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Search Results (18,309)

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23 pages, 4982 KiB  
Article
Emission Estimation and Spatiotemporal Distribution of Passenger Ships Using Multi-Source Data: A Case from Zhoushan (China)
by Xubiao Xu, Xingyu Liu, Lin Feng, Wei Yim Yap and Hongxiang Feng
J. Mar. Sci. Eng. 2025, 13(1), 168; https://doi.org/10.3390/jmse13010168 (registering DOI) - 18 Jan 2025
Abstract
Quantifying and estimating shipping emissions is a critical component of global emission reduction research and has become a growing area of interest in recent years. However, emissions from short-distance passenger ships operating on inter-island routes and their environmental impacts have received limited attention. [...] Read more.
Quantifying and estimating shipping emissions is a critical component of global emission reduction research and has become a growing area of interest in recent years. However, emissions from short-distance passenger ships operating on inter-island routes and their environmental impacts have received limited attention. This contribution investigated the temporal and spatial distribution characteristics of pollutants emitted by short-distance passenger ships at Zhoushan (China) using Automatic Identification System (AIS) data and the bottom–up emission model integrated with multi-source meteorological data. A year-long emission inventory was investigated. The results indicated that high-speed passenger ships contributed to the largest share of the emissions. The emissions were predominantly concentrated during daytime hours, with the routes between Zhoushan Island and Daishan, Daishan and Shengsi, and Zhoushan Island and Liuheng Island accounting for most of the emissions. Furthermore, intra-port waterways were identified as the primary emission areas for short-distance passenger ships. This study provides essential data support and references for the relevant authorities to understand the emission patterns of short-distance passenger ships, thereby facilitating the formulation of targeted emission reduction strategies for the maritime passenger transport sector. Full article
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<p>Berthing (<b>a</b>) and unberthing (<b>b</b>) process of a passenger ship.</p>
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<p>Logic framework.</p>
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<p>Map of the study area.</p>
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<p>Passenger ship trajectory distribution in Zhoushan area. (Green for ordinary passenger ships, blue for Ro-Ro passenger ships, red for high-speed passenger ships, and yellow for ferries). (<b>a</b>) Ordinary passenger ships, (<b>b</b>) Ro-Ro passenger ships, (<b>c</b>) high-speed passenger ships, and (<b>d</b>) ferries.</p>
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<p>Variation in emissions of individual pollutants over the year (CO<sub>2</sub> on the <b>left</b>, other pollutants on the <b>right</b>).</p>
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<p>Distribution of emissions throughout the day (CO<sub>2</sub> on the <b>left</b>, other pollutants on the <b>right</b>).</p>
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<p>Annual emission distribution of each pollutant.</p>
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<p>Daily changes in CO<sub>2</sub> emissions.</p>
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<p>Percentage of emissions of each pollutant from different types of passenger ships.</p>
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<p>Proportion of emissions from passenger ships during different modes of operation.</p>
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<p>Spatial distribution of annual CO<sub>2</sub> passenger ship emissions.</p>
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21 pages, 11316 KiB  
Article
Investigating Human Influence on Offshore Terrestrial Organic Carbon Trends in a High-Energy Delta: The Ayeyarwady Delta, Myanmar
by Evan R. Flynn and Steven A. Kuehl
J. Mar. Sci. Eng. 2025, 13(1), 163; https://doi.org/10.3390/jmse13010163 (registering DOI) - 18 Jan 2025
Viewed by 116
Abstract
The continental margin is a major repository for organic carbon; however, anthropogenic alterations to global sediment and particulate terrestrial organic carbon (TerrOC) fluxes have reduced delivery by rivers and offshore burial in recent decades. Despite the absence of mainstem damming, land use change [...] Read more.
The continental margin is a major repository for organic carbon; however, anthropogenic alterations to global sediment and particulate terrestrial organic carbon (TerrOC) fluxes have reduced delivery by rivers and offshore burial in recent decades. Despite the absence of mainstem damming, land use change in the Ayeyarwady and Thanlwin River catchments in Myanmar has accelerated over the last 50 years. As a result, deforestation and landscape erosion have likely altered fluvial fluxes to the Northern Andaman Sea shelf; however, the magnitude and preservation of geochemical signals associated with development are unknown. Utilizing elemental and bulk stable and radioisotope analysis, this study investigates spatial and temporal trends in sediment sources and TerrOC concentrations to identify the potential impacts of recent (<100 years) offshore development. While our results demonstrate an along-shelf trend in provenance and TerrOC concentrations, temporal (downcore) trends are not observed. We attribute this observation to frequent, large-scale seabed resuspension and suggest that extensive mixing on the inner shelf creates a low-pass filter that effectively attenuates such signatures. This is in contrast to other large Asian deltas, where signals of human landscape disturbance are clearly preserved offshore. We predict that planned mainstem damming in Myanmar will result in larger alterations in sediment and TerrOC supply that may become apparent offshore in the near future. Full article
(This article belongs to the Section Geological Oceanography)
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<p>Reference and core location maps for the Ayeyarwady Delta, Myanmar: (<b>A</b>) Ayeyarwady and Thanlwin Rivers along with other major rivers in Asia; (<b>B</b>) Andaman Sea bathymetry and regional tectonic setting (Bathymetry from [<a href="#B45-jmse-13-00163" class="html-bibr">45</a>]); (<b>C</b>) Study area with coring sites from [<a href="#B40-jmse-13-00163" class="html-bibr">40</a>] (red circles) and Pathein, Yangon, and Thanlwin river sampling locations from [<a href="#B40-jmse-13-00163" class="html-bibr">40</a>,<a href="#B46-jmse-13-00163" class="html-bibr">46</a>] (indicated by green, red, and blue stars, respectively). Black circles around coring sites indicate that no <sup>7</sup>Be was detected in surface sediment, whereas yellow circles indicate the presence of <sup>7</sup>Be. The region of modern sediment accumulation on the shelf is indicated by the black polygon [<a href="#B42-jmse-13-00163" class="html-bibr">42</a>]. Depositional regions are separated by dashed lines into (<b>A</b>) the NW shelf, (<b>B</b>) “Mouths of the Ayeyarwady”, (<b>C</b>) the Gulf of Martaban, and (<b>D</b>) the Martaban Depression. Smoothed bathymetric contours (gray lines) are shown in meters of water depth (adapted from [<a href="#B45-jmse-13-00163" class="html-bibr">45</a>]).</p>
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<p>Core-averaged organic carbon and surface area results including (<b>A</b>) TOC (%), (<b>B</b>) TerrOC wt.%, (<b>C</b>) surface area (SA), and (<b>D</b>) organic carbon loading (OC/SA). Coring locations are shown as black circles. Locations of Pathein, Yangon, and Thanlwin river end-members are shown as green, red, and blue stars, respectively. The black polygon indicates the region of modern sediment accumulation as defined in [<a href="#B42-jmse-13-00163" class="html-bibr">42</a>].</p>
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<p>Organic carbon loading (OC/SA) plotted in relation to grain size parameters for each of the offshore regions with the Gulf and Depression shown in blue, “Mouths of the Ayeyarwady” in yellow, and the NW shelf in red.</p>
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<p>Example downcore plots of δ<sup>13</sup>C, TOC, TerrOC, and OC/SA from the (<b>A</b>) Gulf of Martaban (KC-04), (<b>B</b>) Martaban Depression clinoform forests (KC-02), (<b>C</b>) “Mouths of the Ayeyarwady” (KC-24), and (<b>D</b>) NW shelf (KC-21). Red dashed lines indicate the depth of the SML, and blue dashed lines indicate the depth at which excess <sup>210</sup>Pb is no longer detectable. Overall, cores from all regions demonstrate a lack of downcore change with relatively consistent δ<sup>13</sup>C, TOC, TerrOC, and OC/SA at depth. Organic carbon data for all cores can be found in <a href="#app1-jmse-13-00163" class="html-app">Table S1</a>.</p>
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<p>Example downcore plots of surface area (SA), D<sub>50</sub>, D<sub>90</sub>, and mud content (%) from the (<b>A</b>) Gulf of Martaban (KC-04), (<b>B</b>) Martaban Depression clinoform forests (KC-02), (<b>C</b>) “Mouths of the Ayeyarwady” (KC-24), and (<b>D</b>) NW shelf (KC-21). Red dashed lines indicate the depth of the SML, and blue dashed lines indicate the depth at which excess <sup>210</sup>Pb is no longer detectable. SA and grain size for all cores can be found in <a href="#app1-jmse-13-00163" class="html-app">Tables S2 and S3</a>, respectively.</p>
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<p>Correlations between surface area (SA) and grain size parameters, including D<sub>50</sub>, D<sub>90</sub>, and mud content for all sediment samples analyzed. D<sub>90</sub> exhibits the strongest correlation with SA; however, all grain size parameters show minimal change once SA reaches over 20 m<sup>2</sup>g<sup>−1</sup>. Depositional regions are indicated by color, with the Gulf and Depression shown in blue, “Mouths of the Ayeyarwady” in yellow, and the NW shelf in red.</p>
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<p><sup>210</sup>Pb accumulation rates plotted in relation to (<b>Left</b>) core-averaged OC/SA and (<b>Right</b>) average downcore changes in TerrOC by wt.%. Downcore change in TerrOC by wt.% was calculated for each core by subtracting the observed TerrOC wt.% at the bottom of the core from that at the surface. Positive values thus indicate a decrease in TerrOC at depth, while negative values indicate an increase in TerrOC at depth. In both plots, depositional regions on the shelf are plotted by color, with the Gulf of Martaban and Martaban Depression shown in blue, “Mouths of the Ayeyarwady” shown in yellow, and the NW shelf shown in red.</p>
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<p>XRF ratios (<b>A</b>) Ni/Rb and (<b>B</b>) Zn/La are indicative of sediment sources from the Ayeyarwady and Indo-Burman Range and Thanlwin, respectively. Coring locations are shown as black circles, and Pathein, Yangon, and Thanlwin River end-member sample locations are shown as green, red, and blue stars, respectively. The black polygon on the Northern Andaman Sea shelf represents the region of modern sediment accumulation [<a href="#B42-jmse-13-00163" class="html-bibr">42</a>].</p>
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<p>Examples of downcore XRF elemental ratios and core X-rays from the (<b>A</b>) Gulf of Martaban (GC-29), (<b>B</b>) Martaban Depression (GC-09), and (<b>C</b>,<b>D</b>) NW shelf (GC-21 and GC-17, respectively). High Ni/Rb ratios (blue) are indicative of sediment sourced from Ayeyarwady distributaries, while high Zn/La ratios (pink) are indicative of sediment sourced from the Thanlwin. 3 cm moving average ratios are plotted for both ratios as solid black lines. Core average ratios are plotted as dashed black lines. Red dashed lines indicate the depth of the SML when present. Core X-ray images are from [<a href="#B40-jmse-13-00163" class="html-bibr">40</a>]. XRF ratios for all cores are found in <a href="#app1-jmse-13-00163" class="html-app">Table S5</a>.</p>
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20 pages, 15835 KiB  
Article
Monitoring Sea Surface Temperature and Sea Surface Salinity Around the Maltese Islands Using Sentinel-2 Imagery and the Random Forest Algorithm
by Gareth Craig Darmanin, Adam Gauci, Monica Giona Bucci and Alan Deidun
Appl. Sci. 2025, 15(2), 929; https://doi.org/10.3390/app15020929 (registering DOI) - 18 Jan 2025
Viewed by 116
Abstract
Marine regions are undergoing rapid evolution, primarily driven by natural and anthropogenic activities. Safeguarding these ecosystems necessitates the ability to observe their physical features and control processes with precision in both space and time. This demands the acquisition of precise and up-to-date information [...] Read more.
Marine regions are undergoing rapid evolution, primarily driven by natural and anthropogenic activities. Safeguarding these ecosystems necessitates the ability to observe their physical features and control processes with precision in both space and time. This demands the acquisition of precise and up-to-date information regarding several marine parameters. Thus, to gain a comprehensive understanding of these ecosystems, this study employs remote sensing techniques, Machine Learning algorithms and traditional in situ approaches. Together, these serve as valuable tools to help comprehend the distinctive parametric characteristics and mechanisms occurring within these regions of the Maltese archipelago. An empirical workflow was implemented to predict the spatial and temporal variations in sea surface salinity and sea surface temperature from 2022 to 2024. This was achieved by leveraging Sentinel-2 satellite platforms, the random forest Machine Learning algorithm, and in situ data collected from sea gliders and floats. Subsequently, the numerical data generated by the random forest algorithm were validated with different error metrics and converted into visual representations to illustrate the sea surface salinity and sea surface temperature variations across the Maltese Islands. The random forest algorithm demonstrated strong performance in predicting sea surface salinity and sea surface temperature, indicating its capability to handle dynamic parameters effectively. Additionally, the parametric maps generated for all three years provided a clear understanding of both the spatial and temporal changes for these two parameters. Full article
(This article belongs to the Special Issue Advances and Applications of Complex Data Analysis and Computing)
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<p>A cartographic representation of the Mediterranean Sea delineating the position of the Maltese Islands with a star symbol (Latitude: 35.99° N, Longitude: 14.31° E).</p>
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<p>(<b>a</b>) Sea Explorer sea glider and (<b>b</b>) ARGO Float. Reproduced from (<b>a</b>) <a href="https://www.alseamar-alcen.com" target="_blank">https://www.alseamar-alcen.com</a>, accessed on 17 May 2024 (<b>b</b>) <a href="https://www.teledynemarine.com" target="_blank">https://www.teledynemarine.com</a>, accessed on 17 May 2024.</p>
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<p>Satellite and in situ data used for the training and testing stages of SSS and SST for 2022 and 2023.</p>
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<p>Satellite and in situ data used for the training and testing stages of SSS and SST for 2024.</p>
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<p>(<b>a</b>) SST satellite data in raster form. (<b>b</b>) SST satellite data in vector form superimposed on a satellite-derived image.</p>
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<p>SSS and SST model data obtained from Marine Copernicus Data Hub used for validation.</p>
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<p>Complete predictive modelling process.</p>
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<p>Correlation plots visualising the relationship between the in situ and predicted SSS and SST of RF for October 2022, October 2023, and June 2024.</p>
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<p>Maps illustrating the spatial and temporal SSS and SST variations generated by the RF algorithms for three separate years.</p>
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<p>Scatter plots demonstrating the predictive accuracy of the RF algorithm for 2022, 2023, and 2024 in comparison to model data.</p>
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23 pages, 74396 KiB  
Article
Change of NDVI in the Upper Reaches of the Yangtze River and Its Influence on the Water–Sand Process in the Three Gorges Reservoir
by Yiming Ma, Mingyue Li, Huaming Yao, Peng Chen and Hongzhong Pan
Sustainability 2025, 17(2), 739; https://doi.org/10.3390/su17020739 (registering DOI) - 18 Jan 2025
Viewed by 137
Abstract
Vegetation coverage in the upper reaches of the Yangtze River is very important to the ecological balance in this area, and it also has an impact on the inflow runoff and sediment transport processes of the Three Gorges Reservoir. Based on the normalized [...] Read more.
Vegetation coverage in the upper reaches of the Yangtze River is very important to the ecological balance in this area, and it also has an impact on the inflow runoff and sediment transport processes of the Three Gorges Reservoir. Based on the normalized vegetation index data (NDVI) with 250 m resolution in the upper reaches of the Yangtze River, annual runoff, sediment transport, land use, meteorology, and other data—and by using the methods of Sen + Mann–Kendall trend analysis, partial correlation analysis, and Hurst index—this paper analyzes the temporal and spatial variation characteristics, driving factors, and the influence on the water and sediment inflow processes of the Three Gorges Reservoir in each sub-basin in the upper reaches of the Yangtze River. The results show that (1) NDVI in the upper Yangtze River showed a fluctuating upward trend from 2001 to 2022, and the overall vegetation cover continued to increase, showing a spatial pattern of low in the west and high in the east. At the same time, the runoff volume of the upper reaches of the Yangtze River did not show a significant upward trend from 2006 to 2022, while the sand transport decreased significantly; (2) Among the NDVI-influencing factors in the upper reaches of the Yangtze River, the area driven by the land use factor accounts for about 43% of the whole study area, followed by precipitation; (3) Precipitation significantly affected runoff, and NDVI was negatively correlated with sand transport in most of the watersheds, suggesting that improved vegetation could help reduce sediment loss. In addition, the future trend of vegetation change was predicted to be dominated by improvement (Hurst > 0.5) based on the Hurst index, which will provide a reference for the NDVI change in the upper Yangtze River and the prediction of sediment inflow to the Three Gorges Reservoir. Full article
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<p>Schematic diagram of the location, scope, and terrain of the research area.</p>
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<p>Annual variation of NDVI in various basins in the upper reaches of the Yangtze River from 2001 to 2022.</p>
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<p>Spatial distribution of NDVI in the Upper Yangtze River Basin from 2001 to 2022.</p>
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<p>Significance of spatial variation in NDVI in the Upper Yangtze River Basin from 2001 to 2022.</p>
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<p>Spatial fluctuation of annual NDVI in the Upper Yangtze River Basin from 2001 to 2022.</p>
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<p>Interannual variability of runoff (<b>a</b>) and sand transport (<b>b</b>) in the Yangtze River Basin. Error bars indicate percentage of data for each year (5%).</p>
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<p>Spatial distribution of NDVI and precipitation correlation coefficients (<b>a</b>) and correlation coefficients significance (<b>b</b>) in the upper Yangtze River Basin from 2001 to 2022.</p>
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<p>Distribution of land cover types in the Upper Yangtze River Basin in 2001, 2010, and 2022.</p>
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<p>Vegetation change for different land cover types in the upper Yangtze River Basin from 2001 to 2022.</p>
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<p>Spatial distribution of partial correlation coefficient (<b>A</b>–<b>C</b>) and partial correlation significance (<b>D</b>–<b>F</b>) between NDVI and climate factors in the upper Yangtze River Basin from 2000 to 2022.</p>
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<p>Spatial distribution of dominant climate factors for NDVI changes in the upper Yangtze River Basin from 2001 to 2022.</p>
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<p>Persistence of NDVI in the Upper Yangtze River Basin from 2001 to 2022.</p>
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<p>Future trends of NDVI changes in the upper reaches of the Yangtze River.</p>
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19 pages, 2202 KiB  
Review
Advanced Deep Learning Algorithms for Energy Optimization of Smart Cities
by Izabela Rojek, Dariusz Mikołajewski, Krzysztof Galas and Adrianna Piszcz
Energies 2025, 18(2), 407; https://doi.org/10.3390/en18020407 (registering DOI) - 18 Jan 2025
Viewed by 226
Abstract
Advanced deep learning algorithms play a key role in optimizing energy usage in smart cities, leveraging massive datasets to increase efficiency and sustainability. These algorithms analyze real-time data from sensors and IoT devices to predict energy demand, enabling dynamic load balancing and reducing [...] Read more.
Advanced deep learning algorithms play a key role in optimizing energy usage in smart cities, leveraging massive datasets to increase efficiency and sustainability. These algorithms analyze real-time data from sensors and IoT devices to predict energy demand, enabling dynamic load balancing and reducing waste. Reinforcement learning models optimize power distribution by learning from historical patterns and adapting to changes in energy usage in real time. Convolutional neural networks (CNNs) and recurrent neural networks (RNNs) facilitate detailed analysis of spatial and temporal data to better predict energy usage. Generative adversarial networks (GANs) are used to simulate energy usage scenarios, supporting strategic planning and anomaly detection. Federated learning ensures privacy-preserving data sharing in distributed energy systems, promoting collaboration without compromising security. These technologies are driving the transformation towards sustainable and energy-efficient urban environments, meeting the growing demands of modern smart cities. However, there is a view that if the pace of development is maintained with large amounts of data, the computational/energy costs may exceed the benefits. The article aims to conduct a comparative analysis and assess the development potential of this group of technologies, taking into account energy efficiency. Full article
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<p>Genesis of DL support for energy optimization of smart cities (own version).</p>
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<p>Process of possible DL support for energy optimization of smart cities (own version).</p>
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<p>PRISMA flow diagram of the review process using selected PRISMA 2020 guidelines.</p>
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<p>Publications (<b>a</b>) by year, (<b>b</b>) by type, (<b>c</b>) by leading area of science.</p>
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<p>Publications (<b>a</b>) by year, (<b>b</b>) by type, (<b>c</b>) by leading area of science.</p>
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<p>Applications of DL in energy optimization of smart cities. Colors: green: well defined, orange: partly defined, red: not defined yet.</p>
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<p>Role of DL in smart city applications (own version).</p>
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19 pages, 4695 KiB  
Article
Spatio-Temporal Feature Aware Vision Transformers for Real-Time Unmanned Aerial Vehicle Tracking
by Hao Zhang, Hengzhou Ye, Xiaoyu Guo, Xu Zhang, Yao Rong and Shuiwang Li
Drones 2025, 9(1), 68; https://doi.org/10.3390/drones9010068 (registering DOI) - 17 Jan 2025
Viewed by 190
Abstract
Driven by the rapid advancement of Unmanned Aerial Vehicle (UAV) technology, the field of UAV object tracking has witnessed significant progress. This study introduces an innovative single-stream UAV tracking architecture, dubbed NT-Track, which is dedicated to enhancing the efficiency and accuracy of real-time [...] Read more.
Driven by the rapid advancement of Unmanned Aerial Vehicle (UAV) technology, the field of UAV object tracking has witnessed significant progress. This study introduces an innovative single-stream UAV tracking architecture, dubbed NT-Track, which is dedicated to enhancing the efficiency and accuracy of real-time tracking tasks. Addressing the shortcomings of existing tracking systems in capturing temporal relationships between consecutive frames, NT-Track meticulously analyzes the positional changes in targets across frames and leverages the similarity of the surrounding areas to extract feature information. Furthermore, our method integrates spatial and temporal information seamlessly into a unified framework through the introduction of a temporal feature fusion technique, thereby bolstering the overall performance of the model. NT-Track also incorporates a spatial neighborhood feature extraction module, which focuses on identifying and extracting features within the neighborhood of the target in each frame, ensuring continuous focus on the target during inter-frame processing. By employing an improved Transformer backbone network, our approach effectively integrates spatio-temporal information, enhancing the accuracy and robustness of tracking. Our experimental results on several challenging benchmark datasets demonstrate that NT-Track surpasses existing lightweight and deep learning trackers in terms of precision and success rate. It is noteworthy that, on the VisDrone2018 benchmark, NT-Track achieved a precision rate of 90% for the first time, an accomplishment that not only showcases its exceptional performance in complex environments, but also confirms its potential and effectiveness in practical applications. Full article
16 pages, 1163 KiB  
Article
Real-Time Quantification of Gas Leaks Using a Snapshot Infrared Spectral Imager
by Nathan Hagen
Sensors 2025, 25(2), 538; https://doi.org/10.3390/s25020538 - 17 Jan 2025
Viewed by 175
Abstract
We describe the various steps of a gas imaging algorithm developed for detecting, identifying, and quantifying gas leaks using data from a snapshot infrared spectral imager. The spectral video stream delivered by the hardware allows the system to combine spatial, spectral, and temporal [...] Read more.
We describe the various steps of a gas imaging algorithm developed for detecting, identifying, and quantifying gas leaks using data from a snapshot infrared spectral imager. The spectral video stream delivered by the hardware allows the system to combine spatial, spectral, and temporal correlations into the gas detection algorithm, which significantly improves its measurement sensitivity in comparison to non-spectral video, and also in comparison to scanning spectral imaging. After describing the special calibration needs of the hardware, we show how to regularize the gas detection/identification for optimal performance, provide example SNR spectral images, and discuss the effects of humidity and absorption nonlinearity on detection and quantification. Full article
(This article belongs to the Special Issue Feature Papers in Sensing and Imaging 2024)
17 pages, 4281 KiB  
Article
GravelSens: a Smart Gravel Sensor for High-Resolution, Non-Destructive Monitoring of Clogging Dynamics
by Kaan Koca, Eckhard Schleicher, André Bieberle, Stefan Haun, Silke Wieprecht and Markus Noack
Sensors 2025, 25(2), 536; https://doi.org/10.3390/s25020536 - 17 Jan 2025
Viewed by 187
Abstract
Engineers, geomorphologists, and ecologists acknowledge the need for temporally and spatially resolved measurements of sediment clogging (also known as colmation) in permeable gravel-bed rivers due to its adverse impacts on water and habitat quality. In this paper, we present a novel method for [...] Read more.
Engineers, geomorphologists, and ecologists acknowledge the need for temporally and spatially resolved measurements of sediment clogging (also known as colmation) in permeable gravel-bed rivers due to its adverse impacts on water and habitat quality. In this paper, we present a novel method for non-destructive, real-time measurements of pore-scale sediment deposition and monitoring of clogging by using wire-mesh sensors (WMSs) embedded in spheres, forming a smart gravel bed (GravelSens). The measuring principle is based on one-by-one voltage excitation of transmitter electrodes, followed by simultaneous measurements of the resulting current by receiver electrodes at each crossing measuring pores. The currents are then linked to the conductive component of fluid impedance. The measurement performance of the developed sensor is validated by applying the Maxwell Garnett and parallel models to sensor data and comparing the results to data obtained by gamma ray computed tomography (CT). GravelSens is tested and validated under varying filling conditions of different particle sizes ranging from sand to fine gravel. The close agreement between GravelSens and CT measurements indicates the technology’s applicability in sediment–water research while also suggesting its potential for other solid–liquid two-phase flows. This pore-scale measurement and visualization system offers the capability to monitor clogging and de-clogging dynamics within pore spaces up to 10,000 Hz, making it the first laboratory equipment capable of performing such in situ measurements without radiation. Thus, GravelSens is a major improvement over existing methods and holds promise for advancing the understanding of flow–sediment–ecology interactions. Full article
(This article belongs to the Section Environmental Sensing)
25 pages, 3212 KiB  
Article
In-Depth Collaboratively Supervised Video Instance Segmentation
by Yunnan Deng, Yinhui Zhang and Zifen He
Electronics 2025, 14(2), 363; https://doi.org/10.3390/electronics14020363 - 17 Jan 2025
Viewed by 186
Abstract
Video instance segmentation (VIS) is plagued by the high cost of pixel-level annotation and defects of weakly supervised segmentation, leading to the urgent need for a trade-off between annotation cost and performance. We propose a novel In-Depth Collaboratively Supervised video instance segmentation (IDCS) [...] Read more.
Video instance segmentation (VIS) is plagued by the high cost of pixel-level annotation and defects of weakly supervised segmentation, leading to the urgent need for a trade-off between annotation cost and performance. We propose a novel In-Depth Collaboratively Supervised video instance segmentation (IDCS) with efficient training. A collaborative supervised training pipeline is designed to flow samples of different labeling levels and carry out multimodal training, in which instance clues are obtained from mask-annotated instances to guide the box-annotated training through an in-depth collaborative paradigm: (1) a trident learning method is proposed, which leverages the video temporal consistency to match instances with multimodal annotation across frames for effective instance relation learning without additional network parameters; (2) spatial clues in the first frames are captured to implement multidimensional pixel affinity evaluation of box-annotated instances and augment the noise-disturbed spatial affinity map. Experiments on YoutTube-VIS validate the performance of IDCS with mask-annotated instances in the first frames and the bounding-box-annotated samples in the remaining frames. IDCS achieves up to 92.0% fully supervised performance and average 1.4 times faster, 2.2% mAP higher than the weakly supervised baseline. The results show that IDCS can efficiently utilize multimodal data, while providing advanced guidance for effective trade-off in VIS training. Full article
18 pages, 9333 KiB  
Article
Spatial–Temporal Dynamics of Adventitious Roots of Typha domingensis Pers. Seedlings Grown with Auxin/Cytokinin
by Guadalupe Hernández-Piedra, Violeta Ruiz-Carrera, Alberto J. Sánchez, Erika Escalante-Espinosa and Graciano Calva-Calva
Life 2025, 15(1), 121; https://doi.org/10.3390/life15010121 - 17 Jan 2025
Viewed by 213
Abstract
The spatial–temporal dynamics of an in vitro radicular system of Typha domingensis for the development of rhizofiltration technologies, with the potential for use as a phytotreatment of eutrophicated water, were studied for the first time in the roots of seedlings and in rhizotron [...] Read more.
The spatial–temporal dynamics of an in vitro radicular system of Typha domingensis for the development of rhizofiltration technologies, with the potential for use as a phytotreatment of eutrophicated water, were studied for the first time in the roots of seedlings and in rhizotron systems. The effect of indole-3-acetic acid (AIA) in combination with kinetin (CIN) or 6-benzylaminopurine (BAP) on seedlings cultivated in the light and dark in three radicular systems and in a rhizotrophic regime for the screening of dynamic rhizogenic lines, by weekly allometric measurements of the length and number of roots, were studied. Inhibition of the elongation and branching velocities of roots by BAP and light was observed but CIN increased elongation and branching. In rhizotrons cultivated in light and dark conditions with different AIA/CIN ratios, isolated root explants remained inactive; however, roots attached to a meristematic base presented a significant increase in growth development, with values comparable to those of roots attached to seedlings cultivated in light without hormones. The results revealed that six adventitious rhizogenic root lines with basal meristems have the potential for use in a wide range of environmental and innovative applications in phytotreatment technologies involving eutrophicated water. Full article
(This article belongs to the Section Plant Science)
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<p>Explant type and rhizotron system used for evaluating the rhizogenesis of <span class="html-italic">Typha domingensis</span>. The semisolid phase with the nutrient medium in the rhizotron was covered with 1 mm film of sterile distilled water.</p>
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<p>Diagrammatic summary of the overall methodology of the experimental strategy used to evaluate rhizogenesis in cultures of complete <span class="html-italic">Typha domingensis</span> seedlings and their explants by phenotyping image-based analysis. Two factorial experimental designs focused on discerning the effects and interaction of AIA and CIN (Exp 1) or AIA and BAP (Exp 2) on rhizogenesis in complete seedlings, and two Latin square experimental designs were used to study the main effects of the concentrations of AIA and CIN and the explant type under light (Exp 3) and darkness (Exp 4) on the rhizogenesis in rhizotron cultures.</p>
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<p>Effect of the concentration of growth regulators on the phenotyping traits of root systems of complete seedlings cultivated under a light/dark photoperiod of 16/8 h by 7 days for the branching rate (TRAM) and the elongation rate (TE), and by 21 days for the branching density (DRAM) and the root length density (DLR). Data represent the corresponding means for each growth regulator level from 4 × 4 factorial experimental designs to study the effect of the balance and concentrations of AIA/CIN (Exp 1) and AIA/BAP (Exp 2). Treatments included six replicates. Error bars represent the SD from each factor level mean (n = 24) from the 16 treatments. Different letters above the error bars indicate significant differences at the 0.05 level (ANOVA and post hoc Tukey’s multiple range test).</p>
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<p>Weekly dynamics of phenotyping the root system development of seedlings of <span class="html-italic">Typha domingensis</span> cultivated for 28 days in rhizotrons under photoperiods to study the effect of the balance and concentrations of AIA/CIN (Exp 1) and AIA/BAP (Exp 2) by factorial experimental designs. (<b>A</b>) frames of representative pictures contrasting the growth pattern and weekly phenotyping of roots in seedlings cultivated without any growth regulator (−) versus those cultivated with 10 mg/L of CIN (+). Dynamic curves (<b>B</b>–<b>F</b>) show the weekly changes in the overall mean value from the factorial design conducted with AIA and CIN (blue lines), and that conducted with AIA and BAP (red lines) on the branching rate (<b>B</b>), total elongation rate (<b>C</b>), growth rate (<b>D</b>), branching density (<b>E</b>), and root length density (<b>F</b>). Error bars represent the SD of the weekly overall means from the 16 treatments with 6 replicas (n = 96). Different letters on the error bars indicate groups of means with significant differences at the 0.05 level (ANOVA and Tukey’s multiple range test).</p>
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<p>Effect of the balance and concentrations of AIA/CIN (Exp 1) and AIA/BAP (Exp 2) by complete 4 × 4 factorial experimental designs (1–16 dots) on the phenotypes related to the growth rate (TE (<b>A</b>) and TRAM (<b>B</b>)), and the contact surface (DRAM (<b>C</b>) and DLR (<b>D</b>)) parameters of the root system of <span class="html-italic">Typha domingensis</span> seedlings cultivated for 28 days in rhizotrons under photoperiods. Different letters in the dots (size and color intensity are related to the mean value) indicate means with significant differences at 0.05 level (ANOVA and Tukey’s multiple range test).</p>
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<p>Effect of the balance and concentrations of AIA/CIN (Exp 1) and AIA/BAP (Exp 2) by complete 4 × 4 factorial experimental designs (1–16 dots) on the phenotypes related to the growth rate (TE (<b>A</b>) and TRAM (<b>B</b>)), and the contact surface (DRAM (<b>C</b>) and DLR (<b>D</b>)) parameters of the root system of <span class="html-italic">Typha domingensis</span> seedlings cultivated for 28 days in rhizotrons under photoperiods. Different letters in the dots (size and color intensity are related to the mean value) indicate means with significant differences at 0.05 level (ANOVA and Tukey’s multiple range test).</p>
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<p>(<b>a</b>) Changes in the means of the spatial–temporal dynamics of phenotypes of adventitious roots in explants cultivated in rhizotron under the Latin square experiments in light (Exp 3) and darkness (Exp 4) to evaluate the effect of the AIA and CIN concentrations and the explant type (complete seedling (seed), isolated SR without cauline base (root), and SR with cauline base (CBAS); and (<b>b</b>) frames of representative pictures highlighting the weekly phenotyping of the branching density DRAM (<b>left</b>) and branching rate TRAM (<b>right</b>) of the explants cultivated with seedlings (T1, T6, T8), and CBAS (T3, T5, T7) explants, and 0, 0 (T1), 0, 1 (T3), 0.1, 0.1 (T5), 0.1, 1 (T6), 1, 0 (T7), 1, 0.1 (T8) mg/L of CIN, AIA, and under light (L) conditions. TE = elongation rate; DLR = length density.</p>
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<p>The 12 adventitious rhizogenic root strains of in vitro cultures of <span class="html-italic">Typha domingensis</span> seedling explants were grouped based on the quality level of the 4 phenotypic traits examined by image analysis of their root system. (<b>A</b>) Dendrogram of the rhizogenic strains; (<b>B</b>) identity regarding cultivation treatment; (<b>C</b>) matrix of the quality level (averages) of the phenotypic traits: high (red), medium (blue), and low (green).</p>
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19 pages, 137082 KiB  
Article
Classification and Monitoring of Salt Marsh Vegetation in the Yellow River Delta Based on Multi-Source Remote Sensing Data Fusion
by Ran Xu, Yanguo Fan, Bowen Fan, Guangyue Feng and Ruotong Li
Sensors 2025, 25(2), 529; https://doi.org/10.3390/s25020529 - 17 Jan 2025
Viewed by 240
Abstract
Salt marsh vegetation in the Yellow River Delta, including Phragmites australis (P. australis), Suaeda salsa (S. salsa), and Tamarix chinensis (T. chinensis), is essential for the stability of wetland ecosystems. In recent years, salt marsh vegetation has [...] Read more.
Salt marsh vegetation in the Yellow River Delta, including Phragmites australis (P. australis), Suaeda salsa (S. salsa), and Tamarix chinensis (T. chinensis), is essential for the stability of wetland ecosystems. In recent years, salt marsh vegetation has experienced severe degradation, which is primarily due to invasive species and human activities. Therefore, the accurate monitoring of the spatial distribution of these vegetation types is critical for the ecological protection and restoration of the Yellow River Delta. This study proposes a multi-source remote sensing data fusion method based on Sentinel-1 and Sentinel-2 imagery, integrating the temporal characteristics of optical and SAR (synthetic aperture radar) data for the classification mapping of salt marsh vegetation in the Yellow River Delta. Phenological and polarization features were extracted to capture vegetation characteristics. A random forest algorithm was then applied to evaluate the impact of different feature combinations on classification accuracy. Combining optical and SAR time-series data significantly enhanced classification accuracy, particularly in differentiating P. australis, S. salsa, and T. chinensis. The integration of phenological features, polarization ratio, and polarization difference achieved a classification accuracy of 93.51% with a Kappa coefficient of 0.917, outperforming the use of individual data sources. Full article
(This article belongs to the Section Remote Sensors)
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<p>Location of the study area. (<b>a</b>) Approximate location of the study area. (<b>b</b>) The purple outlined area represents the specific study area.</p>
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<p>Field data.</p>
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<p>Mean time series variation of sample points. PA = <span class="html-italic">P. australis</span>, SS = <span class="html-italic">S. salsa</span>, TC = <span class="html-italic">T. chinensis</span>, TF = tidal flat.</p>
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<p>Fitted curve for <span class="html-italic">P. australis</span>.</p>
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<p>Box plot of phenological features for representative vegetation. Figure (<b>a</b>) shows the distribution of the seasonal start and end times for three typical vegetation types. The vertical axes of (<b>b</b>–<b>d</b>) are unitless, as NDVI, ROI, and ROD are all dimensionless. PA = <span class="html-italic">P. australis</span>, SS = <span class="html-italic">S. salsa</span>, TC = <span class="html-italic">T. chinensis</span>.</p>
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<p>(<b>a</b>) Polarization difference time series. PA = <span class="html-italic">P. australis</span>, SS = <span class="html-italic">S. salsa</span>, TC = <span class="html-italic">T. chinensis</span>. (<b>b</b>) Polarization ratio time series. PA = <span class="html-italic">P. australis</span>, SS = <span class="html-italic">S. salsa</span>, TC = <span class="html-italic">T. chinensis</span>.</p>
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<p>Extraction results of typical salt marsh vegetation. (<b>a</b>) Classification results based on optical phenological characteristics; (<b>b</b>) classification results based on SAR polarization characteristics; (<b>c</b>) classification results integrating optical phenological characteristics and polarization ratio features; (<b>d</b>) classification results integrating optical phenological characteristics and polarization difference features; (<b>e</b>) classification results integrating optical phenological characteristics and polarization features.</p>
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<p>Producer’s accuracy bar chart.</p>
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<p>User’s accuracy bar chart.</p>
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<p>Detailed comparison of typical salt marsh vegetation classification.</p>
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19 pages, 9946 KiB  
Article
Three-Dimensional Morphological Characterisation of Human Cortical Organoids Using a Customised Image Analysis Workflow
by Sarah Handcock, Kay Richards, Timothy J. Karle, Pamela Kairath, Alita Soch, Carolina A. Chavez, Steven Petrou and Snezana Maljevic
Organoids 2025, 4(1), 1; https://doi.org/10.3390/organoids4010001 - 17 Jan 2025
Viewed by 269
Abstract
Summary Statement: A tailored image analysis workflow was applied to quantify cortical organoid health, development, morphology and cellular composition over time. The assessment of cellular composition and viability of stem cell-derived organoid models is a complex but essential approach to understanding the [...] Read more.
Summary Statement: A tailored image analysis workflow was applied to quantify cortical organoid health, development, morphology and cellular composition over time. The assessment of cellular composition and viability of stem cell-derived organoid models is a complex but essential approach to understanding the mechanisms of human development and disease. Aim: Our study was motivated by the need for an image-analysis workflow, including high-cell content, high-throughput methods, to measure the architectural features of developing organoids. We assessed stem cell-derived cortical organoids at 4 and 6 months post-induction using immunohistochemistry-labelled sections as the analysis testbed. The workflow leveraged fluorescence imaging tailored to classify cells as viable and dying or non-viable and assign neuronal and astrocytic perinuclear markers to count cells. Results/Outcomes: Image acquisition was accelerated by capturing the organoid slice in 3D using widefield-fluorescence microscopy. This method used computational clearing to resolve nuclear and perinuclear markers and retain their spatial information within the organoid’s heterogeneous structure. The customised workflow analysed over 1.5 million cells using DAPI-stained nuclei, filtering and quantifying viable and non-viable cells and the necrotic-core regions. Temporal analyses of neuronal cell number derived from perinuclear labelling were consistent with organoid maturation from 4 to 6 months of in vitro differentiation. Overall: We have provided a comprehensive and enhanced image analysis workflow for organoid structural evaluation, creating the ability to gather cellular-level statistics in control and disease models. Full article
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<p>Summary of the workflow for organoid analysis included cortical organoid sectioning, immunohistochemistry and image acquisition. (<b>A</b>) Single organoid, representing one of 31 analysed. (<b>B</b>) Schematic of a slide with ten organoid sections, nine tiles were imaged per organoid section. (<b>C</b>) Tiled images shown across a single section in the x-y plane (dotted lines). (<b>D</b>) Individual tile illustrates (3D) z-stack acquired for all images. (<b>E</b>–<b>G</b>) Example immuno-histochemistry for the organoid sections: (<b>E</b>) staining with DAPI (blue) and S100β (green), marking mature astrocytes; (<b>F</b>) DAPI (blue) and MAP2 (red), indicating mature neurons; (<b>G</b>) DAPI (blue) and GABA (yellow), highlighting inhibitory neurons. 6-diamidino-2-phenyl-indole (DAPI); S-100 calcium-binding β-subunit (S100β); Microtubule-associated Protein 2 (MAP2); Gamma-aminobutyric Acid (GABA). Scale 50 µm.</p>
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<p>Method for processing tiled images of cortical organoid section boundary refinement. (<b>A</b>) Composite of a 4 × 3 tile grid merging DAPI and marker channels, showing the outer boundary of the section and a section tear (yellow). (<b>B</b>) Schematic of the entire section, illustrating the outer boundary and section tear (yellow), with viable cells (blue), and non-viable cells (red). (<b>C</b>) Schematic of the non-viable core (red), which was excluded from analysis and viable region (green) in a cortical organoid section. The viable region represents the area between the outer boundary of the section and the core boundary. (<b>D</b>) Schematic of the viable region, with the outer and inner boundaries (green), and viable cells only (blue). Scale 400 µm.</p>
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<p>Segmentation and classification of DAPI-labelled cell nuclei in cortical organoid sections. (<b>A</b>–<b>D</b>) Comparative segmentation tools of DAPI-labelled cell nuclei in a cortical organoid section. (<b>A</b>) Original grayscale image. (<b>B</b>) Segmentation by CellProfiler v4.2.5, with distinct colours marking individual nuclei. (<b>C</b>) Segmentation by Imaris v9.9, highlighting the boundaries of nuclei in distinct colours. (<b>D</b>) Segmentation by Cellpose v2.2, with nuclei identified in cyan; pixel intensity indicates individual cells. (<b>E</b>) Panel of two-tiered GMM classification of cell nuclei post-segmentation. (Left to right) Initial classification distinguishes small volume fragments or improperly segmented cells (blue). Subsequent analysis categorises cells as non-viable (red) and viable (green). Example large volume or clustered cells (yellow) and overlay of all cell classifications (colour merge). (<b>F</b>) Panel illustrates individual segmented nuclei based on GMM classification (above), including (left-right) fragmented and non-viable nuclei, which were excluded from analysis, and viable and clustered nuclei, which were included. Gaussian Mixture Model (GMM). Scale 50 µm (<b>A</b>–<b>D</b>).</p>
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<p>Delineation and classification of peri-nucleic protein distribution. (<b>A</b>) Schematic representation of a cell nucleus (blue) with nuclear proteins (red) and extranuclear proteins (yellow). (<b>B</b>) Illustration of a DAPI-labelled cell nucleus (blue) segmented using the Cellpose algorithm, with antibody-positive pixels (yellow) detected in the surrounding area. (<b>C</b>) Visualisation of the peri-nucleic region (green), defined by applying a dilation algorithm to the boundaries of the segmented nucleus. Antibody-positive pixels located within this region are highlighted (yellow). (<b>D</b>) Classification criteria for cell nuclei based on antibody presence: nuclei were deemed positive when their peri-nucleic shell contained the minimum cutoff value for the antibody marker; otherwise, they were deemed as negative. (<b>E</b>) Examples of antibody-positive cells visually classified for markers S100β, MAP2 and GABA. Arrows indicate cells identified as positive based on the extent of peri-nucleic antibody label. 6-diamidino-2-phenylindole (DAPI); S-100 (β-subunit) antibody (S100β); Microtubule-associated Protein 2 (MAP2); Gamma-aminobutyric Acid (GABA). Scale 20 µm.</p>
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<p>Schematic representation of antibody-positive and -negative cells within the viable region of cortical organoid sections. (<b>A</b>) The viable region, defined by the outer and inner boundaries (teal). Cells identified as antibody-positive are shown in green, while antibody-negative cells are shown in red. (<b>B</b>) The viable region with the outer and inner boundaries (teal), showing only antibody-positive cells (green). Scale 400 µm.</p>
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<p>hESC-derived cortical organoid morphology features assessed at 4- and 6 months post-induction using the image analysis workflow. Blue diamonds represent organoid sections at 4 months and red circles at 6 months. Error bars SEM. Results refer to Welch’s <span class="html-italic">t</span>-tests performed with Benjamini–Hochberg correction (Q = 0.05). (<b>A</b>) No discovery was made regarding differences in total section volume. (<b>B</b>) A discovery was made as to the volume of the non-viable core as a percentage of total section volume, with a reduction observed at 6 months post-induction. (<b>C</b>) No discovery was made in relation to the percentage of cells within the viable region that were non-viable. (<b>D</b>) Overall cell density within the viable region was reduced at 6 months compared to 4 months post-induction. (<b>E</b>) Representative DAPI-stained cortical organoid section at 4 months post-induction. Left: Single-plane raw image of nuclei. Right: Processed image showing segmented nuclei identified by the Cellpose algorithm, with individual nuclei displayed in greyscale. (<b>F</b>) Representative DAPI-stained cortical organoid section at 6 months post-induction. Left: Single-plane raw image of nuclei. Right: Processed image showing segmented nuclei identified by Cellpose. The reduced density of segmented nuclei at 6 months reflects the decrease in cell density quantified in panel (<b>D</b>). Standard Error Mean (SEM). Scale 40 µm.</p>
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<p>Temporal analysis of percentage and density of marker positive cells in ESC-derived cortical organoids. Blue diamonds represent sections at 4 months and red circles at 6 months. Error bars SEM. Results refer to Welch’s <span class="html-italic">t</span>-tests performed with a Benjamini–Hochberg correction (Q = 0.05). (<b>A</b>–<b>D</b>) No discoveries were made when comparing the percentage of cells positive for either S100β or MAP2 within the viable region, nor when considering positive cell density. (<b>E</b>) A discovery was made as to the percentage of cells positive for GABA within the viable region, with an increase observed at 6 months post-induction. (<b>F</b>) A discovery was not observed as to the density of GABA-positive cells. (<b>G</b>) Representative image of a cortical organoid section at 4 months post-induction, stained for DAPI (blue) and GABA (red). Left: Single-plane raw image. Right: Peri-nuclear regions showing pixels without GABA staining (blue) and pixels positive for GABA (pink). (<b>H</b>) Representative image of a cortical organoid section at 6 months post-induction, stained for DAPI (blue) and GABA (red). Left: Single-plane raw image. Right: Peri-nuclear regions showing GABA-negative pixels (blue) and GABA-positive pixels (pink). The increased proportion of GABA-positive cells at 6 months aligns with the quantitative findings shown in panel (<b>E</b>). Standard error mean (SEM). Scale 40 µm.</p>
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30 pages, 9113 KiB  
Article
Harnessing Multi-Source Data and Deep Learning for High-Resolution Land Surface Temperature Gap-Filling Supporting Climate Change Adaptation Activities
by Katja Kustura, David Conti, Matthias Sammer and Michael Riffler
Remote Sens. 2025, 17(2), 318; https://doi.org/10.3390/rs17020318 - 17 Jan 2025
Viewed by 224
Abstract
Addressing global warming and adapting to the impacts of climate change is a primary focus of climate change adaptation strategies at both European and national levels. Land surface temperature (LST) is a widely used proxy for investigating climate-change-induced phenomena, providing insights into the [...] Read more.
Addressing global warming and adapting to the impacts of climate change is a primary focus of climate change adaptation strategies at both European and national levels. Land surface temperature (LST) is a widely used proxy for investigating climate-change-induced phenomena, providing insights into the surface radiative properties of different land cover types and the impact of urbanization on local climate characteristics. Accurate and continuous estimation across large spatial regions is crucial for the implementation of LST as an essential parameter in climate change mitigation strategies. Here, we propose a deep-learning-based methodology for LST estimation using multi-source data including Sentinel-2 imagery, land cover, and meteorological data. Our approach addresses common challenges in satellite-derived LST data, such as gaps caused by cloud cover, image border limitations, grid-pattern sensor artifacts, and temporal discontinuities due to infrequent sensor overpasses. We develop a regression-based convolutional neural network model, trained on ECOSTRESS (ECOsystem Spaceborne Thermal Radiometer Experiment on Space Station) mission data, which performs pixelwise LST predictions using 5 × 5 image patches, capturing contextual information around each pixel. This method not only preserves ECOSTRESS’s native resolution but also fills data gaps and enhances spatial and temporal coverage. In non-gap areas validated against ground truth ECOSTRESS data, the model achieves LST predictions with at least 80% of all pixel errors falling within a ±3 °C range. Unlike traditional satellite-based techniques, our model leverages high-temporal-resolution meteorological data to capture diurnal variations, allowing for more robust LST predictions across different regions and time periods. The model’s performance demonstrates the potential for integrating LST into urban planning, climate resilience strategies, and near-real-time heat stress monitoring, providing a valuable resource to assess and visualize the impact of urban development and land use and land cover changes. Full article
(This article belongs to the Special Issue Remote Sensing: 15th Anniversary)
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Graphical abstract

Graphical abstract
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<p>Location of the two areas of interest within Austria: AREA I (Innsbruck; WGS84 coordinates 47.27°N, 11.39°E), AREA II (Vienna; WGS84 coordinates 48.21°N, 16.37°E). The zoomed-in insets are displayed with standard true color composites.</p>
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<p>Overview of the datasets used in the training, shown for AREA I. The datasets are displayed in their native resolution. (<b>a</b>) ECOSTRESS LST in °C after masking by the quality control layer; see <a href="#sec2dot4dot1-remotesensing-17-00318" class="html-sec">Section 2.4.1</a> for more details on masking (date and time of observation: 13 June 2023, 12:40:05, resolution 70 m). Data gaps due to clouds and instrument artifacts are visible. (<b>b</b>) INCA air temperature in °C (date and time of observation: 13 June 2023, 13:00:00, resolution 1 km). The image represents the closest INCA observation to the ECOSTRESS observation shown in (<b>a</b>). (<b>c</b>) Sentinel-2 band B4 reflectance (date and time of observation: 15 July 2023, 10:16:01, resolution 10 m). The image represents the cloud-free observation with all valid pixels closest to the ECOSTRESS observation shown in (<b>a</b>). (<b>d</b>) Digital elevation model (resolution 25 m). (<b>e</b>) Tree cover density. (<b>f</b>) Water and wetness index. (<b>g</b>) Imperviousness. The datasets (<b>e</b>–<b>g</b>) are from the reference year 2018, and they are shown in 10 m resolution.</p>
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<p>A flowchart outlining the main components of the LST gap-filling methodology: data collection, image processing (including preprocessing, data matching, and processing into input for CNN), CNN model training, and model assessment.</p>
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<p>Scheme of the CNN architecture used for the LST gap-filling methodology.</p>
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<p>Comparison between LST ECOSTRESS measurements and model predictions in °C. The images display LST data for two areas of interest, outlined by a bounding box in each image. (<b>a</b>) Masked ECOSTRESS measurement and (<b>b</b>) corresponding model prediction for AREA I. Date and time of observation: 12 June 2022, 13:26:01. (<b>c</b>) Masked ECOSTRESS measurement and (<b>d</b>) corresponding LST prediction over AREA II. Date and time of observation: 4 August 2022, 16:31:34.</p>
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<p>(<b>a</b>) Close-up of grid artifacts in ECOSTRESS LST observation, shown in grayscale to enhance visibility. (<b>b</b>) The corresponding model prediction corrects the artifacts and increases spatial details. (Location: WGS84 coordinates 48.65398°N, 16.31361°E. Observation date and time: 4 June 2022, 16:39:50).</p>
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<p>Histograms for the disjoint (above) and joint (below) distribution of LST for all pixels across all the predictions considered in <a href="#remotesensing-17-00318-t004" class="html-table">Table 4</a>. The colored bars in the bivariate histograms indicate pixel count. (<b>a</b>,<b>b</b>) Results for tile 32TPT; the MAE and <math display="inline"><semantics> <mrow> <msup> <mrow> <mi>r</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msup> </mrow> </semantics></math> are, respectively, 1.93 °C and 0.87. (<b>c</b>,<b>d</b>) Results for tile 33UWP; the MAE and <math display="inline"><semantics> <mrow> <msup> <mrow> <mi>r</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msup> </mrow> </semantics></math> are, respectively, 1.6 °C and 0.87.</p>
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<p>Histograms for the disjoint (above) and joint (below) distribution of the LST for all pixels across all afternoon model predictions considered in <a href="#remotesensing-17-00318-t004" class="html-table">Table 4</a>. The colored bars in the bivariate histograms indicate pixel count. (<b>a</b>,<b>b</b>) Results for tile 32TPT; the MAE and <math display="inline"><semantics> <mrow> <msup> <mrow> <mi>r</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msup> </mrow> </semantics></math> are, respectively, 1.96 °C and 0.81. (<b>c</b>,<b>d</b>) Results for tile 33UWP; the MAE and <math display="inline"><semantics> <mrow> <msup> <mrow> <mi>r</mi> </mrow> <mrow> <mn>2</mn> </mrow> </msup> </mrow> </semantics></math> are, respectively, 1.39 °C and 0.73.</p>
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<p>Examples of data quality issues for ECOSTRESS observations showing LST in °C. (<b>a</b>) Issues identified in a single observation: missing data due to masking by the ECOSTRESS-QC layer (background image visible); fringe-pattern sensor artifacts that remain even after the QC mask is applied; incorrect georeferencing (cf. position of the river in the ECOSTRESS observation and the background image, the displacement is further accentuated by the double arrow). (Location: WGS84 coordinates: 47.26646°N, 11.38075°E. Observation date and time: 11 June 2022, 14:49:19). (<b>b</b>) Summer observation before masking by the QC layer. A cloud is clearly identifiable by the negative temperature values, inconsistent with the season in which the observation was taken, as well as by the spatial extent which does not follow any spatial features in the area. (Location: WGS84 coordinates: 47.1852°N, 16.8806°E. Observation date and time: 9 July 2022, 03:02:29). (<b>c</b>) The same observation as in (<b>b</b>) after masking by the QC layer, demonstrating that the cloud was not sufficiently masked.</p>
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12 pages, 1763 KiB  
Data Descriptor
A Comprehensive Parcel-Level Dataset on Farmland Assessment: Addressing Grid-Cell Data Bias Estimation
by Wai Yan Siu, Man Li and Arthur J. Caplan
Data 2025, 10(1), 10; https://doi.org/10.3390/data10010010 - 17 Jan 2025
Viewed by 264
Abstract
Grid-cell data are increasingly used in research due to the growing availability and accessibility of remote sensing products. However, grid-cell data often fails to represent the actual decision-making unit, leading to biased estimates in socio-economic analysis. To this end, this paper presents a [...] Read more.
Grid-cell data are increasingly used in research due to the growing availability and accessibility of remote sensing products. However, grid-cell data often fails to represent the actual decision-making unit, leading to biased estimates in socio-economic analysis. To this end, this paper presents a comprehensive parcel-level dataset for Salt Lake County, Utah, spanning from 2008 to 2018. This dataset combines detailed spatial and temporal data on land ownership, land use, and preferential farmland tax assessments under the Greenbelt program. Compiled from multiple geospatial sources, the dataset includes nearly 200,000 parcel-year observations, providing valuable insights into landowner decision-making and the impact of tax abatement incentives at the decision-making level. This resource is beneficial for researchers, educators, and practitioners in sustainable development, environmental studies, and farmland conservation. Full article
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<p>Greenbelt program enrollment criteria and Greenbelt designation.</p>
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<p>The correlation of the drivers of farmland development. Note: “***” if the <span class="html-italic">p</span>-value is &lt;0.001, “**”if the <span class="html-italic">p</span>-value is &lt;0.01, “*” if the <span class="html-italic">p</span>-value is &lt;0.05, “.” if the <span class="html-italic">p</span>-value is &lt;0.10, and “ ” otherwise.</p>
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<p>The workflow diagram for the <span class="html-italic">EVI.elgb</span> variable. Note: Square boxes represent inputs, blue circles represent processes, and the yellow box represents output.</p>
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15 pages, 1054 KiB  
Article
Early Spatio-Temporal and Cognitive Deficits in Alzheimer’s Disease
by Tina Iachini, Mariachiara Rapuano, Francesco Ruotolo, Alessandro Iavarone, Sabrina Iuliano and Gennaro Ruggiero
J. Clin. Med. 2025, 14(2), 579; https://doi.org/10.3390/jcm14020579 - 17 Jan 2025
Viewed by 147
Abstract
Background/Objectives: Mental representation of spatial information relies on egocentric (body-based) and allocentric (environment-based) frames of reference. Research showed that spatial memory deteriorates as Alzheimer’s disease (AD) progresses and that allocentric spatial memory is among the earliest impaired areas. Most studies have been conducted [...] Read more.
Background/Objectives: Mental representation of spatial information relies on egocentric (body-based) and allocentric (environment-based) frames of reference. Research showed that spatial memory deteriorates as Alzheimer’s disease (AD) progresses and that allocentric spatial memory is among the earliest impaired areas. Most studies have been conducted in static situations despite the dynamic nature of real-world spatial processing. Thus, this raises the question: Does temporal order affect spatial memory? The present study, by adopting a dynamic spatial memory task, explored how the temporal order of item presentation influences egocentric and allocentric spatial judgments in individuals with early-stage Alzheimer’s disease (eAD) and healthy elderly individuals (normal controls—NC). Method: Participants were required to memorize dyads of simple 3D geometrical objects presented one at a time on a desk along with a bar. Afterwards, they had to choose what stimulus appeared either closest to them (egocentric judgment) or closest to the bar (allocentric judgment). Results: Results revealed that the temporal order significantly affected spatial judgments in eAD patients but not in NC participants. While eAD patients remain anchored to the item presented first, which is more accurate regardless of the frame used, NC are equally accurate with the item that appears first or second. This is presumably because eAD patients struggle to flexibly shift attention and update spatial representations in dynamic situations, which leads to reliance on initial information and difficulties with information presented later. Conclusions: This highlights the importance of further understanding the cognitive strategies employed by AD patients. Full article
(This article belongs to the Section Clinical Neurology)
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<p>The figure depicts the position of the 3D geometrical objects (e.g., cube and pyramid) on the panel such that in each dyad the metric difficulty for allocentric and egocentric judgments was the same. In this case, the egocentric metric difficulty based on the distance of both the cube and pyramid from the participant’s body was 5 cm (i.e., 19 cm–14 cm), and the allocentric metric difficulty based on the distance of both the cube and pyramid from the Black Bar was also 5 cm (i.e., 21 cm–16 cm).</p>
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<p>The figure depicts an example of one trial. Each trial started with a fixation cross (100 ms) followed by a blank screen. After 1 s the first object was shown for 400 ms. It could be the egocentric target (i.e., nearest to the participant’s body) or the allocentric target (i.e., nearest to the black bar). Thereafter, only the panel with the black bar was left. Subsequently, the second stimulus was shown for 400 ms: again, this could be the egocentric target or the allocentric target. Finally, the virtual table disappeared, and after a 1 s blank, the word indicating the related question (“you”, “bar”) was presented.</p>
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<p>The figure depicts the mean accuracy for egocentric/allocentric judgments as a function of the eAD (early Alzheimer’s disease) and NC (normal control) groups. The small vertical black bars depict the standard error. Significant differences (<span class="html-italic">p</span> &lt; 0.05) are indicated by the asterisk.</p>
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<p>The graph depicts the mean accuracy of first and second egocentric and allocentric judgments as a function of the two eAD and NC groups. The black bars represent the standard error. Significant differences (<span class="html-italic">p</span> &lt; 0.05) are indicated by the asterisk.</p>
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