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Search Results (10,321)

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16 pages, 1315 KiB  
Article
Growth Ring and Its Climatic Signal on Shrub Species of the Semi-Desert Area in the Northern Foot of Yinshan Mountain, Inner Mongolia, China
by Zhenyu Yao, Zongshan Li, Shaoteng Chen, Jianying Guo and Yihe Lv
Forests 2025, 16(2), 379; https://doi.org/10.3390/f16020379 - 19 Feb 2025
Abstract
Desert and semi-desert ecosystems cover a large proportion of global land area, but their tree-ring materials had traditionally been studied less intensively than that of forest ecosystems. In this study, we presented the time series of growth rings from eight typical shrub species [...] Read more.
Desert and semi-desert ecosystems cover a large proportion of global land area, but their tree-ring materials had traditionally been studied less intensively than that of forest ecosystems. In this study, we presented the time series of growth rings from eight typical shrub species of the semi-desert region in the northern foot of Yinshan Mountain, Inner Mongolia, China. The results showed that all those shrub species had recognizably demarcated annual rings of main stems, and tree-ring chronologies could been constructed successfully. The climate-growth analysis indicated that the chronologies was positively correlated with precipitation and PDSI but negatively correlated with temperature variables, indicating that drought stress had primary importance in the control of the relative ring width from year to year for those shrub species. Interestingly, the annual growth rate of those shrub species had no noticeable downward trend in recent decades, indicating that shrub growth had not negatively impacted the recently developed warm–dry climate in the sample sites. Our results provide evidence that growth rings in the main stems of shrub species in the northern foot of Yinshan Mountain should be a reliable proxy of annual fluctuation in the semi-desert environment of China. Full article
19 pages, 7319 KiB  
Article
A Dual-Branch U-Net for Staple Crop Classification in Complex Scenes
by Jiajin Zhang, Lifang Zhao and Hua Yang
Remote Sens. 2025, 17(4), 726; https://doi.org/10.3390/rs17040726 - 19 Feb 2025
Abstract
Accurate information on crop planting and spatial distribution is critical for understanding and tracking long-term land use changes. The method of using deep learning (DL) to extract crop information has been applied in large-scale datasets and plain areas. However, current crop classification methods [...] Read more.
Accurate information on crop planting and spatial distribution is critical for understanding and tracking long-term land use changes. The method of using deep learning (DL) to extract crop information has been applied in large-scale datasets and plain areas. However, current crop classification methods face some challenges, such as poor image time continuity, difficult data acquisition, rugged terrain, fragmented plots, and diverse planting conditions in complex scenes. In this study, we propose the Complex Scene Crop Classification U-Net (CSCCU), which aims to improve the mapping accuracy of staple crops in complex scenes by combining multi-spectral bands with spectral features. CSCCU features a dual-branch structure: the main branch concentrates on image feature extraction, while the auxiliary branch focuses on spectral features. In our method, we use the hierarchical feature-level fusion mechanism. Through the hierarchical feature fusion of the shallow feature fusion module (SFF) and the deep feature fusion module (DFF), feature learning is optimized and model performance is improved. We conducted experiments using GaoFen-2 (GF-2) images in Xiuwen County, Guizhou Province, China, and established a dataset consisting of 1000 image patches of size 256, covering seven categories. In our method, the corn and rice accuracies are 89.72% and 88.61%, and the mean intersection over union (mIoU) is 85.61%, which is higher than the compared models (U-Net, SegNet, and DeepLabv3+). Our method provides a novel solution for the classification of staple crops in complex scenes using high-resolution images, which can help to obtain accurate information on staple crops in larger regions in the future. Full article
25 pages, 25542 KiB  
Article
Automatic Mapping of 10 m Tropical Evergreen Forest Cover in Central African Republic with Sentinel-2 Dynamic World Dataset
by Wenqiong Zhao, Xinyan Zhong, Xiaodong Li, Xia Wang, Yun Du and Yihang Zhang
Remote Sens. 2025, 17(4), 722; https://doi.org/10.3390/rs17040722 - 19 Feb 2025
Abstract
Tropical evergreen forests represent the richest biodiversity in terrestrial ecosystems, and the fine spatial-temporal resolution mapping of these forests is essential for the study and conservation of this vital natural resource. The current methods for mapping tropical evergreen forests frequently exhibit coarse spatial [...] Read more.
Tropical evergreen forests represent the richest biodiversity in terrestrial ecosystems, and the fine spatial-temporal resolution mapping of these forests is essential for the study and conservation of this vital natural resource. The current methods for mapping tropical evergreen forests frequently exhibit coarse spatial resolution and lengthy production cycles. This can be attributed to the inherent challenges associated with monitoring diverse surface changes and the persistence of cloudy, rainy conditions in the tropics. We propose a novel approach to automatically map annual 10 m tropical evergreen forest covers from 2017 to 2023 with the Sentinel-2 Dynamic World dataset in the biodiversity-rich and conservation-sensitive Central African Republic (CAR). The Copernicus Global Land Cover Layers (CGLC) and Global Forest Change (GFC) products were used first to track stable evergreen forest samples. Then, initial evergreen forest cover maps were generated by determining the threshold of evergreen forest cover for each of the yearly median forest cover probability maps. From 2017 to 2023, the annual modified 10 m tropical evergreen forest cover maps were finally produced from the initial evergreen forest cover maps and NEFI (Non-Evergreen Forest Index) images with the estimated thresholds. The results produced by the proposed method achieved an overall accuracy of >94.10% and a Cohen’s Kappa of >87.63% across all years (F1-Score > 94.05%), which represents a significant improvement over the performance of previous methods, including the CGLC evergreen forest cover maps and yearly median forest cover probability maps based on Sentinel-2 Dynamic World. Our findings demonstrate that the proposed method provides detailed spatial characteristics of evergreen forests and time-series change in the Central African Republic, with substantial consistency across all years. Full article
(This article belongs to the Section Forest Remote Sensing)
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Figure 1

Figure 1
<p>Study site and dataset. (<b>a</b>) Geolocation of the Central African Republic in Africa, evergreen forest sourced from CGLS-LC100 land cover map in 2019; (<b>b</b>) Zoomed CGLS-LC100 land cover map in 2019, highlighting the classification for evergreen forest only, from this dataset; (<b>c</b>) Monthly dynamics of the forest cover possibilities in the Sentinel-2 Dynamic World dataset, in which A, B and C refer to typical evergreen forest, and D, E and F refer to non-forest or non-evergreen forest samples. These six samples were selected in the free-clouds area of the monthly Sentinel-2 Dynamic World images in 2020.</p>
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<p>Flowchart of the proposed method.</p>
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<p>Monthly and yearly median forest cover probability maps in the Central African Republic based on Sentinel-2 near real-time Dynamic World data in 2020. The red box in January denotes the zoomed area in the following <a href="#remotesensing-17-00722-f004" class="html-fig">Figure 4</a>.</p>
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<p>The subarea of monthly and yearly median forest cover probability maps in <a href="#remotesensing-17-00722-f003" class="html-fig">Figure 3</a> based on Sentinel-2 near real-time Dynamic World data in 2020.</p>
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<p>Evergreen forest cover sample points in the Dynamic World forest cover probability map and the NEFI image. (<b>a</b>) Evergreen forest cover sample points in the Dynamic World forest cover probability map of 2020; (<b>b</b>) Evergreen forest cover sample points in the Non-Evergreen Forest Index (NEFI) image of 2020; (<b>c</b>) Statistical histogram of evergreen forest cover sample points in the forest cover probability map; (<b>d</b>) Statistical histogram of evergreen forest cover sample points in the NEFI image.</p>
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<p>Evergreen forest cover maps for different products and methods. (<b>a</b>) CGLS-LC100 evergreen forest cover map in the year of 2020; (<b>b</b>) Evergreen forest cover map generated from yearly median Dynamic World forest cover probability in 2020 only using threshold T1, filtered by GFC; (<b>c</b>) Modified evergreen forest cover map in the year of 2020. The Subarea 1 and Subarea 2 show two zoomed areas in (<b>a</b>–<b>c</b>) and the corresponding Google Earth RGB images, of which the acquisition times are 23 January 2014 for Subarea 1 and 29 July 2012 for Subarea 2.</p>
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<p>Annual evergreen forest cover maps for different years from 2017 to 2023 produced by the proposed method. Subarea 1 and Subarea 2 show zoomed maps of localized evergreen forest cover by year with the Google Earth image for reference.</p>
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<p>Evergreen forest cover change maps for different years from 2017 to 2023. (<b>a</b>) Annual evergreen forest cover decreases year map from 2018 to 2023 (red labeling); (<b>b</b>) Annual evergreen forest cover increases year map from 2018 to 2023 (green labeling). The different shaded colors indicate the year in which the first increase and decrease occurred for baseline evergreen forests in 2017. Four columns of southeastern, central-south, central, and southwestern, showing annual evergreen forest cover decreases and increases, respectively aligning with the red box in (<b>a</b>,<b>b</b>).</p>
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<p>Frequency map of evergreen forest cover maps for different years from 2017 to 2023. Label numbers represent the frequency of occurrences of evergreen forest cover at pixel scale.</p>
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<p>Comparison of evergreen forest cover mapping with different composites of yearly median and mean Dynamic World Sentinel-2 forest cover probability images. (<b>a</b>) Evergreen forest cover map using mean composite; (<b>b</b>) Evergreen forest cover map using median composite; (<b>c</b>) Dynamic World forest cover probability median map; (<b>d</b>) RGB Google Earth imagery. (<b>e</b>) Overall accuracy assessments of evergreen forest cover maps produced from yearly mean, median, and integration of yearly mean and NEFI image composites in the year of 2020.</p>
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32 pages, 1118 KiB  
Article
Assessment of Chemical Pollution Load in Surface Waters of the Turkestan Region and Its Indirect Impact on Landscapes: A Comprehensive Study
by Dana Akhmetova, Zhanar Ozgeldinova, Nurgul Ramazanova, Saltanat Sadvakassova, Zhansulu Inkarova, Rabiga Kenzhebay, Zhadra Shingisbayeva, Roza Abildaeva, Zakhida Kozhabekova, Manira Alagujayeva and Zhamila Sikhynbayeva
Geosciences 2025, 15(2), 73; https://doi.org/10.3390/geosciences15020073 - 19 Feb 2025
Abstract
This study is aimed at a comprehensive assessment of the chemical composition of surface waters in the Turkestan region and their impact on regional landscapes. The primary objective of the research is to systematically evaluate the level of chemical pollution in the region’s [...] Read more.
This study is aimed at a comprehensive assessment of the chemical composition of surface waters in the Turkestan region and their impact on regional landscapes. The primary objective of the research is to systematically evaluate the level of chemical pollution in the region’s water resources and determine its indirect effects on landscape-ecological stability. In August 2024, water samples from eight sampling points (S1–S8) were analyzed for 24 physicochemical parameters, including total hardness (mg*eq/L), pH, dry residue (mg/L), electrical conductivity (µS/cm), total salinity (mg/L), Al, As, B, Ca, Cd, Co, Cr, Ti, Fe, Pb, Cu, Mg, K, Mn, Na, Ni, Zn, SO₄²⁻, and C₆H₅OH. To determine the degree of pollution, variational-statistical analysis, principal component analysis (PCA), as well as the calculation of the OIP, NPI, and HPI indices were performed. For land use and land cover change (LULC) analysis, LULC classification was carried out based on Landsat data from 2000 to 2020, forming the basis for land resource management and planning. The research results showed a deterioration in the ecological condition of water resources and an increasing anthropogenic impact. Specifically, at point S8, the concentration of Al was found to be 56 times higher than the maximum allowable limit, while the concentration of Fe was 42 times higher. High levels of pollution were also recorded at points S1, S4, S5, and S6, where the increase in Al and Na concentrations caused a sharp rise in the OIP value. The main factors influencing water pollution include industrial effluents, agricultural waste, and irrigation drainage waters. The pollution’s negative impact on regional landscapes has led to issues related to the distribution of vegetation, soil fertility, and landscape stability. To improve the current ecological situation and restore natural balance, the phytoremediation method is proposed. The research results will serve as the foundation for developing water resource management strategies for the Turkestan region and making informed decisions aimed at ensuring ecological sustainability. Full article
(This article belongs to the Section Geochemistry)
23 pages, 10921 KiB  
Article
A Weakly Supervised and Self-Supervised Learning Approach for Semantic Segmentation of Land Cover in Satellite Images with National Forest Inventory Data
by Daniel Moraes, Manuel L. Campagnolo and Mário Caetano
Remote Sens. 2025, 17(4), 711; https://doi.org/10.3390/rs17040711 - 19 Feb 2025
Abstract
National Forest Inventories (NFIs) provide valuable land cover (LC) information but often lack spatial continuity and an adequate update frequency. Satellite-based remote sensing offers a viable alternative, employing machine learning to extract thematic data. State-of-the-art methods such as convolutional neural networks rely on [...] Read more.
National Forest Inventories (NFIs) provide valuable land cover (LC) information but often lack spatial continuity and an adequate update frequency. Satellite-based remote sensing offers a viable alternative, employing machine learning to extract thematic data. State-of-the-art methods such as convolutional neural networks rely on fully pixel-level annotated images, which are difficult to obtain. Although reference LC datasets have been widely used to derive annotations, NFIs consist of point-based data, providing only sparse annotations. Weakly supervised and self-supervised learning approaches help address this issue by reducing dependence on fully annotated images and leveraging unlabeled data. However, their potential for large-scale LC mapping needs further investigation. This study explored the use of NFI data with deep learning and weakly supervised and self-supervised methods. Using Sentinel-2 images and the Portuguese NFI, which covers other LC types beyond forest, as sparse labels, we performed weakly supervised semantic segmentation with a convolutional neural network to create an updated and spatially continuous national LC map. Additionally, we investigated the potential of self-supervised learning by pretraining a masked autoencoder on 65,000 Sentinel-2 image chips and then fine-tuning the model with NFI-derived sparse labels. The weakly supervised baseline achieved a validation accuracy of 69.60%, surpassing Random Forest (67.90%). The self-supervised model achieved 71.29%, performing on par with the baseline using half the training data. The results demonstrated that integrating both learning approaches enabled successful countrywide LC mapping with limited training data. Full article
(This article belongs to the Section Earth Observation Data)
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Figure 1

Figure 1
<p>Study area and location of sample areas used for model training and validation.</p>
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<p>Example of NFI photo-points: (<b>a</b>) with matching point-patch labels; (<b>b</b>) located at the interface between distinct land covers; and (<b>c</b>) with mismatching point-patch labels.</p>
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<p>Illustration of distinctly labeled training data. High-resolution image (<b>a</b>), dense labels used in typical fully supervised methods (<b>b</b>) and sparse labels used in our weakly supervised approach (<b>c</b>). Colored and grey pixels correspond to labeled and unlabeled pixels, respectively. The labels in (<b>c</b>) are derived from the photo-point, seen in the center of the 3 × 3 window.</p>
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<p>Network architecture of our ConvNext-V2 Atto U-Net. The figure also exhibits the ConvNext-V2 block. LN, GRN and GELU stand for Layer Normalization, Global Response Normalization and Gaussian Error Linear Unit, respectively. Conv K × K refers to a convolutional layer with a kernel size of K × K.</p>
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<p>MAE architecture, illustrating the reconstruction of masked patches. Image representations learned at the encoder can be transferred and applied to different downstream tasks. Each patch corresponds to 8 × 8 pixels.</p>
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<p>Overall accuracy of the baseline and self-supervised pretrained models. The values represent the average of 10 runs with a 95% confidence interval and were computed on the validation split.</p>
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<p>Validation split accuracy of the three tested models with distinct training set sizes. The reported values are the average of 10 runs with a 95% confidence interval.</p>
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<p>Model performance per land cover class measured by the F1-score. For other coniferous, no F1-score was reported for Random Forest, as the model did not predict any sampling units belonging to this class.</p>
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<p>Example of land cover maps produced by Random Forest, ConvNext-V2 baseline and ConvNext-V2 self-supervised pretrained models.</p>
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<p>Land cover map of Portugal (2023).</p>
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<p>Example of 30 × 30 m windows used for training a Random Forest classifier for the homogeneity filter. Annotations as non-homogeneous or homogeneous considered not only the high-resolution images (seen in the figure) but also Sentinel-2 images.</p>
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23 pages, 16814 KiB  
Article
A New Method for Automatic Glacier Extraction by Building Decision Trees Based on Pixel Statistics
by Xiao Liu, Hongyi Cheng, Jiang Liu, Xianbao Su, Yuchen Wang, Bin Qiao, Yipeng Wang and Nai’ang Wang
Remote Sens. 2025, 17(4), 710; https://doi.org/10.3390/rs17040710 - 19 Feb 2025
Abstract
Automatic glacier extraction from remote sensing images is the most important approach for large scale glacier monitoring. Commonly used band calculation indices to enhance glacier information are not effective in identifying shadowed glaciers and debris-covered glaciers. In this study, we used the Kolmogorov–Smirnov [...] Read more.
Automatic glacier extraction from remote sensing images is the most important approach for large scale glacier monitoring. Commonly used band calculation indices to enhance glacier information are not effective in identifying shadowed glaciers and debris-covered glaciers. In this study, we used the Kolmogorov–Smirnov test as the theoretical basis and determined the most suitable band calculation indices to distinguish different land cover classes by comparing inter-sample separability and reasonable threshold range ratios of different indices. We then constructed a glacier classification decision tree. This approach resulted in the development of a method to automatically extract glacier areas at given spatial and temporal scales. In comparison with the commonly used indices, this method demonstrates an improvement in Cohen’s kappa coefficient by more than 3.8%. Notably, the accuracy for shadowed glaciers and debris-covered glaciers, which are prone to misclassification, is substantially enhanced by 108.0% and 6.3%, respectively. By testing the method in the Qilian Mountains, the positive prediction value of glacier extraction was calculated to be 91.8%, the true positive rate was 94.0%, and Cohen’s kappa coefficient was 0.924, making it well suited for glacier extraction. This method can be used for monitoring glacier changes in global mountainous regions, and provide support for climate change research, water resource management, and disaster early warning systems. Full article
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Figure 1
<p>Distribution of mountains where the sampling sites are located.</p>
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<p>Distribution of spectral digital numbers (DNs) from seven land cover samples. The colored dot indicates the DNs in the land cover sample that was stretched to its maximum value during image pre-processing.</p>
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<p>The conceptual model diagram for land cover classification evaluation metrics.</p>
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<p>Cumulative distribution functions for <math display="inline"><semantics> <mrow> <mi>S</mi> <mi>W</mi> <mi>I</mi> <mi>R</mi> <mn>1</mn> <mo>−</mo> <mi>S</mi> <mi>W</mi> <mi>I</mi> <mi>R</mi> <mn>2</mn> </mrow> </semantics></math> (<b>a</b>,<b>b</b>), <math display="inline"><semantics> <mrow> <mi>B</mi> <mi>l</mi> <mi>u</mi> <mi>e</mi> <mo>−</mo> <mi>S</mi> <mi>W</mi> <mi>I</mi> <mi>R</mi> <mn>2</mn> </mrow> </semantics></math> (<b>c</b>,<b>d</b>), <math display="inline"><semantics> <mrow> <mi>S</mi> <mi>T</mi> <mo>−</mo> <mi>B</mi> <mi>l</mi> <mi>u</mi> <mi>e</mi> </mrow> </semantics></math> (<b>e</b>,<b>f</b>) and <math display="inline"><semantics> <mrow> <mrow> <mrow> <mi>R</mi> <mi>e</mi> <mi>d</mi> </mrow> <mo>/</mo> <mrow> <mi>S</mi> <mi>W</mi> <mi>I</mi> <mi>R</mi> <mn>1</mn> </mrow> </mrow> </mrow> </semantics></math> (<b>g</b>,<b>h</b>) in Landsat 8 (<b>a</b>,<b>c</b>,<b>e</b>,<b>g</b>) and 5 (<b>b</b>,<b>d</b>,<b>f</b>,<b>h</b>). The red dotted line is the threshold determined in this study.</p>
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<p>Decision tree for remote sensing image pixel classification (<b>a</b>) and schematic diagram of glacier extraction multi-temporal algorithm (<b>b</b>). Thresholds for Landsat 8 images are shown outside of parentheses, and thresholds for Landsat 5 images are shown in parentheses.</p>
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<p>Glacier area in the Qilian Mountains. The blue area shows the glacier area in the Qilian Mountains from 2013 to 2017 extracted using this method, the thin line shows the glacier distribution data in 2015, and the brightness of the background color indicates the number of images participating in the calculation at that location. (<b>a</b>–<b>d</b>) represent four different regions in the Qilian Mountains.</p>
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<p>ROC curves of the results of glacier extraction using four methods. The red line shows the ROC curves of the methods in this study, and the gray line shows the other three methods. (<b>b</b>) shows a local zoom of (<b>a</b>).</p>
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<p>Comparison of glacier extraction results from four methods. The red line represents the RGI data, and the blue areas indicate the extracted glacier results.</p>
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15 pages, 9545 KiB  
Proceeding Paper
Origami-Inspired Photovoltaic Modules—Development of Ecofriendly Solutions for Naval and Mining Operations
by Enrique Pujada-Gamarra, Daniel Lavayen-Farfán, Davy Olivera-Oliva and Jorge Rodríguez-Hernández
Eng. Proc. 2025, 83(1), 26; https://doi.org/10.3390/engproc2025083026 - 19 Feb 2025
Abstract
In recent years, ecofriendly and renewable energy solutions have gained relevance mainly to lessen the effects of climate change. Governments and companies across the world have commitments to reduce fuel consumption and emissions as part of the 2030 Sustainable Development Goals. Solar energy [...] Read more.
In recent years, ecofriendly and renewable energy solutions have gained relevance mainly to lessen the effects of climate change. Governments and companies across the world have commitments to reduce fuel consumption and emissions as part of the 2030 Sustainable Development Goals. Solar energy systems have great importance as a renewable energy source; however, they often have large space requirements to be effective, e.g., large areas covered by solar panels, as well as low efficiency and strong dependance on the weather. On the other hand, origami, the art of folding paper, can be a source of inspiration for new technologies and solutions for modern problems. In this paper, origami-inspired solar panels are presented as a potential solution for naval and mining operations. Prototype panels are manufactured based on the Miura-Ori pattern. Using this pattern, the photovoltaic modules can be folded by just one movement, thus reducing their footprint by up to 90%. The prototype photovoltaic modules are then tested on land and on board a vessel, where their efficiency and resistance can be tested. It is shown that naval and mining operations, where fuel consumption can be extremely high and available space is a major constraint, benefit greatly from this kind of development. Full article
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Figure 1

Figure 1
<p>Miura-Ori pattern for a solar panel array. (<b>a</b>) Unfolded pattern; (<b>b</b>) folded pattern.</p>
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<p>Multiple applications of the Miura-Ori pattern. (<b>a</b>) Foldable bean leaves [<a href="#B4-engproc-83-00026" class="html-bibr">4</a>]; (<b>b</b>) foldable panels inspired on the bean leaves [<a href="#B4-engproc-83-00026" class="html-bibr">4</a>]; (<b>c</b>,<b>d</b>) foldable bullet resistant police shields [<a href="#B5-engproc-83-00026" class="html-bibr">5</a>]; (<b>e</b>,<b>f</b>) foldable solar panels for space applications [<a href="#B7-engproc-83-00026" class="html-bibr">7</a>]; (<b>g</b>,<b>h</b>) foldable and deployable solar panels [<a href="#B6-engproc-83-00026" class="html-bibr">6</a>].</p>
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<p>Multiple research related to thick origami: (<b>a</b>,<b>b</b>) analyses of self-intersection in thick-origami [<a href="#B8-engproc-83-00026" class="html-bibr">8</a>]; (<b>c</b>,<b>d</b>) foldable thick origami patent [<a href="#B9-engproc-83-00026" class="html-bibr">9</a>]; (<b>e</b>,<b>f</b>) thick origami crease proposals [<a href="#B10-engproc-83-00026" class="html-bibr">10</a>]; (<b>g</b>,<b>h</b>) development of offset linkages as hinges for thick origami [<a href="#B11-engproc-83-00026" class="html-bibr">11</a>].</p>
Full article ">Figure 3 Cont.
<p>Multiple research related to thick origami: (<b>a</b>,<b>b</b>) analyses of self-intersection in thick-origami [<a href="#B8-engproc-83-00026" class="html-bibr">8</a>]; (<b>c</b>,<b>d</b>) foldable thick origami patent [<a href="#B9-engproc-83-00026" class="html-bibr">9</a>]; (<b>e</b>,<b>f</b>) thick origami crease proposals [<a href="#B10-engproc-83-00026" class="html-bibr">10</a>]; (<b>g</b>,<b>h</b>) development of offset linkages as hinges for thick origami [<a href="#B11-engproc-83-00026" class="html-bibr">11</a>].</p>
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<p>Basic folding unit—degree-4 vertex. Source: [<a href="#B12-engproc-83-00026" class="html-bibr">12</a>].</p>
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<p>General dimensions and scheme of the proposed pattern for solar panels. (<b>a</b>) Dimensions of proposal panel (<b>b</b>) Movement behavior showing displacement through the major fold angle axes.</p>
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<p>(<b>a</b>) Folding angles and (<b>b</b>) minimum distance along the major fold angle as a function of the ruling angle.</p>
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<p>Paper origami with different configurations of the Miura-Ori fold. (<b>a</b>) Miura-Ori unfolding and (<b>b</b>) folding.</p>
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<p>Prototype of the elected configuration on cardboard. (<b>a</b>) Unfolded; (<b>b</b>) mid-fold; (<b>c</b>) completely folded.</p>
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<p>Layout of the solar cells in the Miura-Ori pattern.</p>
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<p>Several six-cell prototypes used for testing.</p>
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<p>Diagram of the full-scale prototype. (<b>a</b>) Unfolded; (<b>b</b>) folded.</p>
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<p>Manufacturing of the full-scale prototypes on the lamination table. (<b>a</b>) Solar Cells connection and (<b>b</b>) Layers alignment.</p>
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<p>Finalized prototype on the lamination table.</p>
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<p>Folding and unfolding tests of the six-cell prototypes. (<b>a</b>) Unfolded panel; (<b>b</b>) mid-fold panel; (<b>c</b>) folded panel.</p>
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<p>Transportation of the prototypes to the boat. (<b>a</b>) Unfolded panel before transportation, (<b>b</b>) Folding process and (<b>c</b>) ordering the solar panel inside the car. (<b>d</b>) Showing the folded solar in the port before (<b>e</b>,<b>f</b>) being transported in a boat, demonstrating the advantages of the volume reduction.</p>
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<p>Installation of full-size solar prototypes on vessel. (<b>a</b>) Unfolded and (<b>b</b>) folded status of the solar panel installed on the vessel.</p>
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26 pages, 8496 KiB  
Article
Land Degraded by Gold Mining in the Ecuadorian Amazon: A Proposal for Boosting Ecosystem Restoration Through Induced Revegetation
by Fiodor N. Mena-Quintana, Willin Álvarez, Wilfredo Franco, Luis Moncayo, Myriam Tipán and Jholaus Ayala
Forests 2025, 16(2), 372; https://doi.org/10.3390/f16020372 - 19 Feb 2025
Viewed by 38
Abstract
Deforestation caused by gold mining in the Ecuadorian Amazon has increased by 300% in the last decade, leading to severe environmental degradation of water and land resources. Effective remediation and revegetation technologies are still needed to address this issue. This study aimed to [...] Read more.
Deforestation caused by gold mining in the Ecuadorian Amazon has increased by 300% in the last decade, leading to severe environmental degradation of water and land resources. Effective remediation and revegetation technologies are still needed to address this issue. This study aimed to foster revegetation on 0.5 hectares of degraded land in Naranjalito, a mining site in the Ecuadorian Amazon, by applying plant-based biocompost and biochar and planting Ochroma pyramidale and Arachis pintoi, two pioneer species. The project’s objective was to evaluate the impact of these treatments on vegetation cover recovery through physicochemical and microbiological improvements in the soil. Four blocks and sixteen experimental plots were established: eight plots received treatments with varying doses of biocompost+biol (BIOC), four plots included plantations without biocompost (Not-BIOC), and four served as control plots (bare land). Over six months, dasometric characteristics of O. pyramidale and the expansion of A. pintoi were recorded. The data were analyzed using multivariate methods. The results revealed significant differences between treatments, with BIOC plots T4 and T1 showing greater improvements in vegetation development compared to Not-BIOC plots T3 and T2, confirming the positive influence of biocompost+biol. The BIOC treatment favored not only the planted species but also the secondary successional plant communities including certain grasses, leguminous plants, and other shrub and tree species, thus accelerating the revegetation process. This study demonstrates that biocompost application is an effective strategy to enhance plant recolonization on land severely degraded by gold mining in the Ecuadorian Amazon. Full article
(This article belongs to the Section Forest Ecology and Management)
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<p>Geographic location and layout of the experimental site for revegetation in the Naranjalito sector, Napo province, Ecuador. The study area covers approximately 0.5 hectares along the Jatunyacu River and is divided into four experimental blocks (A, B, C, and D), each with treatment plots (T1, T2, T3, and T4) designated for different biocompost dosages and controls. Insets show the location of the Napo province within Ecuador and South America.</p>
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<p>Revegetation methods applied to 0.5 ha of degraded soil: overview of nine sequential stages.</p>
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<p>Experimental design showing four blocks and 16 plots (300 m<sup>2</sup> each) with the distribution of Ochroma pyramidale and Arachis pintoi plants.</p>
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<p>Soil geochemical analysis showing elemental concentrations of 13 elements that exceed the maximum permissible limits (indicated by the red lines) according to Ecuadorian environmental standards.</p>
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<p>Evolution of organic matter in plots before and after treatment with plant biocompost.</p>
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<p>Temporal analysis of dasometric parameters in <span class="html-italic">Ochroma pyramidale</span> over a 6-month period, including basal area (<b>A</b>), height (<b>B</b>), stem volume (<b>C</b>), crown diameter (<b>D</b>), and number of leaves (<b>E</b>), with data recorded at three different time points.</p>
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<p>Biplot representation of the <span class="html-italic">Ochroma pyramidale</span> dasometric variables using the treatments and blocks as illustrative variables with records at 15 days, 90 days, and 180 days.</p>
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<p>Survival rate of <span class="html-italic">Ochroma pyramidale</span> according to generalized linear model where significant differences are observed between treatments.</p>
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<p>(<b>A</b>) Percentage of <span class="html-italic">Arachis pintoi</span> ground cover by plot. (<b>B</b>) Percentage of <span class="html-italic">Arachis pintoi</span> ground cover achieved by treatments over a 6-month period.</p>
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<p>Dry mass of <span class="html-italic">Ochroma pyramidale</span> after 3 months of planting according to vegetative tissue (<b>A</b>) and treatments (<b>B</b>).</p>
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<p>Dry mass biomass data of <span class="html-italic">Arachis pintoi</span> according to plots (<b>A</b>) and treatments (<b>B</b>) in a period of 3 months.</p>
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<p>Q–Q plot to evaluate the normality of the transformed residuals.</p>
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<p>Orthophoto images with the vegetation cover reached after 6 months (<b>A</b>). Remote sensing images with vegetation cover RGB (3.45 cm/pixel) in 6 months (<b>B</b>).</p>
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<p>(<b>A</b>) Vegetation coverage surface (m<sup>2</sup>) according to treatments and blocks. (<b>B</b>) Vegetative cover in the plots after 6 months of study.</p>
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18 pages, 2418 KiB  
Article
Lagged and Instantaneous Effects Between Vegetation and Surface Water Storage in the Yellow River Basin
by Jian Teng, Jun Chang, Yongbo Zhai, Xiaomin Qin, Zuotang Yin, Liangjie Guo and Wei Liu
Sustainability 2025, 17(4), 1709; https://doi.org/10.3390/su17041709 - 18 Feb 2025
Viewed by 91
Abstract
In recent years, large-scale afforestation in the Yellow River Basin (YRB) has attracted widespread attention due to its significant impact on surface water, playing a crucial role in the ecological sustainability and high-quality development of the basin. In this study, we used a [...] Read more.
In recent years, large-scale afforestation in the Yellow River Basin (YRB) has attracted widespread attention due to its significant impact on surface water, playing a crucial role in the ecological sustainability and high-quality development of the basin. In this study, we used a combination of Theil–Sen and Mann–Kendall trend analysis to detect the spatiotemporal dynamic changes of NDVI, surface water storage (SWS), and its components in the YRB from 2001 to 2020, and explored the time lag and instantaneous effects between them using methods such as cross-correlation. The results show that from 2001 to 2020, NDVI and SWS in the YRB increased at rates of 0.41%/year and 1.95 mm/year, respectively, with fluctuations. Spatially, NDVI exhibited a significant upward trend in most areas of the YRB, while regions with significant increases in SWS, canopy surface water (CSW), snow water equivalent (SWE), and soil moisture (SM) were primarily located in the upper reaches. There was a time lag effect of about 2 months between NDVI and SWS in the YRB, and the time lags between SWE, SM, and NDVI were 5 months and 2 months, respectively. Except for CSW, the lag between NDVI and SWE was longer than that between NDVI and SWS or SM across all land cover types. Regarding the instantaneous effect, we found that the effect of vegetation on SWS in the upstream area is mainly the water storage function. In some areas of the middle and lower reaches, vegetation intensifies the consumption of SWS. Our study provides valuable insights into the response mechanism between vegetation restoration and SWS changes, facilitating better coordination between water resource management and ecological conservation in the YRB, thereby achieving sustainable regional economic and ecological development. Full article
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<p>The location, elevation, and distribution of land cover types in the study area.</p>
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<p>The spatiotemporal distribution of NDVI, surface water storage, and its components in the Yellow River Basin from 2001 to 2020. (<b>a</b>) NDVI; (<b>b</b>) surface water storage; (<b>c</b>) canopy surface water; (<b>d</b>) snow water equivalent; (<b>e</b>) soil moisture content; (<b>f</b>) temporal changes of each factor.</p>
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<p>The trend and significance statistics of NDVI, surface water storage, and its components in the Yellow River Basin from 2001 to 2020. (<b>a</b>) NDVI; (<b>b</b>) surface water storage; (<b>c</b>) canopy surface water; (<b>d</b>) snow water equivalent; (<b>e</b>) soil moisture.</p>
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<p>The time-lag correlation between NDVI and surface water storage (SWS) (<b>a</b>), canopy surface water (CSW) (<b>b</b>), snow water equivalent (SWE) (<b>c</b>), and soil moisture (SM) (<b>d</b>) of vegetation in the Yellow River Basin from 2001 to 2020.</p>
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<p>The spatial distribution of correlations between NDVI and surface water storage (SWS) (<b>a</b>), canopy surface water (CSW) (<b>b</b>), snow water equivalent (SWE) (<b>c</b>), and soil moisture (SM) (<b>d</b>) in the Yellow River Basin from 2001 to 2020.</p>
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<p>The correlation statistics between NDVI and surface water storage (SWS) (<b>a</b>), canopy surface water (CSW) (<b>b</b>), snow water equivalent (SWE) (<b>c</b>), and soil moisture (SM) (<b>d</b>) of different land cover types in the Yellow River Basin from 2001 to 2020.</p>
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20 pages, 2298 KiB  
Article
Effects of Land Use Changes on CO2 Emission Dynamics in the Amazon
by Adriano Maltezo da Rocha, Mauricio Franceschi, Alan Rodrigo Panosso, Marco Antonio Camillo de Carvalho, Mara Regina Moitinho, Marcílio Vieira Martins Filho, Dener Marcio da Silva Oliveira, Diego Antonio França de Freitas, Oscar Mitsuo Yamashita and Newton La Scala Jr.
Agronomy 2025, 15(2), 488; https://doi.org/10.3390/agronomy15020488 - 18 Feb 2025
Viewed by 168
Abstract
Global climate change is closely tied to CO2 emissions, and implementing conservation-agricultural systems can help mitigate emissions in the Amazon. By maintaining forest cover and integrating sustainable agricultural practices in pasture, these systems help mitigate climate change and preserve the carbon stocks [...] Read more.
Global climate change is closely tied to CO2 emissions, and implementing conservation-agricultural systems can help mitigate emissions in the Amazon. By maintaining forest cover and integrating sustainable agricultural practices in pasture, these systems help mitigate climate change and preserve the carbon stocks in Amazon forest soils. In addition, these systems improve soil health, microclimate regulation, and promote sustainable agricultural practices in the Amazon region. This study aimed to evaluate the CO2 emission dynamics and its relationship with soil attributes under different uses in the Amazon. The experiment consisted of four treatments (Degraded Pasture—DP; Managed Pasture—MP; Native Forest—NF; and Livestock Forest Integration—LF), with 25 replications. Soil CO2 emission (FCO2), soil temperature, and soil moisture were evaluated over a period of 114 days, and the chemical, physical, and biological attributes of the soil were measured at the end of this period. The mean FCO2 reached values of 4.44, 3.88, 3.80, and 3.14 µmol m−2 s−1 in DP, MP, NF, and LF, respectively. In addition to the direct relationship between soil CO2 emissions and soil temperature for all land uses, soil bulk density indirectly influenced emissions in NF. The amount of humic acid induced the highest emission in DP. Soil organic carbon and carbon stock were higher in MP and LF. These values demonstrate that FCO2 was influenced by the Amazon land uses and highlight LF as a low CO2 emission system with a higher potential for carbon stock in the soil. Full article
(This article belongs to the Section Farming Sustainability)
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<p>Experimental areas. (<b>A</b>) DP—Degraded Pasture, (<b>B</b>) MP—Managed Pasture, (<b>C</b>) LF—Livestock–Forest Integration, and (<b>D</b>) NF—Native Forest. Paranaíta, MT, Brazil.</p>
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<p>Daily means and mean standard error bars of soil CO<sub>2</sub> emission (<b>A</b>), soil moisture (<b>B</b>), and soil temperature (<b>C</b>) in different land uses, Paranaíta, MT, Brazil, 2018 to 2019.</p>
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<p>Linear regression between soil CO<sub>2</sub> emission and soil temperature in different land use typologies.</p>
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<p>Biplot graph with soil attributes, management systems, and confidence ellipses (95% confidence). FCO<sub>2</sub>: soil CO<sub>2</sub> emission, Ts: soil temperature, Ms: soil moisture. pH: potential of hydrogen, H + Al: potential acidity, Cstock: soil carbon stock, CEC: cation exchange capacity, Macro: macroporosity, Micro: microporosity, BD: soil bulk density, FA: fulvic acid, HA: humic acid, MBC: soil microbial biomass carbon, BSR: basal soil respiration.</p>
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17 pages, 24593 KiB  
Article
Enhanced PolSAR Image Segmentation with Polarization Channel Fusion and Diffusion-Based Probability Modeling
by Hao Chen, Yuzhuo Hou, Xiaoxiao Fang and Chu He
Electronics 2025, 14(4), 791; https://doi.org/10.3390/electronics14040791 - 18 Feb 2025
Viewed by 116
Abstract
With the advancement of polarimetric synthetic aperture radar (PolSAR) imaging technology and the growing demand for image interpretation, extracting meaningful land cover information from PolSAR images has become a key research focus. To address the segmentation challenge, we propose an innovative method. First, [...] Read more.
With the advancement of polarimetric synthetic aperture radar (PolSAR) imaging technology and the growing demand for image interpretation, extracting meaningful land cover information from PolSAR images has become a key research focus. To address the segmentation challenge, we propose an innovative method. First, features from co-polarization and cross-polarization channels are separately used as dual inputs, and a cross-attention mechanism effectively fuses these features to capture correlations between different polarization information. Second, a diffusion framework is employed to jointly model target features and class probabilities, aiming to improve segmentation accuracy by learning and fitting the probabilistic distribution of target labels. Finally, experimental results demonstrate that the proposed method achieves superior performance in PolSAR image segmentation, effectively managing complex polarization relationships while offering robustness and broad application potential. Full article
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<p>PolSAR image segmentation framework.</p>
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<p>Conditional diffusion for image segmentation.</p>
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<p>Hybrid modeling framework for PolSAR segmentation.</p>
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<p>Dual-path polarization channel feature fusion module by cross attention (DCFM).</p>
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<p>The used PolSAR datasets.</p>
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<p>Segmentation rResults of the SanALOS2 dataset. (<b>a</b>) Ground truth. (<b>b</b>) FCNs. (<b>c</b>) PSPNet. (<b>d</b>) EmaNet. (<b>e</b>) DANet. (<b>f</b>) SETR. (<b>g</b>) Segformer. (<b>h</b>) Proposal.</p>
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<p>Segmentation results of the HainanC dataset. (<b>a</b>) Ground truth. (<b>b</b>) FCNs. (<b>c</b>) PSPNet. (<b>d</b>) EmaNet. (<b>e</b>) DANet. (<b>f</b>) SETR. (<b>g</b>) Segformer. (<b>h</b>) Proposal.</p>
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<p>OA curves of different methods in the training process on the Hainan dataset.</p>
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15 pages, 7070 KiB  
Article
Assessment of Fire Dynamics in the Amazon Basin Through Satellite Data
by Humberto Alves Barbosa, Catarina Oliveira Buriti and Tumuluru Venkata Lakshmi Kumar
Atmosphere 2025, 16(2), 228; https://doi.org/10.3390/atmos16020228 - 18 Feb 2025
Viewed by 86
Abstract
The Amazon region is becoming more vulnerable to wildfires occurring in the dry season, a crisis amplified by climate change, which affects biomass burning across a wide range of forest environments. In this study, we examined the impact of seasonal fire on greenhouse [...] Read more.
The Amazon region is becoming more vulnerable to wildfires occurring in the dry season, a crisis amplified by climate change, which affects biomass burning across a wide range of forest environments. In this study, we examined the impact of seasonal fire on greenhouse (GHG) emissions over the study region during the last two decades of the 21st century by integrating calibrated and validated satellite-derived products of estimations of burned biomass area, land cover, vegetation greenness, rainfall, land surface temperature (LST), carbon monoxide (CO), and nitrogen dioxide (NO2) through geospatial techniques. The results revealed a strong impact of fire activity on GHG emissions, with abrupt changes in CO and NO2 emission factors between early and middle dry season fires (July–September). Among these seven variables analyzed, we found a positive relationship between the total biomass burned area and fire-derived GHG emission factors (r2 = 0.30) due to the complex dynamics of plant moisture and associated CO and NO2 emissions generated by fire. Nevertheless, other land surface drivers showed the weakest relationships (r2~0.1) with fire-derived GHG emissions due to other factors that drive their regional distribution. Our analysis suggests the importance of continued research on the response of fire season to other land surface characteristics that represent the processes driving fire over the study region such as fuel load, composition, and structure, as well as prevailing weather conditions. These determinants drive fire-related GHG emissions and fire-related carbon cycling relationships and can, therefore, appropriately inform policy fire-abatement guidelines. Full article
(This article belongs to the Section Air Quality)
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<p>The Amazon basin. (<b>a</b>) the spatial distribution of annual burned biomass areas from 2001 to 2020 in four distinct seasons. The colors of each plot indicate: rainy season (December to June), early dry season (July), middle dry season (August–September), or late dry season (October–November). (<b>b</b>) The monthly distribution of total number of fire events identified in the years 2015 to 2020.</p>
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<p>Schematic representation of the hydrographic network superimposed over the Amazon basin. (<b>a</b>) Average annual rainfall from the Climate Hazards Group Infrared Precipitation with Stations (CHIRPS) for the baseline (2001–2020). (<b>b</b>) The land-cover map. (<b>c</b>) Topographic relief based on 250 m Digital Elevation Model—Shuttle Radar Topographic Mission (DEM-SRTM) images. (<b>d</b>) Köppen–Geiger climate classification map.</p>
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<p>(<b>a</b>) The annual forest cover change (% of grid cell area) between 2001 and 2020 calculated using the percentage change method applied to the MODIS land-cover data. (<b>b</b>) Variability of monthly normalized values of NDVI (the green curve), CO (the orange curve), NO<sub>2</sub> (the yellow curve), and burned biomass (the red curve) parameters for their available periods between 2001 and 2020 over the study region. The three parameters (CO, NO<sub>2</sub>, and burned biomass) were normalized to be between 0 and 1, using the min-max normalization method. Fire-derived CO and NO<sub>2</sub> emission parameters are usually quantified using an emission factor, a ratio indicating the proportion of each chemical species that is emitted per unit of biomass burning.</p>
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<p>Scatterplot of (<b>a</b>) six different parameters of principal components (PC2 versus PC1 loadings). Scatterplot of (<b>b</b>) fire per month of PC2 versus PC1 loadings. The percentage indicates the total variance. The arrow widths on the figures are proportional to the PC loadings (positive or negative) regressed upon a fire driver and fire per month. Color symbols indicate mean loadings of PC1 and PC2.</p>
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19 pages, 7061 KiB  
Article
Monitoring and Evaluation of Ecological Environment Quality in the Tianshan Mountains of China Using Remote Sensing from 2001 to 2020
by Yuting Liu, Chunmei Chai, Qifei Zhang, Xinyao Huang and Haotian He
Sustainability 2025, 17(4), 1673; https://doi.org/10.3390/su17041673 - 17 Feb 2025
Viewed by 298
Abstract
High-altitude mountainous regions are highly vulnerable to climate and environmental shifts, with the current global climate change exerting a profound influence on the ecological landscape of the Tianshan Mountains in China. This study assesses the ecological security quality in the Tianshan Mountains of [...] Read more.
High-altitude mountainous regions are highly vulnerable to climate and environmental shifts, with the current global climate change exerting a profound influence on the ecological landscape of the Tianshan Mountains in China. This study assesses the ecological security quality in the Tianshan Mountains of China from 2001 to 2020 by employing various remote sensing techniques such as the Remote Sensing Ecological Index (RSEI) for evaluation, Normalized Difference Vegetation Index (NDVI) for fractional vegetation cover (FVC) analysis, the CASA model for estimating vegetation primary productivity (NPP), and a carbon source/sink model for calculating the net ecosystem productivity (NEP) of vegetation. The research also delves into the evolutionary trends and impact mechanisms on the ecological environment using land use and meteorological data. The findings reveal that the RSEI’s principal component (PC1) exhibits significant explanatory power, showing a notable increase of 5.90% from 2001 to 2020. Despite relatively stable changes in the RSEI over the past two decades covering 61.37% of the study area, there is a prevalent anti-persistence pattern at 72.39%. Notably, NDVI, FVC, and NPP display upward trends in vegetation characteristics. While most areas in the Tianshan Mountains continue to emit carbon, there is a marked increase in NEP, signifying an enhanced carbon absorption capacity. The partial correlation coefficients between the RSEI and temperature, as well as precipitation, demonstrate statistically significant relationships (p < 0.05), encompassing 6.36% and 1.55% of the study area, respectively. Temperature displays a predominantly negative correlation in 98.71% of the significantly correlated zones, while precipitation exhibits a prevalent positive correlation. An in-depth analysis of how climate change affects the quality of the ecological environment provides crucial insights for strategic interventions to enhance regional environmental protection and promote ecological sustainability. Full article
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<p>Overview of the study area.</p>
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<p>(<b>a</b>) Spatiotemporal characteristics of RSEI in 2001, (<b>b</b>) spatiotemporal characteristics of RSEI in 2010, (<b>c</b>) spatiotemporal characteristics of RSEI in 2020, and (<b>d</b>) spatiotemporal characteristics of the average RSEI values from 2001 to 2020.</p>
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<p>Proportion of different levels of RSEI in the Tianshan Mountains from 2001 to 2020.</p>
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<p>The sustainability and stability of the ecological environment in the Tianshan Mountains of China from 2001 to 2020. (<b>a</b>) Spatial distribution of the RSEI coefficient of variation; (<b>b</b>) spatial distribution of Hurst exponent of the RSEI.</p>
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<p>(<b>a</b>) Spatiotemporal characteristics of the average NDVI values from 2001 to 2020; (<b>b</b>) temporal changes in NDVI from 2001 to 2020.</p>
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<p>(<b>a</b>) Spatiotemporal characteristics of FVC in 2001, (<b>b</b>) spatiotemporal characteristics of FVC in 2010, (<b>c</b>) spatiotemporal characteristics of FVC in 2020, and (<b>d</b>) spatiotemporal characteristics of the average FVC values from 2001 to 2020.</p>
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<p>Area and proportion of vegetation coverage grades in the Tianshan Mountains from 2001 to 2020.</p>
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<p>(<b>a</b>) Spatiotemporal characteristics of NPP in 2001, (<b>b</b>) spatiotemporal characteristics of NPP in 2010, (<b>c</b>) spatiotemporal characteristics of NPP in 2020, and (<b>d</b>) temporal changes in NPP in China’s Tianshan Mountains from 2001 to 2020.</p>
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<p>(<b>a</b>) Spatiotemporal characteristics of NEP in 2001, (<b>b</b>) spatiotemporal characteristics of NEP in 2010, (<b>c</b>) spatiotemporal characteristics of NEP in 2020, and (<b>d</b>) temporal changes in NEP in China’s Tianshan Mountains from 2001 to 2020.</p>
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<p>Annual spatiotemporal characteristics of climate factors in Tianshan Mountains from 2001 to 2020. (<b>a</b>) Precipitation spatial patterns, (<b>b</b>) precipitation temporal trends, (<b>c</b>) temperature spatial patterns, and (<b>d</b>) temperature temporal trends.</p>
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<p>Correlation coefficients between the RSEI and precipitation, temperature in the Tianshan Mountains from 2001 to 2020.</p>
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<p>Dynamic changes in land types in the Chinese Tianshan Mountains from 2000 to 2020.</p>
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22 pages, 4795 KiB  
Article
Exploring the Drivers of Ecosystem Service Changes from a Spatio-Temporal Perspective in Vulnerable Nanling Mountainous Areas in SE China
by Lingyue Huang, Lichen Yuan, Meiyun Li, Yongyan Xia, Tingting Che, Jianyi Liu, Ziling Luo and Jiangang Yuan
Land 2025, 14(2), 417; https://doi.org/10.3390/land14020417 - 17 Feb 2025
Viewed by 173
Abstract
Mountains support many kinds of ecosystem services (ESs) for human beings, emphasizing the need to understand the characteristics and drivers of ES changes in mountainous regions. In this study, Nanling, the most significant mountains of southern China, was selected as a case study. [...] Read more.
Mountains support many kinds of ecosystem services (ESs) for human beings, emphasizing the need to understand the characteristics and drivers of ES changes in mountainous regions. In this study, Nanling, the most significant mountains of southern China, was selected as a case study. Utilizing the GlobeLand30 dataset, we employed InVEST, Geodetector and MGWR to identify the spatio-temporal characteristics and drivers of ES changes, investigate trade-offs and synergies between ESs, and examine the relationship between ESs and the landscape ecological risk index (LERI) to provide a new perspective for ecosystem management in vulnerable mountain regions. The results showed that carbon storage (CS) and habitat quality (HQ) slightly decreased, while the water yield (WY) increased slightly. Soil conservation (SC) significantly decreased, but the total ES (TES) slightly increased. All ES bundles demonstrated a synergistic relationship, but most of the synergies exhibited a decreasing trend. The ESs in the study area were mainly affected by climate factors, and anthropogenic factors also had a significant impact on ESs. LERI exhibited a negative correlation with the provision of ESs and demonstrated a high explanatory power for ES changes, especially for CS, HQ and TES, suggesting that areas with more stable landscape patterns are likely to harbor greater levels of ESs. The results provide insights into the analysis of the characteristics of ES change in vulnerable mountainous areas, also providing the practical implications for introducing LERI as a driver for ES change. Full article
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<p>Study area [<a href="#B21-land-14-00417" class="html-bibr">21</a>].</p>
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<p>Spatial distribution of ESs from 2000 to 2020. Abbreviations: CS: carbon storage; WY: water yield; SC: soil conservation; HQ: habitat quality; TES: total ecosystem services.</p>
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<p>Spatial distribution of changes in ESs from 2000 to 2020. Abbreviations: CS: carbon storage; WY: water yield; SC: soil conservation; HQ: habitat quality; TES: total ecosystem services.</p>
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<p>Bivariate spatial autocorrelation analysis among ESs. Abbreviations: CS: carbon storage; WY: water yield; SC: soil conservation; HQ: habitat quality.</p>
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<p>Individual and cross effects of the drivers on changes in ESs. Note: CF: climate factor; GF: geomorphological factor; AF: anthropogenic factor; VF: vegetation factor; LERI: landscape ecological risk index; CS: carbon storage; HQ: habitat quality; SC: soil conservation; WY: water yield; TES: total ecosystem services.</p>
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<p>MGWR coefficients between drivers and ESs. Except for geomorphological factors, other ESs and drivers represent the net value of change between the years 2000 and 2020. Note: CS: carbon storage; HQ: habitat quality; SC: soil conservation; WY: water yield; TES: total ecosystem services; LERI: landscape ecological risk index.</p>
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25 pages, 8413 KiB  
Article
Flood Exposure Dynamics and Quantitative Evaluation of Low-Cost Flood Control Measures in the Bengawan Solo River Basin of Indonesia
by Badri Bhakta Shrestha, Mohamed Rasmy and Daisuke Kuribayashi
Hydrology 2025, 12(2), 38; https://doi.org/10.3390/hydrology12020038 - 17 Feb 2025
Viewed by 283
Abstract
The frequent occurrence of floods puts additional pressure on people to change their activities and alter land use practices, consequently making exposed lands more vulnerable to floods. It is thus crucial to investigate dynamic changes in flood exposures and conduct quantitative evaluations of [...] Read more.
The frequent occurrence of floods puts additional pressure on people to change their activities and alter land use practices, consequently making exposed lands more vulnerable to floods. It is thus crucial to investigate dynamic changes in flood exposures and conduct quantitative evaluations of flood risk-reduction strategies to minimize damage to exposed items. This study quantitatively assessed dynamics of flood exposure and flood risk, and evaluated the effectiveness of flood control measures in the Bengawan Solo River basin, Indonesia. The Water and Energy Budget-Based Rainfall–Runoff–Inundation Model was employed for flood simulation for different return periods, and then dynamics of flood exposures and flood risk were assessed. After that, the effectiveness of flood control measures was quantitively evaluated. The results show that settlement/built-up areas and population are increasing in flood-prone areas. The flood-exposed paddy field and settlement areas for 100-year flood were estimated to be more than 950 and 212.58 km2, respectively. The results also show that the dam operation for flood control in the study area reduces the flood damage to buildings, contents, and agriculture by approximately 21.2%, 20.9%, and 25.1%, respectively. The river channel improvements were also found effective to reduce flood damage in the study area. The flood damage can be reduced by more than 60% by implementing a combination of a flood control dam and river channel improvements. The findings can be useful for planning and implementing effective flood risk reduction measures. Full article
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<p>Example of river channel-improvement activities in the Pampanga River basin of the Philippines. (Photos: Mr. Hilton Hernando, Pampanga River Basin Flood Forecasting and Warning Centre).</p>
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<p>(<b>a</b>) Location of the Bengawan Solo River Basin (BSRB) and elevation distribution based on HydroSHEDS digital elevation model (<a href="https://www.hydrosheds.org/products/hydrosheds" target="_blank">https://www.hydrosheds.org/products/hydrosheds</a>, accessed on 10 December 2023) and (<b>b</b>) soil types in the study area based on digital soil map of FAO/UNESCO (<a href="https://data.apps.fao.org/" target="_blank">https://data.apps.fao.org/</a>, accessed on 21 July 2022).</p>
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<p>Overview of flood exposure assessment.</p>
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<p>River reach considered (red line) for river channel improvements in the analysis.</p>
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<p>Time-series plots of calculated and observed daily discharges at Cepu station for flood events in 2007/2008 and 2009.</p>
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<p>Calculated flood inundation depth and extent areas for 10-, 50-, and 100-year floods.</p>
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<p>Flood inundation probability from high frequency to low frequency.</p>
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<p>Land cover maps for past years (source: Ministry of Environment and Forestry, Indonesia).</p>
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<p>Loss and gain areas of each land cover class during 1990–2006 and 2006–2020 (plotted using circlize–Circular Visualization R-package by Gu et al. [<a href="#B41-hydrology-12-00038" class="html-bibr">41</a>]).</p>
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<p>Calculated flood exposed areas of each land cover class in the cases of 10-, 50- and 100-year floods.</p>
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<p>Spatial distribution of population over the basin based on WorldPop Population for 2000, 2010, and 2020.</p>
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<p>(<b>a</b>) Total estimated population in the study area for 2000, 2010, and 2020; and (<b>b</b>) calculated flood exposed population using different years’ population data (2000, 2010, and 2020) for 10-, 50-, and 100-year flood event cases.</p>
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<p>Calculated flood damage to buildings and contents for 10-, 50-, and 100-year floods, without any flood control measures: (<b>a</b>) building damage and (<b>b</b>) content damage.</p>
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<p>Calculated flood damage to agricultural crops (rice crops) for 10-, 50-, and 100-year floods, without any flood control measures.</p>
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<p>Calculated inflow discharge into reservoir and outflow discharge from the dam for 10-, 50-, and 100-year flood cases.</p>
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<p>Calculated expected annual damage (EAD) of building, content, and rice-crop damages, with and without dam control function and percentage reduction in EAD by the use of dam for flood control: (<b>a</b>) buildings and contents and (<b>b</b>) rice crops.</p>
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<p>Calculated expected annual damage with and without river channel-improvement options and percentage reduction in EAD by the river channel-improvement options: (<b>a</b>) building-damage case, (<b>b</b>) content-damage case, and (<b>c</b>) rice crop-damage case. (Note: Riv in the figures means River).</p>
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<p>Calculated flood damage in the cases of combination of flood control dam with river channel improvement options for 100-year flood: (<b>a</b>) buildings damage, (<b>b</b>) contents damage, and (<b>c</b>) rice-crop damage (C1, <span class="html-italic">Dam</span> + <span class="html-italic">Depth_5%</span>; C2, <span class="html-italic">Dam</span> + <span class="html-italic">Depth_10%</span>; C3, <span class="html-italic">Dam</span> + <span class="html-italic">Width_5%</span>; C4, <span class="html-italic">Dam</span> + <span class="html-italic">Width_10%</span>; C5, <span class="html-italic">Dam</span> + <span class="html-italic">Levee_3m</span>; C6, <span class="html-italic">Dam</span> + <span class="html-italic">Depth_5%</span> + <span class="html-italic">Width_5%</span> + <span class="html-italic">Levee_3m</span>; and C7, <span class="html-italic">Dam</span> + <span class="html-italic">Depth_10%</span> + <span class="html-italic">Width_10%</span> + <span class="html-italic">Levee_3m</span>).</p>
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<p>Calculated damage with and without land use restriction (LUR) alone in the flood-prone areas with high flood depth: (<b>a</b>) 50-year flood case and (<b>b</b>) 100-year flood case.</p>
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