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Search Results (433)

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16 pages, 2895 KiB  
Article
Accuracy Assessment of NOAA IMS 4 km Products on the Tibetan Plateau with Landsat-8 OLI Images
by Duo Chu
Atmosphere 2024, 15(10), 1234; https://doi.org/10.3390/atmos15101234 (registering DOI) - 15 Oct 2024
Viewed by 236
Abstract
The NOAA IMS (Interactive Multisensor Snow and Ice Mapping System) is a blended snow and ice product based on active and passive satellite sensors, ground observation, and other auxiliary information, providing the daily cloud-free snow cover extent in the Northern Hemisphere (NH) and [...] Read more.
The NOAA IMS (Interactive Multisensor Snow and Ice Mapping System) is a blended snow and ice product based on active and passive satellite sensors, ground observation, and other auxiliary information, providing the daily cloud-free snow cover extent in the Northern Hemisphere (NH) and having great application potential in snow cover monitoring and research in the Tibetan Plateau (TP). However, accuracy assessment of products is crucial for various aspects of applications. In this study, Landsat-8 OLI images were used to evaluate and validate the accuracy of IMS products in snow cover monitoring on the TP. The results show that (1) average overall accuracy of IMS 4 km products is 76.0% and average mapping accuracy is 88.3%, indicating that IMS 4 km products are appropriate for large-scale snow cover monitoring on the TP. (2) IMS 4 km products tend to overestimate actual snow cover on the TP, with an average commission rate of 45.4% and omission rate of 11.7%, and generally present that the higher the proportion of snow-covered area, the lower the probability of omission rate and the higher the probability of commission rate. (3) Mapping accuracy of IMS 4 km snow cover on the TP generally is higher at the high altitudes, and commission and omission errors increase with the decrease of elevation. (4) Compared with less regional representativeness of ground observations, the spatial characteristics of snow cover based on high-resolution remote sensing data are much more detailed, and more reliable verification results can be obtained. (5) In addition to commission and omission error metrics, the overall accuracy and mapping accuracy based on the reference image instead of classified image can better reveal the general monitoring accuracy of IMS 4 km products on the TP area. Full article
(This article belongs to the Section Atmospheric Techniques, Instruments, and Modeling)
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<p>Study area and location of Landsat-8 OLI images selected for validation. The background image is snow cover extent from IMS 4 km products on 25 December 2018.</p>
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<p>IMS 4 km snow cover extent in the NH on 25 February 2018.</p>
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<p>First 10 Landsat-8 band 6-3-2 composite images (<b>a1</b>,<b>a2</b>) and corresponding snow cover maps at 1 km spatial resolution of Landsat-8 (<b>b1</b>,<b>b2</b>) and IMS (<b>c1</b>,<b>c2</b>) in row. The date, path, and row of Landsat-8 OLI images are shown at the top of images.</p>
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<p>Overall accuracy of IMS 4 km products on the TP based on Landsat-8 images.</p>
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<p>Omission and commission errors of IMS 4 km products on the TP based on Landsat-8 images.</p>
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<p>(<b>a</b>) Spatial distribution of accuracy errors of IMS 4 km products on 8 January 2018. (<b>b</b>) Accuracy errors of IMS 4 km products along with elevations on 8 January 2018.</p>
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<p>(<b>a</b>) Spatial distribution of accuracy errors of IMS 4 km products on 19 January 2017. (<b>b</b>) Accuracy errors of IMS 4 km products along with elevations on 19 January 2017.</p>
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25 pages, 17434 KiB  
Article
Using UAV RGB Images for Assessing Tree Species Diversity in Elevation Gradient of Zao Mountains
by Thi Cam Nhung Tran, Maximo Larry Lopez Caceres, Sergi Garcia i Riera, Marco Conciatori, Yoshiki Kuwabara, Ching-Ying Tsou and Yago Diez
Remote Sens. 2024, 16(20), 3831; https://doi.org/10.3390/rs16203831 (registering DOI) - 15 Oct 2024
Viewed by 281
Abstract
Vegetation biodiversity in mountainous regions is controlled by altitudinal gradients and their corresponding microclimate. Higher temperatures, shorter snow cover periods, and high variability in the precipitation regime might lead to changes in vegetation distribution in mountains all over the world. In this study, [...] Read more.
Vegetation biodiversity in mountainous regions is controlled by altitudinal gradients and their corresponding microclimate. Higher temperatures, shorter snow cover periods, and high variability in the precipitation regime might lead to changes in vegetation distribution in mountains all over the world. In this study, we evaluate vegetation distribution along an altitudinal gradient (1334–1667 m.a.s.l.) in the Zao Mountains, northeastern Japan, by means of alpha diversity indices, including species richness, the Shannon index, and the Simpson index. In order to assess vegetation species and their characteristics along the mountain slope selected, fourteen 50 m × 50 m plots were selected at different altitudes and scanned with RGB cameras attached to Unmanned Aerial Vehicles (UAVs). Image analysis revealed the presence of 12 dominant tree and shrub species of which the number of individuals and heights were validated with fieldwork ground truth data. The results showed a significant variability in species richness along the altitudinal gradient. Species richness ranged from 7 to 11 out of a total of 12 species. Notably, species such as Fagus crenata, despite their low individual numbers, dominated the canopy area. In contrast, shrub species like Quercus crispula and Acer tschonoskii had high individual numbers but covered smaller canopy areas. Tree height correlated well with canopy areas, both representing tree size, which has a strong relationship with species diversity indices. Species such as F. crenata, Q. crispula, Cornus controversa, and others have an established range of altitudinal distribution. At high altitudes (1524–1653 m), the average shrubs’ height is less than 4 m, and the presence of Abies mariesii is negligible because of high mortality rates caused by a severe bark beetle attack. These results highlight the complex interactions between species abundance, canopy area, and altitude, providing valuable insights into vegetation distribution in mountainous regions. However, species diversity indices vary slightly and show some unusually low values without a clear pattern. Overall, these indices are higher at lower altitudes, peak at mid-elevations, and decrease at higher elevations in the study area. Vegetation diversity indices did not show a clear downward trend with altitude but depicted a vegetation composition at different altitudes as controlled by their surrounding environment. Finally, UAVs showed their significant potential for conducting large-scale vegetation surveys reliably and in a short time, with low costs and low manpower. Full article
(This article belongs to the Special Issue Biomass Remote Sensing in Forest Landscapes II)
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<p>The location of the study area in the Zao Mountains. Site 1 (mixed forest); Site 2 (transition from mix to monoculture forest); Site 3 (monoculture).</p>
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<p>The orthomosaics were generated using raw RGB photos in Metashape software v2.1.3.</p>
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<p>The figure shows the 3D model of Site 1 was generated from the DPC.</p>
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<p>The 3D Models of Plot 4 with 5 directions, facilitating vegetation visualization.</p>
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<p>The Canopy Height Models (CHMs) were generated using 3D Models with the software Global Mapper v21.1.</p>
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<p>An example for one of the posters that were used for fieldwork purposes.</p>
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<p>Fourteen sample plots were set up in the study area regarding the increase in elevation.</p>
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<p>Workflow in this study.</p>
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<p>The number of individuals and the canopy area of dominant species in the 14 plots along the altitudinal gradient.</p>
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<p>The number of individuals and the canopy area of dominant species in the 14 plots along the altitudinal gradient.</p>
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<p>Change in tree species composition at different altitude layers within the study area.</p>
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<p>Change in alpha-diversity indices in the plots along the altitudinal gradient (1336–1667 m).</p>
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19 pages, 1558 KiB  
Article
Genome of Russian Snow-White Chicken Reveals Genetic Features Associated with Adaptations to Cold and Diseases
by Ivan S. Yevshin, Elena I. Shagimardanova, Anna S. Ryabova, Sergey S. Pintus, Fedor A. Kolpakov and Oleg A. Gusev
Int. J. Mol. Sci. 2024, 25(20), 11066; https://doi.org/10.3390/ijms252011066 (registering DOI) - 15 Oct 2024
Viewed by 255
Abstract
Russian Snow White (RSW) chickens are characterized by high egg production, extreme resistance to low temperatures, disease resistance, and by the snow-white color of the day-old chicks. Studying the genome of this unique chicken breed will reveal its evolutionary history and help to [...] Read more.
Russian Snow White (RSW) chickens are characterized by high egg production, extreme resistance to low temperatures, disease resistance, and by the snow-white color of the day-old chicks. Studying the genome of this unique chicken breed will reveal its evolutionary history and help to understand the molecular genetic mechanisms underlying the unique characteristics of this breed, which will open new breeding opportunities and support future studies. We have sequenced and made a de novo assembly of the whole RSW genome using deep sequencing (250×) by the short reads. The genome consists of 40 chromosomes with a total length of 1.1 billion nucleotide pairs. Phylogenetic analysis placed the RSW near the White Leghorn, Fayoumi, and Houdan breeds. Comparison with other chicken breeds revealed a wide pool of mutations unique to the RSW. The functional annotation of these mutations showed the adaptation of genes associated with the development of the nervous system, thermoreceptors, purine receptors, and the TGF-beta pathway, probably caused by selection for low temperatures. We also found adaptation of the immune system genes, likely driven by selection for resistance to viral diseases. Integration with previous genome-wide association studies (GWAS) suggested several causal single nucleotide polymorphisms (SNPs). Specifically, we identified an RSW-specific missense mutation in the RALYL gene, presumably causing the snow-white color of the day-old chicks, and an RSW-specific missense mutation in the TLL1 gene, presumably affecting the egg weight. Full article
(This article belongs to the Special Issue Molecular Research in Avian Genetics)
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<p>The BUSCO assessment results for the 4 genome assemblies, showing the percentages and categories of the single-copy orthologs from the aves_odb10 data set (total genes = 8338) in each genome assembly: GGRsw1—the genome assembly of the RSW in this study; GGswu—the genome assembly of the Huxu breed [<a href="#B9-ijms-25-11066" class="html-bibr">9</a>]; GRCg6a—the genome assembly of the Red Junglefowl (official reference genome from the Genome Reference Consortium); and GRCg7b—the genome assembly of the broiler (official reference genome from the Genome Reference Consortium). GGRSw1 contains a greater number of single-copy orthologs, and lower numbers of missing and fragmented genes.</p>
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<p>A phylogenetic tree based on the comparison of the whole genome sequences of chickens of different breeds. Red—The Red Junglefowl is a chicken from Southeast Asia, from which domestic chickens probably originate; blue—“European” breeds; purple—American breeds; green—broiler breeds; yellow—Chinese breeds from Yunnan province; Brown—Chinese breeds not of Yunnan origin; and gray—other breeds.</p>
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<p>(<b>A</b>). The genomic regions unique to the Russian Snow White longer than 1000 bp. A map of all GGRsw1 chromosomes is shown, with green bars marking the genomic regions unique to the Russian White breed. (<b>B</b>). The figure shows, for each RSW-specific sequence, what proportion of that sequence is composed of G4s and tandem repeats: X axis—the fraction of G4s; Y axis—the fraction of tandem repeats.</p>
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<p>(<b>A</b>). The genomic regions unique to the Russian Snow White longer than 1000 bp. A map of all GGRsw1 chromosomes is shown, with green bars marking the genomic regions unique to the Russian White breed. (<b>B</b>). The figure shows, for each RSW-specific sequence, what proportion of that sequence is composed of G4s and tandem repeats: X axis—the fraction of G4s; Y axis—the fraction of tandem repeats.</p>
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22 pages, 5856 KiB  
Article
Automated Recognition of Snow-Covered and Icy Road Surfaces Based on T-Net of Mount Tianshan
by Jingqi Liu, Yaonan Zhang, Jie Liu, Zhaobin Wang and Zhixing Zhang
Remote Sens. 2024, 16(19), 3727; https://doi.org/10.3390/rs16193727 - 7 Oct 2024
Viewed by 792
Abstract
The Tianshan Expressway plays a crucial role in China’s “Belt and Road” strategy, yet the extreme climate of the Tianshan Mountains poses significant traffic safety risks, hindering local economic development. Efficient detection of hazardous road surface conditions (RSCs) is vital to address these [...] Read more.
The Tianshan Expressway plays a crucial role in China’s “Belt and Road” strategy, yet the extreme climate of the Tianshan Mountains poses significant traffic safety risks, hindering local economic development. Efficient detection of hazardous road surface conditions (RSCs) is vital to address these challenges. The complexity and variability of RSCs in the region, exacerbated by harsh weather, make traditional surveillance methods inadequate for real-time monitoring. To overcome these limitations, a vision-based artificial intelligence approach is urgently needed to ensure effective, real-time detection of dangerous RSCs in the Tianshan road network. This paper analyzes the primary structures and architectures of mainstream neural networks and explores their performance for RSC recognition through a comprehensive set of experiments, filling a research gap. Additionally, T-Net, specifically designed for the Tianshan Expressway engineering project, is built upon the optimal architecture identified in this study. Leveraging the split-transform-merge structure paradigm and asymmetric convolution, the model excels in capturing detailed information by learning features across multiple dimensions and perspectives. Furthermore, the integration of channel, spatial, and multi-head attention modules enhances the weighting of key features, making the T-Net particularly effective in recognizing the characteristics of snow-covered and icy road surfaces. All models presented in this paper were trained on a custom RSC dataset, compiled from various sources. Experimental results indicate that the T-Net outperforms fourteen once state-of-the-art (SOTA) models and three models specifically designed for RSC recognition, with 97.44% accuracy and 9.79% loss on the validation set. Full article
(This article belongs to the Special Issue Deep Learning and Computer Vision in Remote Sensing-III)
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<p>Dataset samples. (<b>a</b>) dry road; (<b>b</b>) fully snowy road; (<b>c</b>) icy road; (<b>d</b>) snow-blowing road; (<b>e</b>) snow-melting road; (<b>f</b>) wet road.</p>
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<p>Brightness adjustment of dataset samples. (<b>a</b>) dry road; (<b>b</b>) fully snowy road; (<b>c</b>) icy road; (<b>d</b>) snow-blowing road; (<b>e</b>) snow-melting road; (<b>f</b>) wet road.</p>
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<p>The architecture of T-Net. This model employs a split-transform-merge structural paradigm, extracting feature information from image to linear tensor. The white cubes represent the “Out Layer” that comes after every convolutional layer, or pooling layer, which has 32 channels.</p>
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<p>The structure of the channel and spatial attention module [<a href="#B46-remotesensing-16-03727" class="html-bibr">46</a>]. The module comprises two sequential sub-modules: channel attention and spatial attention. After each merging operation in T-Net, CBAM adaptively refines intermediate feature maps, amplifying the weights of key features to enhance their prominence.</p>
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<p>The diagram of channel attention. The sub-module leverages max-pooling and average-pooling outputs, enhancing channel feature representation.</p>
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<p>The diagram of spatial attention. The sub-module processes max-pooled and average-pooled features along the channel axis and passes them through a convolutional layer, enhancing spatial feature representation.</p>
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<p>Multi-head attention [<a href="#B47-remotesensing-16-03727" class="html-bibr">47</a>] consists of several attention layers running in parallel.</p>
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<p>Performance curves of top five networks.</p>
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<p>Performance curves of five lightweight networks.</p>
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<p>Performance curves of four RSC networks.</p>
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<p>Confusion matrix of T-Net on test set.</p>
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23 pages, 8867 KiB  
Article
Synergistic Potential of Optical and Radar Remote Sensing for Snow Cover Monitoring
by Jose-David Hidalgo-Hidalgo, Antonio-Juan Collados-Lara, David Pulido-Velazquez, Steven R. Fassnacht and C. Husillos
Remote Sens. 2024, 16(19), 3705; https://doi.org/10.3390/rs16193705 - 5 Oct 2024
Viewed by 662
Abstract
This research studies the characteristics of snow-covered area (SCA) from two vastly different sensors: optical (Moderate-Resolution Imaging Spectroradiometer, or MODIS, equipped on board the Terra satellite) and radar (Synthetic Aperture Radar (SAR) on-board Sentinel-1 satellites). The focus are the five mountain ranges of [...] Read more.
This research studies the characteristics of snow-covered area (SCA) from two vastly different sensors: optical (Moderate-Resolution Imaging Spectroradiometer, or MODIS, equipped on board the Terra satellite) and radar (Synthetic Aperture Radar (SAR) on-board Sentinel-1 satellites). The focus are the five mountain ranges of the Iberian Peninsula (Cantabrian System, Central System, Iberian Range, Pyrenees, and Sierra Nevada). The MODIS product was selected to identify SCA dynamics in these ranges using the Probability of Snow Cover Presence Index (PSCPI). In addition, we evaluate the potential advantage of the use of SAR remote sensing to complete optical SCA under cloudy conditions. For this purpose, we utilize the Copernicus High-Resolution Snow and Ice SAR Wet Snow (HRS&I SWS) product. The Pyrenees and the Sierra Nevada showed longer-lasting SCA duration and a higher PSCPI throughout the average year. Moreover, we demonstrate that the latitude gradient has a significant influence on the snowline elevation in the Iberian mountains (R2 ≥ 0.84). In the Iberian mountains, a general negative SCA trend is observed due to the recent climate change impacts, with a particularly pronounced decline in the winter months (December and January). Finally, in the Pyrenees, we found that wet snow detection has high potential for the spatial gap-filling of MODIS SCA in spring, contributing above 27% to the total SCA. Notably, the additional SCA provided in winter is also significant. Based on the results obtained in the Pyrenees, we can conclude that implementing techniques that combine SAR and optical satellite sensors for SCA detection may provide valuable additional SCA data for the other Iberian mountains, in which the radar product is not available. Full article
(This article belongs to the Special Issue Multi-Source Remote Sensing Data in Hydrology and Water Management)
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<p>Location of the main snow-dominated mountain ranges of the Iberian Peninsula. The circle points indicate the centroid of each mountain range.</p>
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<p>Flowchart of the methodology.</p>
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<p>Aggregated climate variables sourced from the AEMET 5 km dataset to appraise the differences between Iberian montane regions over an average year for (<b>a</b>) mean monthly accumulated precipitation and (<b>b</b>) minimum, average, and maximum temperature.</p>
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<p>Distribution of the Probability of Snow Cover Presence Index (PSCPI) per elevation over the main mountain ranges of the Iberian Peninsula: (<b>a</b>) Sierra Nevada, (<b>b</b>) Pyrenees, (<b>c</b>) Cantabrian System, (<b>d</b>) Iberian Range and (<b>e</b>) Central System. The red color scatterplots indicate the average PSCPI per elevation. The shaded area represents PSCPI values within the confidence interval between 5% and 95%.</p>
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<p>Daily distribution of the Probability of Snow Cover Presence Index (PSCPI) over the main Iberian mountains taking into account different elevation ranges. The right numbers indicate the percentage of area relative to the total area corresponding to each elevation band.</p>
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<p>(<b>a</b>) Linear correlation between latitude and snowline elevation based on different thresholds (THR) of the average PSCPI over the main snow-dominated Iberian mountains; (<b>b</b>) Determination coefficient of the simple linear regression between latitude and snowline elevation associated with the examined average PSCPI thresholds.</p>
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<p>Five-year period temporal evolution of SCA in terms of the average PSCPI for the entire domain of the mountain ranges of the Iberian Peninsula on a monthly basis.</p>
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<p>(<b>a</b>) Monthly PWSAI distribution and contribution of MODIS and HRS&amp;I SWS (wet snow) products in relation to the total SCA over an average year in the Pyrenees. (<b>b</b>) Monthly variation of the contribution of HRS&amp;I SWS product to the total SCA over an average year in the Pyrenees. The red line indicates the median, and the edges of the box (blue color) represent the first quartile (bottom edge) and third quartile (top edge). The upper adjacent is the furthest observation within one and a half times the interquartile range of the lower end of the box, and the upper adjacent is the furthest observation within one and a half times the interquartile range of the upper end of the box. Outliers are considered as the values greater than the upper adjacent.</p>
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<p>Examples of the combination of SAR (HRS&amp;I SWS) and optical (MODIS) remote sensing products for the following dates: 04-February-2017 (winter) and 18-April-2018 (spring).</p>
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<p>Monthly distribution of the Probability of Cloud Presence Index (PCPI) for an average year over the main Iberian mountains.</p>
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<p>Distribution of the tree-cover density (TCD) per elevation over the main mountain ranges of the Iberian Peninsula: (<b>a</b>) Sierra Nevada, (<b>b</b>) Pyrenees, (<b>c</b>) Cantabrian System, (<b>d</b>) Iberian Range, and (<b>e</b>) Central System. The red color scatterplots indicate the average TCD per elevation. The shaded area represents TCD values within the confidence interval between 10% and 90%.</p>
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<p>Distribution of the tree-cover density (TCD) per elevation over the main mountain ranges of the Iberian Peninsula: (<b>a</b>) Sierra Nevada, (<b>b</b>) Pyrenees, (<b>c</b>) Cantabrian System, (<b>d</b>) Iberian Range, and (<b>e</b>) Central System. The red color scatterplots indicate the average TCD per elevation. The shaded area represents TCD values within the confidence interval between 10% and 90%.</p>
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17 pages, 14569 KiB  
Article
Cross-Country Ski Skating Style Sub-Technique Detection and Skiing Characteristic Analysis on Snow Using High-Precision GNSS
by Shunya Uda, Naoto Miyamoto, Kiyoshi Hirose, Hiroshi Nakano, Thomas Stöggl, Vesa Linnamo, Stefan Lindinger and Masaki Takeda
Sensors 2024, 24(18), 6073; https://doi.org/10.3390/s24186073 - 19 Sep 2024
Viewed by 539
Abstract
A comprehensive analysis of cross-country skiing races is a pivotal step in establishing effective training objectives and tactical strategies. This study aimed to develop a method of classifying sub-techniques and analyzing skiing characteristics during cross-country skiing skating style timed races on snow using [...] Read more.
A comprehensive analysis of cross-country skiing races is a pivotal step in establishing effective training objectives and tactical strategies. This study aimed to develop a method of classifying sub-techniques and analyzing skiing characteristics during cross-country skiing skating style timed races on snow using high-precision kinematic GNSS devices. The study involved attaching GNSS devices to the heads of two athletes during skating style timed races on cross-country ski courses. These devices provided precise positional data and recorded vertical and horizontal head movements and velocity over ground (VOG). Based on these data, sub-techniques were classified by defining waveform patterns for G2, G3, G4, and G6P (G6 with poling action). The validity of the classification was verified by comparing the GNSS data with video analysis, a process that yielded classification accuracies ranging from 95.0% to 98.8% for G2, G3, G4, and G6P. Notably, G4 emerged as the fastest technique, with sub-technique selection varying among skiers and being influenced by skiing velocity and course inclination. The study’s findings have practical implications for athletes and coaches as they demonstrate that high-precision kinematic GNSS devices can accurately classify sub-techniques and detect skiing characteristics during skating style cross-country skiing races, thereby providing valuable insights for training and strategy development. Full article
(This article belongs to the Special Issue Sensors and Wearable Technologies in Sport Biomechanics)
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Figure 1
<p>The figure shows the Ikenotaira cross-country ski course, Japan, used in this study. The plotted data were obtained from the study subject, covering one lap of 0.8 km. The figure shows the course profile’s plan view data (<b>a</b>) and course inclination data (<b>b</b>).</p>
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<p>This picture and image show the experimental setup. The GNSS antenna was attached to the skier’s head, and the receiver and mobile router were stored in a small bag at the skier’s waist. This setup obtained head positioning data (latitude, longitude, altitude, and VOG) during the timed race.</p>
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<p>The figure shows the typical waveform patterns of subject A (<b>a</b>) and subject B (<b>b</b>) for G2, G3, G4, and G6P. The black dashed lines indicate the points where the net vertical head movement reaches a peak. The interval between two black lines represents one cycle. The green lines indicate the VOG. The blue waveform shows the trajectory of the net vertical head movement. The red waveform shows the trajectory of the net horizontal head movement. The red bars indicate the amplitude of the net horizontal head movement.</p>
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<p>The figure shows the quality of the positional data obtained from the RTK GNSS devices for subject A and subject B. The green color indicates the fix solution, the orange color indicates the float solution, and the blue color indicates the dGNSS solution.</p>
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<p>This figure shows the usage ratio over time (<b>a</b>) and the ratio over distance (<b>b</b>) for each sub-technique during the timed race.</p>
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<p>The distribution of sub-techniques used by two subjects during the second lap of the timed race is shown on the course profile’s plan view data.</p>
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<p>The course inclination data show the distribution of sub-techniques used by two subjects during the second lap of the timed race.</p>
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<p>The distribution of sub-techniques used by two subjects during the second lap of the timed race. The <span class="html-italic">X</span>-axis indicates the distance traveled, and the <span class="html-italic">Y</span>-axis indicates the VOG of the skier’s head.</p>
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<p>This figure shows the CL, CT, skiing velocity, and course inclination data for subjects A and B’s sub-techniques during the timed race. Each sub-technique cycle was defined from the vertical movement peak at the waveform data’s head to the next peak. The horizontal line within each box represents the median value of the dataset, while the “x” symbol denotes the mean value. ** indicates a significance level of <span class="html-italic">p</span> &lt; 0.01.</p>
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<p>The distribution of four sub-techniques used by two subjects during the timed race is shown with skiing velocity (<span class="html-italic">X</span>-axis) and course inclination (<span class="html-italic">Y</span>-axis).</p>
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<p>The distribution of four sub-techniques used by two subjects during the timed race is shown as a histogram of skiing velocity frequencies.</p>
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<p>The distribution of four sub-techniques used by two subjects during the timed race is shown as a histogram of course inclination frequencies.</p>
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15 pages, 11836 KiB  
Article
Variation in Glacier Albedo on the Tibetan Plateau between 2001 and 2022 Based on MODIS Data
by Ping Liu, Guangjian Wu, Bo Cao, Xuanru Zhao and Yuxuan Chen
Remote Sens. 2024, 16(18), 3472; https://doi.org/10.3390/rs16183472 - 19 Sep 2024
Viewed by 355
Abstract
Albedo is a primary driver of the glacier surface energy balance and consequent melting. As glacier albedo decreases, it further accelerates glacier melting. Over the past 20 years, glaciers on the Tibetan Plateau have experienced significant melting. However, our understanding of the variations [...] Read more.
Albedo is a primary driver of the glacier surface energy balance and consequent melting. As glacier albedo decreases, it further accelerates glacier melting. Over the past 20 years, glaciers on the Tibetan Plateau have experienced significant melting. However, our understanding of the variations in glacier albedo and its driving factors in this region remains limited. This study used MOD10A1 data to examine the average characteristics and variations in glacier albedo on the Tibetan Plateau from 2001 to 2022; the MOD10A1 snow cover product, developed at the National Snow and Ice Data Center, was employed to analyze spatiotemporal variations in surface albedo. The results indicate that the albedo values of glaciers on the Tibetan Plateau predominantly range between 0.50 and 0.60, with distinctly higher albedo in spring and winter, and lower albedo in summer and autumn. Glacier albedo on the Tibetan Plateau decreased at an average linear regression rate of 0.06 × 10−2 yr−1 over the past two decades, with the fastest declines occurring in autumn at an average rate of 0.18 × 10−2 yr−1, contributing to the prolongation of the melting period. Furthermore, significant variations in albedo change rates with altitude were found near the snowline, which is attributed to the transformation of the snow and ice surface. The primary factors affecting glacier albedo on the Tibetan Plateau are temperature and snowfall, whereas in the Himalayas, black carbon and dust primarily influence glacier albedo. Our findings reveal a clear decrease in glacier albedo on the Tibetan Plateau and demonstrate that seasonal and spatial variations in albedo and temperature are the most important driving factors. These insights provide valuable information for further investigation into surface albedo and glacier melt. Full article
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Graphical abstract

Graphical abstract
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<p>Glacier distribution on the Tibetan Plateau in 12 subregions (sourced from RGI 6.0).</p>
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<p>Spatial distribution characteristics of glacier albedo on the Tibetan Plateau between 2001 and 2022. Each circle represents the albedo data for one glacier.</p>
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<p>Trends of glacier albedo change on the Tibetan Plateau and in its various subregions from 2001 to 2022. Each circle represents the albedo data for one glacier.</p>
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<p>Relationship between glacier albedo and its rate of change with elevation in various subregions. The red bar in each graph represents the range of glacier snowline altitude [<a href="#B44-remotesensing-16-03472" class="html-bibr">44</a>]. The blue band represents the glacier albedo values, the red band represents the rate of change of glacier albedo, and the blue dashed line indicates where albedo’s change rate equals zero.</p>
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<p>Correlations between annual average albedo and driving factors in the Tibetan Plateau and its various subregions are represented by the Pearson correlation coefficient |R|. Blue dots indicate positive correlations between albedo and driving factors, while red dots indicate negative correlations between albedo and driving factors. The color change from red to green represents the rate of change in glacier albedo, with red indicating a decreasing rate and green indicating an increasing rate. Pre, Sf, Temp, BC, and Dust represent total precipitation, snowfall, temperature, black carbon, and dust, respectively.</p>
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<p>Correlation between glacier albedo (red dots and lines) and mass balance (blue columns) in different subregions and the zero-reference line for mass balance (blue dashed lines). The mass balance values were derived for the periods 2000–2004, 2005–2009, 2010–2014, and 2015–2019, and the corresponding albedo values were obtained for those four time periods. R represents Pearson’s correlation coefficient.</p>
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12 pages, 5379 KiB  
Article
Snow Leopard (Panthera uncia) Activity Patterns Using Camera Traps in the Qilian Mountain National Park (Qinghai Area), China
by Hu Ma, Bading Qiuying, Zhanlei Rong, Jinhu Zhang, Guozhu Liang, Shuguang Ma, Yayue Gao and Shengyun Chen
Animals 2024, 14(18), 2680; https://doi.org/10.3390/ani14182680 - 14 Sep 2024
Viewed by 496
Abstract
In recent years, there has been growing concern about the condition of snow leopards. The snow leopard (Panthera uncia), an apex predator of alpine ecosystems, is essential for the structural and functional stability of ecosystems. Monitoring of snow leopards’ activity patterns [...] Read more.
In recent years, there has been growing concern about the condition of snow leopards. The snow leopard (Panthera uncia), an apex predator of alpine ecosystems, is essential for the structural and functional stability of ecosystems. Monitoring of snow leopards’ activity patterns based on camera traps in the Qilian Mountain National Park (Qinghai area) between August 2020 to October 2023 was performed. The results showed that autumn is the peak period of snow leopard activity, especially in September when the frequency of activity is the highest, and there is one peak in the frequency of snow leopard daily activity in the time period of 18:00–22:00, while the highest overlap of the daily activity curves of snow leopards in different months was from spring to autumn (Δ = 0.97), and there were significant differences in diurnal activity rhythm between spring and autumn (p = 0.002). Snow leopards prefer sunny days, and they tend to be active at temperatures of −10–9 °C. Our research aimed to uncover the activity patterns of snow leopards at different scales within the study area and provide data for further studies on snow leopards and other wildlife by researchers. This study can be used to gain a comprehensive understanding of the ecological characteristics of snow leopards and to assess their habitats, and it will also serve as a reference for the local wildlife management authorities in formulating snow leopard conservation measures. Full article
(This article belongs to the Special Issue Ecology and Conservation of Large Carnivores)
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<p>A map of the study area showing the distribution of camera traps for monitoring snow leopard activity.</p>
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<p>Relative activity intensity of snow leopard daily activity and seasonal variation.</p>
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<p>Snow leopard daily activity and daily activity curves across different seasons.</p>
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<p>Relative activity intensity of monthly snow leopard activity.</p>
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<p>Relative activity intensity of seasonal snow leopard activity.</p>
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<p>Relative activity intensity of snow leopard activity at different temperature intervals.</p>
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<p>Percentages of valid snow leopard photographs in all weather types. Note: Sunny day—bright sunlight visible (includes visible sunrise and sunset light); cloudy day—sunlight not visible and weather is overcast; snowy day—weather in which snow is falling (includes nighttime when snow is falling).</p>
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13 pages, 2632 KiB  
Article
Effects of Cultivar Factors on Fermentation Characteristics and Volatile Organic Components of Strawberry Wine
by Wei Lan, Mei Zhang, Xinyu Xie, Ruilong Li, Wei Cheng, Tingting Ma and Yibin Zhou
Foods 2024, 13(18), 2874; https://doi.org/10.3390/foods13182874 - 11 Sep 2024
Cited by 1 | Viewed by 618
Abstract
Strawberry wine production is a considerable approach to solve the problem of the Chinese concentrated harvesting period and the short shelf life of strawberries, but the appropriative strawberry cultivars for fermentation are still undecided. In this study, the strawberry juice and wines of [...] Read more.
Strawberry wine production is a considerable approach to solve the problem of the Chinese concentrated harvesting period and the short shelf life of strawberries, but the appropriative strawberry cultivars for fermentation are still undecided. In this study, the strawberry juice and wines of four typical strawberry cultivars named Akihime (ZJ), Sweet Charlie (TCL), Snow White (BX), and Tongzhougongzhu (TZ) were thoroughly characterized for their physicochemical indicators, bioactive compounds, and volatile organic components (VOCs) to determine the optimal strawberry cultivars for winemaking. The results showed that there were significant differences in the total sugar content, pH, total acid, and other physicochemical indexes in the strawberry juice of different cultivars, which further affected the physicochemical indexes of fermented strawberry wine. Moreover, the content of polyphenols, total flavonoids, vitamin C, and color varied among the four strawberry cultivars. A total of 42 VOCs were detected in the strawberry juice and wines using headspace solid-phase microextraction coupled with gas chromatography–mass spectrometry (HS-SPME-GC-MS), and 3-methyl-1-butanol, linalool, trans-2-pinanol, hexanoic acid, and hexanoic acid ethyl ester were the differential VOCs to identify the strawberry wine samples of different cultivars. Overall, strawberry cultivar ZJ had a relatively high VOC and bioactive compound content, indicating that it is the most suitable cultivar for strawberry wine fermentation. In addition to determining the relatively superior fermentation characteristics of cultivar ZJ, the results may provide a theoretical basis for the raw material quality control and quality improvement of strawberry wine. Full article
(This article belongs to the Section Food Engineering and Technology)
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<p>Fermentation kinetics analysis of different cultivars of strawberry wine. (<b>A</b>) Brix; (<b>B</b>) residual sugar content; (<b>C</b>) ethanol content; (<b>D</b>) glucose content; (<b>E</b>) fructose content; BX: Snow White; TCL: Sweet Charlie; TZ: Tongzhougongzhu; ZJ: Akihime.</p>
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<p>Ethanol and residual sugar content of different cultivars of strawberry wine. (<b>A</b>) Ethanol content; (<b>B</b>) residual sugar content; BX: Snow White; TCL: Sweet Charlie; TZ: Tongzhougongzhu; ZJ: Akihime. Means with the same letter are not significantly different from each other (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>Total acid content and pH of different cultivars of strawberry juice and wines. (<b>A</b>) pH; (<b>B</b>) total acid content; BX: Snow White; TCL: Sweet Charlie; TZ: Tongzhougongzhu; ZJ: Akihime. Means with the same letter are not significantly different from each other (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>Total polyphenol, total flavonoid, and ascorbic acid content of different cultivars of strawberry juice and wines. (<b>A</b>) Total polyphenol content; (<b>B</b>) total flavonoid content; (<b>C</b>) ascorbic acid content; BX: Snow White; TCL: Sweet Charlie; TZ: Tongzhougongzhu; ZJ: Akihime. Means with the same letter are not significantly different from each other (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>Coordinate analysis and variable importance in the projection (VIP) analysis of VOCs in strawberry juice and wines of different cultivars. (<b>A</b>) PCA; (<b>B</b>) OPLS-DA; (<b>C</b>) VIP value. BX: Snow White; TCL: Sweet Charlie; TZ: Tongzhougongzhu; ZJ: Akihime. Juice (m) samples, BXm: Snow White; TCLm: Sweet Charlie; TZm: Tongzhougongzhu; ZJm: Akihime.</p>
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<p>Cluster heatmap analysis based on differential VOCs in strawberry juice and wine samples. Wine samples, BX: Snow White; TCL: Sweet Charlie; TZ: Tongzhougongzhu; ZJ: Akihime. Juice (m) samples, BXm: Snow White; TCLm: Sweet Charlie; TZm: Tongzhougongzhu; ZJm: Akihime.</p>
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21 pages, 20841 KiB  
Article
Snow Detection in Gaofen-1 Multi-Spectral Images Based on Swin-Transformer and U-Shaped Dual-Branch Encoder Structure Network with Geographic Information
by Yue Wu, Chunxiang Shi, Runping Shen, Xiang Gu, Ruian Tie, Lingling Ge and Shuai Sun
Remote Sens. 2024, 16(17), 3327; https://doi.org/10.3390/rs16173327 - 8 Sep 2024
Viewed by 592
Abstract
Snow detection is imperative in remote sensing for various applications, including climate change monitoring, water resources management, and disaster warning. Recognizing the limitations of current deep learning algorithms in cloud and snow boundary segmentation, as well as issues like detail snow information loss [...] Read more.
Snow detection is imperative in remote sensing for various applications, including climate change monitoring, water resources management, and disaster warning. Recognizing the limitations of current deep learning algorithms in cloud and snow boundary segmentation, as well as issues like detail snow information loss and mountainous snow omission, this paper presents a novel snow detection network based on Swin-Transformer and U-shaped dual-branch encoder structure with geographic information (SD-GeoSTUNet), aiming to address the above issues. Initially, the SD-GeoSTUNet incorporates the CNN branch and Swin-Transformer branch to extract features in parallel and the Feature Aggregation Module (FAM) is designed to facilitate the detail feature aggregation via two branches. Simultaneously, an Edge-enhanced Convolution (EeConv) is introduced to promote snow boundary contour extraction in the CNN branch. In particular, auxiliary geographic information, including altitude, longitude, latitude, slope, and aspect, is encoded in the Swin-Transformer branch to enhance snow detection in mountainous regions. Experiments conducted on Levir_CS, a large-scale cloud and snow dataset originating from Gaofen-1, demonstrate that SD-GeoSTUNet achieves optimal performance with the values of 78.08%, 85.07%, and 92.89% for IoU_s, F1_s, and MPA, respectively, leading to superior cloud and snow boundary segmentation and thin cloud and snow detection. Further, ablation experiments reveal that integrating slope and aspect information effectively alleviates the omission of snow detection in mountainous areas and significantly exhibits the best vision under complex terrain. The proposed model can be used for remote sensing data with geographic information to achieve more accurate snow extraction, which is conducive to promoting the research of hydrology and agriculture with different geospatial characteristics. Full article
(This article belongs to the Section Environmental Remote Sensing)
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<p>Overview of the proposed SD-GeoSTUNet. Hereinafter referred to as CNN branch and Swin-T branch, respectively. (<b>a</b>) Overview of Decoder Layer. (<b>b</b>) Overview of Feature Aggregation Module (FAM). (<b>c</b>) Overview of Residual Layer.</p>
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<p>(<b>a</b>) Overview of Edge-enhanced Convolution (EeConv), including a vanilla convolution, a central difference convolution (CDC), an angular difference convolution (ADC), a horizontal difference convolution (HDC), and a vertical difference convolution (VDC). (<b>b</b>) the principle of vertical difference convolution (VDC).</p>
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<p>The global distribution of the images in the experiment. Base map from Cartopy.</p>
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<p>Segmentation results of cloud and snow under different module combinations. (<b>a</b>) RGB true color image, (<b>b</b>) Label, (<b>c</b>) Concatenation, (<b>d</b>) FAM, (<b>e</b>) FAM + EeConv. In (<b>b</b>–<b>e</b>), black, blue, and white pixels represent background, cloud, and snow, respectively. The scene of the first row is at the center of 109.6°E, 48.8°N, and the date is 17 October 2017. The scene of the second row is at the center of 86.6°E, 28.5°N, and the date is 30 November 2016.</p>
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<p>Detection results of snow in mountain regions under different geographic information feature combination ablation experiments, and enlarged views marked with blue, green, and red boxes. (<b>a</b>) RGB true color image. (<b>b</b>) Label. (<b>c</b>) Experiment 1 detection results. (<b>d</b>) Experiment 2 detection results. (<b>e</b>) Experiment 3 detection results. In (<b>b</b>–<b>e</b>), black and white pixels represent the background and snow, respectively. The scene is at the center of 128.9°E, 44.7°N, and the date is 27 January 2018.</p>
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<p>Except for the background, the detection results of clouds and snow coexistence and the enlarged views (marked with the red box in the figure). (<b>a</b>) RGB true color image. (<b>b</b>) Label. (<b>c</b>) PSPNet. (<b>d</b>) Segformer. (<b>e</b>) U-Net. (<b>f</b>) CDNetV2. (<b>g</b>) GeoInfoNet. (<b>h</b>) SD-GeoSTUNet. In (<b>b</b>–<b>h</b>), black, blue, and white pixels represent the background, cloud, and snow, respectively. The scene of the first row is at the center of 104.2°E, 31.3°N, and the date is 29 March 2018. The scene of the third row is at the center of 104.6°E, 33.0°N, and the date is 29 March 2018.</p>
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<p>Except for the background, the detection results of pure snow and the enlarged views (marked with the red box in the figure). (<b>a</b>) RGB true color image. (<b>b</b>) Label. (<b>c</b>) PSPNet. (<b>d</b>) Segformer. (<b>e</b>) U-Net. (<b>f</b>) CDNetV2. (<b>g</b>) GeoInfoNet. (<b>h</b>) SD-GeoSTUNet. In (<b>b</b>–<b>h</b>), black, blue, and white pixels represent the background, cloud, and snow, respectively. The scene of the first row is at the center of 128.6°E, 51.3°N, and the date is 4 January 2016. The scene of the third row is at the center of 133.7°E, 50.9°N, and the date is 4 February 2018.</p>
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<p>Except for the background, the detection results of pure cloud and the enlarged views (marked with the red box in the figure). (<b>a</b>) RGB true color image. (<b>b</b>) Label. (<b>c</b>) PSPNet. (<b>d</b>) Segformer. (<b>e</b>) U-Net. (<b>f</b>) CDNetV2. (<b>g</b>) GeoInfoNet. (<b>h</b>) SD-GeoSTUNet. In (<b>b</b>–<b>h</b>), black, blue, and white pixels represent the background, cloud, and snow, respectively. This scene is at the center of 4.1°W, 54.2°N, and the date is 13 July 2016.</p>
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24 pages, 32875 KiB  
Article
Integrating Sequential Backward Selection (SBS) and CatBoost for Snow Avalanche Susceptibility Mapping at Catchment Scale
by Sinem Cetinkaya and Sultan Kocaman
ISPRS Int. J. Geo-Inf. 2024, 13(9), 312; https://doi.org/10.3390/ijgi13090312 - 29 Aug 2024
Viewed by 635
Abstract
Snow avalanche susceptibility (AS) mapping is a crucial step in predicting and mitigating avalanche risks in mountainous regions. The conditioning factors used in AS modeling are diverse, and the optimal set of factors depends on the environmental and geological characteristics of the region. [...] Read more.
Snow avalanche susceptibility (AS) mapping is a crucial step in predicting and mitigating avalanche risks in mountainous regions. The conditioning factors used in AS modeling are diverse, and the optimal set of factors depends on the environmental and geological characteristics of the region. Using a sub-optimal set of input features with a data-driven machine learning (ML) method can lead to challenges like dealing with high-dimensional data, overfitting, and reduced model generalization. This study implemented a robust framework involving the Sequential Backward Selection (SBS) algorithm and a decision-tree based ML model, CatBoost, for the automatic selection of predictive variables for AS mapping. A comprehensive inventory of a large avalanche period, previously derived from satellite images, was used for the investigations in three distinct catchment areas in the Swiss Alps. The integrated SBS-CatBoost approach achieved very high classification accuracies between 94% and 97% for the three catchments. In addition, the Shapley additive explanations (SHAP) method was employed to analyze the contributions of each feature to avalanche occurrences. The proposed methodology revealed the benefits of integrating advanced feature selection algorithms with ML techniques for AS assessment. We aimed to contribute to avalanche hazard knowledge by assessing the impact of each feature in model learning. Full article
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<p>A schematic overview of the proposed framework.</p>
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<p>Engelberger Aa, Meienreuss, and Göschenerreuss catchments (sub-catchments of the Reuss River Basin).</p>
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<p>Altitude maps of Engelberger Aa, Meienreuss, and Göschenerreuss catchments.</p>
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<p>LULC classification maps for Engelberger Aa, Meienreuss, and Göschenenreuss.</p>
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<p>Flowchart of iterative feature elimination using CatBoost with GridSearchCV.</p>
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<p>(<b>a</b>) The AS map of the Engelberger Aa catchment using the optimal feature set and (<b>b</b>) SHAP summary plot.</p>
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<p>(<b>a</b>) The AS map of the Meienreuss catchment using the optimal feature set and (<b>b</b>) SHAP summary plot.</p>
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<p>(<b>a</b>) The AS map of the Göschenerreuss catchment using the optimal feature set and (<b>b</b>) SHAP summary plot.</p>
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<p>The AS maps for Engelberger Aa, Meienreuss, and Göschenerreuss catchments, based on models with varying numbers of features (16, 15, 14, 13, and 12).</p>
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<p>The AS maps for Engelberger Aa, Meienreuss, and Göschenerreuss catchments, based on models with varying numbers of features (11, 10, 9, 8, and 7).</p>
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<p>The AS maps for Engelberger Aa, Meienreuss, and Göschenerreuss catchments, based on models with varying numbers of features (6, 5, 4, 3, and 2).</p>
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15 pages, 3986 KiB  
Article
Ecological Niche Characteristics of the Diets of Three Sympatric Rodents in the Meili Snow Mountain, Yunnan
by Feng Qin, Mengru Xie, Jichao Ding, Yongyuan Li and Wenyu Song
Animals 2024, 14(16), 2392; https://doi.org/10.3390/ani14162392 - 18 Aug 2024
Viewed by 544
Abstract
Understanding the dietary preferences and ecological niche characteristics of mammals not only reveals their adaptive strategies under environmental changes but also reveals the interspecific relationships and coexistence mechanisms among sympatric species. Nevertheless, such data are scarce for rodents inhabiting areas spanning a wide [...] Read more.
Understanding the dietary preferences and ecological niche characteristics of mammals not only reveals their adaptive strategies under environmental changes but also reveals the interspecific relationships and coexistence mechanisms among sympatric species. Nevertheless, such data are scarce for rodents inhabiting areas spanning a wide altitude range. This study employed DNA metabarcoding technology to analyze the stomach contents of Apodemus ilex, Apodemus chevrieri, and Niviventer confucianus, aiming to investigate their dietary compositions and diversity in the Meili Snow Mountain in Yunnan Province, China. Levins’s and Pianka’s indices were used to compare the interspecific niche breadth and niche overlaps. The results revealed the following: (1) Insecta (relative abundance: 59.4–78.4%) and Clitellata (relative abundance: 5.2–25.5%) were the primary animal food sources for the three species, while Magnoliopsida (relative abundance: 90.3–99.9%) constitutes their main plant food source. Considerable interspecific differences were detected in the relative abundance of primary animal and plant foods among the three species; (2) There was partial overlap in the genus-level animal food between A. ilex and N. confucianus (Ojk = 0.4648), and partial overlap in plant food between A. ilex and A. chevrieri (Ojk = 0.3418). However, no overlap exists between A. chevrieri and N. confucianus, either in animal or plant food; (3) There were no significant interspecific differences in the α-diversity of animal and plant foods among the three species. The feeding strategies and ecological niche variations of these rodents support the niche differentiation hypothesis, indicating that they have diversified in their primary food sources. This diversification may be a strategy to reduce competition and achieve long-term coexistence by adjusting the types and proportions of primary foods consumed. Full article
(This article belongs to the Section Ecology and Conservation)
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<p>Relative abundance (RA) of the top 15 food items for three species. The components of animal-based food are classified at the (<b>A</b>) order and (<b>B</b>) genus levels, and the components of plant-based food are classified at the (<b>C</b>) order and (<b>D</b>) genus levels.</p>
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<p>Taxonomic hierarchy tree of the dietary composition of the three species. (<b>A</b>) Animal-based foods; and (<b>B</b>) plant-based foods.</p>
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<p>Box-and-whisker plots for α-diversity of the diet compositions of the three species. The <span class="html-italic">X</span>-axis shows sample type. The <span class="html-italic">Y</span>-axis shows the value of each diversity. The <span class="html-italic">p</span>-value for each diversity index according to the Kruskal–Wallis test is located above the box-and-whisker plots. (<b>A</b>) Animal-based foods; and (<b>B</b>) plant-based foods.</p>
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<p>Non-metric multidimensional scaling (NMDS) of the dietary composition of the three species based on Jaccard distance. (<b>A</b>) Animal-based foods; and (<b>B</b>) plant-based foods.</p>
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<p>LEfSe analysis identified biomarkers in the food components of the three species. LDA scores above 2 and <span class="html-italic">p</span> values smaller than 0.05 were shown. (<b>A</b>,<b>B</b>) The histogram of Linear Discriminant Analysis (LDA) scores displays distinct species (biomarkers) with significantly different abundances across the three species. The length of each bar, representing the LDA score, indicates the effect size, which is the degree to which a biomarker accounts for the phenotypic variation among the groups. (<b>C</b>,<b>D</b>) The cladogram depicts taxonomic levels from phylum to genus (species) through concentric circles, with each circle’s diameter reflecting the taxon’s relative abundance. (<b>A</b>,<b>C</b>) Animal-based foods; and (<b>B</b>,<b>D</b>) plant-based foods.</p>
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14 pages, 7934 KiB  
Article
Assimilating Satellite-Derived Snow Cover and Albedo Data to Improve 3-D Weather and Photochemical Models
by Colleen Jones, Huy Tran, Trang Tran and Seth Lyman
Atmosphere 2024, 15(8), 954; https://doi.org/10.3390/atmos15080954 - 10 Aug 2024
Viewed by 520
Abstract
During wintertime temperature inversion episodes, ozone in the Uinta Basin sometimes exceeds the standard of 70 ppb set by the US Environmental Protection Agency. Since ozone formation depends on sunlight, and less sunlight is available during winter, wintertime ozone can only form if [...] Read more.
During wintertime temperature inversion episodes, ozone in the Uinta Basin sometimes exceeds the standard of 70 ppb set by the US Environmental Protection Agency. Since ozone formation depends on sunlight, and less sunlight is available during winter, wintertime ozone can only form if snow cover and albedo are high. Researchers have encountered difficulties replicating high albedo values in 3-D weather and photochemical transport model simulations for winter episodes. In this study, a process to assimilate MODIS satellite data into WRF and CAMx models was developed, streamlined, and tested to demonstrate the impacts of data assimilation on the models’ performance. Improvements to the WRF simulation of surface albedo and snow cover were substantial. However, the impact of MODIS data assimilation on WRF performance for other meteorological quantities was minimal, and it had little impact on ozone concentrations in the CAMx photochemical transport model. The contrast between the data assimilation and reference cases was greater for a period with no new snow since albedo appears to decrease too rapidly in default WRF and CAMx configurations. Overall, the improvement from MODIS data assimilation had an observed enhancement in the spatial distribution and temporal evolution of surface characteristics on meteorological quantities and ozone production. Full article
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<p>WRF one-way nested 12-4-1.33 km domains (<b>A</b>) and details of a 1.33 km domain, including topography and location of oil and gas wells (<b>B</b>). The white rectangle is Domain 2 and the red rectangle is Domain 3 from Table 4.</p>
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<p>Diagram of the MODIS data assimilation into the WRF and CAMx models.</p>
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<p>Comparison of the surface albedo fraction obtained in simulations using the WRF default configuration (<b>left</b>) and MODIS data assimilation (<b>right</b>). (Thin black lines = county outlines; heavy black outline = Uinta Basin ozone nonattainment area; and two-letter abbreviations = air quality monitoring stations.)</p>
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<p>Comparison of snow cover fraction (SNOWC) obtained in simulations using the WRF default configuration (<b>left</b>) and MODIS data assimilation (<b>right</b>). (Thin black lines = county outlines; heavy black outline = Uinta Basin ozone nonattainment area; and two-letter abbreviations = air quality monitoring stations.)</p>
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<p>Comparison of snow cover fraction, snow water equivalent, and snow depth using the WRF default configuration (REF) and MODIS data assimilation (MODIS). Green bars show periods where WRF reinitialized snow characteristics using the SNOWDAS dataset.</p>
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<p>Comparison of planetary boundary layer height (P.B.L.H.) and lapse rate using the WRF default configuration (REF) and MODIS data assimilation (MODIS).</p>
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<p>Comparison of photolysis rates simulated by CAMx using the default configuration (REF) and MODIS data assimilation (MODIS). (Green line = a new snow event.)</p>
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<p>Comparison of ozone at Ouray as simulated by CAMx using the default configuration (REF) and MODIS data assimilation (MODIS). (Red dash line = EPA National Ambient Air Quality Standard (NAAQS) for ozone).</p>
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14 pages, 7749 KiB  
Article
Analysis of Arctic Sea Ice Concentration Anomalies Using Spatiotemporal Clustering
by Yongheng Li, Yawen He, Yanhua Liu and Feng Jin
J. Mar. Sci. Eng. 2024, 12(8), 1361; https://doi.org/10.3390/jmse12081361 - 10 Aug 2024
Viewed by 551
Abstract
The dynamic changes of sea ice exhibit spatial clustering, and this clustering has characteristics extending from its origin, through its development, and to its dissipation. Current research on sea ice change primarily focuses on spatiotemporal variation trends and remote correlation analysis, and lacks [...] Read more.
The dynamic changes of sea ice exhibit spatial clustering, and this clustering has characteristics extending from its origin, through its development, and to its dissipation. Current research on sea ice change primarily focuses on spatiotemporal variation trends and remote correlation analysis, and lacks an analysis of spatiotemporal evolution characteristics. This study utilized monthly sea ice concentration (SIC) data from the National Snow and Ice Data Center (NSIDC) for the period from 1979 to 2022, utilizing classical spatiotemporal clustering algorithms to analyze the clustering patterns and evolutionary characteristics of SIC anomalies in key Arctic regions. The results revealed that the central-western region of the Barents Sea was a critical area where SIC anomaly evolutionary behaviors were concentrated and persisted for longer durations. The relationship between the intensity and duration of SIC anomaly events was nonlinear. A positive correlation was observed for shorter durations, while a negative correlation was noted for longer durations. Anomalies predominantly occurred in December, with complex evolution happening in April and May of the following year, and concluded in July. Evolutionary state transitions mainly occurred in the Barents Sea. These transitions included shifts from the origin state in the northwestern margin to the dissipation state in the central-north Barents Sea, from the origin state in the central-north to the dissipation state in the central-south, and from the origin state in the northeastern to the dissipation state in the central-south Barents Sea and southeastern Kara Sea. Various evolutionary states were observed in the same area on the southwest edge of the Barents Sea. These findings provide insights into the evolutionary mechanism of sea ice anomalies. Full article
(This article belongs to the Special Issue Recent Research on the Measurement and Modeling of Sea Ice)
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<p>Map of the distribution trends of SIC anomalies in different Arctic regions.</p>
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<p>Evolution process of an SIC anomaly event in the Barents–Kara Seas from July 1988 to September 1989.</p>
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<p>Spatial distribution of SIC anomaly event frequency in the Barents–Kara Seas.</p>
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<p>The average number of months with SIC anomaly events in the four key regions.</p>
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<p>Statistics on the duration and corresponding SSTC values of SIC anomaly events.</p>
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<p>The kernel density distribution of the (<b>a</b>) origin and (<b>b</b>) dissipation of SIC anomaly events in the Barents–Kara Seas.</p>
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<p>The spatial distribution of complex evolutionary behaviors of SIC anomaly events in the Barents–Kara Seas: (<b>a</b>) splitting; (<b>b</b>) merging; (<b>c</b>) merging–splitting; (<b>d</b>) complex evolution zones.</p>
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<p>Spatial transformation of SIC anomaly events in key sea areas.</p>
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14 pages, 1754 KiB  
Review
Micro- and Nano-Plastics Induced Release of Protein-Enriched Microbial Exopolymeric Substances (EPSs) in Marine Environments
by Wei-Chun Chin, Peter H. Santschi, Antonietta Quigg, Chen Xu, Peng Lin and Manoj Kamalanathan
Environments 2024, 11(8), 165; https://doi.org/10.3390/environments11080165 - 5 Aug 2024
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Abstract
Plastics are produced, consumed, and disposed of worldwide, with more than eight million tons of plastic litter entering the ocean each year. Plastic litter accumulates in marine and terrestrial environments through a variety of pathways. Large plastic debris can be broken down into [...] Read more.
Plastics are produced, consumed, and disposed of worldwide, with more than eight million tons of plastic litter entering the ocean each year. Plastic litter accumulates in marine and terrestrial environments through a variety of pathways. Large plastic debris can be broken down into micro- and nano-plastic particles through physical/mechanical mechanisms and biologically or chemically mediated degradation. Their toxicity to aquatic organisms includes the scavenging of pollutant compounds and the production of reactive oxygen species (ROS). Higher levels of ROS cause oxidative damages to microalgae and bacteria; this triggers the release of large amounts of exopolymeric substances (EPSs) with distinct molecular characteristics. This review will address what is known about the molecular mechanisms phytoplankton and bacteria use to regulate the fate and transport of plastic particles and identify the knowledge gaps, which should be considered in future research. In particular, the microbial communities react to plastic pollution through the production of EPSs that can reduce the plastic impacts via marine plastic snow (MPS) formation, allowing plastics to settle into sediments and facilitating their removal from the water column to lessen the plastic burden to ecosystems. Full article
(This article belongs to the Special Issue Plastics Pollution in Aquatic Environments)
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Figure 1

Figure 1
<p>Model of hypothetical pathways and processes for micro- and nano-plastic interactions with aquatic microbes in the environment. Plastic particles, when contacting microbes, induce the generation of radical oxygen species (ROS), which themselves induce changes in the expression of genes to produce more protein-enriched EPSs with higher protein-to-carbohydrate (P/C) ratios, making EPS aggregates more hydrophobic. Such EPSs are stickier and tend to promote aggregation with other particles, including denser mineral particles (scavenging), producing larger agglomerates that allow the lighter plastic particles to sink to sediments without disaggregation.</p>
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<p>Micro-plastics and laboratory-formed aggregates (MPS) consisting of marine phytoplankton (<span class="html-italic">Thalassiosira pseudonana</span>) and micro-plastics (1 μm polystyrene). Red, chlorophyll-containing structures; blue, carbohydrate-containing structures (e.g., EPSs); green, polystyrene microparticles ([<a href="#B48-environments-11-00165" class="html-bibr">48</a>,<a href="#B63-environments-11-00165" class="html-bibr">63</a>], with permission of the publisher).</p>
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<p>Diagram of interrelated aggregation steps (marked in blue) and questions, suggestions and tests for future research (marked in white), and experimental approaches (marked in orange).</p>
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