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Search Results (2,276)

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Keywords = digital elevation models

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24 pages, 1087 KiB  
Article
Lidar-Derived Decadal Change in Barrier Morphology: A Case Study of Waisanding, Taiwan
by Hsien-Kuo Chang, Jin-Cheng Liou, Wen-Son Chiang and Wei-Wei Chen
Geosciences 2024, 14(12), 318; https://doi.org/10.3390/geosciences14120318 - 23 Nov 2024
Viewed by 157
Abstract
Barrier change is a complex process of evolution of coastal topography, which is related to the interaction of driving forces such as waves, tides and sea level rise (SLR) with beaches. The Waisanding Barrier (WSDB) in Taiwan has suffered from continuous beach erosion [...] Read more.
Barrier change is a complex process of evolution of coastal topography, which is related to the interaction of driving forces such as waves, tides and sea level rise (SLR) with beaches. The Waisanding Barrier (WSDB) in Taiwan has suffered from continuous beach erosion in recent decades. Some short-term studies have been carried out to understand the characteristics of the barrier change to provide a reference for future barrier protection. In this paper, the digital elevation model (DEM) measured by LiDAR (Light Detection and Ranging), over nearly two decades was used to analyze the morphological changes, the land area and volume. The changes in the morphology, including the whole shoreline, duneline height, width of forebeach and backbarrier, are investigated. The WSDB’s land area and land volume were analyzed to show a continuous decrease by a rate of −0.418 × 106 m2/year and −3.96 × 105 m3/year, respectively. The corresponding average land volume (LV) decrease in elevation can be estimated to be −0.0286 m/year. The changes in these features are discussed and relate to land subsidence, sea level rise and large waves induced by typhoons passing near WSDB. Full article
12 pages, 2746 KiB  
Article
The Intensity of BCL2A1 Expression Increases According to the Stage Progression of Acute Histologic Chorioamnionitis in the Extra-Placental Membranes of Spontaneous Preterm Birth
by Chan-Wook Park, Eun-Mi Lee, Seung-Han Shin, Chul Lee and Jae-Kyung Won
Life 2024, 14(12), 1535; https://doi.org/10.3390/life14121535 - 22 Nov 2024
Viewed by 319
Abstract
Our prior findings showed that BCL2A1 in neutrophils is highly expressed in the extra-placental membranes (EPMs) of both the human spontaneous preterm-birth (PTB) (i.e., PTL or preterm PROM) and nonhuman-primate PTB model. However, no data exist on whether the intensity of BCL2A1 expression [...] Read more.
Our prior findings showed that BCL2A1 in neutrophils is highly expressed in the extra-placental membranes (EPMs) of both the human spontaneous preterm-birth (PTB) (i.e., PTL or preterm PROM) and nonhuman-primate PTB model. However, no data exist on whether the intensity of BCL2A1 expression quantitatively increases according to the stage progression of acute histologic chorioamnionitis (acute HCA) in EPM. The objective is to investigate whether the intensity of BCL2A1 expression quantitatively increases according to the stage progression of acute HCA in EPM among spontaneous PTB cases, as measured using QuPath. The study population included 121 singleton PTBs (gestational age [GA] at delivery < 34 weeks) due to either preterm labor or preterm PROM. With digital image analysis, we calculated the percentage of BCL2A1-positive cells in immunohistochemistry according to the stage progression of acute HCA in EPMs as the primary outcome and examined the relationship between the percentage of BCL2A1-positive cells and either the GA at delivery or the amniotic-fluid (AF) WBC count as the secondary outcome. The median percentage of BCL2A1-positive cells progressively increases with the stage progression of acute HCA in EPM (group-1 vs. group-2 vs. group-3 vs. group-4 vs. group-5; 7.62 vs. 5.15 vs. 43.57 vs. 71.07; γ = 0.552, p < 0.000001). The percentage of BCL2A1-positive cells in EPMs and the AFWBC count shows a positive correlation (γ = 0.492, p = 0.000385). Moreover, the percentage of BCL2A1-positive cells in EPMs continuously decreased with increasing GA at delivery (γ = −0.253, p = 0.005148). In conclusion, the intensity of BCL2A1 expression increases according to the stage progression of acute HCA in EPMs and the elevation of AFWBC among spontaneous PTB cases. This finding suggests BCL2A1 in EPMs may be a promising marker and target for acute HCA. Full article
(This article belongs to the Special Issue Clinical Management and Prevention of Adverse Pregnancy Outcomes)
33 pages, 10134 KiB  
Article
Study on the Microscopic Distribution Pattern of Residual Oil and Exploitation Methods Based on a Digital Pore Network Model
by Xianda Sun, Xudong Qin, Chengwu Xu, Ling Zhao and Huili Zhang
Polymers 2024, 16(23), 3246; https://doi.org/10.3390/polym16233246 - 22 Nov 2024
Viewed by 270
Abstract
With the persistent rise in global energy demand, the efficient extraction of petroleum resources has become an urgent and critical issue. Polymer flooding technology, widely employed for enhancing crude oil recovery, still lacks an in-depth understanding of the distribution of residual oil within [...] Read more.
With the persistent rise in global energy demand, the efficient extraction of petroleum resources has become an urgent and critical issue. Polymer flooding technology, widely employed for enhancing crude oil recovery, still lacks an in-depth understanding of the distribution of residual oil within the microscopic pore structure and the associated displacement mechanisms. To address this, a digital pore network model was established based on mercury intrusion experimental data, and pore structure visualization was achieved through 3Dmax software, simulating the oil displacement process under various polymer concentrations, molecular weights, and interfacial tension conditions. The findings reveal that moderately increasing the polymer concentration (from 1000 [mg/L] to 2000 [mg/L]) improves the recovery factor during polymer flooding by approximately 1.45%, effectively emulsifying larger masses of residual oil and reducing the proportion of throats with high oil saturation. However, when the concentration exceeds 2500 [mg/L], the dispersion of residual oil is hindered, and the enhancement in displacement efficiency becomes marginal. Increasing the molecular weight from 12 million to 16 million and subsequently to 24 million elevates the recovery factor by approximately 1.07% and 1.37%, respectively, reducing clustered residual oil while increasing columnar residual oil; high molecular weight polymers exhibit a more significant effect on channels with high oil saturation. Lowering the interfacial tension (from 30 [mN/m] to 0.005 [mN/m]) markedly enhances the binary flooding recovery factor, with the overall recovery reaching 71.72%, effectively reducing the residual oil within pores of high oil saturation. The study concludes that adjusting polymer concentration, molecular weight, and interfacial tension can optimize the microscopic distribution of residual oil, thereby enhancing oil displacement efficiency and providing a scientific foundation for further improving oilfield recovery and achieving efficient reservoir development. Full article
(This article belongs to the Special Issue Stimuli-Responsive Polymers: Advances and Prospects)
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Graphical abstract
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<p>Simplified schematic of orifice–throat connection: (<b>a</b>) regular array; (<b>b</b>) irregular array.</p>
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<p>Digital pore and throat network model.</p>
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<p>Simplified pore-throat model.</p>
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<p>Dynamic simulation results of model flooding. (<b>a</b>) Initial model state (oil saturation: 75%); (<b>b</b>) model state after water flooding (oil saturation: 44.72%); (<b>c</b>) model state after polymer flooding (oil saturation: 31.18%).</p>
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<p>Models of different polymer concentrations.</p>
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<p>Models of different polymer concentrations.</p>
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<p>The proportion of oil content after polymer flooding with different concentrations.</p>
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<p>Oil saturation ratio in throats of relative molecular weight (16 million) after polymer flooding.</p>
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<p>Oil saturation ratio in pores of relative molecular weight (16 million) after polymer flooding.</p>
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<p>Oil saturation ratio in pore throat after polymer flooding with relative molecular weight (16 million).</p>
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<p>Effects of different polymer concentrations on residual oil distribution: (<b>a</b>) 1000 [mg/L]; (<b>b</b>) 2000 [mg/L]; (<b>c</b>) 2500 [mg/L].</p>
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<p>Effects of different polymer concentrations on residual oil types.</p>
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<p>Models of different polymers’ relative molecular masses.</p>
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<p>Oil saturation ratio in pore throat after polymer flooding.</p>
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<p>Oil saturation ratio of pore throats after polymer flooding (1000 [mg/L]).</p>
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<p>Effects of different polymer molecular weights on residual oil distribution.</p>
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<p>Effects of different polymer molecular weights on residual oil types.</p>
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<p>Influence of interfacial tension on recovery factor in polymer–surfactant binary flooding.</p>
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<p>Oil saturation ratio in pore throat after polymer–surfactant binary flooding.</p>
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<p>Oil saturation ratio in pore throat.</p>
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<p>Influence of different interfacial tensions on residual oil distribution.</p>
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<p>Effect of different interfacial tensions on residual oil types.</p>
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<p>Different oil saturation ratios in pore throat after high-concentration polymer flooding (molecular weight 20 million).</p>
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<p>Different oil saturation ratios in pore throat after high-molecular-weight polymer flooding (concentration 1500 [mg/L]).</p>
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<p>Different oil saturation ratios in pore throat.</p>
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27 pages, 15683 KiB  
Article
GLBWOA: A Global–Local Balanced Whale Optimization Algorithm for UAV Path Planning
by Qiwu Wu, Weicong Tan, Renjun Zhan, Lingzhi Jiang, Li Zhu and Husheng Wu
Electronics 2024, 13(23), 4598; https://doi.org/10.3390/electronics13234598 - 21 Nov 2024
Viewed by 349
Abstract
To tackle the challenges of path planning for unmanned aerial vehicle (UAV) in complex environments, a global–local balanced whale optimization algorithm (GLBWOA) has been developed. Initially, to prevent the population from prematurely converging, a bubble net attack enhancement strategy is incorporated, and mutation [...] Read more.
To tackle the challenges of path planning for unmanned aerial vehicle (UAV) in complex environments, a global–local balanced whale optimization algorithm (GLBWOA) has been developed. Initially, to prevent the population from prematurely converging, a bubble net attack enhancement strategy is incorporated, and mutation operations are introduced at different stages of the algorithm to mitigate early convergence. Additionally, a failure parameter test mutation mechanism is integrated, along with a predefined termination rule to avoid excessive computation. The algorithm’s convergence is accelerated through mutation operations, further optimizing performance. Moreover, a random gradient-assisted optimization approach is applied, where the negative gradient direction is identified during each iteration, and an appropriate step size is selected to enhance the algorithm’s exploration capability toward finding the optimal solution. The performance of GLBWOA is benchmarked against several other algorithms, including SCA, BWO, BOA, and WOA, using the IEEE CEC2017 test functions. The results indicate that the GLBWOA outperforms other algorithms. Path-planning simulations are also conducted across four benchmark scenarios of varying complexity, revealing that the proposed algorithm achieves the lowest average total cost for flight path planning and exhibits high convergence accuracy, thus validating its reliability and superiority. Full article
(This article belongs to the Special Issue Innovative Technologies and Services for Unmanned Aerial Vehicles)
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Figure 1
<p>Cylindrical obstacle threat.</p>
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<p>Altitude cost explanation.</p>
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<p>Calculation of turning and climbing angles.</p>
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<p>Terrain environment model for UAV path planning. (Blue cylinders are artificially added obstacles).</p>
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<p>Global–local balanced whale optimization algorithm process.</p>
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<p>Average convergence curves of the algorithms.</p>
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<p>Average convergence curves of the algorithms.</p>
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<p>Path Planning in Scenario 1 (<span class="html-italic">n</span> = 10).</p>
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<p>Path Planning in Scenario 2 (<span class="html-italic">n</span> = 10).</p>
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<p>Path Planning in Scenario 3 (<span class="html-italic">n</span> = 10).</p>
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<p>Path Planning in Scenario 4 (<span class="html-italic">n</span> = 10).</p>
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7 pages, 1227 KiB  
Proceeding Paper
Modeling the Current Suitable Habitat Range of the Yellow-Bellied Gecko (Hemidactylus flaviviridis Rüppell, 1835) in Iran
by Saman Ghasemian Sorboni, Mehrdad Hadipour and Narina Ghasemian Sorboni
Biol. Life Sci. Forum 2024, 39(1), 1; https://doi.org/10.3390/blsf2024039001 - 20 Nov 2024
Viewed by 113
Abstract
Studying the current range of species presence is crucial for ecologists and related scientists to understand potential habitats and the influence of environmental factors on species distribution. In this study, we used species distribution modeling (SDM) to look into where the yellow-bellied gecko, [...] Read more.
Studying the current range of species presence is crucial for ecologists and related scientists to understand potential habitats and the influence of environmental factors on species distribution. In this study, we used species distribution modeling (SDM) to look into where the yellow-bellied gecko, also known as the northern house gecko (Hemidactylus flaviviridis Rüppell, 1835), lives in Iran. We achieved this by combining four machine learning algorithms: Random Forest (RF), the Support Vector Machine (SVM), Maximum Entropy (Maxent), and the Generalized Linear Model (GLM). We utilized 19 historical bioclimatic variables, the Digital Elevation Model (DEM), slope, aspect, and the Normalized Difference Vegetation Index (NDVI). After calculating their correlations, we selected variables for modeling with a variance inflation factor (VIF) of less than 10. The findings indicate that the variables “Precipitation of the Coldest Quarter” (BIO19) and “Mean Temperature of Wettest Quarter” (BIO8) have the most significant influence on the species’ distribution. The gecko primarily inhabits low elevations and slopes, particularly those below 400 m above sea level with slopes less than 8 degrees, primarily in southern Iran. Additionally, we found that the NDVI had a minimal impact on the distribution of the species. Therefore, we identify the provinces of Khuzestan, Bushehr, Hormozgan, and Fars, along with parts of the coastal strip of Sistan and Baluchistan, as suitable areas for the current presence of this species. Full article
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<p>Predicted distribution of <span class="html-italic">H. flaviviridis</span> in Iran.</p>
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<p>Relative variable importance in the modeling process based on Pearson correlation and AUC metrics.</p>
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<p>Binary distribution map of <span class="html-italic">H. flaviviridis</span> overlaid on an elevation map of Iran. The red areas indicate the suitable habitat range for the species.</p>
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24 pages, 21738 KiB  
Article
New Method to Correct Vegetation Bias in a Copernicus Digital Elevation Model to Improve Flow Path Delineation
by Gabriel Thomé Brochado and Camilo Daleles Rennó
Remote Sens. 2024, 16(22), 4332; https://doi.org/10.3390/rs16224332 - 20 Nov 2024
Viewed by 349
Abstract
Digital elevation models (DEM) are widely used in many hydrologic applications, providing key information about the topography, which is a major driver of water flow in a landscape. Several open access DEMs with near-global coverage are currently available, however, they represent the elevation [...] Read more.
Digital elevation models (DEM) are widely used in many hydrologic applications, providing key information about the topography, which is a major driver of water flow in a landscape. Several open access DEMs with near-global coverage are currently available, however, they represent the elevation of the earth’s surface including all its elements, such as vegetation cover and buildings. These features introduce a positive elevation bias that can skew the water flow paths, impacting the extraction of hydrological features and the accuracy of hydrodynamic models. Many attempts have been made to reduce the effects of this bias over the years, leading to the generation of improved datasets based on the original global DEMs, such as MERIT DEM and, more recently, FABDEM. However, even after these corrections, the remaining bias still affects flow path delineation in a significant way. Aiming to improve on this aspect, a new vegetation bias correction method is proposed in this work. The method consists of subtracting from the Copernicus DEM elevations their respective forest height but adjusted by correction factors to compensate for the partial penetration of the SAR pulses into the vegetation cover during the Copernicus DEM acquisition process. These factors were calculated by a new approach where the slope around the pixels at the borders of each vegetation patch were analyzed. The forest height was obtained from a global dataset developed for the year 2019. Moreover, to avoid temporal vegetation cover mismatch between the DEM and the forest height dataset, we introduced a process where the latter is automatically adjusted to best match the Copernicus acquisition year. The correction method was applied for regions with different forest cover percentages and topographic characteristics, and the result was compared to the original Copernicus DEM and FABDEM, which was used as a benchmark for vegetation bias correction. The comparison method was hydrology-based, using drainage networks obtained from topographic maps as reference. The new corrected DEM showed significant improvements over both the Copernicus DEM and FABDEM in all tested scenarios. Moreover, a qualitative comparison of these DEMs was also performed through exhaustive visual analysis, corroborating these findings. These results suggest that the use of this new vegetation bias correction method has the potential to improve DEM-based hydrological applications worldwide. Full article
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Graphical abstract

Graphical abstract
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<p>Position of study areas overlayed to a natural color Sentinel-2 cloud free composite of the year 2020 of South America.</p>
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<p>Sentinel-2 cloud free composite of the year 2020 and color representation of Copernicus DEM elevations of the study areas. The numbers in the top left corner of each panel refer to the study area depicted on it.</p>
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<p>Comparison between the forest height datasets. The figure presents a natural color Sentinel-2 cloud free composite of the year 2020 of the entire Area 1, with the subset area marked by the red rectangle (<b>top left</b>); the Sentinel-2 image of the subset area (<b>top center</b>); a grayscale representation of Copernicus DEM elevations on the subset area (<b>top right</b>); the Sentinel-2 composite overlayed by a color representation of Potapov et al. [<a href="#B44-remotesensing-16-04332" class="html-bibr">44</a>] (<b>bottom left</b>), Lang et al. [<a href="#B45-remotesensing-16-04332" class="html-bibr">45</a>] (<b>bottom center</b>) and Tolan et al. [<a href="#B46-remotesensing-16-04332" class="html-bibr">46</a>] (<b>bottom right</b>) forest height datasets, where heights equal to zero are transparent.</p>
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<p>Effect of forest height overestimation and canopy elevation underestimation on the estimated ground elevation. The illustration represents the difference (Δh1) between the estimated and actual forest heights, the original and corrected DEMs elevation profiles (dotted lines), the differences between the actual and estimated canopy elevations (Δh2), and ground elevations (Δh1 + Δh2).</p>
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<p>Copernicus DEM vegetation bias correction workflow.</p>
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<p>Stream flow paths comparison workflow.</p>
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<p>Flow path displacement area calculation. The illustration shows the drainage network overlayed by an initial point from where the reference and DEM-extracted flow paths are traced, until they the circle with radius <span class="html-italic">r</span> centered around the point. The flow path displacement area, highlighted in gray, is the sum of the areas located between these lines.</p>
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<p>Example of flow paths selection. The panels present the reference drainage network for Area 1 (<b>left</b>), the set of flow paths extracted from it using a 2000 m radius (<b>center</b>), and the flow paths selected from the latter (<b>right</b>). The lines are represented in yellow color in all panels, with the Sentinel-2 composite of the year 2020 in the background.</p>
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<p>Comparison between DEMs and vertical profiles in Area 1. The figure presents color representations of Copernicus, FABDEM, and the new corrected DEM elevation data over the study area (<b>top</b>); its natural color Sentinel-2 cloud-free composite of the year 2020, overlayed by the elevation profile lines identified by their respective numbers (<b>bottom left</b>); and charts showing the observed DEM elevations along the profile lines, with the background colored gray in areas covered by vegetation, according to the adjusted forest height obtained for the area (<b>bottom right</b>).</p>
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<p>Example of a region within Area 1 where the blurring effect was identified. The figure presents a natural color Sentinel-2 cloud-free composite of the year 2020 of the study area, overlayed by red rectangle highlighting the region featured in the other panels (<b>top left</b>); a color representation of the elevations of Copernicus DEM (<b>top right</b>), FABDEM (<b>bottom left</b>) and the new corrected DEM (<b>bottom right</b>), showing the different level of degradation of the finer topographic features visible in the original DEM.</p>
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<p>Comparison between DEMs and vertical profiles in Area 2. The figure presents color representations of Copernicus, FABDEM, and the new corrected DEM elevation data over the study area (<b>top</b>); its natural color Sentinel-2 cloud-free composite of the year 2020, overlayed by the elevation profile lines identified by their respective numbers (<b>bottom left</b>); and charts showing the observed DEM elevations along the profile lines, with the background colored gray in areas covered by vegetation, according to the adjusted forest height obtained for the area (<b>bottom right</b>).</p>
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<p>Comparison between DEMs and vertical profiles in Area 3. The figure presents color representations of Copernicus, FABDEM, and the new corrected DEM elevation data over the study area (<b>top</b>); its natural color Sentinel-2 cloud-free composite of the year 2020, overlayed by the elevation profile lines identified by their respective numbers (<b>bottom left</b>); and charts showing the observed DEM elevations along the profile lines, with the background colored gray in areas covered by vegetation, according to the adjusted forest height obtained for the area (<b>bottom right</b>).</p>
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<p>Example of a region within Area 3 where the blurring effect was identified. The figure presents a natural color Sentinel-2 cloud-free composite of the year 2020 of the study area, overlayed by red rectangle highlighting the region featured in the other panels (<b>top left</b>); a color representation of the elevations of Copernicus DEM (<b>top right</b>), FABDEM (<b>bottom left</b>) and the new corrected DEM (<b>bottom right</b>), showing the different level of degradation of the finer topographic features visible in the original DEM.</p>
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<p>Comparison between DEMs and vertical profiles in Area 4. The figure presents color representations of Copernicus, FABDEM and our corrected DEM elevation data over the study area (<b>top</b>); its natural color Sentinel-2 cloud-free composite of the year 2020, overlayed by the elevation profile lines identified by their respective numbers (<b>bottom left</b>); and charts showing the observed DEM elevations along the profile lines, with the background colored gray in areas covered by vegetation, according to the adjusted forest height obtained for the area (<b>bottom right</b>).</p>
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<p>Comparison of drainage networks extracted from the DEMs. The figure is composed of the natural color Sentinel-2 cloud-free composite of the year 2020 of the study areas overlayed by a red rectangle/highlighting the regions featured in the panels below (<b>first row</b>); Sentinel-2 composite of the highlighted regions, overlayed by the reference drainage lines and the ones extracted from Copernicus DEM, FABDEM, and the new corrected DEM, all in yellow color and placed side by side, organized in rows per study area.</p>
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21 pages, 8795 KiB  
Article
Morphometric Characterization and Dual Analysis for Flash Flood Hazard Assessment of Wadi Al-Lith Watershed, Saudi Arabia
by Bashar Bashir and Abdullah Alsalman
Water 2024, 16(22), 3333; https://doi.org/10.3390/w16223333 - 20 Nov 2024
Viewed by 323
Abstract
Flash floods are one of the most hazardous natural events globally, characterized by their rapid onset and unpredictability, often overwhelming emergency preparedness and response systems. In the arid environment of Saudi Arabia, Wadi Al-Lith watershed is particularly prone to flash floods, exacerbated by [...] Read more.
Flash floods are one of the most hazardous natural events globally, characterized by their rapid onset and unpredictability, often overwhelming emergency preparedness and response systems. In the arid environment of Saudi Arabia, Wadi Al-Lith watershed is particularly prone to flash floods, exacerbated by sudden storms and the region’s distinct topographical features. This study focuses on the morphometric characterization and comparative analysis of flash flood risk within the Wadi Al-Lith basin. To assess flood susceptibility, two widely adopted methodologies were employed: the morphometric ranking approach and El-Shamy’s method. A 12.5-m resolution ALOS PALSAR digital elevation model (DEM) was used to delineate the watershed and generate a detailed drainage network via Arc-Hydro tools in the ArcGIS 10.4 software. Fifteen morphometric parameters were analyzed to determine their influence on flood potential and hazard prioritization. The findings of this study provide crucial insights for regional flood risk management, offering an improved understanding of flash flood dynamics and assisting in developing effective mitigation strategies for Wadi Al-Lith and similar environments. The findings reveal that Wadi Al-Lith comprises multiple sub-catchments with varying degrees of vulnerability to flash flooding. According to the morphometric hazard analysis (MHA), certain sub-catchments, including sc-2, sc-4, sc-5, sc-6, sc-10, sc-12, sc-13, and sc-15, emerge as highly susceptible to flood hazards, while others (sc-1 and sc-9) fall into moderate risk categories. In contrast, the application of El-Shamy’s method provides a different ranking of flood risks across the watershed’s sub-catchments, offering a comparative view of flood susceptibility. The insights gained from this dual-analysis approach are expected to support the development of targeted flood prevention and mitigation strategies, which are essential for minimizing the future impacts of flash flooding in the Wadi Al-Lith watershed and ensuring better preparedness for local communities. Full article
(This article belongs to the Special Issue Use of Remote Sensing Technologies for Water Resources Management)
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Figure 1
<p>(<b>a</b>) Regional map of Saudi Arabia and (<b>b</b>) hillshade map showing location of the Wadi Al-Lith watershed.</p>
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<p>(<b>a</b>) A digital elevation model map and (<b>b</b>) the geomorphological zones of the Wadi Al-Lith watershed.</p>
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<p>Chart illustrating the drainage systems and morphometric parameters analysis of the Wadi Al-Lith watershed.</p>
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<p>(<b>a</b>) sub-catchments (1–15) and (<b>b</b>) different stream orders of the Wadi Al-Lith watershed.</p>
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<p>Distribution of the morphometric parameter values for the 15 sub-catchments. Lb: basin length; Wb: basin width; Rlw: length width ratio; Os: stream order; Ns: stream number; Ls: stream length; Rb: bifurcation ratio; A: total area; P: perimeter; Re: elongation ratio; Rc: circulation ratio; sh-f: shape factor; Dd: drainage density; F: stream factor; Dt: stream texture.</p>
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<p>Distribution of the morphometric parameter values for the 15 sub-catchments. Lb: basin length; Wb: basin width; Rlw: length width ratio; Os: stream order; Ns: stream number; Ls: stream length; Rb: bifurcation ratio; A: total area; P: perimeter; Re: elongation ratio; Rc: circulation ratio; sh-f: shape factor; Dd: drainage density; F: stream factor; Dt: stream texture.</p>
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<p>Flood susceptibility levels based on the ranking hazard approach.</p>
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<p>El-Shamy method diagrams for assigning flash flood susceptibility classes. (<b>a</b>) Bifurcation ratio (Rb) against drainage density (Dd) and (<b>b</b>) bifurcation ratio (Rb) against stream frequency (Fs).</p>
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<p>Flood susceptibility levels according to the El-Shamy method. (<b>a</b>) Rb ve Dd and (<b>b</b>) Rb ve Fs.</p>
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15 pages, 9270 KiB  
Communication
Effect of DEM Used for Terrain Correction on Forest Windthrow Detection Using COSMO SkyMed Data
by Michele Dalponte, Daniele Marinelli and Yady Tatiana Solano-Correa
Remote Sens. 2024, 16(22), 4309; https://doi.org/10.3390/rs16224309 - 19 Nov 2024
Viewed by 255
Abstract
Preprocessing Synthetic Aperture Radar (SAR) data is a crucial initial stage in leveraging SAR data for remote sensing applications. Terrain correction, both radiometric and geometric, and the detection of layover/shadow areas hold significant importance when SAR data are collected over mountainous regions. This [...] Read more.
Preprocessing Synthetic Aperture Radar (SAR) data is a crucial initial stage in leveraging SAR data for remote sensing applications. Terrain correction, both radiometric and geometric, and the detection of layover/shadow areas hold significant importance when SAR data are collected over mountainous regions. This study aims at investigating the impact of the Digital Elevation Model (DEM) used for terrain correction (radiometric and geometric) and for mapping layover/shadow areas on windthrow detection using COSMO SkyMed SAR images. The terrain correction was done using a radiometric and geometric terrain correction algorithm. Specifically, we evaluated five different DEMs: (i–ii) a digital terrain model and a digital surface model derived from airborne LiDAR flights; (iii) the ALOS Global Digital Surface Model; (iv) the Copernicus global DEM; and (v) the Shuttle Radar Topography Mission (SRTM) DEM. All five DEMs were resampled at 2 m and 30 m pixel spacing, obtaining a total of 10 DEMs. The terrain-corrected COSMO SkyMed SAR images were employed for windthrow detection in a forested area in the north of Italy. The findings revealed significant variations in windthrow detection across the ten corrections. The detailed LiDAR-derived terrain model (i.e., DTM at 2 m pixel spacing) emerged as the optimal choice for both pixel spacings considered. Full article
(This article belongs to the Section Forest Remote Sensing)
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<p>The location of PAT in Italy and Europe (inset (<b>a</b>)), the location of the two reference sites inside the territory of PAT and the DTM of PAT (inset (<b>b</b>)), and the DTM of the two reference areas A and B (inset (<b>c</b>)).</p>
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<p>Architecture of the processing chain adopted in this study.</p>
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<p>(<b>A</b>) Difference images at 2 m pixel spacing between the local LiDAR DSM, the three global DEMs, and the local LiDAR DTM; (<b>B</b>) a zoom over a flat area (cropland); (<b>C</b>) zoom over a forest area; and (<b>D</b>) two vertical profiles of the five DEMs at 2 m pixel spacing.</p>
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<p>(<b>A</b>) Difference images at 30 m pixel spacing between the local LiDAR DSM, the three global DEMs, and the local LiDAR DTM; (<b>B</b>) a zoom over a flat area (cropland); (<b>C</b>) zoom over a forest area; and (<b>D</b>) two vertical profiles of the five DEMs at 30 m pixel spacing.</p>
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<p>Windthrow detection maps for a subset of the study area.</p>
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22 pages, 24817 KiB  
Article
Construction of Mining Subsidence Basin and Inversion of Predicted Subsidence Parameters Based on UAV Photogrammetry Products Considering Horizontal Displacement
by Jinqi Zhao, Yufen Niu, Zhengpei Zhou, Zhong Lu, Zhimou Wang, Zhaojiang Zhang, Yiyao Li and Ziheng Ju
Remote Sens. 2024, 16(22), 4283; https://doi.org/10.3390/rs16224283 - 17 Nov 2024
Viewed by 305
Abstract
Constructing high-precision subsidence basins is of paramount importance for mining subsidence monitoring. Traditional unmanned aerial vehicle (UAV) photogrammetry techniques typically construct subsidence basins by directly differencing digital elevation models (DEMs) from different monitoring periods. However, this method often neglects the influence of horizontal [...] Read more.
Constructing high-precision subsidence basins is of paramount importance for mining subsidence monitoring. Traditional unmanned aerial vehicle (UAV) photogrammetry techniques typically construct subsidence basins by directly differencing digital elevation models (DEMs) from different monitoring periods. However, this method often neglects the influence of horizontal displacement on the accuracy of the subsidence basin. Taking a mining area in Ordos, Inner Mongolia, as an example, this study employed the normalized cross-correlation (NCC) matching algorithm to extract horizontal displacement information between two epochs of a digital orthophoto map (DOM) and subsequently corrected the horizontal position of the second-epoch DEM. This ensured that the planar positions of ground feature points remained consistent in the DEM before and after subsidence. Based on this, the vertical displacement in the subsidence area (the subsidence basin) was obtained via DEM differencing, and the parameters of the post-correction subsidence basin were inverted using the probability integral method (PIM). The experimental results indicate that (1) the horizontal displacement was influenced by the gully topography, causing the displacement within the working face to be segmented on both sides of the gully; (2) the influence of the terrain on the subsidence basin was significantly reduced after correction; (3) the post-correction surface subsidence curve was smoother than the pre-correction curve, with abrupt error effects markedly diminished; (4) the accuracy of the post-correction subsidence basin increased by 43.12% compared with the total station data; and (5) comparing the measured horizontal displacement curve with that derived using the probability integral method revealed that the horizontal displacement on the side of an old goaf adjacent to the newly excavated working face shifted toward the advancing direction of the new working face as mining progressed. This study provides a novel approach and insights for using low-cost UAVs to construct high-precision subsidence basins. Full article
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<p>Schematic diagram of the study area location. (<b>a</b>) Map of China; (<b>b</b>) DEM of Ordos; (<b>c</b>) study area.</p>
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<p>Technical flow chart of this research.</p>
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<p>Schematic diagram of the DEM correction process.</p>
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<p>(<b>a</b>) East–west displacement; (<b>b</b>) north–south displacement.</p>
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<p>Illustration of the relationship between horizontal displacement and topography. (<b>a</b>,<b>b</b>) are cross-sectional views of profile A-A′; (<b>c</b>,<b>d</b>) are cross-sectional views of profile B-B′.</p>
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<p>Horizontal displacement in gully topography. (<b>a</b>) A-A′ cross-section; (<b>b</b>) local displacement field.</p>
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<p>Subsidence basin. (<b>a</b>) Pre-correction subsidence basin; (<b>b</b>) post-correction subsidence basin.</p>
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<p>Local maps of areas I and II. (<b>a</b>) Magnified view of area I pre-correction; (<b>b</b>) magnified view of area I post-correction; (<b>c</b>) magnified view of area II pre-correction; (<b>d</b>) magnified view of area II post-correction; (<b>e</b>) 1-1′ cross-section; (<b>f</b>) 2-2′ cross-section.</p>
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<p>Subsidence curves of pre-correction and post-correction. (<b>a</b>) A-A′ cross-section; (<b>b</b>) C-C′ cross-section.</p>
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<p>Inverted subsidence basin.</p>
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<p>Measured subsidence basin.</p>
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<p>(<b>a</b>) Strike main profile; (<b>b</b>) dip main profile.</p>
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<p>Horizontal displacement of strike main profile. (<b>a</b>) Strike main profile; (<b>b</b>) partial enlarged detail.</p>
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<p>Horizontal displacement of dip main profile. (<b>a</b>) Dip main profile; (<b>b</b>) partial enlarged detail.</p>
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<p>Horizontal displacement error.</p>
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<p>Statistical chart of residuals for subsidence basin.</p>
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<p>Statistical chart of strike residuals.</p>
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<p>Statistical chart of dip residuals.</p>
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<p>Statistical analysis of errors in subsidence basin.</p>
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19 pages, 7362 KiB  
Article
Highly Efficient JR Optimization Technique for Solving Prediction Problem of Soil Organic Carbon on Large Scale
by Harsh Vazirani, Xiaofeng Wu, Anurag Srivastava, Debajyoti Dhar and Divyansh Pathak
Sensors 2024, 24(22), 7317; https://doi.org/10.3390/s24227317 - 15 Nov 2024
Viewed by 366
Abstract
We utilized remote sensing and ground cover data to predict soil organic carbon (SOC) content across a vast geographic region. Employing a combination of machine learning and deep learning techniques, we developed a novel data fusion approach that integrated Digital Elevation Model (DEM) [...] Read more.
We utilized remote sensing and ground cover data to predict soil organic carbon (SOC) content across a vast geographic region. Employing a combination of machine learning and deep learning techniques, we developed a novel data fusion approach that integrated Digital Elevation Model (DEM) data, MODIS satellite imagery, WOSIS soil profile data, and CHELSA environmental data. This combined dataset, named GeoBlendMDWC, was specifically designed for SOC prediction. The primary aim of this research is to develop and evaluate a novel optimization algorithm for accurate SOC prediction by leveraging multi-source environmental data. Specifically, this study aims to (1) create an integrated dataset combining remote sensing and ground data for comprehensive SOC analysis, (2) develop a new optimization technique that enhances both machine learning and deep learning model performance, and (3) evaluate the algorithm’s efficiency and accuracy against established optimization methods like Jaya and GridSearchCV. This study focused on India, Australia, and South Africa, countries known for their significant agricultural activities. We introduced a novel optimization technique for both machine learning and deep neural networks, comparing its performance to established methods like the Jaya optimization technique and GridSearchCV. The models evaluated included XGBoost Regression, LightGBM, Gradient Boosting Regression (GBR), Random Forest Regression, Decision Tree Regression, and a Multilayer Perceptron (MLP) model. Our research demonstrated that the proposed optimization algorithm consistently outperformed existing methods in terms of execution time and performance. It achieved results comparable to GridSearchCV, reaching an R2 of 90.16, which was a significant improvement over the base XGBoost model’s R2 of 79.08. In deep learning optimization, it significantly outperformed the Jaya algorithm, achieving an R2 of 61.34 compared to Jaya’s 30.04. Moreover, it was 20–30 times faster than GridSearchCV. Given its speed and accuracy, this algorithm can be applied to real-time data processing in remote sensing satellites. This advanced methodology will greatly benefit the agriculture and farming sectors by providing precise SOC predictions. Full article
(This article belongs to the Section Remote Sensors)
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<p>Soil organic carbon content by region in tons-per-hectare (ton/ha) in India [<a href="#B34-sensors-24-07317" class="html-bibr">34</a>], Australia [<a href="#B35-sensors-24-07317" class="html-bibr">35</a>], and Africa [<a href="#B36-sensors-24-07317" class="html-bibr">36</a>] respectively.</p>
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<p>Research workflow.</p>
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<p>Flowchart of the optimization algorithm.</p>
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<p>Correlation matrix for the Indian–Australian–African combined dataset. Pearson correlation methodology is used to calculate the correlation values.</p>
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<p>Average execution time comparison in milliseconds between the machine learning models when using different optimization techniques.</p>
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15 pages, 14788 KiB  
Article
The DEM Registration Method Without Ground Control Points for Landslide Deformation Monitoring
by Yunchuan Wang, Jia Li, Ping Duan, Rui Wang and Xinrui Yu
Remote Sens. 2024, 16(22), 4236; https://doi.org/10.3390/rs16224236 - 14 Nov 2024
Viewed by 333
Abstract
Landslides are geological disasters that are harmful to both humans and society. Digital elevation model (DEM) time series data are usually used to monitor dynamic changes or surface damage. To solve the problem of landslide deformation monitoring without ground control points (GCPs), a [...] Read more.
Landslides are geological disasters that are harmful to both humans and society. Digital elevation model (DEM) time series data are usually used to monitor dynamic changes or surface damage. To solve the problem of landslide deformation monitoring without ground control points (GCPs), a multidimensional feature-based coregistration method (MFBR) was studied to achieve accurate registration of multitemporal DEMs without GCPs and obtain landslide deformation information. The method first derives the elevation information of the DEM into image pixel information, and the feature points are extracted on the basis of the image. The initial plane position registration of the DEM is implemented. Therefore, the expected maximum algorithm is applied to calculate the stable regions that have not changed between multitemporal DEMs and to perform accurate registrations. Finally, the shape variables are calculated by constructing a DEM differential model. The method was evaluated using simulated data and data from two real landslide cases, and the experimental results revealed that the registration accuracies of the three datasets were 0.963 m, 0.368 m, and 2.459 m, which are 92%, 50%, and 24% better than the 12.189 m, 0.745 m, and 3.258 m accuracies of the iterative closest-point algorithm, respectively. Compared with the GCP-based method, the MFBR method can achieve 70% deformation acquisition capability, which indicates that the MFBR method has better applicability in the field of landslide monitoring. This study provides an idea for landslide deformation monitoring without GCPs and is helpful for further understanding the state and behavior of landslides. Full article
(This article belongs to the Special Issue Advances in GIS and Remote Sensing Applications in Natural Hazards)
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<p>Workflow of the MFBR method.</p>
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<p>Image-based DEM position registration method.</p>
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<p>3D spatial-feature-based precision registration method.</p>
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<p>Simulation dataset.</p>
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<p>Luchun landslide and data collection.</p>
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<p>The Gongshan landslide.</p>
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<p>Deformation detection results of the simulation data. (<b>a</b>) Raw deformation. (<b>b</b>) Based on the MFBR method.</p>
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<p>Deformation detection results for the Luchun landslide. (<b>a</b>) Based on GCPs. (<b>b</b>) Based on MFBR. (<b>c</b>) ICP-based method.</p>
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<p>Deformation detection results for the Gongshan landslide. (<b>a</b>) Based on GCPs. (<b>b</b>) Based on MFBR. (<b>c</b>) ICP-based method.</p>
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<p>Stable region extraction results.</p>
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17 pages, 2907 KiB  
Article
Differential Glial Response and Neurodegenerative Patterns in CA1, CA3, and DG Hippocampal Regions of 5XFAD Mice
by Tahsin Nairuz, Jin-Chul Heo and Jong-Ha Lee
Int. J. Mol. Sci. 2024, 25(22), 12156; https://doi.org/10.3390/ijms252212156 - 12 Nov 2024
Viewed by 621
Abstract
In this study, the distinct patterns of glial response and neurodegeneration within the CA1, CA3, and dentate gyrus (DG) regions of the hippocampus were examined in 5XFAD mice at 6 and 12 months of age. The primary feature of this transgenic mouse model [...] Read more.
In this study, the distinct patterns of glial response and neurodegeneration within the CA1, CA3, and dentate gyrus (DG) regions of the hippocampus were examined in 5XFAD mice at 6 and 12 months of age. The primary feature of this transgenic mouse model is the rapid onset of amyloid pathology. We employed quantitative assessments via immunohistochemistry, incorporating double staining techniques, followed by observation with light microscopy and subsequent digital analysis of microscopic images. We identified significantly increased Aβ deposition in these three hippocampal regions at 6 and 12 months of transgenic mice. Moreover, the CA1 and CA3 regions showed higher vulnerability, with signs of reactive astrogliosis such as increased astrocyte density and elevated GFAP expression. Additionally, we observed a significant rise in microglia density, along with elevated inflammatory markers (TNFα) in these hippocampal regions. These findings highlight a non-uniform glial and neuronal response to Aβ plaque deposition within the hippocampal regions of 5xFAD mice, potentially contributing to the neurodegenerative and memory deficit characteristics of Alzheimer’s disease in this model. Full article
(This article belongs to the Section Molecular Neurobiology)
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<p>Representative sections of organotypic hippocampal slices of 5xFAD mice and WT control mice brains at 6 and 12 months of age stained with hematoxylin-eosin. (Scale bar 100 and 30 μm).</p>
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<p>Analysis of Aβ1-42 plaques in the CA1, CA3, and DG regions of WT control, 6 M and 12 M 5XFAD Mice. (<b>A</b>) Representative sections of hippocampal organotypic slices stained with anti-Aβ1-42 antibodies and counterstained for hematoxylin/eosin. Arrows, asterisks, and arrowheads indicate positively immunostained cells. (<b>B</b>) Quantitative analysis of Aβ1-42-stained cells in the CA1, CA3, and DG hippocampal regions. The graph shows the density of Aβ1-42 staining in these hippocampal regions of 6 M and 12 M 5XFAD Mice relative to WT control. Data reported in all graph bars are expressed as mean ± SEM. ** <span class="html-italic">p</span> &lt; 0.001 vs. WT control, * <span class="html-italic">p</span> &lt; 0.05 vs. WT control. Scale bar: 30 μm.</p>
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<p>Analysis of Aβ1-40 plaques in the CA1, CA3, and DG regions of WT control, 6 M and 12 M 5XFAD Mice. (<b>A</b>) Representative sections of hippocampal organotypic slices stained with anti-Aβ1-40 antibodies and counterstained for hematoxylin/eosin. Arrows, asterisks, and arrowheads indicate positively immunostained cells. (<b>B</b>) Quantitative analysis of Aβ1-40-stained cells in the CA1, CA3, and DG hippocampal regions. The graph shows the density of Aβ1-40 staining in these hippocampal regions of 6 M and 12 M 5XFAD Mice relative to WT control. Data reported in all graph bars are expressed as mean ± SEM. ** <span class="html-italic">p</span> &lt; 0.001 vs. WT control, * <span class="html-italic">p</span> &lt; 0.05 vs. WT control. Scale bar: 30 μm.</p>
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<p>Analysis of astrocytes in the CA1, CA3, and DG regions of WT control, 6 M and 12 M 5XFAD Mice. (<b>A</b>) Representative sections of hippocampal organotypic slices stained with anti-GFAP antibodies and counterstained for hematoxylin/eosin. Arrows, asterisks, and arrowheads indicate positively immunostained cells. (<b>B</b>) Quantitative analysis of GFAP-positive astrocytes in the CA1, CA3, and DG hippocampal regions. The graph shows the density of GFAP-positive astrocytes in these hippocampal regions of 6 M and 12 M 5XFAD Mice relative to WT control. Data reported in all graph bars are expressed as mean ± SEM. ** <span class="html-italic">p</span> &lt; 0.001 vs. WT control, * <span class="html-italic">p</span> &lt; 0.05 vs. WT control. Scale bar: 30 μm.</p>
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<p>Analysis of microglia in the CA1, CA3, and DG regions of WT control, 6 M and 12 M 5XFAD Mice. (<b>A</b>) Representative sections of hippocampal organotypic slices stained with anti-IBA antibodies and counterstained for hematoxylin/eosin. Arrows, asterisks, and arrowheads indicate positively immunostained cells. (<b>B</b>) Quantitative analysis of IBA-positive microglia in the CA1, CA3, and DG hippocampal regions. The graph shows the density of IBA-positive microglia in these hippocampal regions of 6 M and 12 M 5XFAD Mice relative to WT control. Data reported in all graph bars are expressed as mean ± SEM. ** <span class="html-italic">p</span> &lt; 0.001 vs. WT control, * <span class="html-italic">p</span> &lt; 0.05 vs. WT control. Scale bar: 30 μm.</p>
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<p>Analysis of TNF-α-positive cells in the CA1, CA3, and DG regions of WT control, 6 M and 12 M 5XFAD Mice. (<b>A</b>) Representative sections of hippocampal organotypic slices stained with anti-TNF-α antibodies and counterstained for hematoxylin/eosin. Arrows, asterisks, and arrowheads indicate positively immunostained cells. (<b>B</b>) Quantitative analysis of TNF-α-positive cells in the CA1, CA3, and DG hippocampal regions. The graph shows the density of TNF-α-positive cells in these hippocampal regions of 6 M and 12 M 5XFAD Mice relative to WT control. Data reported in all graph bars are expressed as mean ± SEM. ** <span class="html-italic">p</span> &lt; 0.001 vs. WT control, * <span class="html-italic">p</span> &lt; 0.05 vs. WT control. Scale bar: 30 μm.</p>
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34 pages, 15986 KiB  
Article
A Comprehensive Framework for Transportation Infrastructure Digitalization: TJYRoad-Net for Enhanced Point Cloud Segmentation
by Zhen Yang, Mingxuan Wang and Shikun Xie
Sensors 2024, 24(22), 7222; https://doi.org/10.3390/s24227222 - 12 Nov 2024
Viewed by 521
Abstract
This research introduces a cutting-edge approach to traffic infrastructure digitization, integrating UAV oblique photography with LiDAR point clouds for high-precision, lightweight 3D road modeling. The proposed method addresses the challenge of accurately capturing the current state of infrastructure while minimizing redundancy and optimizing [...] Read more.
This research introduces a cutting-edge approach to traffic infrastructure digitization, integrating UAV oblique photography with LiDAR point clouds for high-precision, lightweight 3D road modeling. The proposed method addresses the challenge of accurately capturing the current state of infrastructure while minimizing redundancy and optimizing computational efficiency. A key innovation is the development of the TJYRoad-Net model, which achieves over 85% mIoU segmentation accuracy by including a traffic feature computing (TFC) module composed of three critical components: the Regional Coordinate Encoder (RCE), the Context-Aware Aggregation Unit (CAU), and the Hierarchical Expansion Block. Comparative analysis segments the point clouds into road and non-road categories, achieving centimeter-level registration accuracy with RANSAC and ICP. Two lightweight surface reconstruction techniques are implemented: (1) algorithmic reconstruction, which delivers a 6.3 mm elevation error at 95% confidence in complex intersections, and (2) template matching, which replaces road markings, poles, and vegetation using bounding boxes. These methods ensure accurate results with minimal memory overhead. The optimized 3D models have been successfully applied in driving simulation and traffic flow analysis, providing a practical and scalable solution for real-world infrastructure modeling and analysis. These applications demonstrate the versatility and efficiency of the proposed methods in modern traffic system simulations. Full article
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<p>The technical roadmap of the entire paper.</p>
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<p>DJI M300RTK UAV with Zenith P1 gimbal camera.</p>
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<p>Dense UAV point cloud of road infrastructure.</p>
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<p>Laser point cloud of road infrastructure.</p>
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<p>TJYRoad-Net network.</p>
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<p>TJYRoad-Net network.</p>
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<p>Traditional machine learning versus transfer learning.</p>
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<p>Fine-tuning ideas of enhanced TJYRoad-Net.</p>
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<p>Image point cloud and laser point cloud.</p>
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<p>Semantic segmentation result of laser point cloud.</p>
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<p>Semantic segmentation results of image point cloud.</p>
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<p>Semantic segmentation results of image point clouds from a road intersection scene, showing Input (original point cloud), Ground Truth (manually annotated labels), and Predicted Value (model output with misclassifications circled).</p>
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<p>Comparison of segmentation results across different state-of-the-art methods, with red circles highlighting the segmentation outputs at identical locations for each method.</p>
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<p>ICP fine alignment error of pavement point cloud.</p>
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<p>Registered results of road surface point clouds.</p>
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<p>Process of building façade precision.</p>
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<p>ICP fine alignment error of building façade point clouds.</p>
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<p>Alignment result of point clouds.</p>
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<p>Variation in model error with downsampling voxel size.</p>
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<p>Downsampling results of road surface point clouds.</p>
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<p>Result of road reconstruction.</p>
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<p>Marker triangle network structure based on Poisson reconstruction.</p>
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<p>A section of the grid center of mass.</p>
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<p>Design of road marking template library.</p>
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<p>Marking reconstruction results.</p>
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<p>Vegetation reconstruction results.</p>
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<p>Real scene of road infrastructure.</p>
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<p>Driving simulation data visualization platform.</p>
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21 pages, 7370 KiB  
Article
Submarine Landslide Identification Based on Improved DeepLabv3 with Spatial and Channel Attention
by Jingwen Huang, Weijing Song, Tao Liu, Xiaoyu Cui, Jining Yan and Xiaoyu Wang
Remote Sens. 2024, 16(22), 4205; https://doi.org/10.3390/rs16224205 - 12 Nov 2024
Viewed by 454
Abstract
As one of the most destructive, hazardous, and frequent marine geohazards, correctly recognizing submarine landslides holds substantial importance for regional risk assessment, disaster prevention, and marine resource development. Many conventional approaches to prediction and mapping necessitate the involvement of expert insights, oversight, and [...] Read more.
As one of the most destructive, hazardous, and frequent marine geohazards, correctly recognizing submarine landslides holds substantial importance for regional risk assessment, disaster prevention, and marine resource development. Many conventional approaches to prediction and mapping necessitate the involvement of expert insights, oversight, and extensive field investigations, which can result in significant time and effort invested in the prediction process. This paper focuses on employing a deep neural network semantic segmentation technique to detect submarine landslides to replace previous methods, such as numerical analysis and physical modeling, to predict and identify the landslide areas quickly. The peripheral zone of the western Iberian Sea is selected as the study area. Since the neural network image recognition task usually requires RGB images as input data, factors such as slope, hillshade, and elevation extracted from digital elevation model (DEM) data are used to synthesize RGB images through band synthesis methods, and the number and diversity of data are increased utilizing data enhancement. Based on the classical semantic segmentation model DeepLabV3, this paper proposes an improved deep learning method, which strengthens the ability of model feature extraction for complex situations by adding an attention mechanism module, improving the spatial pyramid pooling module, and improving the landslide intersection over union metric from 0.4257 to 0.5219 and the F1-score metric from 0.609 to 0.6631 to achieve effective identification of submarine landslides. Full article
(This article belongs to the Special Issue Artificial Intelligence and Big Data for Oceanography)
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<p>The black area represents a geographical map of the study area.</p>
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<p>Elevation images and bathymetry data in the western Iberian Sea area.</p>
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<p>Areas of submarine landslides in the western Iberian Sea area. Three areas have been selected to zoom in and show.</p>
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<p>An area was selected to show the slope schematic of the landslide area containing the evacuation length, deposit length, and deposit area.</p>
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<p>Schematic diagram of data process. Firstly, the three topographic features of features, slope, elevation, and hillshade, are extracted from the DEM image, then band synthesis is carried out to a three-channel image, and finally, clipping is performed.</p>
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<p>Comparison of the final data obtained after data processing with the source data. Comparison of images on the left, masks on the right.</p>
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<p>Framework structure for the improved DeepLabV3 models.</p>
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<p>The overall workflow of the entire experimental procedure.</p>
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<p>Framework for AttentionModule and ASPP module.</p>
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<p>Framework for SEBlock attention module.</p>
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<p>Image spatial transformation.</p>
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<p>Image appearance disturbance.</p>
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<p>Experimental results. (1) RGB image, (2) label, (3) UNet, (4) PSPNet, (5) GCN, (6) FCN, (7) DeepLabV3plus, (8) DeepLabV3, (9) Improved DeepLabv3.</p>
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29 pages, 15878 KiB  
Article
Description and In-Flight Assessment of the POSEIDON-3C Altimeter of the SWOT Mission
by Alexandre Guérin, Fanny Piras, Nicolas Cuvillon, Alexandre Homerin, Sophie Le Gac, Claire Maraldi, François Bignalet-Cazalet, Marta Alves and Laurent Rey
Remote Sens. 2024, 16(22), 4183; https://doi.org/10.3390/rs16224183 - 9 Nov 2024
Viewed by 614
Abstract
The Surface Water and Ocean Topography (SWOT) mission was launched on 16 December 2022 to measure water levels over both open ocean and inland waters. To achieve these objectives, the SWOT Payload contains an innovative Ka-band radar interferometer, called KaRIn, completed with a [...] Read more.
The Surface Water and Ocean Topography (SWOT) mission was launched on 16 December 2022 to measure water levels over both open ocean and inland waters. To achieve these objectives, the SWOT Payload contains an innovative Ka-band radar interferometer, called KaRIn, completed with a nadir altimeter called POSEIDON-3C that was switched on a month after launch and a few days before KaRIn. POSEIDON-3C measurements provide a link between large-scale phenomena and high resolution. The POSEIDON-3C design is based on POSEIDON-3B, its predecessor on board JASON-3. It is also a dual-frequency radar altimeter operating in C- and Ku-bands, but with some improvements to enhance its performance. Even though it is a Low Resolution Mode altimeter, its performance over open ocean, inland waters and coastal zones are indeed excellent. This paper first describes the POSEIDON-3C design and its modes with a focus on its new features and the Digital Elevation Model that drives its open-loop tracking mode. Then, we assess the in-flight performances of the altimeter from an instrumental point of view. For that purpose, special and routine calibrations have been realized. They show the good performance and stability of the radar. In-flight assessments thus provide confidence when it comes to ensuring excellent altimeter measurement stability throughout the mission duration. Full article
(This article belongs to the Section Engineering Remote Sensing)
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<p>The full deramp technique: the received echo is mixed with a chirp replica in analog before being digitally processed by a Fast Fourier Transform.</p>
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<p>POSEIDON-3C raw Ku-band echoes measured over ocean on 16 January 2023 (the Gates axis represents the range bins; the Echoes axis represents each recorded echo; and the vertical axis represents the amplitude of digitized echoes).</p>
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<p>(<b>a</b>) POSEIDON 3C architecture. The nadir altimeter is composed of an antenna, a radio frequency unit (RFU) and a processing and control unit (PCU); (<b>b</b>) RFU (right) and PCU (left) units on flight panel (credit: CNES and Thales Alenia Space); (<b>c</b>) overall payload module with nadir dual-frequency antenna (white reflector).</p>
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<p>POSEIDON-3C tracking mode transitions.</p>
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<p>Local repartition of the hydrological targets database for the SWOT 1-day orbit. The targets are colored by type as follows: LAK for lakes, RES for reservoirs, RIV for rivers.</p>
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<p>Hydrological targets database for the SWOT 21-day science orbit. The targets are colored by type: LAK for lakes (33,741 targets, in light blue); RES for reservoirs (3239 targets, in blue); and RIV for rivers (21,701, in magenta).</p>
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<p>(<b>a</b>) Histograms of Ku-band AGC in blue and C-band AGC in red; (<b>b</b>) gridded maps (1° × 1°) of Ku-band AGC; (<b>c</b>) gridded maps (1° × 1°) of C-band AGC.</p>
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<p>(<b>a</b>) SWOT gridded maps (1 × 1°) of Signal-to-Noise Ratio; (<b>b</b>) SWOT-corresponding SNR histogram; (<b>c</b>) JASON-3 gridded maps (1 × 1°) of Signal-to-Noise Ratio; (<b>d</b>) JASON-3-corresponding SNR histogram.</p>
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<p>Typical waveform echoes shown by 104 useful gates, corresponding to gates [12:116] of the full analysis window. (<b>a</b>) Typical oceanic waveform for SWOT/POSEIDON-3C (blue) and JASON-3/POSEIDON-3B (red) for the full analysis window; (<b>b</b>) zoom on the first gates.</p>
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<p>Example of automatic transitions (blue circles, numbered from 1 to 6) between open-loop and closed-loop tracking modes over land areas.</p>
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<p>Example of an open-loop to closed-loop transition, acquired under M4 mode (<b>left</b>, cycle 447) and M4bis mode (<b>right</b>, cycle 470). The mode mask from the OLTC is shown at the bottom of each graph: green for OL, and red for CL. On top of the graphs, the effective pursuit mode of SWOT is shown as read in the level-2 products.</p>
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<p>Examples of radargrams at the transition between the Atlantic Ocean and Suriname (Descending Pass 464) for the closed-loop (<b>left</b> panel) and the open-loop (<b>right</b> panel), represented on Google Earth. The orange arrow represents the satellite’s tracking direction.</p>
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<p>Examples of radargrams at the transition between Spain and the Atlantic Ocean (Ascending Pass 475) for the closed-loop (<b>left</b> panel) and the open-loop (<b>right</b> panel), represented on Google Earth. The orange arrow represents the satellite’s tracking direction.</p>
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<p>(<b>a</b>) Example of a saturated waveform zoomed around the peak; (<b>b</b>) location of all saturated waveforms (purple points) over cycle 6 of SWOT.</p>
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<p>Locations of the routine CAL1 and CAL2 calibrations delimited by red rectangles.</p>
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<p><b>LTM</b> time series of the in-orbit THR temperatures (in °C) for the RFU SSPA board, RFU Rx board and PCU DC/DC board in Ku-band (in blue), averaged over a 1-day sliding window. In orange is the sun beta prime angle.</p>
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<p><b>LTM</b> time series of the in-orbit THR temperatures (in °C) for the RFU SSPA and Rx boards in C-band (in blue), averaged over a 1-day sliding window. In orange is the sun beta prime angle.</p>
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<p>Example of an in-flight CAL1 in blue compared to perfect sinc<sup>2</sup> corrected from the internal path delay (in red) and associated zoom on the main lobe for the Ku-band (<b>top</b> panel) and the C-band (<b>bottom</b> panel). The orange dashed line represents the center of the receiving window (0-frequency).</p>
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<p>Long-term monitoring of the PTR IPD, total power and WML for the Ku-band since altimeter switch-on. The SSPA house-keeping temperature is represented in gray on the secondary <span class="html-italic">y</span>-axis.</p>
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<p>Long-term monitoring of the PTR IPD, total power and WML for the C-band since altimeter switch-on. The SSPA house-keeping temperature is represented in gray on the secondary <span class="html-italic">y</span>-axis.</p>
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<p>Time series of the evolution of the first five sidelobes peak position (in meters) of the Ku-band PTR: (<b>a</b>) for the left-hand side; (<b>b</b>) for the right-hand side.</p>
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<p>Time series of the evolution of the first five sidelobes peak power (in dB) of the Ku-band PTR: (<b>a</b>) for the left-hand side; (<b>b</b>) for the right-hand side.</p>
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<p>(<b>a</b>) Time series of the difference in peak position between the first 5 sidelobes on the right-hand side and the left-hand side, for the Ku-band PTR. (<b>b</b>) Time series of the difference in peak power between the first 5 sidelobes on the right-hand side and the left-hand side, for the Ku-band PTR.</p>
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<p>Example of measured LPF in blue, compared to the ground calibrations in red: for the Ku-band (<b>a</b>) and the C-band (<b>b</b>). The top panel represents the full 128-gate window and bottom panel focuses on the useful 104 gates.</p>
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<p>(<b>a</b>) Time series of the LPF standard deviation [dB] in black, slope [dB/104-gates] in blue and ripple [dB]. (<b>b</b>) Time series of the full normalized 128-gate LPF. The top panel represents the Ku-band and the bottom panel represents the C-band.</p>
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<p>Localization of the Point Target Response measurements (red crosses) performed to calibrate the Automatic Gain Control on 9 September 2023.</p>
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<p>Difference between actual and theoretical POSEIDONC-3C AGC values since SWOT launch.</p>
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<p>Localization of the special PTR measurements (red crosses) to assess in-orbit stability. The first (#1) and the last (#30 calibrations are circled in blue with an associated number.</p>
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<p>In-orbit short-term monitoring of the Ku-band PTR main characteristics in blue: (<b>a</b>) IPD; (<b>b</b>) total power; (<b>c</b>) WML; (<b>d</b>) Sidelobes Peak Power Dissymmetry (bottom right panel). The SSPA house-keeping temperature is represented in gray on the secondary <span class="html-italic">y</span>-axis.</p>
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<p>In-orbit short-term monitoring of the Ku-band PTR main characteristics in blue: (<b>a</b>) IPD; (<b>b</b>) total power; (<b>c</b>) WML; (<b>d</b>) Sidelobes Peak Power Dissymmetry (bottom right panel). The SSPA house-keeping temperature is represented in gray on the secondary <span class="html-italic">y</span>-axis.</p>
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<p>Oversampled LPF characteristics for typical ocean AGC codes, focusing on the 104 useful gates. The measurements are normalized by the average power calculated between gates 64 and 68.</p>
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