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Search Results (2,642)

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Keywords = remote-sensed reflectance

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21 pages, 2508 KiB  
Article
A Service-Learning Project to Acquire GIS Skills and Knowledge: A Case Study for Environmental Undergraduate Students
by Montserrat Ferrer-Juliá, Inés Pereira, Juncal A. Cruz and Eduardo García-Meléndez
Sustainability 2025, 17(5), 2276; https://doi.org/10.3390/su17052276 - 5 Mar 2025
Viewed by 114
Abstract
The service-learning (SL) approach has shown effectiveness in fulfilling both academic and community-oriented objectives. This paper focuses on a specific case study for a Cartography, Remote Sensing, and Geographical Information Systems (GIS) course for Environmental Sciences undergraduate students. The main goals for implementing [...] Read more.
The service-learning (SL) approach has shown effectiveness in fulfilling both academic and community-oriented objectives. This paper focuses on a specific case study for a Cartography, Remote Sensing, and Geographical Information Systems (GIS) course for Environmental Sciences undergraduate students. The main goals for implementing SL practice were (1) to enhance students’ GIS knowledge and to develop cross-cutting skills by working with real-world problems; (2) to share with society the knowledge acquired by students and ensure that it is valued; and (3) to prompt reflection on urban waste issues among students. The activity consisted of analyzing the waste containers along the 1 km riverbanks in León (Spain) and elaborating a proposal for the location of new rubbish bins to deliver to a City Council’s environmental technician. The results showed an improvement in students’ GIS management skills to solve environmental problems compared to those from the previous 3 years and a satisfactory response from environmental professionals with delivering the results. Together, an increase in students discussing urban waste was observed during the sessions. Projects like this not only teach technical skills but also provide a deeper understanding of data collection and implementation processes in environmental issues, which are closely aligned with professional experiences, and awareness of the practical application of the knowledge acquired. Full article
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<p>Flowchart with the service performance and reflection sessions.</p>
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<p>Map chosen from students to incorporate in the final report submitted to the City Council. Different colors refer to different neighborhoods in the location maps (Leon municipality and study area).</p>
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<p>(<b>A</b>) Schema developed by students evaluated (<b>A</b>) with a low mark and (<b>B</b>) with a high mark.</p>
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<p>Temporal evolution of the % of students passing, failing and not submitting the complete Cartography, Remote Sensing, and GIS course.</p>
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<p>Answers to the satisfaction survey completed by the students of the Cartography, Remote Sensing, and GIS course. The answers corresponding to the last two questions are not included as these are open-ended questions.</p>
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21 pages, 2017 KiB  
Review
Current Capabilities and Challenges of Remote Sensing in Monitoring Freshwater Cyanobacterial Blooms: A Scoping Review
by Jianyong Wu, Yanni Cao, Shuqi Wu, Smita Parajuli, Kaiguang Zhao and Jiyoung Lee
Remote Sens. 2025, 17(5), 918; https://doi.org/10.3390/rs17050918 - 5 Mar 2025
Viewed by 89
Abstract
Remote sensing (RS) has been widely used to monitor cyanobacterial blooms in inland water bodies. However, the accuracy of RS-based monitoring varies significantly depending on factors such as waterbody type, sensor characteristics, and analytical methods. This study comprehensively evaluates the current capabilities and [...] Read more.
Remote sensing (RS) has been widely used to monitor cyanobacterial blooms in inland water bodies. However, the accuracy of RS-based monitoring varies significantly depending on factors such as waterbody type, sensor characteristics, and analytical methods. This study comprehensively evaluates the current capabilities and challenges of RS for cyanobacterial bloom monitoring, with a focus on achievable accuracy. We find that chlorophyll-a (Chl-a) and phycocyanin (PC) are the primary indicators used, with PC demonstrating greater accuracy and stability than Chl-a. Sentinel and Landsat satellites are the most frequently used RS data sources, while hyperspectral images, particularly from unmanned aerial vehicles (UAVs), have shown high accuracy in recent years. In contrast, the Medium-Resolution Imaging Spectrometer (MERIS) and Moderate-Resolution Imaging Spectroradiometer (MODIS) have exhibited lower performance. The choice of analytical methods is also essential for monitoring accuracy, with regression and machine learning models generally outperforming other approaches. Temporal analysis indicates a notable improvement in monitoring accuracy from 2021 to 2023, reflecting advances in RS technology and analytical techniques. Additionally, the findings suggest that a combined approach using Chl-a for large-scale preliminary screening, followed by PC for more precise detection, can enhance monitoring effectiveness. This integrated strategy, along with the careful selection of RS data sources and analytical models, is crucial for improving the accuracy and reliability of cyanobacterial bloom monitoring, ultimately contributing to better water management and public health protection. Full article
(This article belongs to the Special Issue Recent Advances in Water Quality Monitoring)
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<p>Flowchart illustrating the article selection process used in this study.</p>
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<p>Collected metric types with reference counts and percentages.</p>
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<p>Descriptive statistics of selected articles. (<b>A</b>): Number of selected articles by publication year. (<b>B</b>): Number of articles selected by study area. (<b>C</b>): Number of selected articles by waterbody type. (<b>D</b>): Number of articles selected by cyanobacterial bloom indicators. (<b>E</b>): Number of selected articles by RS image type. (<b>F</b>): Number of selected articles by RS data analytical methods. BO: bio-optical models; BR: band-ratio algorithms; E: empirical models; H: hybrid approaches; HS: hyperspectral; IB: index-based algorithms; ML: machine learning models; MS: multispectral; O: other statistical analyses; R: regression analysis; SA: semi-analytical models; SE: semi-empirical models; UAV: unmanned aerial vehicle.</p>
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<p>Distribution of RS accuracy for Chl-a under the influence of various factors. (<b>A</b>): in different periods; (<b>B</b>): in different types of water bodies; (<b>C</b>): with different RS images; (<b>D</b>): based on different data analytical methods. Note: Hyperspectral images exclude the images from UAVs.</p>
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<p>Distribution of RS accuracy for phycocyanin (PC) under the influence of various factors: (<b>A</b>): in different periods; (<b>B</b>): in different types of water bodies; (<b>C</b>): with different RS images; (<b>D</b>): based on different data analytical methods. Note: Hyperspectral images exclude the images from UAVs.</p>
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21 pages, 3101 KiB  
Article
Microplastic Deposits Prediction on Urban Sandy Beaches: Integrating Remote Sensing, GNSS Positioning, µ-Raman Spectroscopy, and Machine Learning Models
by Anderson Targino da Silva Ferreira, Regina Célia de Oliveira, Eduardo Siegle, Maria Carolina Hernandez Ribeiro, Luciana Slomp Esteves, Maria Kuznetsova, Jessica Dipold, Anderson Zanardi de Freitas and Niklaus Ursus Wetter
Microplastics 2025, 4(1), 12; https://doi.org/10.3390/microplastics4010012 - 5 Mar 2025
Viewed by 154
Abstract
This study focuses on the deposition of microplastics (MPs) on urban beaches along the central São Paulo coastline, utilizing advanced methodologies such as remote sensing, GNSS altimetric surveys, µ-Raman spectroscopy, and machine learning (ML) models. MP concentrations ranged from 6 to 35 MPs/m [...] Read more.
This study focuses on the deposition of microplastics (MPs) on urban beaches along the central São Paulo coastline, utilizing advanced methodologies such as remote sensing, GNSS altimetric surveys, µ-Raman spectroscopy, and machine learning (ML) models. MP concentrations ranged from 6 to 35 MPs/m2, with the highest densities observed near the Port of Santos, attributed to industrial and port activities. The predominant MP types identified were foams (48.7%), fragments (27.7%), and pellets (23.2%), while fibers were rare (0.4%). Beach slope and orientation were found to facilitate the concentration of MP deposition, particularly for foams and pellets. The study’s ML models showed high predictive accuracy, with Random Forest and Gradient Boosting performing exceptionally well for specific MP categories (pellet, fragment, fiber, foam, and film). Polymer characterization revealed the prevalence of polyethylene, polypropylene, and polystyrene, reflecting sources such as disposable packaging and industrial raw materials. The findings emphasize the need for improved waste management and targeted urban beach cleanups, which currently fail to address smaller MPs effectively. This research highlights the critical role of combining in situ data with predictive models to understand MP dynamics in coastal environments. It provides actionable insights for mitigation strategies and contributes to global efforts aligned with the Sustainable Development Goals, particularly SDG 14, aimed at conserving marine ecosystems and reducing pollution. Full article
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<p>Flowchart of the steps in the methodology used in this research. RS: orbital remote sensing images; MNDWI: modified normalized difference water index; HD<sub>sat</sub>: horizontal distance derived by satellite; VD<sub>tide</sub>: vertical distance derived by tide; tanβ<sub>sat</sub>: slope derived by satellite; GNSS: global navigation satellite system; Alt<sub>GNSS</sub>: altitude derived by GNSS; tanβ<sub>GNSS</sub>: slope derived by GNSS; μ-Raman: micro-Raman analysis; ML: machine learning models; and MP deposits: microplastic deposits.</p>
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<p>Sediment sampling sites and GNSS positioning locations. Urban areas are highlighted in red, with emphasis on the Port of Santos and the industrial region of Cubatão.</p>
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<p>Beach sampling point (P1), modified from [<a href="#B1-microplastics-04-00012" class="html-bibr">1</a>]. Examples of GNSS base, rover surveys, and area (1 m<sup>2</sup>) of superficial sediment collection.</p>
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<p>SHAP analysis of variable contributions for predicting microplastic deposition using multiple machine learning models: (<b>a</b>) SVR—Support Vector Regression for pellets; (<b>b</b>) GB—Gradient Boosting for fragments; (<b>c</b>) RF—Random Forest for fibers; (<b>d</b>) RF—Random Forest for foams; and (<b>e</b>) GB—Gradient Boosting for total MP. The intensity of each variable is represented by the color scale, ranging from blue (low values) to red (high values), indicating the magnitude of the feature’s influence.</p>
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<p>GNSS sediment samples and transect models: (<b>a</b>) beach slope (tanβ); (<b>b</b>) beach face direction (Aspect).</p>
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<p>Modeled points and GNSS sediment sample points: (<b>a</b>) pellet, (<b>b</b>) foam, (<b>c</b>) fragment, (<b>d</b>) fiber, and (<b>e</b>) total MP (m<sup>2</sup>).</p>
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<p>Perceptual maps showing the standardized adjusted residual (ASR) values between the microplastic deposition models: (<b>a</b>) pellet, (<b>b</b>) foam, (<b>c</b>) fragment, and (<b>d</b>) total MP (m<sup>2</sup>) in relation to beaches’ modeled points (PG, SVS, GUA, and BER). The colored cells indicate significant relationships between variables (+1.96 ≤ good SAR). VL (very low), L (low), M (medium), H (high), and VH (very high) represent the different levels of MP/m<sup>2</sup> deposition by CA.</p>
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<p>Raman spectra of polymers: (<b>a</b>,<b>b</b>) polyethylene; (<b>c</b>) polypropylene; and (<b>d</b>) polystyrene.</p>
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29 pages, 27723 KiB  
Article
A Geospatial Analysis Approach to Investigate Effects of Wildfires on Vegetation, Hydrological Response, and Recovery Trajectories in a Mediterranean Watershed
by Konstantinos Soulis, Stergia Palli Gravani, Rigas Giovos, Evangelos Dosiadis and Dionissios Kalivas
Hydrology 2025, 12(3), 47; https://doi.org/10.3390/hydrology12030047 - 4 Mar 2025
Viewed by 160
Abstract
Wildfires are frequently observed in watersheds with a Mediterranean climate and seriously affect vegetation, soil, hydrology, and ecosystems as they cause abrupt changes in land cover. Assessing wildfire effects, as well as the recovery process, is critical for mitigating their impacts. This paper [...] Read more.
Wildfires are frequently observed in watersheds with a Mediterranean climate and seriously affect vegetation, soil, hydrology, and ecosystems as they cause abrupt changes in land cover. Assessing wildfire effects, as well as the recovery process, is critical for mitigating their impacts. This paper presents a geospatial analysis approach that enables the investigation of wildfire effects on vegetation, soil, and hydrology. The prediction of regeneration potential and the period needed for the restoration of hydrological behavior to pre-fire conditions is also presented. To this end, the catastrophic wildfire that occurred in August 2021 in the wider area of Varybobi, north of Athens, Greece, is used as an example. First, an analysis of the extent and severity of the fire and its effect on the vegetation of the area is conducted using satellite imagery. The history of fires in the specific area is then analyzed using remote sensing data and a regrowth model is developed. The effect on the hydrological behavior of the affected area was then systematically analyzed. The analysis is conducted in a spatially distributed form in order to delineate the critical areas in which immediate interventions are required for the rapid restoration of the hydrological behavior of the basin. The period required for the restoration of the hydrological response is then estimated based on the developed vegetation regrowth models. Curve Numbers and post-fire runoff response estimations were found to be quite similar to those derived from measured data. This alignment shows that the SCS-CN method effectively reflects post-fire runoff conditions in this Mediterranean watershed, which supports its use in assessing hydrological changes in wildfire-affected areas. The results of the proposed approach can provide important data for the restoration and protection of wildfire-affected areas. Full article
(This article belongs to the Section Hydrological and Hydrodynamic Processes and Modelling)
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<p>Geographic location of the burn scars created by the 2021 Varybobi wildfire and the adjacent watersheds. The above layers’ creation is described in the methodology section of the present study.</p>
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<p>Flowchart outlining the proposed methodology for the analysis of wildfires hydrological impact and recovery process.</p>
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<p>The CN–Rainfall data of the studied watershed and the fitted lines describing this relationship according to the Two-CN method [<a href="#B14-hydrology-12-00047" class="html-bibr">14</a>] and the Asymptotic CN [<a href="#B85-hydrology-12-00047" class="html-bibr">85</a>]. The corresponding CN values and the areas they cover are also shown.</p>
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<p>Variables used for the implementation of the model: (<b>a</b>) slope, (<b>b</b>) precipitation, (<b>c</b>) NDVI-produced 1-year vegetation regeneration, (<b>d</b>) TPI index, (<b>e</b>) dNBR index, and (<b>f</b>) model’s final regeneration prediction for the year 2031.</p>
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<p>Diachronic evolution of the NDVI index at the sites of the 1986 (red) and 1987 (blue) wildfires.</p>
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<p>NDVI difference between the pre-fire values (2021) and the 10-year regeneration prediction (2031).</p>
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<p>Diachronic evolution of soil–land use complexes, based on CLC data.</p>
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<p>Pre-fire CN ranges in the watersheds studied in the CLC reference years.</p>
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<p>Post-fire CN ranges in the study area after the implementation of the two methods on the 2018 CLC reference year; (<b>a</b>) 5, 10, 15, and 20 unit increases in the runoff CN value according to the burn severity classes [<a href="#B80-hydrology-12-00047" class="html-bibr">80</a>], and (<b>b</b>) post-fire CN values according to [<a href="#B28-hydrology-12-00047" class="html-bibr">28</a>].</p>
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<p>Direct runoff (mm) for the three return periods (5, 50, and 1000 years) estimated for the 2018 CLC reference year pre-fire and post-fire using two methods.</p>
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<p>Graphical illustration of runoff volume (mm) of the three study sub-areas for return periods of 5, 50, and 1000 years, respectively (<b>a</b>–<b>c</b>).</p>
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<p>Direct runoff values estimated with the post-fire CNs obtained by the two examined methods (Est. Direct Runoff—1 and 2 are the direct runoff estimations with method 1 and 2, correspondingly) plotted in comparison with the observed direct runoff.</p>
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21 pages, 4194 KiB  
Article
Predicting Olive Tree Chlorophyll Fluorescence Using Explainable AI with Sentinel-2 Imagery in Mediterranean Environment
by Leonardo Costanza, Beatriz Lorente, Francisco Pedrero Salcedo, Francesco Pasanisi, Vincenzo Giannico, Francesca Ardito, Carlota María Martí Martínez and Simone Pietro Garofalo
Appl. Sci. 2025, 15(5), 2746; https://doi.org/10.3390/app15052746 - 4 Mar 2025
Viewed by 244
Abstract
Chlorophyll fluorescence is a useful indicator of a plant’s physiological status, particularly under stress conditions. Remote sensing is an increasingly adopted technology in modern agriculture, allowing the acquisition of crop information (e.g., chlorophyll fluorescence) without direct contact, reducing fieldwork. The objective of this [...] Read more.
Chlorophyll fluorescence is a useful indicator of a plant’s physiological status, particularly under stress conditions. Remote sensing is an increasingly adopted technology in modern agriculture, allowing the acquisition of crop information (e.g., chlorophyll fluorescence) without direct contact, reducing fieldwork. The objective of this study is to improve the monitoring of olive tree fluorescence (Fv′/Fm′) via remote sensing in a Mediterranean environment, where the frequency of stress factors, such as drought, is increasing. An advanced approach combining explainable artificial intelligence and multispectral Sentinel-2 satellite data was developed to predict olive tree fluorescence. Field measurements were conducted in southeastern Italy on two olive groves: one irrigated and the other one under rainfed conditions. Sentinel-2 reflectance bands and vegetation indices were used as predictors and different machine learning algorithms were tested and compared. Random Forest showed the highest predictive accuracy, particularly when Sentinel-2 reflectance bands were used as predictors. Using spectral bands preserves more information per observation, enabling models to detect variations that VIs might miss. Additionally, raw reflectance data minimizes potential bias that could arise from selecting specific indices. SHapley Additive exPlanations (SHAP) analysis was performed to explain the model. Random Forest showed the highest predictive accuracy, particularly when using Sentinel-2 reflectance bands as predictors. Key spectral regions associated with Fv′/Fm′, such as red-edge and NIR, were identified. The results highlight the potential of integrating remote sensing and machine learning to improve olive grove management, providing a useful tool for early stress detection and targeted interventions. Full article
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<p>Apulia region, southeastern Italy (blue boundaries) (OpenStreetMap Contributors, 2025); Sentinel-2 RGB images of the experimental olive orchards in Bitonto (field A) and Palombaio (field B) (black boundaries). Red points indicate sampled trees within the orchards (<span class="html-italic">n</span> = 18 per field).</p>
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<p>Weather conditions around the area of the fields investigated (field A, (<b>a</b>); field B, (<b>b</b>)) during the irrigation season (Civil Protection Agency of Apulia).</p>
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<p>Boxplot showing the distribution of the measured Fv′/Fm′ between field A and field B for the dates of sampling. Symbols indicate statistical differences according to the Wilcoxon test (* <span class="html-italic">p</span> &lt; 0.05; ** <span class="html-italic">p</span> &lt; 0.01; **** <span class="html-italic">p</span> &lt; 0.0001).</p>
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<p>Ridgeline plot of Sentinel-2 bands reflectance (<b>a</b>) and vegetation indices values (<b>b</b>) for the investigated dates.</p>
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<p>Panels (<b>a</b>,<b>b</b>) present the results of Recursive Feature Elimination (RFE) applied to Sentinel-2 spectral bands (S2Bs) and vegetation indices (VIs), respectively. In each panel, the upper plot shows the Root Mean Squared Error (RMSE) computed via a bootstrap-based Bayesian Ridge Regression, plotted against the number of maintained variables. The red marker identifies the subset size yielding the lowest RMSE, indicating the optimal number of predictors. The lower bar chart displays all candidate variables in descending order of their contribution to RMSE reduction (%). Variables included in the optimal subset are shown in blue, while those excluded are in gray.</p>
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<p>(<b>a</b>) Scatterplot of the overall cross-validated Random forest Prediction of olive tree Fv′/Fm′ (<span class="html-italic">n</span> = 144); (<b>b</b>) scatterplot of the cross-validated Random Forest prediction of olive tree Fv′/Fm′ considering the two fields (<span class="html-italic">n</span> field A = 72; <span class="html-italic">n</span> field B = 72). The dashed line is the bisector while the blue and red ones are the regression lines.</p>
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<p>SHAP plot showing the importance of the features (Sentinel-2 bands reflectance values) in contributing to Random Forest predictions. Each point represents an individual data instance, with its horizontal position indicating the contribution of a specific feature to the deviation from the model’s average prediction. The color of the points indicates the value of the feature.</p>
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<p>SHAP dependence plots illustrate the marginal contributions of the selected features according to their SHAP values. Each panel shows how a single feature’s SHAP value (<span class="html-italic">y</span>-axis) varies with the actual values of that feature (<span class="html-italic">x</span>-axis). Higher (or lower) SHAP values indicate a greater impact—positive or negative—on the Random Forest model’s predictions of Fv′/Fm′.</p>
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19 pages, 5591 KiB  
Article
Mapping Vegetation-Covered Water Areas Using Sentinel-2 and RadarSat-2 Data: A Case Study of the Caohai Wetland in Guizhou Province
by Guanglai Zhu, Yu Zhang, Chaoyong Shen, Xuling Luo, Xin Yao, Guanwen Chen, Tao Xie and Zhuo Dong
Water 2025, 17(5), 729; https://doi.org/10.3390/w17050729 - 2 Mar 2025
Viewed by 319
Abstract
Vegetation-covered water bodies (VCW) are a vital component of wetlands, and their distribution information is crucial for studying the dynamic interactions between vegetation and water. However, due to vegetation obstruction, optical remote sensing has limitations in extracting such water bodies, as it typically [...] Read more.
Vegetation-covered water bodies (VCW) are a vital component of wetlands, and their distribution information is crucial for studying the dynamic interactions between vegetation and water. However, due to vegetation obstruction, optical remote sensing has limitations in extracting such water bodies, as it typically identifies only open water areas effectively. In contrast, microwave remote sensing, with its vegetation-penetrating capability and specular reflection characteristics, provides a more comprehensive identification of wetland water bodies. Previous studies have shown that the additional water body areas (SW) identified by SAR but not by optical sensors are often accompanied by significant vegetation cover. However, a systematic assessment of SW’s potential in mapping VCW is still lacking. This study uses the Caohai Wetland in Guizhou, China, as an example, leveraging Sentinel-2A and RadarSat-2 imagery from adjacent periods and multiple water body extraction methods to extract SW and explore its performance in mapping VCW during the dry season. Results show that during the initial stage of vegetation senescence (7 January 2019), the use of SW achieved high accuracy in mapping VCW, with overall accuracy, kappa coefficient, and F1 score reaching 84.2%, 68.4%, and 85.3%, respectively. However, as vegetation senescence deepened (12 January 2020), these metrics dropped to 76.2%, 60.7%, and 87%, respectively, indicating a significant decline in accuracy. During the vegetation regrowth stage (7 April 2020), the overall accuracy, kappa coefficient, and F1 score were 71.1%, 57.2%, and 70.9%, respectively. As vegetation continued to grow (21 April 2019), these metrics improved to 79.4%, 67.2%, and 86.6%. In summary, SW extracted from high-resolution optical and SAR imagery can preliminarily map VCW during the dry season. Furthermore, its identification accuracy improves significantly with increasing vegetation density. This study provides a novel perspective for wetland water body monitoring and the study of vegetation-water interactions. Full article
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<p>Location map of the study area: (<b>a</b>) Guizhou Province; (<b>b</b>) Weining Country; (<b>c</b>) Caohai National Nature Reserve.</p>
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<p>Water level changes in 2019–2020: (<b>a</b>) January; (<b>b</b>) April.</p>
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<p>Technical workflow: (1)preprocessing and co-registering the raw Sentinel-2A and RadarSat-2 images; (2) applying four classification methods and performing accuracy assessments to select the optimal water body extraction results for each period; (3) conducting vector fusion of the extracted water bodies, removing permanent water bodies, and evaluating the performance of SW in mapping water bodies beneath vegetation cover.</p>
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<p>Ground sample point distribution map (example from 7 January 2019): (<b>a</b>) first survey. (<b>b</b>) second survey.</p>
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<p>Photographs of different types of water bodies.</p>
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<p>Water extraction results based on optical images: (<b>a</b>) Sentinel-2A/MSI image; (<b>b</b>) SVM; (<b>c</b>) RF; (<b>d</b>) RBO; (<b>e</b>) MLC.</p>
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<p>Water extraction results based on SAR images: (<b>a</b>) RadarSat-2/HH; (<b>b</b>) SVM; (<b>c</b>) RF; (<b>d</b>) RBO.</p>
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<p>Local comparison of two water body extraction results for January 2019. (Panels (<b>a</b>,<b>c</b>) compare the differences in identifying small water bodies; panels (<b>d</b>,<b>f</b>) compare the differences in identifying VCW; panels (<b>b</b>,<b>e</b>) compare the differences in identifying open water areas).</p>
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<p>Distribution map of vegetation cover water body area based on SW: (<b>a</b>) January 2019; (<b>b</b>) April 2019; (<b>c</b>) January 2020; (<b>d</b>) April 2020.</p>
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<p>Evaluation of SW’s performance in drawing VCW based on ground survey sample points: (<b>a</b>,<b>b</b>) January 2019; (<b>c</b>,<b>d</b>) January 2020; (<b>e</b>,<b>f</b>) April 2019; (<b>g</b>,<b>h</b>) April 2020.</p>
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24 pages, 5117 KiB  
Article
Estimation of Aboveground Biomass of Picea schrenkiana Forests Considering Vertical Zonality and Stand Age
by Guohui Zhang, Donghua Chen, Hu Li, Minmin Pei, Qihang Zhen, Jian Zheng, Haiping Zhao, Yingmei Hu and Jingwei Fan
Forests 2025, 16(3), 445; https://doi.org/10.3390/f16030445 - 1 Mar 2025
Viewed by 177
Abstract
The aboveground biomass (AGB) of forests reflects the productivity and carbon-storage capacity of the forest ecosystem. Although AGB estimation techniques have become increasingly sophisticated, the relationships between AGB, spatial distribution, and growth stages still require further exploration. In this study, the Picea schrenkiana [...] Read more.
The aboveground biomass (AGB) of forests reflects the productivity and carbon-storage capacity of the forest ecosystem. Although AGB estimation techniques have become increasingly sophisticated, the relationships between AGB, spatial distribution, and growth stages still require further exploration. In this study, the Picea schrenkiana (Picea schrenkiana var. tianschanica) forest area in the Kashi River Basin of the Ili River Valley in the western Tianshan Mountains was selected as the research area. Based on forest resources inventory data, Gaofen-1 (GF-1), Gaofen-6 (GF-6), Gaofen-3 (GF-3) Polarimetric Synthetic Aperture Radar (PolSAR), and DEM data, we classified the Picea schrenkiana forests in the study area into three cases: the Whole Forest without vertical zonation and stand age, Vertical Zonality Classification without considering stand age, and Stand-Age Classification without considering vertical zonality. Then, for each case, we used eXtreme Gradient Boosting (XGBoost), Back Propagation Neural Network (BPNN), and Residual Networks (ResNet), respectively, to estimate the AGB of forests in the study area. The results show that: (1) The integration of multi-source remote-sensing data and the ResNet can effectively improve the remote-sensing estimation accuracy of the AGB of Picea schrenkiana. (2) Furthermore, classification by vertical zonality and stand ages can reduce the problems of low-value overestimation and high-value underestimation to a certain extent. Full article
(This article belongs to the Special Issue Modeling Aboveground Forest Biomass: New Developments)
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<p>Geographic location map of the study area. (<b>a</b>) Position of the study area within China. (<b>b</b>) Position of the study area within Xinjiang Province. (<b>c</b>) Elevation map of the study area, along with the forest sample locations.</p>
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<p>Topographic feature map of the study area. (<b>a</b>) altitude map of the study area. (<b>b</b>) vertical zonality division map of the study area. (<b>c</b>) slope division map of the study area. (<b>d</b>) aspect division map of the study area.</p>
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<p>Classification map of stand ages of <span class="html-italic">Picea schrenkiana</span> forests.</p>
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<p>The framework of the Back Propagation Neural Network model.</p>
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<p>The framework of the Residual Network model. k represents the convolution kernel, s represents the stride, and p represents the padding.</p>
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<p>The accuracy of each model using multi-source data in the case of vertical zonality.</p>
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<p>The accuracy of each model using multi-source data in the case of stand ages.</p>
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<p>Accuracy of each model using multi-source data in the case of whole forest.</p>
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<p>AGB estimation results under three different modeling methods. (<b>a</b>) shows the output map of estimated AGB for the whole forest. (<b>b</b>) based on the classification of vertical zonality, shows the output map of estimated AGB. (<b>c</b>) based on the classification of stand ages, shows the output map of estimated AGB.</p>
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<p>The comparison of AGB estimation results between this study and Yang’s study. (<b>a</b>) the results of this experimental study; (<b>b</b>) The results of Yang’s study.</p>
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23 pages, 5172 KiB  
Article
Lake SkyWater—A Portable Buoy for Measuring Water-Leaving Radiance in Lakes Under Optimal Geometric Conditions
by Arthur Coqué, Guillaume Morin, Tiphaine Peroux, Jean-Michel Martinez and Thierry Tormos
Sensors 2025, 25(5), 1525; https://doi.org/10.3390/s25051525 - 28 Feb 2025
Viewed by 314
Abstract
This study introduces Lake SkyWater (LSW), a novel radiometric buoy designed for the reliable measurement of remote sensing reflectance (Rrs) in lakes using the Skylight-Blocked Approach (SBA). LSW addresses key challenges in “on-water” field radiometry owing to its motorised rotating system, [...] Read more.
This study introduces Lake SkyWater (LSW), a novel radiometric buoy designed for the reliable measurement of remote sensing reflectance (Rrs) in lakes using the Skylight-Blocked Approach (SBA). LSW addresses key challenges in “on-water” field radiometry owing to its motorised rotating system, which maintains the radiance sensor in optimal geometrical conditions (i.e., facing the sun). Our device is easy to transport and deploy and can be controlled with a smartphone over Wi-Fi. Its modular design, which uses standard components and custom 3D-printed parts, facilitates customisation. A field experiment demonstrated excellent performance in the visible spectrum (400–700 nm) and no significant differences compared with handheld SBA measurements when measuring Rrs (coefficient of determination > 0.99 and general accuracy (median symmetric accuracy) of ~2.43%). Areas for potential improvement were identified, such as refinement of orientation control and addressing the occasional rotation of the float. Nonetheless, LSW shortens the acquisition time, reduces the risk of fore-optics contamination, and ensures that the measurements are conducted under optimal geometric conditions. In conclusion, LSW is a promising instrument for the operational collection of high-quality Rrs spectra in lakes, which is important for advancing both research and monitoring applications in aquatic remote sensing. Full article
(This article belongs to the Section Environmental Sensing)
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<p>Lake SkyWater design and geometry. Sun-relative azimuths of the tilt and the radiance sensor (θ<sub>t</sub> and θ<sub>Lw</sub>, respectively). The waterline at a given tilt (φ<sub>t</sub>) is a plain line, and the submerged part of the device is hatched. The waterline if φ<sub>t</sub> were 0° is materialised as a dashed line.</p>
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<p>Study area (Bimont reservoir). (<b>a</b>) Location of Bimont reservoir; (<b>b</b>) Location of the sampling stations (+drift of the boat/buoy during measurements). (<b>c</b>) Lake SkyWater deployed on the reservoir.</p>
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<p>LSW measurements at the 1st station. (<b>a</b>) Sun-relative azimuth of the radiance sensor θ<sub>Lw</sub>; (<b>b</b>) R<sub>rs</sub> spectra; (<b>c</b>) sun-relative azimuth of the tilt θ<sub>t</sub>; (<b>d</b>) tilt of the buoy φ<sub>t</sub>. The markers in panels (<b>a</b>,<b>c</b>,<b>d</b>) indicate the sampling time of all radiometric measurements. The period delimited by the two vertical dotted lines (<b>a</b>,<b>c</b>,<b>d</b>) corresponds to the time when the IMU was not working properly. Measurements made during this period (indicated by orange squares and dashed R<sub>rs</sub> spectra) were excluded from further analysis.</p>
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<p>As in <a href="#sensors-25-01525-f003" class="html-fig">Figure 3</a>, but for the 2nd station. The vertical dotted line (on panels (<b>a</b>,<b>c</b>,<b>d</b>)) shows the time at which the buoy started to be in position. Measurements made prior to this time (<b>b</b>) (indicated by orange squares and dashed R<sub>rs</sub> spectra) were excluded from further analysis.</p>
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<p>As in <a href="#sensors-25-01525-f003" class="html-fig">Figure 3</a>, but for the 3rd station. The vertical dotted lines (on panels (<b>a</b>,<b>c</b>,<b>d</b>)) mark a period when the viewing geometry was not optimal. Measurements made during this period (<b>b</b>) (indicated by orange squares and dashed R<sub>rs</sub> spectra) have been excluded from further analysis.</p>
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<p>As in <a href="#sensors-25-01525-f003" class="html-fig">Figure 3</a>, but for the 4th station. The vertical dotted line (on panels (<b>a</b>,<b>c</b>,<b>d</b>)) shows the time at which the buoy started to be in a stable position. Measurements made prior to this time (<b>b</b>) (indicated by orange squares and dashed R<sub>rs</sub> spectra) have been excluded from further analysis.</p>
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<p>R<sub>rs</sub>/L<sub>w</sub>/E<sub>s</sub> measurements at the four sampling stations in Bimont reservoir using LSW and the handheld SBA protocol. The mean spectra and CV are represented with solid and dashed lines, respectively.</p>
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<p>Comparison of R<sub>rs</sub> measured by both LSW and the handheld SBA protocol in the 320–800 nm wavelength range. We used spectra with a 10 nm spectral step for the scatterplots, but statistics were computed with a spectral step of 1 nm. The solid and dashed lines represent the 1:1 and regression lines, respectively.</p>
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<p>Comparison of R<sub>rs</sub> measured by both LSW and the handheld SBA protocol. (<b>a</b>) Regression between <math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi mathvariant="normal">R</mi> </mrow> <mrow> <mi mathvariant="normal">r</mi> <mi mathvariant="normal">s</mi> </mrow> <mrow> <mi mathvariant="normal">L</mi> <mi mathvariant="normal">S</mi> <mi mathvariant="normal">W</mi> <mi mathvariant="normal">*</mi> </mrow> </msubsup> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi mathvariant="normal">R</mi> </mrow> <mrow> <mi mathvariant="normal">r</mi> <mi mathvariant="normal">s</mi> </mrow> <mrow> <mi mathvariant="normal">H</mi> <mi mathvariant="normal">H</mi> </mrow> </msubsup> </mrow> </semantics></math> on the visible part of the spectrum (400–700 nm); (<b>b</b>) regression between <math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi mathvariant="normal">R</mi> </mrow> <mrow> <mi mathvariant="normal">r</mi> <mi mathvariant="normal">s</mi> </mrow> <mrow> <mi mathvariant="normal">L</mi> <mi mathvariant="normal">S</mi> <mi mathvariant="normal">W</mi> <mi mathvariant="normal">*</mi> </mrow> </msubsup> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi mathvariant="normal">R</mi> </mrow> <mrow> <mi mathvariant="normal">r</mi> <mi mathvariant="normal">s</mi> </mrow> <mrow> <mi mathvariant="normal">H</mi> <mi mathvariant="normal">H</mi> </mrow> </msubsup> </mrow> </semantics></math> on the two spectral ends of the spectrum (320–400 nm and 700–800 nm). We used spectra with a 10 nm spectral step for the scatterplots, but statistics were computed with a spectral step of 1 nm. The solid and dashed lines represent the 1:1 and regression lines, respectively.</p>
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27 pages, 14257 KiB  
Article
Exploring Sentinel-1 Radar Polarisation and Landsat Series Data to Detect Forest Disturbance from Dust Events: A Case Study of the Paphos Forest in Cyprus
by Christos Theocharidis, Marinos Eliades, Polychronis Kolokoussis, Milto Miltiadou, Chris Danezis, Ioannis Gitas, Charalampos Kontoes and Diofantos Hadjimitsis
Remote Sens. 2025, 17(5), 876; https://doi.org/10.3390/rs17050876 - 28 Feb 2025
Viewed by 211
Abstract
Monitoring forest health has become essential due to increasing pressures caused by climate change and dust events, particularly in semi-arid regions. This study investigates the impact of dust events on forest vegetation in Paphos forest in Cyprus, which is a semi-arid area prone [...] Read more.
Monitoring forest health has become essential due to increasing pressures caused by climate change and dust events, particularly in semi-arid regions. This study investigates the impact of dust events on forest vegetation in Paphos forest in Cyprus, which is a semi-arid area prone to frequent dust storms. Using multispectral and radar satellite data from Sentinel-1 and Landsat series, vegetation responses to eight documented dust events between 2015 and 2019 were analysed, employing BFAST (Breaks For Additive Season and Trend) algorithms to detect abrupt changes in vegetation indices and radar backscatter. The outcomes showed that radar data were particularly effective in identifying only the most significant dust events (PM10 > 100 μg/m3, PM2.5 > 30 μg/m3), indicating that SAR (Synthetic Aperture Radar) is more responsive to pronounced dust deposition, where backscatter changes reflect more substantial vegetation stress. Conversely, optical data were sensitive to a wider range of events, capturing responses even at lower dust concentrations (PM10 > 50 μg/m3, PM2.5 > 20 μg/m3) and detecting minor vegetation stress through indices like SAVI, EVI, and AVI. The analysis highlighted that successful detection relies on multiple factors beyond sensor type, such as rainfall timing and imagery availability close to the dust events. This study highlights the importance of an integrated remote sensing approach for effective forest health monitoring in regions prone to dust events. Full article
(This article belongs to the Section Forest Remote Sensing)
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<p>(<b>Left</b>): Paphos forest, Cyprus with green colour (AoI). (<b>Right</b>): Heights distribution of the AoI. The red dot indicates the location of the Ayia Marina Xyliatou air quality monitoring station. The blue dots concern the sites of the four meteorological stations of the Department of Meteorology, Cyprus.</p>
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<p>Detection of abrupt changes with the BFAST decomposition algorithm for AVI (<b>a</b>), SAVI (<b>b</b>), EVI (<b>c</b>), and VV polarisation (<b>d</b>). The red line indicates the breaks in the trend component. Labelled breakpoints correspond to dust events, while other detected changes may result from different environmental factors.</p>
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<p>Detection of abrupt changes with the BFAST lite decomposition algorithm for VH (<b>a</b>), VV (<b>b</b>), SAVI (<b>c</b>), AVI polarisation (<b>d</b>), and EVI (<b>e</b>). Green and vertical blue lines indicate the breaks in the trend component. Labelled breakpoints correspond to dust events, while other detected changes may result from different environmental factors.</p>
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<p>Detection of an abrupt change in VV polarisation with the BFAST01 decomposition algorithm. The blue line indicates the break in the trend component. Labelled breakpoints correspond to dust events.</p>
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<p>PM2.5 data from the Ayia Marina Xyliatou station for the period 2015–2021 (blue lines). PM10 data from the Ayia Marina Xyliatou station for the period 2015–2021 (red lines).</p>
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<p>(<b>Left</b>) Dust storm in September 2015 in Cyprus captured by Terra–MODIS. (<b>Middle</b>) Dust score in the day (Daytime: 1:30 p.m.) as seen from the Advanced Infrared Sound (AIRS) on NASA’s Aqua satellite. (<b>Right</b>) Dust score in the night (Nighttime: 1:30 a.m.).</p>
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<p>(<b>Left</b>) Dust storm in May 2016 in Cyprus captured by Terra–MODIS. (<b>Middle</b>) Dust score in the day (Daytime: 1:30 p.m.) as seen from the Advanced Infrared Sound (AIRS) on NASA’s Aqua satellite. (<b>Right</b>) Dust score in the night (Nighttime: 1:30 a.m.).</p>
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<p>(<b>Left</b>) Dust storm in April 2017 in Cyprus captured by Terra–MODIS. (<b>Middle</b>) Dust score in the day (Daytime: 1:30 p.m.) as seen from the Advanced Infrared Sound (AIRS) on NASA’s Aqua satellite. (<b>Right</b>) Dust score in the night (Nighttime: 1:30 a.m.).</p>
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<p>(<b>Left</b>) Dust storm in March 2018 in Cyprus captured by Terra–MODIS. (<b>Middle</b>) Dust score in the day (Daytime: 1:30 p.m.) as seen from the Advanced Infrared Sound (AIRS) on NASA’s Aqua satellite. (<b>Right</b>) Dust score in the night (Nighttime: 1:30 a.m.).</p>
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<p>(<b>Left</b>) Dust storm in May 2018 in Cyprus captured by Terra–MODIS. (<b>Middle</b>) Dust score in the day (Daytime: 1:30 p.m.) as seen from the Advanced Infrared Sound (AIRS) on NASA’s Aqua satellite. (<b>Right</b>) Dust score in the night (Nighttime: 1:30 a.m.).</p>
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<p>(<b>Left</b>) Dust storm in October 2018 in Cyprus captured by Terra–MODIS. (<b>Middle</b>) Dust score in the day (Daytime: 1:30 p.m.) as seen from the Advanced Infrared Sound (AIRS) on NASA’s Aqua satellite. (<b>Right</b>) Dust score in the night (Nighttime: 1:30 a.m.).</p>
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<p>(<b>Left</b>) Dust storm in April 2019 in Cyprus captured by Terra–MODIS. (<b>Middle</b>) Dust score in the day (Daytime: 1:30 p.m.) as seen from the Advanced Infrared Sound (AIRS) on NASA’s Aqua satellite. (<b>Right</b>) Dust score in the night (Nighttime: 1:30 a.m.).</p>
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20 pages, 6737 KiB  
Article
Estimating Leaf Chlorophyll Fluorescence Parameters Using Partial Least Squares Regression with Fractional-Order Derivative Spectra and Effective Feature Selection
by Jie Zhuang and Quan Wang
Remote Sens. 2025, 17(5), 833; https://doi.org/10.3390/rs17050833 - 27 Feb 2025
Viewed by 136
Abstract
Chlorophyll fluorescence (ChlF) parameters serve as non-destructive indicators of vegetation photosynthetic function and are widely used as key input parameters in photosynthesis–fluorescence models. The rapid acquisition of the spatiotemporal dynamics of ChlF parameters is crucial for enhancing remote sensing applications and improving carbon [...] Read more.
Chlorophyll fluorescence (ChlF) parameters serve as non-destructive indicators of vegetation photosynthetic function and are widely used as key input parameters in photosynthesis–fluorescence models. The rapid acquisition of the spatiotemporal dynamics of ChlF parameters is crucial for enhancing remote sensing applications and improving carbon cycle modeling. While hyperspectral reflectance offers a promising data source for estimating ChlF parameters, previous studies have relied primarily on spectral indices derived from specific datasets, which often lack robustness. In this study, we simultaneously monitored ChlF parameters and spectral reflectance in leaves from different species, growth stages, and canopy positions within a temperate deciduous forest. We developed a data-driven partial least squares regression (PLSR) model by integrating fractional-order derivative (FOD) spectral transformation with multiple feature selection methods to predict ChlF parameters. The results demonstrated that FOD spectra effectively improved prediction accuracy compared to conventional PLSR attempts. Among the feature selection algorithms, the least absolute shrinkage and selection operator (LASSO) and stepwise regression (Stepwise) methods outperformed others. Furthermore, the LASSO-based PLSR model that used low-order (<1) FOD spectra achieved high predictive performance for NPQ (R2 = 0.60, RPD = 1.60, NRMSE = 0.16), ΦP (R2 = 0.73, RPD = 1.94, NRMSE = 0.11), ΦN (R2 = 0.62, RPD = 1.62, NRMSE = 0.12), and ΦF (R2 = 0.54, RPD = 1.48, NRMSE = 0.15). These findings suggest that the integration of FOD spectral transformation and appropriate feature selection enables the simultaneous estimation of multiple ChlF parameters, providing valuable insights for the retrieval of ChlF parameters from hyperspectral data. Full article
(This article belongs to the Collection Feature Paper Special Issue on Forest Remote Sensing)
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<p>Distribution and properties of six chlorophyll fluorescence (ChlF) parameters in the dataset: maximum quantum yield of PSII (PSII<sub>max</sub>), non-photochemical quenching (NPQ), the fraction of open reaction centers in photosystem II (qL), the quantum yield of photochemistry (ΦP), the quantum yield of non-regulated energy dissipation (ΦN), and the quantum yield of fluorescence emission (ΦF). The violin shapes represent the distribution density of the parameter values, with the width indicating the frequency of values at different levels. The box plots show the interquartile range, with the white line inside each box marking the median. The red dot in each plot represents the mean value of the parameter.</p>
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<p>Correlation coefficient (r) between wavelength and ChlF parameters across different FOD spectra (<b>a</b>–<b>u</b>). Different ChlF parameters are represented by distinct colors. Only statistically significant correlations (<span class="html-italic">p</span> &lt; 0.05) are displayed, while non-significant points are omitted.</p>
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<p>The correlation coefficient (r) matrix between wavelength and ChlF parameters across different FOD spectra. Only statistically significant correlations (<span class="html-italic">p</span> &lt; 0.05) are displayed, while non-significant points are omitted.</p>
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<p>The number of bands significantly correlated with the ChlF parameter varies across different derivative orders.</p>
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<p>Comparison of R<sup>2</sup>, RPD, NRMSE, and AICc for PLSR models based on different FOD spectra and feature selection methods using the test dataset (141 samples). Different feature selection methods are distinguished by color. Additionally, AICc is standardized (AICc<sub>scale</sub>) for easier comparison. Red circles indicate the best-performing models based on the highest R<sup>2</sup> and RPD values, and the lowest NRMSE and AICc values. For ΦF, the selected LASSO-PLSR model using 0.8-order FOD spectra is highlighted by a red square to balance model complexity and performance.</p>
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<p>The optimal PLSR model selected informative wavelengths for estimating ChlF parameters, with each parameter represented by a distinct color. The number of selected wavelengths is 49 for PSII<sub>max</sub>, 74 for NPQ, 77 for qL, 105 for ΦP, 25 for ΦN, and 73 for ΦF.</p>
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<p>The relative contribution of wavelengths in predicting ChlF parameters within the optimal PLSR model. Different ChlF parameters are represented by distinct colors. The figure shows the top ten wavelengths with the highest contributions.</p>
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<p>The variable importance in projection (VIP) scores of wavelengths for predicting ChlF parameters in the optimal PLSR model. Different ChlF parameters are represented by distinct colors. The black dashed line indicates a VIP score of 1, while the three wavelengths with the highest VIP scores are highlighted in red text.</p>
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<p>The distribution of wavelengths selected by the LASSO-based PLSR model across different FOD spectra for estimating ChlF parameters. Different spectral regions are represented by distinct colors.</p>
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<p>The number of wavelengths selected by the LASSO algorithm for estimating ChlF parameters varies across spectral regions and different FOD orders. Each region is represented by a distinct color. The black dashed line indicates the optimal FOD order, and the total number of bands selected for estimating PSII<sub>max</sub> (49), NPQ (74), qL (77), ΦP (105), ΦN (25), and ΦF (73) are shown.</p>
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15 pages, 2655 KiB  
Article
Environmental Heterogeneity Drives Secondary Metabolite Diversity from Mesquite Pods in Semiarid Regions
by Alfredo Esparza-Orozco, Liliana Carranza-Becerra, Lucía Delgadillo-Ruiz, Juan José Bollaín y Goytia, Norma Angélica Gaytán-Saldaña, Cruz Daniel Mandujano-García, Eladio Delgadillo-Ruiz, Claudia Yared Michel-López, Josefina Huerta-García, Benjamín Valladares-Carranza and Héctor Emmanuel Valtierra-Marín
Ecologies 2025, 6(1), 19; https://doi.org/10.3390/ecologies6010019 - 27 Feb 2025
Viewed by 146
Abstract
Secondary metabolites (SM) in plants play crucial pharmacological, ecological, and nutritional roles for humans, wildlife, and livestock. Environmental Heterogeneity (EH) encompasses the variability of biotic and abiotic factors that influence biological responses of plant species. Advancements in remote sensing have enhanced the ability [...] Read more.
Secondary metabolites (SM) in plants play crucial pharmacological, ecological, and nutritional roles for humans, wildlife, and livestock. Environmental Heterogeneity (EH) encompasses the variability of biotic and abiotic factors that influence biological responses of plant species. Advancements in remote sensing have enhanced the ability to assess plant functional traits more affordably and comprehensively by integrating spectral reflectance data with detailed plant metabolomics. However, studies investigating the relationship between EH—quantified using Rao’s Q heterogeneity index from remote sensing data—and SM diversity remain limited. Here, we present the first report demonstrating that the biotic component of EH, measured as Rao’s Q, is positively associated with SM diversity in mesquite pod extracts—higher Rao’s Q values correspond to greater SM diversity. Generalized additive models (GAMs) revealed that Rao’s Q contributed the most explanatory power, accounting for 21.2% of the deviance, compared to pod weight (13.7%) and pod length (2.03%). However, only the relationship between Rao’s Q and SM diversity was statistically significant (p = 0.029). The Rao’s Q index derived from remote sensing serves as a scalable proxy for identifying SM hotspots, facilitating the targeted discovery of regions with high pharmacological or nutritional value. Full article
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<p>Geographic distribution of mesquite trees sampled in three regions. The background shows the 30 × 30 m pixel scale map for land use and vegetation of Zacatecas, Mexico [<a href="#B37-ecologies-06-00019" class="html-bibr">37</a>]. The map was created using the QGIS version 3.28.7 [<a href="#B38-ecologies-06-00019" class="html-bibr">38</a>] software.</p>
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<p>Boxplot of (<b>a</b>) pod weight and (<b>b</b>) pod size across the southern, central, and northern regions. Each box represents the interquartile range (IQR), spanning from the first quartile (Q1) to the third quartile (Q3). The line inside the box indicates the median (Q2). The whiskers extend to the smallest and largest values within 1.5 × IQR beyond the quartiles.</p>
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<p>Boxplot showing the number of secondary metabolite classes detected in mesquite pod extracts (SM diversity; y axis) across the southern, central, and northern regions (x axis) using two extraction methods: ultrasound-assisted extraction (UAE) and ethanolic extraction (EE). Each box represents the interquartile range (IQR), spanning from the first quartile (Q1) to the third quartile (Q3). The line inside the box indicates the median (Q2). The whiskers extend to the smallest and largest values within 1.5 × IQR beyond the quartiles.</p>
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<p>Boxplot of the (<b>a</b>) Soil-Adjusted Vegetation Index (SAVI) and (<b>b</b>) environmental heterogeneity in terms of Rao’s Q observed across the southern, central, and northern regions. Each box represents the interquartile range (IQR), spanning from the first quartile (Q1) to the third quartile (Q3). The line inside the box indicates the median (Q2). The whiskers extend to the smallest and largest values within 1.5 × IQR beyond the quartiles.</p>
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<p>Principal component analysis (PCA) biplot shows the relationships between explanatory variables (dashed lines)—environmental heterogeneity in terms of Rao’s Q, pod length (cm), and pod weight (g)—and secondary metabolite classes detected (solid lines) in mesquite pods from ultrasound-assisted extraction (UAE), across the southern (gray color), central (blue color), and northern (yellow color) regions. The ellipses represent the three sampled regions based on the abundance of SM classes in each region.</p>
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<p>Relationships between secondary metabolite diversity (SM diversity; <span class="html-italic">y</span>-axis) and (<b>a</b>) environmental heterogeneity in terms of Rao’s Q, mesquite (<b>b</b>) pod weight and (<b>c</b>) pod size. The black line showed that the generalized additive models fit with the 95% confidence intervals (shaded blue area). The Adjusted coefficient of determination, Adjusted (<span class="html-italic">R</span><sup>2</sup><sub>Adjusted</sub>); probability (<span class="html-italic">p</span>); and Akaike Information Criterion (AIC) are shown.</p>
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<p>Boxplot showing the secondary metabolite diversity (SM diversity) across the low and high levels of (<b>a</b>) environmental heterogeneity in terms of Rao’s Q, (<b>b</b>) mesquite pod weight, (<b>c</b>) small and large sizes of mesquite pods. Each box represents the interquartile range (IQR), spanning from the first quartile (Q1) to the third quartile (Q3). The line inside the box indicates the median (Q2). The whiskers extend to the smallest and largest values within 1.5 × IQR beyond the quartiles.</p>
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25 pages, 15584 KiB  
Article
Inland Water Quality Monitoring Using Airborne Small Cameras: Enhancing Suspended Sediment Retrieval and Mitigating Sun Glint Effects
by Diogo Olivetti, Henrique L. Roig, Jean-Michel Martinez, Alexandre M. R. Ferreira, Rogério R. Marinho, Ronaldo L. Mincato and Eduardo Sávio P. R. Martins
Drones 2025, 9(3), 173; https://doi.org/10.3390/drones9030173 - 26 Feb 2025
Viewed by 224
Abstract
The ongoing advancement of unmanned aerial vehicles (UAVs) and the evolution of small-scale cameras have bridged the gap between traditional ground-based surveys and orbital sensors. However, these systems present challenges, including limited coverage area, image stabilization constraints, and complex image processing. In water [...] Read more.
The ongoing advancement of unmanned aerial vehicles (UAVs) and the evolution of small-scale cameras have bridged the gap between traditional ground-based surveys and orbital sensors. However, these systems present challenges, including limited coverage area, image stabilization constraints, and complex image processing. In water quality monitoring, these difficulties are further compounded by sun glint effects, which hinder the construction of accurate orthomosaics in homogeneous water surfaces and affect radiometric accuracy. This study focuses on evaluating these challenges by comparing two distinct airborne imaging platforms with different spectral resolutions, emphasizing Total Suspended Solids (TSS) monitoring. Hyperspectral airborne surveys were undertaken utilizing a pushbroom system comprising 276 bands, whereas multispectral airborne surveys were conducted employing a global shutter frame with 4 bands. Fifteen aerial survey campaigns were carried out over water bodies from two biomes in Brazil (Amazon and Savanna), at varying concentrations of TSS (0.6–130.7 mg L−1, N: 53). Empirical models using near-infrared channels were applied to accurately monitor TSS in all areas (Hyperspectral camera—RMSE = 3.6 mg L−1, Multispectral camera—RMSE = 9.8 mg L−1). Furthermore, a key contribution of this research is the development and application of Sun Glint mitigation techniques, which significantly improve the reliability of airborne reflectance measurements. By addressing these radiometric challenges, this study provides critical insights into the optimal UAV platform for TSS monitoring in inland waters, enhancing the accuracy and applicability of airborne remote sensing in aquatic environments. Full article
(This article belongs to the Special Issue Applications of UVs in Digital Photogrammetry and Image Processing)
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<p>Study areas across various basins and biomes in Brazil. (<b>A</b>) turbid and dark waters in the Amazon basin; (<b>B</b>) small inflows and river confluences into urban (<span class="html-italic">Paranoá</span>) and rural (<span class="html-italic">Corumbá IV</span>) reservoirs in the <span class="html-italic">Paraná</span> basin; (<b>C</b>) inflow area of a large reservoir (<span class="html-italic">Três marias</span>) and the entire open water area of a medium reservoir (<span class="html-italic">Retiro Baixo</span>) in the <span class="html-italic">São Francisco</span> basin; and (<b>D</b>) stretches of the <span class="html-italic">Paraopeba</span> river under the influence of sediment originating from a tailing dam collapse during the <span class="html-italic">Brumadinho</span> disaster in 2019.</p>
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<p>Depiction of the Sequoia (<b>c</b>,<b>d</b>) camera affixed to the Parrot Disco Pro AG (<b>b</b>) and DJI Phantom 4 (<b>a</b>) UAVs, facilitated by the utilization of a bracket and 3D printing. Source: Parrot 2020.</p>
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<p>Hedawall Nano-Hyperspec camera (<b>a</b>) and its IMU (<b>b</b>) installed on a helicopter using a metal bracket and supported by the DJI RONIM MX gimbal. (<b>c</b>): image captured during the flight over the <span class="html-italic">Três Marias</span> reservoir (<a href="#drones-09-00173-f001" class="html-fig">Figure 1</a>C).</p>
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<p>Flowchart of methodological procedures for TSS mapping from the multispectral and hyperspectral airborne platforms and the indication of an ideal platform for effectively monitoring TSS for small and large inland water bodies.</p>
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<p>Image excerpt extracted from the orthomosaic generation process using Pix4D Mapper software. Sequoia images were acquired in Amazon. The red annotations signify images that did not align with adjacent overlapping images, particularly those acquired farther inland along the <span class="html-italic">Solimões</span> River. The green/blue dots represent images that have been successfully aligned with their neighboring images in heterogeneous areas.</p>
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<p>Scanned images captured by the Nano-Hyperspec camera during helicopter flights over the <span class="html-italic">Três Marias</span> reservoir (<b>left</b>) and the <span class="html-italic">Retiro Baixo</span> reservoir (<b>right</b>).</p>
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<p>Example of Sequoia camera images affected and unaffected by the sun glint effect. At the confluence of the <span class="html-italic">Negro</span> and <span class="html-italic">Solimões</span> rivers (<b>A</b>: RGB lens, <b>B</b>: NIR band), sun glint is visible in images acquired at a solar angle of 0.17°. In contrast, images from the Paranoá Reservoir (<b>C</b>: RGB lens, <b>D</b>: NIR band) show no sun glint, as they were captured at a solar angle of 0.72°. All images were captured with the camera angle at 90°.</p>
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<p>Dense point cloud depiction, created using the Pix4D Mapper software, originating from the Sequoia camera images in Amazon. The frame (<b>A</b>) emphasizes a randomly selected point within the mapped region, with all corresponding covering images marked by the green line. In frame (<b>B</b>), various images covering this point are showcased, both with and without sun glint presence.</p>
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<p>Orthomosaic comparison of NIR asSR from the Sequoia camera in Amazon, depicting (<b>A</b>) the pre-processed state and (<b>B</b>) the post-processed condition removing images presenting sun glint.</p>
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<p>In situ water remote sensing reflectance and the associated r and R<sup>2</sup> values in relation to the TSS concentrations for each band (~2 nm). Grayscale variations correspond to TSS levels. TSS range: 0.6–130.7 mg L<sup>−1</sup>, N: 88.</p>
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<p>Scatter plot illustrates the correlation between simulated and empirical individual bands of the Sequoia camera (<a href="#drones-09-00173-t001" class="html-table">Table 1</a>).</p>
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<p>Scatter plot depicting the relationship between asSR values of the Sequoia camera bands and TSS concentrations (<a href="#drones-09-00173-t001" class="html-table">Table 1</a>).</p>
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<p>TSS maps depicting different areas, including: (<b>A</b>,<b>B</b>) confluence area between tributary rivers and the <span class="html-italic">Corumbá IV</span> and <span class="html-italic">Paranoá</span> reservoirs, emphasizing the sediment plume from urban drainage; (<b>C</b>) high concentrations in the <span class="html-italic">Solimões</span> River and low concentrations in the <span class="html-italic">Negro</span> River, and the mingling of waters between the two rivers (<b>C</b>); (<b>D</b>) Contrast between the turbid waters of the <span class="html-italic">Solimões</span> River and certain artificial ponds, juxtaposed with the clear waters of <span class="html-italic">igarapés</span> and other artificial ponds.</p>
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<p>(<b>above</b>): R<sub>rs</sub> in situ spectra (Equation (1)) acquired <span class="html-italic">by</span> the Ramses spectroradiometer during the field campaign in <span class="html-italic">Brumadinho</span>. (<b>below</b>): asSR spectra of the Nano-Hyperspec camera (<a href="#sec2dot2-drones-09-00173" class="html-sec">Section 2.2</a>) acquired during the helicopter aerosurveys in <span class="html-italic">Brumadinho</span>. Both graphs also include the plotted r and R<sup>2</sup> values concerning TSS concentrations for each respective band. TSS: 0.6–30.2, N: 18. The R<sub>rs</sub> spectra (<b>above</b>) are taken as a reference. Therefore, it can be concluded that the asSR spectra (<b>below</b>) were consistently calibrated, as indicated by their similarity to the upper graph.</p>
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<p>TSS map of the <span class="html-italic">Paraopeba</span> River, accentuating the confluence area with the tailing’s slurry.</p>
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<p>TSS map of the <span class="html-italic">Três Marias</span> and <span class="html-italic">Retiro Baixo</span> reservoirs, indicating low concentrations and confirming that the tailings sludge did not reach the reservoirs or the <span class="html-italic">São Francisco</span> River.</p>
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19 pages, 5600 KiB  
Article
Antarctic Sea Ice Extraction for Remote Sensing Images via Modified U-Net Based on Feature Enhancement Driven by Graph Convolution Network
by Wu Feng, Xiulin Geng, Xiaoyu He, Miao Hu, Jie Luo and Meihua Bi
J. Mar. Sci. Eng. 2025, 13(3), 439; https://doi.org/10.3390/jmse13030439 - 25 Feb 2025
Viewed by 352
Abstract
Antarctic true-color imagery synthesized using multispectral remote sensing data is effective in reflecting sea ice conditions, which is crucial for monitoring. Deep learning has been explored for sea ice extraction, but traditional convolutional neural network models are constrained by a limited perceptual field, [...] Read more.
Antarctic true-color imagery synthesized using multispectral remote sensing data is effective in reflecting sea ice conditions, which is crucial for monitoring. Deep learning has been explored for sea ice extraction, but traditional convolutional neural network models are constrained by a limited perceptual field, making it difficult to obtain global contextual information from remote sensing images. A novel model named GEFU-Net, a modification of U-Net, is presented. The self-established graph reconstruction module is employed to convert features into graph data and construct the adjacency matrix using a global adaptive average similarity threshold. Graph convolutional networks are utilized to aggregate the features at each pixel, enabling the rapid capture of global context, enhancing the semantic richness of the features, and improving the accuracy of sea ice extraction through graph reconstruction. Experimental results using the sea ice dataset of the Ross Sea in the Antarctic, produced by Sentinel-2, demonstrate that our GEFU-Net achieves the best performance compared to other commonly used segmentation models. Specifically, it achieves an accuracy of 97.52%, an Intersection over Union of 95.66%, and an F1-Score of 97.78%. Additionally, fewer model parameters and good inference speed are demonstrated, indicating strong potential for practical ice mapping applications. Full article
(This article belongs to the Section Physical Oceanography)
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<p>The area of interest for this study. (<b>a</b>) The red rectangles represent specific geographic areas. (<b>b</b>) The specific location of each scene.</p>
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<p>A schematic diagram of the Sentinel-2 data preprocessing.</p>
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<p>A schematic diagram of the sea ice annotation.</p>
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<p>A flowchart of sea ice extraction using Sentinel-2 data in our scheme.</p>
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<p>The overall structure of the proposed GEFU-Net.</p>
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<p>A schematic diagram of the encoder, consisting of ResBlocks and ConvBlocks.</p>
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<p>Different down-sampling operations in the residual branch. (<b>a</b>) Convolution, (<b>b</b>) average pool.</p>
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<p>A schematic diagram of the decoder, consisting of UpsampleBlocks.</p>
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<p>A schematic diagram of the SEGR module.</p>
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<p>Sea ice extraction results from different models. (<b>a</b>) TCI, (<b>b</b>) ground truth, (<b>c</b>) SegNet, (<b>d</b>) PSPNet, (<b>e</b>) DeepLab, (<b>f</b>) U-Net, (<b>g</b>) TransU-Net, (<b>h</b>) ABU-Net, (<b>i</b>) GEFU-Net.</p>
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<p>Comparison of different adjacency matrix generation methods. (<b>a</b>) Euclidean distance. (<b>b</b>) Manhattan distance.</p>
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<p>Effect of GCN layers in SEGR module on extraction results.</p>
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<p>GEFU-Net applied for automatic ice mapping using Sentinel-2 data. (<b>a</b>) Flowchart of ice mapping. (<b>b</b>) Ice mapping results—dark blue for open water, light blue for sea ice.</p>
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<p>Parameter size and inference time of different models.</p>
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24 pages, 7242 KiB  
Article
Surface Soil Moisture Estimation Taking into Account the Land Use and Fractional Vegetation Cover by Multi-Source Remote Sensing
by Rencai Lin, Xiaohua Xu, Xiuping Zhang, Zhenning Hu, Guobin Wang, Yanping Shi, Xinyu Zhao and Honghui Sang
Agriculture 2025, 15(5), 497; https://doi.org/10.3390/agriculture15050497 - 25 Feb 2025
Viewed by 244
Abstract
Surface soil moisture (SSM) plays a pivotal role various fields, including agriculture, hydrology, water environment, and meteorology. To investigate the impact of land use types and fractional vegetation cover (FVC) on the accuracy of SSM estimation, this study conducted a comprehensive analysis of [...] Read more.
Surface soil moisture (SSM) plays a pivotal role various fields, including agriculture, hydrology, water environment, and meteorology. To investigate the impact of land use types and fractional vegetation cover (FVC) on the accuracy of SSM estimation, this study conducted a comprehensive analysis of SSM estimation performance across diverse land use scenarios (e.g., multiple land use combinations and cropland) and varying FVC conditions. Sentinel-2 NDVI and MOD09A1 NDVI were fused by the Enhanced Spatial and Temporal Adaptive Reflection Fusion Model (ESTARFM) to obtain NDVI with a temporal resolution better than 8 d and a spatial resolution of 20 m, which improved the matching degree between NDVI and the Sentinel-1 backscattering coefficient (σ0). Based on the σ0, NDVI, and in situ SSM, combined with the water cloud model (WCM), the SSM estimation model is established, and the model of each land use and FVC is validated. The model has been applied in Handan. The results are as follows: (1) Compared with vertical–horizontal (VH) polarization, vertical–vertical (VV) polarization is more sensitive to soil backscattering (σsoil0). In the model for multiple land use combinations (Multiple-Model) and the model for the cropland (Cropland-Model), the R2 increases by 0.084 and 0.041, respectively. (2) The estimation accuracy of SSM for the Multiple-Model and Cropland-Model is satisfactory (Multiple-Model, RMSE = 0.024 cm3/cm3, MAE = 0.019 cm3/cm3, R2 = 0.891; Cropland-Model, RMSE = 0.023 cm3/cm3, MAE = 0.018 cm3/cm3, R2 = 0.886). (3) When the FVC > 0.75, the accuracy of SSM by the WCM is low. It is suggested the model should be applied to the cropland where the FVC ≤ 0.75. This study clarified the applicability of SSM estimation by microwave remote sensing (RS) in different land uses and FVCs, which can provide scientific reference for regional agricultural irrigation and agricultural water resources management. The findings highlight that the VV polarization-based model significantly improves SSM estimation accuracy, particularly in croplands with FVC ≤ 0.75, offering a reliable tool for optimizing irrigation schedules and enhancing water use efficiency in agriculture. These results can aid in better water resource management, especially in regions with limited water availability, by providing precise soil moisture data for informed decision-making. Full article
(This article belongs to the Section Digital Agriculture)
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<p>Distribution of SM observation sites and various land uses in the Haihe basin [<a href="#B29-agriculture-15-00497" class="html-bibr">29</a>]. The in situ SSM in Area 1 is used for model construction, and the in situ SSM in Area 2 is used for validation. (<b>a</b>) map of China; (<b>b</b>) distribution of land use in Haihe Basin.</p>
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<p>A sketch of the SM observation instrument.</p>
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<p>Flowchart for mapping SSM. Data sources include RS (i.e., S1, S2, and MOD09A1) and in situ SSM.</p>
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<p>The use of MOD09A1 and S2, as well as the corresponding date of data fusion in 2020. For example, 2 February and 31 January 2020, and 5 March and 1 March 2020 are two pairs of coarse and fine spatial resolution data, which can be fused to obtain NDVI with a spatial resolution of 20 m in 10 February, 18 February, and 26 February 2020.</p>
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<p>Spatial distribution of multi-source NDVI (MODIS-NDVI, S2-NDVI, and EST-NDVI) in a 1 km × 1 km sub-region of Area 1 on selected dates in 2020. The scatter plots show the relationship between S2-NDVI and EST-NDVI pixel values, with statistical metrics indicating the accuracy of the fusion process. Subfigures (<b>a</b>–<b>d</b>), (<b>e</b>–<b>h</b>), (<b>i</b>–<b>l</b>), (<b>m</b>–<b>p</b>), (<b>q</b>–<b>t</b>), and (<b>u</b>–<b>x</b>) represent the MODIS-NDVI, S2-NDVI, EST-NDVI, and the corresponding validation scatter plots for the dates of 13 March, 22 April, 16 May, 1 June, 4 August, and 21 September 2020, respectively.</p>
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<p>The σ<sup>0</sup><sub>soil</sub> for different polarization modes. Blue represents VV polarization and red represents VH polarization.</p>
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<p>SSM estimation model under different polarization modes and different land use types. The first row is VV polarization, and the second row is VH polarization. The first column is multiple land use combinations, the second column is farmland, the third column is forest, and the fourth column is grassland.</p>
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<p>Estimated SSM over the validation site “Area 2” from the entire database (multiple land use combinations and cropland) in different polarizations.</p>
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<p>The SSM estimation model under different FVC intervals in VV polarization: (<b>a</b>) VV-Multiple with low coverage; (<b>b</b>) VV-Multiple with middle coverage; (<b>c</b>) VV-Multiple with mid-high coverage; (<b>d</b>) VV-Multiple with high coverage; (<b>e</b>) VV-Cropland with low coverage; (<b>f</b>) VV-Cropland with middle coverage; (<b>g</b>) VV-Cropland with mid-high coverage; (<b>h</b>) VV-Cropland with high coverage.</p>
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<p>SSM estimation model under different FVC intervals in VH polarization: (<b>a</b>) VH-Multiple with low coverage; (<b>b</b>) VH-Multiple with middle coverage; (<b>c</b>) VH-Multiple with mid-high coverage; (<b>d</b>) VH-Multiple with high coverage; (<b>e</b>) VH-Cropland with low coverage; (<b>f</b>) VH-Cropland with middle coverage; (<b>g</b>) VH-Cropland with mid-high coverage; (<b>h</b>) VH-Cropland with high coverage.</p>
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<p>Estimated SSM over the validation site “Area 2” from the entire database (multiple land use combinations and cropland) in VV polarization: (<b>a</b>) VV-Multiple with low coverage; (<b>b</b>) VV-Multiple with middle coverage; (<b>c</b>) VV-Multiple with mid-high coverage; (<b>d</b>) VV-Multiple with high coverage; (<b>e</b>) VV-Cropland with low coverage; (<b>f</b>) VV-Cropland with middle coverage; (<b>g</b>) VV-Cropland with mid-high coverage; (<b>h</b>) VV-Cropland with high coverage.</p>
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<p>Spatial distribution of SSM in the winter wheat growing season in Handan, Haihe Basin.</p>
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<p>Spatial distribution of SSM in the summer maize growing season in Handan, Haihe Basin.</p>
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16 pages, 2165 KiB  
Review
Decoding Soil Color: Origins, Influences, and Methods of Analysis
by Yaowarat Sirisathitkul and Chitnarong Sirisathitkul
AgriEngineering 2025, 7(3), 58; https://doi.org/10.3390/agriengineering7030058 - 25 Feb 2025
Viewed by 257
Abstract
Soil color serves as a critical indicator of its properties and conditions. It is shaped by a complex interplay of mineral and organic matter content, moisture levels, and other environmental variables. Additionally, human activities such as land-use changes and intensive agricultural practices can [...] Read more.
Soil color serves as a critical indicator of its properties and conditions. It is shaped by a complex interplay of mineral and organic matter content, moisture levels, and other environmental variables. Additionally, human activities such as land-use changes and intensive agricultural practices can profoundly alter soil color. Soil color, driven by the presence of organic matter, plays a crucial role in understanding soil fertility. Its strong correlation with soil organic carbon content makes it a valuable parameter for assessing soil quality in agricultural practices. A variety of techniques have been developed to measure soil color, ranging from traditional Munsell color matching to modern color meters. Digital image colorimetry enables rapid on-site assessments of soil color, but environmental conditions such as soil water content and lighting conditions should be considered. Spectroscopic methods, particularly diffuse reflectance spectroscopy, pave the way for a more reliable and accurate composition analysis. Advances in remote sensing and computational methods are combined to explore the intricate relationships between soil color and environmental factors. Such an integrated approach not only enhances scalability but also leads to more insights and actionable strategies for environmental management and sustainable agriculture. Full article
(This article belongs to the Special Issue Recent Trends and Advances in Agricultural Engineering)
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<p>Summary of content effect on soil color.</p>
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