 (GF-7) high-resolution stereo mapping satellite data. In this study, we [...] Read more.
Building type information is widely used in various fields, such as disaster management, urbanization studies, and population modelling. Few studies have been conducted on fine-grained building classification in rural areas using China’s Gaofen-7 (GF-7) high-resolution stereo mapping satellite data. In this study, we employed a two-stage method combining supervised classification and unsupervised clustering to classify buildings in the rural area of Pingquan, northern China, based on building footprints, building heights, and multispectral information extracted from GF-7 data. In the supervised classification stage, we compared different classification models, including Extreme Gradient Boosting (XGBoost) and Random Forest classifiers. The best-performing XGBoost model achieved an overall roof type classification accuracy of 88.89%. Additionally, we proposed a template-based building height correction method for pitched roof buildings, which combined geometric features of the building footprint, street view photos, and height information extracted from the GF-7 stereo image. This method reduced the RMSE of the pitched roof building heights from 2.28 m to 1.20 m. In the cluster analysis stage, buildings with different roof types were further classified in the color and shape feature spaces and combined with the building height information to produce fine-grained building type codes. The results of the roof type classification and fine-grained building classification reveal the physical and geometric characteristics of buildings and the spatial distribution of different building types in the study area. The building classification method proposed in this study has broad application prospects for disaster management in rural areas. Full article
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<p>The study area: (<b>a</b>) location of the study area; (<b>b</b>) GF-7 MUX multispectral image of the study area.</p>
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<p>Workflow of the fine-grained building classification. The process of extracting building height from GF-7 data is also demonstrated.</p>
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<p>Template-based height correction for pitched roof buildings: (<b>a</b>) image of the pitched roof building; (<b>b</b>) minimum bounding rectangle and the eave zone; (<b>c</b>) street view photo of pitched roof buildings; and (<b>d</b>) template used for height correction.</p>
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<p>Samples of different roof types: (<b>a</b>) pitched; (<b>b</b>) greenhouse; (<b>c</b>) color steel; (<b>d</b>) flat; (<b>e</b>) complex.</p>
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<p>Roof types in the study area. Aggregated to 50 m ground sampling distance (GSD) for visualization.</p>
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<p>Height validation of pitched roof buildings: (<b>a</b>) before correction; (<b>b</b>) after correction.</p>
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<p>Fine-grained building types in the study area. Aggregated to 50 m GSD for visualization.</p>
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<p>Samples of several representative building types.</p>
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<p>Confusion matrices of different supervised classification models.</p>
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<p>Height validation scatterplot of: (<b>a</b>) greenhouses; (<b>b</b>) color steel roof buildings; (<b>c</b>) flat roof buildings; and (<b>d</b>) complex roof buildings.</p>
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<p>Distribution of buildings with different roof types in color and shape dimensions and statistical indicators in cluster analysis. Cluster 1 to cluster 4 are represented by blue, red, green, and yellow colors, respectively.</p>
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19 pages, 4850 KiB  
Article
Single-Nucleus RNA Sequencing Reveals Cellular Transcriptome Features at Different Growth Stages in Porcine Skeletal Muscle
by Ziyu Chen, Xiaoqian Wu, Dongbin Zheng, Yuling Wang, Jie Chai, Tinghuan Zhang, Pingxian Wu, Minghong Wei, Ting Zhou, Keren Long, Mingzhou Li, Long Jin and Li Chen
Cells 2025, 14(1), 37; https://doi.org/10.3390/cells14010037 - 2 Jan 2025
Viewed by 667
Abstract
Porcine latissimus dorsi muscle (LDM) is a crucial source of pork products. Meat quality indicators, such as the proportion of muscle fibers and intramuscular fat (IMF) deposition, vary during the growth and development of pigs. Numerous studies have highlighted the heterogeneous nature of [...] Read more.
Porcine latissimus dorsi muscle (LDM) is a crucial source of pork products. Meat quality indicators, such as the proportion of muscle fibers and intramuscular fat (IMF) deposition, vary during the growth and development of pigs. Numerous studies have highlighted the heterogeneous nature of skeletal muscle, with phenotypic differences reflecting variations in cellular composition and transcriptional profiles. This study investigates the cellular-level transcriptional characteristics of LDM in large white pigs at two growth stages (170 days vs. 245 days) using single-nucleus RNA sequencing (snRNA-seq). We identified 56,072 cells across 12 clusters, including myofibers, fibro/adipogenic progenitor (FAP) cells, muscle satellite cells (MUSCs), and other resident cell types. The same cell types were present in the LDM at both growth stages, but their proportions and states differed. A higher proportion of FAPs was observed in the skeletal muscle of 245-day-old pigs. Additionally, these cells exhibited more active communication with other cell types compared to 170-day-old pigs. For instance, more interactions were found between FAPs and pericytes or endothelial cells in 245-day-old pigs, including collagen and integrin family signaling. Three subclasses of FAPs was identified, comprising FAPs_COL3A1+, FAPs_PDE4D+, and FAPs_EBF1+, while adipocytes were categorized into Ad_PDE4D+ and Ad_DGAT2+ subclasses. The proportions of these subclasses differed between the two age groups. We also constructed differentiation trajectories for FAPs and adipocytes, revealing that FAPs in 245-day-old pigs differentiated more toward fibrosis, a characteristic reminiscent of the high prevalence of skeletal muscle fibrosis in aging humans. Furthermore, the Ad_PDE4D+ adipocyte subclass, predominant in 245-day-old pigs, originated from FAPs_PDE4D+ expressing the same gene, while the Ad_DGAT2+ subclass stemmed from FAPs_EBF1+. In conclusion, our study elucidates transcriptional differences in skeletal muscle between two growth stages of pigs and provides insights into mechanisms relevant to pork meat quality and skeletal muscle diseases. Full article
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<p>(<b>A</b>) Differences in body weight, backfat thickness, and intramuscular fat content of the longest dorsal muscle in 170-day-old and 245-day-old pigs (<span class="html-italic">n</span> = 2; *** indicates <span class="html-italic">p</span> &lt; 0.001, * indicates <span class="html-italic">p</span> &lt; 0.05). (<b>B</b>) Results of cell nuclear population clustering and annotation. (<b>C</b>) Main marker genes and expression levels of cell types in a violin plot. (<b>D</b>) Expression of marker genes in different cell clusters. (<b>E</b>) Heatmap of the top 10 differentially expressed genes across different cell types. (<b>F</b>) Myofiber enrichment pathway results. (<b>G</b>) FAP enrichment pathway results.</p>
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<p>(<b>A</b>) The top five regulons for each cell type. Regulon specificity scores (RSS) of each annotated cell population. A point in a panel shows the RSS of one TF regulon. TF regulons are sorted by the RSSs in each cell type. The top five specific regulons are highlighted in red. (<b>B</b>) The expression activity of the top five regulons in each cell. (<b>C</b>) The unsupervised clustering results of the CSI matrix. Heatmap displays clustered regulon modules based on the CSI matrix along with the included regulons being shown in the right, indicating whether a given regulon is specific to a cell type. Top five RSS for each cluster shown. (<b>D</b>) The correspondence between regulon modules and the cells with the highest average activity of regulons. (<b>E</b>) The top 20 regulons in each cell appear in different modules. (<b>F</b>–<b>I</b>) Pathway enrichment results for M1, M2, M3, and M4, respectively.</p>
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<p>(<b>A</b>) Uniformity of cell types between two stages. (<b>B</b>) Cell composition of pigs at two stages. (<b>C</b>) Number of differentially expressed genes for each cell type between two stages (|logFC| &gt; 1, <span class="html-italic">p.adj</span> &lt; 0.05). (<b>D</b>) Enrichment results for differentially upregulated gene pathways in FAPs and MUSCs. (<b>E</b>) Number of cellular communications between two stages. (<b>F</b>) Violin plot of cell-to-cell communication between FAPs and other cells in the 245-day-old pigs. (<b>G</b>) Differences in expression levels of cell-to-cell communication between the two stages.</p>
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<p>(<b>A</b>) Original clustering results and cell annotation of FAP cells. (<b>B</b>) Expression of marker genes in different subtypes. (<b>C</b>) Violin plot of marker gene expression in major cell types. (<b>D</b>) Proportion of FAP subtypes at different developmental stages. (<b>E</b>) Pseudotime trajectory of FAPs. (<b>F</b>) Developmental pseudotime of FAP subtypes. (<b>G</b>) Distribution of FAP cells along the pseudotime trajectory in individuals at different developmental stages. (<b>H</b>) Differences in differentiation levels of FAP subtypes.</p>
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<p>(<b>A</b>) Original clustering results and cell annotation of adipocyte cells. (<b>B</b>) Expression of marker genes in different subtypes. (<b>C</b>) Violin plot of marker gene expression in major cell types. (<b>D</b>) Proportion of adipocyte subtypes at different developmental stages. (<b>E</b>) RNA velocity plot of FAPs and adipocyte cells. (<b>F</b>) Differences in differentiation levels between FAPs and adipocyte cells. (<b>G</b>) Distribution of FAPs and adipocyte cells along the pseudotime trajectory in individuals at different developmental stages. (<b>H</b>) Pathway enrichment analysis of Ad_<span class="html-italic">DGAT2</span><sup>+</sup> adipocyte cell-specific expressed genes.</p>
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13 pages, 5647 KiB  
Article
A Reliable Medium for Monitoring Atmospheric Deposition near Emission Sources by Using Snow from Agricultural Areas
by Jiayang Liu, Zaijin Sun, Wenkai Lei, Jingwen Xu, Qian Sun, Zhicheng Shen, Yixuan Lyu, Huading Shi, Ying Zhou, Lan Zhang, Zefeng Wu and Yuepeng Pan
Atmosphere 2025, 16(1), 26; https://doi.org/10.3390/atmos16010026 - 29 Dec 2024
Viewed by 423
Abstract
Atmospheric deposition is an important source of heavy metal in soil and the use of dust collection cylinders is a traditional monitoring method. This method has limitations in agricultural areas because polluted soil particles may become resuspended and eventually deposited into these cylinders, [...] Read more.
Atmospheric deposition is an important source of heavy metal in soil and the use of dust collection cylinders is a traditional monitoring method. This method has limitations in agricultural areas because polluted soil particles may become resuspended and eventually deposited into these cylinders, leading to overestimates in the amount of atmospheric deposition in soil. To address this concern, we propose that frequent snowfall can help suppress local soil dust resuspension and that fresh snow can serve as an efficient surrogate surface when collecting atmospheric deposition samples. To investigate the rationality of this method, 52 snow samples were collected from sites surrounding smelting plants in Anyang, an industrial region of North China. The results revealed that the concentration of cadmium in the melted snow ranged between 0.03 and 41.09 μg/L, with mean values three times higher around the industrial sites (5.31 μg/L) than background farmlands (1.54 μg/L). In addition, the cadmium concentration in the snow from sites surrounding the factories was higher in the north than in the south because of prevailing winds blowing from the southwest. Moreover, snow samples from sites with high concentrations of cadmium and sulfate can be categorized into different groups via the clustering method, conforming to the spatial distribution of particulate matter emissions and sulfur dioxide satellite column concentrations. Finally, a positive correlation was found between the cadmium content in the snow and the production capacity (R2 = 0.90, p < 0.05) and total permitted emissions (R2 = 0.69, p > 0.05) of the nearby factories. These findings demonstrate that snow is a reliable medium for documenting atmospheric dry deposition associated with specific industrial emissions. Full article
(This article belongs to the Section Biosphere/Hydrosphere/Land–Atmosphere Interactions)
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<p>The specific location of the area of study in China (<b>a</b>) and snow sampling sites surrounding factories and agricultural fields (<b>b</b>).</p>
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<p>The concentrations of elements in the snow at Anyang for all the samples (<b>a</b>) and for the sites near the factories versus the background farmlands (<b>b</b>). Note: from top to bottom, the three lines in the box plot indicate the upper quartile (Q3), median, and lower quartile (Q1), respectively, and the circular dots indicate outliers in the data, defined as values less than Q1 − 1.5 × IQR or greater than Q3 + 1.5 × IQR, with IQR being the interquartile spacing, the same as below.</p>
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<p>Enrichment factors of metal elements in snow.</p>
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<p>The spatial distribution of Cd concentrations across the entire area studied (<b>a</b>) and surrounding specific factories (<b>b</b>).</p>
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<p>A time series analysis of PM<sub>2.5</sub> and PM<sub>10</sub> (<b>a</b>) and a rose diagram of the wind direction and speed (<b>b</b>) in December in Anyang.</p>
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<p>The relationship between the concentration of Cd in snow and distance from the factories.</p>
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<p>A clustered tree map of the samples (<b>a</b>) and the spatial distribution of the sampling sites (<b>b</b>).</p>
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<p>The spatial distribution of Cd concentration in the snow versus PM<sub>2.5</sub> emissions (<b>a</b>) and the SO<sub>4</sub><sup>2−</sup> concentration in the snow versus the SO<sub>2</sub> satellite column concentration in the air (<b>b</b>).</p>
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<p>The correlation of Cd concentration with the production capacity (<b>a</b>) and total permitted emissions (<b>b</b>) of the factories. Note: the Cd concentration is the mean value across the two sampling sites closest to the emission sources along the upwind and downwind directions to each of the factories G, J, M, N and Q.</p>
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18 pages, 6401 KiB  
Article
Continuous Satellite Image Generation from Standard Layer Maps Using Conditional Generative Adversarial Networks
by Arminas Šidlauskas, Andrius Kriščiūnas and Dalia Čalnerytė
ISPRS Int. J. Geo-Inf. 2024, 13(12), 448; https://doi.org/10.3390/ijgi13120448 - 11 Dec 2024
Viewed by 900
Abstract
Satellite image generation has a wide range of applications. For example, parts of images must be restored in areas obscured by clouds or cloud shadows or areas that must be anonymized. The need to cover a large area with the generated images faces [...] Read more.
Satellite image generation has a wide range of applications. For example, parts of images must be restored in areas obscured by clouds or cloud shadows or areas that must be anonymized. The need to cover a large area with the generated images faces the challenge that separately generated images must maintain the structural and color continuity between the adjacent generated images as well as the actual ones. This study presents a modified architecture of the generative adversarial network (GAN) pix2pix that ensures the integrity of the generated remote sensing images. The pix2pix model comprises a U-Net generator and a PatchGAN discriminator. The generator was modified by expanding the input set with images representing the known parts of ground truth and the respective mask. Data used for the generative model consist of Sentinel-2 (S2) RGB satellite imagery as the target data and OpenStreetMap mapping data as the input. Since forested areas and fields dominate in images, a Kneedle clusterization method was applied to create datasets that better represent the other classes, such as buildings and roads. The original and updated models were trained on different datasets and their results were evaluated using gradient magnitude (GM), Fréchet inception distance (FID), structural similarity index measure (SSIM), and multiscale structural similarity index measure (MS-SSIM) metrics. The models with the updated architecture show improvement in gradient magnitude, SSIM, and MS-SSIM values for all datasets. The average GMs of the junction region and the full image are similar (do not exceed 7%) for the images generated using the modified architecture whereas it is more than 13% higher in the junction area for the images generated using the original architecture. The importance of class balancing is demonstrated by the fact that, for both architectures, models trained on the dataset with a higher ratio of classes representing buildings and roads compared to the models trained on the dataset without clusterization have more than 10% lower FID (162.673 to 190.036 for pix2pix and 173.408 to 195.621 for the modified architecture) and more than 5% higher SSIM (0.3532 to 0.3284 for pix2pix and 0.3575 to 0.3345 for the modified architecture) and MS-SSIM (0.3532 to 0.3284 for pix2pix and 0.3575 to 0.3345 for the modified architecture) values. Full article
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<p>Sentinel-2 study area raster after preprocessing, LKS-94 coordinate format.</p>
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<p>Study area raster of land type.</p>
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<p>Composition of 2 datasets. (<b>a</b>) Dataset 1 composed of standard OSM input and Sentinel-2 output. (<b>b</b>) Dataset 2 composed of OSM input, continuation mask that is taken from a real image, and generation mask that defines the generation boundaries with red being non-generated area and green as generated area.</p>
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<p>Example of a four-image generation for the capture of evaluation zone.</p>
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<p>Architectures of a generator: (<b>a</b>) denotes the standard U-Net architecture with skip connections; (<b>b</b>) denotes modified U-Net architecture, which takes in 3 different inputs, uses the additional inputs in the standard skip connection training in order to provide continuous generation, and additionally uses two extra inputs for locking in which areas the generator is supposed to generate and which are already complete.</p>
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<p>(<b>a</b>) Selection of optimal number of clusters (marked by the red dashed line) after applying Kneedle method, (<b>b</b>) Class distribution in different clusters, in addition to their sample sizes.</p>
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<p>Examples of clusters: (<b>a</b>–<b>c</b>)—data from cluster 1; (<b>d</b>–<b>f</b>)—data from cluster 2; (<b>g</b>–<b>i</b>)—data from cluster 3.</p>
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<p>Examples of clusters: (<b>a</b>–<b>c</b>)—data from cluster 1; (<b>d</b>–<b>f</b>)—data from cluster 2; (<b>g</b>–<b>i</b>)—data from cluster 3.</p>
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<p>Visualization of gradient magnitude evaluation: (<b>a</b>) Example of ground truth image; (<b>b</b>) Example of an image generated with pix2pix model; (<b>c</b>) Example of an image generated with pix2pix I7 model; (<b>d</b>) Zoomed-in junction area from (<b>b</b>) image bounded in green; (<b>e</b>) Zoomed-in junction area from (<b>c</b>) image bounded in green; (<b>f</b>) Example of input sketch image with mapping data; (<b>g</b>) Example of an image generated with pix2pix model illustrated with gradient magnitude filter; (<b>h</b>) Example of an image generated with pix2pix I7 model with gradient magnitude filter; (<b>i</b>) Zoomed-in junction area from (<b>g</b>) image bounded in green; (<b>j</b>) Zoomed-in junction area from (<b>j</b>) image bounded in green.</p>
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<p>Examples of images from specific datasets and the predictions of the respective models trained on them: (<b>a</b>) DS3 ground truth image; (<b>b</b>) DS3 input mask image; (<b>c</b>) DS3 pix2pix model generation on DS1; (<b>d</b>) DS3 pix2pix I7 model generation on DS3; (<b>e</b>) DS4 ground truth image; (<b>f</b>) DS4 input mask image; (<b>g</b>) DS4 pix2pix model generation on DS1; (<b>h</b>) DS4 pix2pix I7 model generation on DS4; (<b>i</b>) DS5 ground truth image; (<b>j</b>) DS5 input mask image; (<b>k</b>) DS5 pix2pix model generation on DS1; (<b>l</b>) DS5 pix2pix I7 model generation on DS5. In the mask images, green represents Forest, red represents Field, blue represents Water, cyan represents Road, yellow represents Building.</p>
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16 pages, 9943 KiB  
Article
Quantitative Characterization of Channel Morphology and Main Controlling Factor of Shallow Water Delta—A Case from Ganjiang Delta, Jiangxi, China
by Hao Cheng, Zhenkui Jin, Rukai Zhu and Jinyi Wang
Water 2024, 16(23), 3531; https://doi.org/10.3390/w16233531 - 8 Dec 2024
Viewed by 548
Abstract
(1) This paper selects the modern delta formed by the Ganjiang tributary in Poyang Lake. By performing high density statistical analysis of distribution channel parameters in the area using satellite images and geographic information processing software (LucaSpaceViewer 4.5.2, ArcGIS Pro 3.0.2, Global Mapper [...] Read more.
(1) This paper selects the modern delta formed by the Ganjiang tributary in Poyang Lake. By performing high density statistical analysis of distribution channel parameters in the area using satellite images and geographic information processing software (LucaSpaceViewer 4.5.2, ArcGIS Pro 3.0.2, Global Mapper v23.1), including length, width, bifurcation angle, bifurcation frequency, and channel sinuosity, the distribution characteristics of delta distribution channels are derived and quantitatively characterized. (2) Classification and evaluation of these characteristics are carried out using factor and cluster analysis, ultimately identifying controlling factors affecting the morphology and distribution of the distribution channels. By statistically analyzing the geometric and bifurcation data of the channels, factor and cluster analysis for data reduction and classification, the channel is finally divided into three categories: Type I channels have relatively high channel length, width, sinuosity, bending amplitude, and a lower bifurcation (or confluence) growth rate; Type II channels are characterized by low channel length, moderate channel width, low sinuosity, low bending amplitude, and a high bifurcation (or confluence) growth rate; Type III channels are defined by moderate channel length, low width, high sinuosity, high bending amplitude, and low bifurcation (or confluence) frequency. (3) After excluding the influence of other factors, it was found that the main controlling factor for the morphology of the Ganjiang Delta channel is flow velocity, which is influenced by changes in the terrain slope. Flow velocity directly affects channel sinuosity, bending amplitude, and bifurcation (or confluence) frequency, and indirectly affects channel length and width. Full article
(This article belongs to the Topic Advances in Hydrogeological Research)
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<p>Geographical Location of the Ganjiang Delta.</p>
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<p>Chart of Channel Distribution and Numbering in Ganjiang Delta.</p>
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<p>Quantitative statistical method for distribution channel morphology parameters. (<b>a</b>) Quantitative statistical method of channel liner length, actual length and channel width; (<b>b</b>) Quantitative statistical method of bifurcation Angle and bifurcation deflection Angle.</p>
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<p>Statistical method for bifurcation frequency (confluence) of distribution channels.</p>
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<p>R-type factor load matrix heatmap.</p>
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<p>Q-type coefficient score matrix heatmap. (AL: Actual Length; LL: Linear Length; CW: Channel Width; BA: Bending Amplitude; BD: Bending Degree).</p>
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<p>Channel parameter similarity coefficient classification dendrogram.</p>
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<p>Distribution channel morphology geometric data variation chart. (<b>a</b>) actual length; (<b>b</b>) channel width; (<b>c</b>) bending degree; (<b>d</b>) bending amplitude; (<b>e</b>) bifurcation angle; (<b>f</b>) deflection angle versus distance from origin.</p>
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<p>Channel Bifurcation Frequency and Confluence Frequency Variation Chart. Count of (<b>a</b>) bifurcation; (<b>b</b>) confluence versus distance from origin. (Orange area: Upper delta plain. Blue area: Lower delta plain. Dashed line: trend line of the value change. Solid line: indicator line of mean value).</p>
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<p>Factor, cluster analysis, and system tract partition diagram. (<b>AL</b>: Actual Length; <b>LL</b>: Linear Length; <b>CW</b>: Channel Width; <b>BA</b>: Bending Amplitude; <b>BD</b>: Bending Degree).</p>
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<p>Plots of (<b>a</b>) Actual Length versus Channel Width, (<b>b</b>) Actual Length versus Bending Degree, (<b>c</b>) Actual Length versus Bending Amplitude, (<b>d</b>) Channel Width versus Bending Degree, (<b>e</b>) Channel Width versus Bending Amplitude, (<b>f</b>) Bending Degree versus Bending Amplitude.</p>
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<p>Elevation variation map of the middle distribution of Ganjiang River.</p>
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26 pages, 23951 KiB  
Article
Development of Methods for Satellite Shoreline Detection and Monitoring of Megacusp Undulations
by Riccardo Angelini, Eduard Angelats, Guido Luzi, Andrea Masiero, Gonzalo Simarro and Francesca Ribas
Remote Sens. 2024, 16(23), 4553; https://doi.org/10.3390/rs16234553 - 4 Dec 2024
Viewed by 724
Abstract
Coastal zones, particularly sandy beaches, are highly dynamic environments subject to a variety of natural and anthropogenic forcings. Instantaneous shoreline is a widely used indicator of beach changes in image-based applications, and it can display undulations at different spatial and temporal scales. Megacusps, [...] Read more.
Coastal zones, particularly sandy beaches, are highly dynamic environments subject to a variety of natural and anthropogenic forcings. Instantaneous shoreline is a widely used indicator of beach changes in image-based applications, and it can display undulations at different spatial and temporal scales. Megacusps, periodic seaward and landward shoreline perturbations, are an example of such undulations that can significantly modify beach width and impact its usability. Traditionally, the study of these phenomena relied on video monitoring systems, which provide high-frequency imagery but limited spatial coverage. Instead, this study explored the potential of employing multispectral satellite-derived shorelines, specifically from Sentinel-2 (S2) and PlanetScope (PLN) platforms, for characterizing and monitoring megacusps’ formation and their dynamics over time. First, a tool was developed and validated to guarantee accurate shoreline detection, based on a combination of spectral indices, along with both thresholding and unsupervised clustering techniques. Validation of this shoreline detection phase was performed on three micro-tidal Mediterranean beaches, comparing with high-resolution orthomosaics and in-situ GNSS data, obtaining a good subpixel accuracy (with a mean absolute deviation of 1.5–5.5 m depending on the satellite type). Second, a tool for megacusp characterization was implemented and subsequent validation with reference data proved that satellite-derived shorelines could be used to robustly and accurately describe megacusps. The methodology could not only capture their amplitude and wavelength (of the order of 10 and 100 m, respectively) but also monitor their weekly–daily evolution using different potential metrics, thanks to combining S2 and PLN imagery. Our findings demonstrate that multispectral satellite imagery provides a viable and scalable solution for monitoring shoreline megacusp undulations, enhancing our understanding and offering an interesting option for coastal management. Full article
(This article belongs to the Section Environmental Remote Sensing)
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<p>Study areas: (<b>a</b>) Southern Llobregat Delta (SLD) coast (Spain), (<b>b</b>) Northern Ombrone Delta (NOD) coast (Italy) and Feniglia beach (FNG) (Italy). The position of wave buoys and tide gauges is also shown. The coordinate reference system is WGS84.</p>
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<p>Exampleof the shoreline extraction method with S2 data: (<b>a</b>) raster file of the spectral index (NDWI), (<b>b</b>) binarization of the image with K-means, (<b>c</b>) contour extraction, (<b>d</b>) comparison between the reference shoreline and the detected one, and (<b>e</b>) validation by using the baseline and transect method.</p>
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<p>Workflow of the shoreline extraction tool and of the megacusp characterization tool.</p>
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<p>Examples of the shoreline detection phase. Results of the best index-method combination for S2 and PLN compared with the reference, for (<b>a</b>) the SLD coast (23 May 2019), (<b>b</b>) FNG beach (20 July 2021), and (<b>c</b>) the NOD coast (20 July 2021). In the background, orthomosaics closest to the satellite overpass dates are displayed for each beach.</p>
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<p>First segment of May 2017 used for the validation phase. (<b>a</b>) On top, the four lines correspond to the shorelines of the reference case (green), the best method–index combination in S2 data (GMM–NDWI, orange), the best method–index combination in PLN data (K-means–NIR, grey), and the CoastSat tool (blue). (<b>b</b>) At the bottom, with the same color, the detrended lines show the automatic peaks (red square) and valleys (green dot) for each detected megacusp. The numbers refer to the megacusp embayments that are visible in the orthomosaic. The <span class="html-italic">x</span>-axis is set to zero at the starting point of the segment.</p>
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<p>Second segment of May 2019 used for the validation phase. (<b>a</b>) On top, the four lines present the shorelines of the reference case (green), the best method–index combination in S2 data (GMM–NDWI, orange), the best method–index combination in PLN data (K-means–NIR, grey), and the CoastSat tool (blue). (<b>b</b>) On the bottom, with the same color, the detrended lines show the automatically detected peaks (red square) and valleys (green dot) for each megacusp. The numbers enumerate the megacusp embayments that are visible in the orthomosaic. The <span class="html-italic">x</span>-axis is set to zero at the starting point of the segment.</p>
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<p>Time series of the megacusp event in the SLD coast in 2023. On the left, Sentinel-2 images in the period between March and October 2023. On the right, the time series enriched by adding PlanetScope images during the peak of the event (May–June 2023).</p>
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<p>Results of the 2023 megacusp event in the SLD coast with the corresponding wave conditions. Time series of (<b>a</b>) significant wave height (<math display="inline"><semantics> <msub> <mi>H</mi> <mi>s</mi> </msub> </semantics></math>), (<b>b</b>) peak wave period (<math display="inline"><semantics> <msub> <mi>T</mi> <mi>p</mi> </msub> </semantics></math>), (<b>c</b>) direction of wave incidence with respect to the north (<math display="inline"><semantics> <mi>θ</mi> </semantics></math>), (<b>d</b>) sinuosity (<span class="html-italic">s</span>), (<b>e</b>) shoreline standard deviation (<math display="inline"><semantics> <msub> <mi>σ</mi> <mi>s</mi> </msub> </semantics></math>), (<b>f</b>) mean megacusp amplitude (<math display="inline"><semantics> <mover> <mi>a</mi> <mo>¯</mo> </mover> </semantics></math>), and (<b>g</b>) mean megacusp wavelength (<math display="inline"><semantics> <mover> <mi>λ</mi> <mo>¯</mo> </mover> </semantics></math>) are shown.</p>
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<p>Time series of the megacusp event in FNG beach in 2022. On the left, Sentinel-2 images in the period between February and June 2022. On the right, the time series enriched by adding PlanetScope images at the peak of the event (March 2022).</p>
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<p>Results of the 2022 megacusp event in FNG beach with the corresponding wave conditions. Time series of (<b>a</b>) significant wave height (<math display="inline"><semantics> <msub> <mi>H</mi> <mi>s</mi> </msub> </semantics></math>), (<b>b</b>) peak wave period (<math display="inline"><semantics> <msub> <mi>T</mi> <mi>p</mi> </msub> </semantics></math>), (<b>c</b>) direction of wave incidence to north (<math display="inline"><semantics> <mi>θ</mi> </semantics></math>), (<b>d</b>) sinuosity (<span class="html-italic">s</span>), (<b>e</b>) shoreline standard deviation (<math display="inline"><semantics> <msub> <mi>σ</mi> <mi>s</mi> </msub> </semantics></math>), (<b>f</b>) mean megacusp amplitude (<math display="inline"><semantics> <mover> <mi>a</mi> <mo>¯</mo> </mover> </semantics></math>), and (<b>g</b>) mean megacusp wavelength (<math display="inline"><semantics> <mover> <mi>λ</mi> <mo>¯</mo> </mover> </semantics></math>) are shown.</p>
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<p>Results of the 2022 megacusp event in FNG beach with the corresponding wave conditions. Time series of (<b>a</b>) significant wave height (<math display="inline"><semantics> <msub> <mi>H</mi> <mi>s</mi> </msub> </semantics></math>), (<b>b</b>) peak wave period (<math display="inline"><semantics> <msub> <mi>T</mi> <mi>p</mi> </msub> </semantics></math>), (<b>c</b>) direction of wave incidence to north (<math display="inline"><semantics> <mi>θ</mi> </semantics></math>), (<b>d</b>) sinuosity (<span class="html-italic">s</span>), (<b>e</b>) shoreline standard deviation (<math display="inline"><semantics> <msub> <mi>σ</mi> <mi>s</mi> </msub> </semantics></math>), (<b>f</b>) mean megacusp amplitude (<math display="inline"><semantics> <mover> <mi>a</mi> <mo>¯</mo> </mover> </semantics></math>), and (<b>g</b>) mean megacusp wavelength (<math display="inline"><semantics> <mover> <mi>λ</mi> <mo>¯</mo> </mover> </semantics></math>) are shown.</p>
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