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Search Results (16,075)

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13 pages, 240 KiB  
Article
Factors Related to Evidence-Based Practices Among Mental Health Nurses in Thailand: A Cross-Sectional Study
by Napapat Manitkul, Kwaunpanomporn Thummathai and Patraporn Bhatarasakoon
Nurs. Rep. 2024, 14(4), 3084-3096; https://doi.org/10.3390/nursrep14040224 (registering DOI) - 18 Oct 2024
Abstract
Background and Objectives: Despite the robustness of evidence-based practice in increasing efficiency in nursing care and improving patient safety, using evidence in practice is still rare in mental health nursing. This correlational descriptive research aimed to explore the factors and examine the relationship [...] Read more.
Background and Objectives: Despite the robustness of evidence-based practice in increasing efficiency in nursing care and improving patient safety, using evidence in practice is still rare in mental health nursing. This correlational descriptive research aimed to explore the factors and examine the relationship between attitudes, knowledge/skills, organizational culture, mentorship, and demographic factors to evidence-based practices among mental health nurses working in psychiatric hospitals in Thailand. Methods: The sample consisted of 255 nurses working in psychiatric hospitals under the Thai Department of Mental Health, located in service units across the country’s four regions. The data collection tools included (1) a demographic questionnaire, (2) the Evidence-Based Practice Questionnaire: EBPQ, (3) Organizational Culture & Readiness for System-wide Integration of Evidence-Based Practice: OCRSIEP, and (4) the Evidence-Based Practice Mentorship Scale. Descriptive statistics and Spearman’s correlation coefficient were used for data analysis. Results: The findings revealed that the factors positively correlated with evidence-based practice among mental health nurses in Thailand were attitude with a mean score of 4.90 (r = 0.39, p-value < 0.001), knowledge/skills with a mean score of 4.69 (r = 0.61, p-value < 0.001), organizational culture with a mean score of 3.94 (r = 0.26, p-value < 0.001), and mentorship with a mean score of 2.77 (r = 0.16, p-value = 0.011). Demographic factors such as educational level (r = 0.21, p-value < 0.001) and work experience in psychiatric and mental health nursing (r = 0.14, p-value = 0.031) were also positively correlated. Conclusions: This research revealed that EBP knowledge and skills are the most significant factors related to evidence-based practice among Thai mental health nurses. Therefore, EBP knowledge and skills should be enhanced in the curriculum during the nursing study and through continuing education once nurses graduate. Organizational culture and mentorship also need to be promoted to strengthen the use of EBP in Thailand. Full article
25 pages, 6047 KiB  
Article
Insurance Coverage and Flood Exposure in the Gulf of Mexico: Scale, Social Vulnerability, Urban Form, and Risk Measures
by Anissa Hyde, Robert Habans, Mariam Valladares-Castellanos and Thomas Douthat
Water 2024, 16(20), 2968; https://doi.org/10.3390/w16202968 (registering DOI) - 17 Oct 2024
Abstract
Increasing flood losses in the Gulf of Mexico related to development patterns and climate hazards pose serious threats to resilience and insurability. The purpose of this study is to understand how scale, social vulnerability, risk, and urban form relate to National Flood Insurance [...] Read more.
Increasing flood losses in the Gulf of Mexico related to development patterns and climate hazards pose serious threats to resilience and insurability. The purpose of this study is to understand how scale, social vulnerability, risk, and urban form relate to National Flood Insurance Program (NFIP) policy coverage and flood exposure. Our multilevel models identify that flooding is significantly clustered by region and counties, especially shoreline counties. Our measures of risk suggest that the Federal Emergency Management Agency (FEMA) special flood hazard area (SFHA) underestimates risk and exposure when compared with the Flood Factor and that there is some compensation in terms of insurance coverage, suggesting a pattern of adverse selection. Older housing stock appears both less insured and less exposed, raising questions of whether current growth patterns are increasing risk independent of environmental change. Our models suggest that census tracts with higher percentages of black residents are less insured and more exposed, and a similar pattern exists for rural areas. Our results highlight the need to seek common solutions across the Gulf of Mexico, concentrating on the most flood-exposed counties, and that specific resilience strategies may be necessary to protect areas with socially vulnerable populations, especially in rural areas. Underlying challenges exist due to the spatial relationship between exposure and social vulnerability and the potential for adverse selection in insurance markets due to different measures of risk. Full article
(This article belongs to the Section Urban Water Management)
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Figure 1
<p>Map of Gulf of Mexico Study Area with (<b>A</b>) commuting zones, (<b>B</b>) counties, and (<b>C</b>) census tracts. The map shows a dynamic view of the scale differences in the study areas, using Orleans Parish as an example.</p>
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<p>Gulf of Mexico Study Area estimated NFIP Insurance Coverage Index. (<b>A</b>) Estimated active NFIP policies divided by total housing units between 2010 and 2014 per census tract and (<b>B</b>) Estimated active NFIP policies divided by total housing units per census tract between 2015 and 2019.</p>
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<p>Gulf of Mexico Study Area NFIP insurance claims. (<b>A</b>) Total count per census tract between 2010 and 2014 and (<b>B</b>) total count per census tract between 2015 and 2019.</p>
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<p>This map depicts a bivariate comparison of the effect size of random effect predictors, represented by counties, between the insurance coverage index model and the exposure model.</p>
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<p>Predicted exposure (NFIP claims) versus insurance coverage index. This Figure depicts the estimated effects of the insurance coverage index on the Gulf-wide exposure (NFIP claims) model using the ggeffects (Ludecke et al., 2024) package.</p>
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<p>SFHA versus “Risk Difference” in coverage versus exposure models. This Figure depicts claims and exposure in tracts with a greater proportion of homes in the SFHA and also the independent effect of “Risk Difference”, implying areas with underestimated risk (F.F. &gt; SFHA) have greater coverage and exposure. This suggests some adaptation to non-SFHA flood risk but also greater exposure for those locations. These findings buttress observations that SFHA-based risk measures may under-communicate the severity of flood risk. Whether the amount of adaptation via insurance is concomitant to increased risk and exposure is something that requires further investigation. We plot these estimates using the ggeffects [<a href="#B33-water-16-02968" class="html-bibr">33</a>] package.</p>
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<p>Coverage and exposure for pct Black at the tract level. This diagram depicts the models’ estimates of decreasing insurance coverage and increasing flood exposure in our Exposed Counties insurance coverage index and Exposed Counties Exposure (NFIP) models. We plot these estimates using the ggeffects [<a href="#B33-water-16-02968" class="html-bibr">33</a>] package.</p>
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<p>Correlation matrix between NFIP claims, estimated NFIP policy count, and estimated NFIP insurance coverage.</p>
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25 pages, 27177 KiB  
Article
Bollard Pull and Self-Propulsion Performance of a Waterjet Propelled Tracked Amphibian
by Taehyung Kim, Donghyeon Yoon, Jeongil Seo and Jihyeun Wang
J. Mar. Sci. Eng. 2024, 12(10), 1863; https://doi.org/10.3390/jmse12101863 - 17 Oct 2024
Abstract
This paper describes the unique full-scale bollard pull and self-propulsion tests of a large amphibious tracked military vehicle with two waterjet propulsors. To provide a reference for the self-propulsion and cavitation performance, a series of sea trials and bollard pull tests were performed [...] Read more.
This paper describes the unique full-scale bollard pull and self-propulsion tests of a large amphibious tracked military vehicle with two waterjet propulsors. To provide a reference for the self-propulsion and cavitation performance, a series of sea trials and bollard pull tests were performed in a military sea bay and in a large test basin, respectively. Good overall agreement between the sea trial and the computation was observed in the speed–power relationship. The cavitation-induced breakdown phenomenon was further explored via numerical simulations. The results indicated that the uncertainties in the numerical results were dominated by the scales of vapor bubbles. The analysis showed that the selection of the vapor bubble scale factors of 1.0 for growth and 0.05 for collapse were in good agreement with the experimental results. Rapid performance breakdown occurred when sufficient suction side-attached cavities were extended into the blade mid-chord and tip-board regions. Full article
(This article belongs to the Special Issue Ship Performance in Actual Seas)
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Figure 1
<p>Test vehicle in land mode (intentionally blurred).</p>
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<p>Test vehicle in sea mode (intentionally blurred).</p>
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<p>Full-scale waterjet pump: (<b>a</b>) impeller; (<b>b</b>) stator.</p>
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<p>Full-scale waterjet propulsor: (<b>a</b>) intake; (<b>b</b>) impeller duct housing.</p>
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<p>Test vehicle in rear view (intentionally blurred).</p>
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<p>Measurement system for seawater speed test.</p>
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<p>Bollard pull test configuration (top view).</p>
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<p>Bollard pull test instrumentation: (<b>a</b>) load cell and chain bridle; (<b>b</b>) field dynamometer; (<b>c</b>) data logger; (<b>d</b>) tow line; (<b>e</b>) test basin with floating tow line before bollard pulling.</p>
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<p>Bollard pull test instrumentation: (<b>a</b>) load cell and chain bridle; (<b>b</b>) field dynamometer; (<b>c</b>) data logger; (<b>d</b>) tow line; (<b>e</b>) test basin with floating tow line before bollard pulling.</p>
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<p>Combustion engine test bench equipped with water brake dynamometer.</p>
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<p>Setup of the combustion engine test bench.</p>
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<p>Surface grids for the amphibian: (<b>a</b>) half of the test vehicle; (<b>b</b>) waterjet propulsor.</p>
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<p>Grid system for the amphibian with the symmetry plane.</p>
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<p>Calculation domain and boundary conditions for the bollard pulling simulation.</p>
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<p>Computational mesh: (<b>a</b>) whole domain with catenary; (<b>b</b>) waterjet pump.</p>
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<p>Grid system: (<b>a</b>) computational domain; (<b>b</b>) propulsor with rotating block.</p>
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<p>Variation in the waterjet shaft delivered power with the speed of the amphibian as predicted by CFD and obtained in sea trial.</p>
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<p>CFD instantaneous dimensionless streamwise velocity at the free surface (left column) and the symmetry plane (right) for a self-propelled amphibian advancing at (<b>a</b>) <span class="html-italic">F<sub>WL</sub></span> = 0.26 and (<b>b</b>) <span class="html-italic">F<sub>WL</sub></span> = 0.50. The reference speed <span class="html-italic">V<sub>0</sub></span> is the amphibian vehicle’s speed.</p>
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<p>Comparison of the tow line installation methods.</p>
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<p>Variation in vehicle trim angle (<b>a</b>) and vehicle heave (<b>b</b>) with physical time as predicted by CFD.</p>
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<p>(<b>a</b>) CFD instantaneous velocity contour with free surface (yellow line) and tow line (red line); (<b>b</b>) zoomed-in view of the stern wake on the symmetry plane with velocity vector contour and velocity vectors.</p>
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<p>Engine shaft revolution speed data for bollard pull test and for CFD.</p>
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<p>(<b>a</b>) Computed total thrust and measured tow line load normalized by the initial peak tow line load of the experiment; (<b>b</b>) zoomed-in view near the initial impact force.</p>
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<p>Vehicle motion with variations in free surfaces (blue lines) and catenary coupling (red lines): (<b>a</b>) initial stage, t = 5.0 s; (<b>b</b>) shortly before initial impact stage, t = 12.5 s; (<b>c</b>) initial impact stage, t = 13.9 s; (<b>d</b>) final stage, t = 90.0 s; (<b>e</b>) corresponding normalized thrust versus time graph.</p>
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<p>(<b>a</b>) Computational mesh; (<b>b</b>) cavitation patterns (bollard pull condition, σ<sub>N</sub> = 1.53).</p>
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<p>A display of the vapor clouds’ (iso-surface = 0.5 for volume fraction of vapor) locations on the suction side of the blades and the inlet duct in the bollard pull condition, σ<sub>N</sub> = 1.25. The cavitation model used is Schnerr–Sauer (<b>a</b>) with the default positive and negative scaling and (<b>b</b>) with modified scaling.</p>
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<p>Thrust breakdown diagram for bollard pull condition. The red line presents the operating point of the amphibian with 100% shaft power. The zero-speed waterjet cavitation full-scale test was conducted with 135.2% increased shaft power.</p>
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<p>Vapor bubble scale factor diagram for bollard pull condition. The red line presents the operating point of the amphibian with 100% shaft power. The zero-speed waterjet cavitation full-scale test was conducted with 135.2% increased shaft power.</p>
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<p>Towing force coefficients at different cavitation numbers.</p>
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<p>Predicted cavitation structures around impeller and intake lip for several bollard pull conditions: (<b>a</b>) σ<sub>N</sub> = 4.14; (<b>b</b>) σ<sub>N</sub> = 2.99; (<b>c</b>) σ<sub>N</sub> = 2.26; (<b>d</b>) σ<sub>N</sub> = 1.92; (<b>e</b>) σ<sub>N</sub> = 1.53.</p>
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<p>Predicted pressure field near the waterjet intake lip for bollard pull condition, σ<sub>N</sub> = 1.25.</p>
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19 pages, 5186 KiB  
Article
Explosion Detection Using Smartphones: Ensemble Learning with the Smartphone High-Explosive Audio Recordings Dataset and the ESC-50 Dataset
by Samuel K. Takazawa, Sarah K. Popenhagen, Luis A. Ocampo Giraldo, Jay D. Hix, Scott J. Thompson, David L. Chichester, Cleat P. Zeiler and Milton A. Garcés
Sensors 2024, 24(20), 6688; https://doi.org/10.3390/s24206688 (registering DOI) - 17 Oct 2024
Abstract
Explosion monitoring is performed by infrasound and seismoacoustic sensor networks that are distributed globally, regionally, and locally. However, these networks are unevenly and sparsely distributed, especially at the local scale, as maintaining and deploying networks is costly. With increasing interest in smaller-yield explosions, [...] Read more.
Explosion monitoring is performed by infrasound and seismoacoustic sensor networks that are distributed globally, regionally, and locally. However, these networks are unevenly and sparsely distributed, especially at the local scale, as maintaining and deploying networks is costly. With increasing interest in smaller-yield explosions, the need for more dense networks has increased. To address this issue, we propose using smartphone sensors for explosion detection as they are cost-effective and easy to deploy. Although there are studies using smartphone sensors for explosion detection, the field is still in its infancy and new technologies need to be developed. We applied a machine learning model for explosion detection using smartphone microphones. The data used were from the Smartphone High-explosive Audio Recordings Dataset (SHAReD), a collection of 326 waveforms from 70 high-explosive (HE) events recorded on smartphones, and the ESC-50 dataset, a benchmarking dataset commonly used for environmental sound classification. Two machine learning models were trained and combined into an ensemble model for explosion detection. The resulting ensemble model classified audio signals as either “explosion”, “ambient”, or “other” with true positive rates (recall) greater than 96% for all three categories. Full article
(This article belongs to the Special Issue Signal Processing and Machine Learning for Sensor Systems)
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Figure 1
<p>The architecture of YAMNet and an example architecture of a transfer learning model using YAMNet.</p>
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<p>The smartphone deployment configuration of (<b>a</b>) the vented encasement and (<b>b</b>) the aluminum foil tube.</p>
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<p>Histograms of (<b>a</b>) the smartphone’s distance from the explosion source, (<b>b</b>) the effective yield of the explosion source, (<b>c</b>) the number of smartphone recordings per explosion event, and (<b>d</b>) the smartphone model used for data collection in SHAReD.</p>
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<p>Flowchart for the ensemble model along with the construction of D-YAMNet and LFM models.</p>
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<p>The confusion matrix of D-YAMNet on the test dataset. The percentages are calculated by rows (true labels) and the count for each cell is listed under these in parenthesis.</p>
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<p>The (<b>a</b>) normalized amplitude and (<b>b</b>) power spectral density of an “explosion” waveform that was misclassified as “ambient” by D-YAMNet. The explosion was in the 10 kg yield category and recorded by a smartphone ~11 km away from the source at a sample rate of 800 Hz.</p>
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<p>The confusion matrix of the LFM on the test dataset. The percentages are calculated by rows (true labels) and the count for each cell is listed under these in parenthesis.</p>
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<p>The (<b>a</b>) normalized amplitude and the (<b>b</b>) power spectral density of an “other” waveform that was misclassified as “explosion” by the LFM. The “other” sound was from an ESC-50 waveform labeled “dog”.</p>
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<p>The confusion matrix of the ensemble model on the test dataset. The percentages are calculated by rows (true labels) and the count for each cell is listed under these in parenthesis.</p>
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<p>The precision-recall curves for (<b>a</b>) D-YAMNet and (<b>b</b>) LFM.</p>
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<p>The average confusion matrix for (<b>a</b>) D-YAMNet and (<b>b</b>) LFM.</p>
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<p>Expanded normalized microphone data from SHAReD for event INL_20220714_07 for smartphone ID (<b>a</b>) 1806169311 and (<b>c</b>) 2122963039 and the corresponding predicted labels from D-YAMNet, LFM, and the ensemble model for smartphone ID (<b>b</b>) 1806169311 and (<b>d</b>) 2122963039. The predicted labels were obtained on segmented section of the full waveform with 0.96 s duration and 50% overlap.</p>
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<p>The (<b>a</b>) confusion matrix and (<b>b</b>) precision-recall curves for the YAMNet model. The average precision (AP) for VINEDA was 0.86.</p>
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<p>The (<b>a</b>) confusion matrix and (<b>b</b>) precision-recall curves for the YAMNet model.</p>
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24 pages, 10327 KiB  
Article
Assessing the Scale Effects of Dynamics and Socio-Ecological Drivers of Ecosystem Service Interactions in the Lishui River Basin, China
by Suping Zeng, Chunqian Jiang, Yanfeng Bai, Hui Wang, Lina Guo and Jie Zhang
Sustainability 2024, 16(20), 8990; https://doi.org/10.3390/su16208990 - 17 Oct 2024
Abstract
Grasping how scale influences the interactions among ecosystem services (ESs) is vital for the sustainable management of multiple ESs at the regional level. However, it is currently unclear whether the actual ES interactions and their driving mechanisms are consistent across different spatial and [...] Read more.
Grasping how scale influences the interactions among ecosystem services (ESs) is vital for the sustainable management of multiple ESs at the regional level. However, it is currently unclear whether the actual ES interactions and their driving mechanisms are consistent across different spatial and temporal scales. Therefore, using the Lishui River Basin of China as a case study, we analyzed the spatial and temporal distribution of five key ESs across three scales (grid, sub-watershed, and county) from 2010 to 2020. We also innovatively used Pearson correlation analysis, Self-organizing Mapping (SOM), and random forest analysis to assess the dynamic trends of trade-offs/synergies among ESs, ecosystem service bundles (ESBs), and their main socio-ecological drivers across different spatiotemporal scales. The findings showed that (1) the spatial distribution of ESs varied with land use types, with high-value areas mainly in the western and northern mountainous regions and lower values in the eastern part. Temporally, significant improvements were observed in soil conservation (SC, 3028.23–5023.75 t/hm2) and water yield (WY, 558.79–969.56 mm), while carbon sequestration (CS) and habitat quality (HQ) declined from 2010 to 2020. (2) The trade-offs and synergies among ESs exhibited enhanced at larger scales, with synergies being the predominant relationship. These relationships remained relatively stable over time, with trade-offs mainly observed in ES pairs related to nitrogen export (NE). (3) ESBs and their socio-ecological drivers varied with scales. At the grid scale, frequent ESB flows and transformations were observed, with land use/land cover (LULC) being the main drivers. At other scales, climate (especially temperature) and topography were dominant. Ecosystem management focused on city bundles or downstream city bundles in the east of the basin, aligning with urban expansion trends. These insights will offer valuable guidance for decision-making regarding hierarchical management strategies and resource allocation for regional ESs. Full article
(This article belongs to the Section Environmental Sustainability and Applications)
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<p>Location of the study area. (<b>a</b>) Geographical location, (<b>b</b>) elevation, and (<b>c</b>) land use type in 2010, 2015, and 2020 of the Lishui River Basin.</p>
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<p>Analysis framework. ESs, ecosystem services; Pre, mean annual precipitation; Eva, evapotranspiration; DTB, root restricting layer depth; PAWC, plant effective water content; DEM, digital elevation model; K, soil erodibility; SOM, Self-organizing Map. * indicates a <span class="html-italic">p</span> &lt; 0.05, ** indicates a <span class="html-italic">p</span> &lt; 0.01.</p>
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<p>Spatial–temporal distribution of ESs at the 1 km × 1 km grid scale.</p>
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<p>Spatial–temporal dynamics of ESs at the sub-watershed scale.</p>
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<p>The spatial–temporal patterns of ESs at the county scale.</p>
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<p>Density and normal distribution of ESs values in different spatial and temporal scales in Lishui River Basin. The red, green, and blue bars represent the ES values of the grid scale, sub-watershed scale, and county scale, respectively. The red curve is the normal distribution curve of ES values.</p>
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<p>Spatial–temporal variations of ESs include (<b>a</b>) the rate of change in ESs in 2010–2020; (<b>b</b>) notable disparities in ESs over various scales and periods, indicated by mean ± standard deviation. Here, distinct uppercase letters denote significant differences across different times, while distinct lowercase letters highlight variations among different scales.</p>
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<p>Correlation between different ESs across varied scales [grid (1 km × 1 km), sub-watershed, and county]. (<b>a</b>–<b>c</b>) represent the correlations of ESs at the grid, sub-watershed, and county scales, respectively. * indicates a <span class="html-italic">p</span> &lt; 0.05, ** indicates a <span class="html-italic">p</span> &lt; 0.01.</p>
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<p>(<b>a</b>) Spatio-temporal distribution of ES bundles at the grid scale. (<b>b</b>) ES composition and magnitude within these bundles, where longer segments indicate higher ES supply. (<b>c</b>) Area transitions between different ES bundles from 2000 to 2010 (left to middle column) and from 2010 to 2020 (middle to right column) at the grid scale. Note: B1, key synergetic bundle; B2, CS bundle; B3, CS-SC-WY synergy bundle; B4, city bundle; B5, CS-WY synergy bundle; B6, CS-NE synergy bundle.</p>
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<p>(<b>a</b>) Spatio-temporal dynamics of ES bundles at the sub-watershed scale from 2010 to 2020. (<b>b</b>) Composition and relative magnitude of ESs within these bundles, where longer segments indicate increased supply. (<b>c</b>) Areas of transformation among various ES bundles. Note: B-1, CS-WY synergy bundle; B-2, key synergetic bundle; B-3, downstream city bundle; B-4, CS bundle.</p>
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<p>(<b>a</b>) Spatio-temporal distribution of ES bundles at the county scale. (<b>b</b>) Composition and scale of ESs within these bundles, where longer segments indicate a higher supply. (<b>c</b>) Transformation areas among different ES bundles. Note: B-a, CS-WY synergy bundle; B-b, CS bundle; B-c, downstream city bundle; B-d, HQ-SC-WY synergy bundle.</p>
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<p>The relative significance of socio-ecological drivers on the distribution of ESBs over time. Here, “mean decrease accuracy” represents how much the accuracy of the random forest model declines when the value of a driver is randomized. A higher mean decrease in accuracy indicates greater importance of the driver. Detailed descriptions of the drivers, including full names for any abbreviations, are provided in <a href="#sustainability-16-08990-t003" class="html-table">Table 3</a>.</p>
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17 pages, 5177 KiB  
Article
A Branched Convolutional Neural Network for Forecasting the Occurrence of Hazes in Paris Using Meteorological Maps with Different Characteristic Spatial Scales
by Chien Wang
Atmosphere 2024, 15(10), 1239; https://doi.org/10.3390/atmos15101239 - 17 Oct 2024
Abstract
A convolutional neural network (CNN) has been developed to forecast the occurrence of low-visibility events or hazes in the Paris area. It has been trained and validated using multi-decadal daily regional maps of many meteorological and hydrological variables alongside surface visibility observations. The [...] Read more.
A convolutional neural network (CNN) has been developed to forecast the occurrence of low-visibility events or hazes in the Paris area. It has been trained and validated using multi-decadal daily regional maps of many meteorological and hydrological variables alongside surface visibility observations. The strategy is to make the machine learn from available historical data to recognize various regional weather and hydrological regimes associated with low-visibility events. To better preserve the characteristic spatial information of input features in training, two branched architectures have recently been developed. These architectures process input features firstly through several branched CNNs with different kernel sizes to better preserve patterns with certain characteristic spatial scales. The outputs from the first part of the network are then processed by the second part, a deep non-branched CNN, to further deliver predictions. The CNNs with new architectures have been trained using data from 1975 to 2019 in a two-class (haze versus non-haze) classification mode as well as a regression mode that directly predicts the value of surface visibility. The predictions of regression have also been used to perform the two-class classification forecast using the same definition in the classification mode. This latter procedure is found to deliver a much better performance in making class-based forecasts than the direct classification machine does, primarily by reducing false alarm predictions. The branched architectures have improved the performance of the networks in the validation and also in an evaluation using the data from 2021 to 2023 that have not been used in the training and validation. Specifically, in the latter evaluation, branched machines captured 70% of the observed low-visibility events during the three-year period at Charles de Gaulle Airport. Among those predicted low-visibility events by the machines, 74% of them are true cases based on observation. Full article
(This article belongs to the Special Issue Data Analysis in Atmospheric Research)
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<p>Daily average surface visibility in km observed at Paris Charles de Gaulle Airport (CDG) since 1975. An unknown systematic switch in statistics occurred during 2000–2002 (the 25th to 27th year after 1975) that affects mostly on the results in the clear (high percentile) than haze (low percentile) days.</p>
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<p>The data domain of meteorological and hydrological input features, consisting of 96 latitudinal and 128 longitudinal grids with an increment of 0.25 degree. The red dot marks the location of Charles de Galle Airport.</p>
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<p>Diagrams of various architectures of HazeNet. Here Max represents a MaxPooling layer, Ave is an Average layer. For 2D convolutional layer, “128, 1 × 1” represents a layer with 128 filter sets and a kernel size of 1 × 1. Each convolutional layer is followed by a batch normalization layer unless otherwise indicated. The bottom part in HazeNetb and HazeNetb2 is a CNN consisting of 8-convolutional layers with 3 × 3 kernels, adopted from the last part of original HazeNet (see [<a href="#B3-atmosphere-15-01239" class="html-bibr">3</a>]). Part of the charts were drawn using visualkeras package (Gavrikov, P., 2020, <a href="https://github.com/paulgavrikov/visualkeras" target="_blank">https://github.com/paulgavrikov/visualkeras</a>; accessed on 14 October 2024).</p>
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<p>Examples of normalized maps (96 by 128 pixels) of meteorological features with different characteristic spatial scales. See <a href="#atmosphere-15-01239-t002" class="html-table">Table 2</a> for the description of plotted features.</p>
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<p>The outputs (62 by 94 pixels) of the first four filters from the second convolutional layer (6 × 6 kernel) in HazeNet. Different color scales are used for various panels to highlight their distributions.</p>
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<p>The outputs of various branches of HazeNetb just before the concatenate layer (Ref. <a href="#atmosphere-15-01239-f003" class="html-fig">Figure 3</a>), shown are those of the first filter set, each has 48 by 64 pixels. Different color scales are used for various panels to highlight their distributions.</p>
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<p>(<b>Left</b>) The outputs from the small kernel branch (input1) just before the concatenate layer of HazeNetb2, shown only the first two filter sets. (<b>Right</b>) The same but for the outputs from the large kernel (input2) branch. Each panel has 48 by 64 pixels. Different color scales are used for various panels to highlight their distributions.</p>
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<p>Dynamically calculated validation scores of statistical performance metrics with training progression in a classification training of HazeNetb. Each score point represents statistics of results calculated using the entire validation dataset. Here Acc and Loss represent the accuracy and loss in training, respectively, VAcc and VLoss the same metrics but in validation; while others are all validation scores commonly used in classification forecasting: precision, recall, and F1 score have a range of [0, 1], ETS is the equitable threat score with a range of [−1/3, 1], and HSS is the Heidke skill score ([−inf, 1]), all derived based on the so-called confusion matrix (Ref. [<a href="#B3-atmosphere-15-01239" class="html-bibr">3</a>]) for their definitions).</p>
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<p>The F1 scores of machines with different architectures obtained from the end of training session validation (last 100-epoch means). Here P25C represents the results from classification mode for events with vis. equal or lower than the 25th percentile of long-term observations, while P25 and P15 are the results from regression–classification mode, here P15 is for events with vis. equal or lower than the 15th percentile of long-term observations.</p>
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<p>The same as <a href="#atmosphere-15-01239-f009" class="html-fig">Figure 9</a> but for performance of various machines in the evaluation using data from 2021 to 2023.</p>
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<p>Evaluation results of HazeNetb2 using data from 2021 to 2023: (<b>a</b>) a scatter plot of predicted versus observed quantities of vis. in km; and (<b>b</b>) the same comparison but displayed as time series. Total number of LVD (P25) during the 3-year period is 118.</p>
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16 pages, 7141 KiB  
Article
Tree-Ring-Based Hydroclimatic Variability in the Southeast Coastal Region of China
by Xinguang Cao, Pei-ken Kao, Yingjun Li, Zheng Zhao, Hongbing Hu, Jing Hu, Di Zhang and Keyan Fang
Forests 2024, 15(10), 1813; https://doi.org/10.3390/f15101813 - 17 Oct 2024
Viewed by 79
Abstract
The frequency and severity of extreme hydroclimatic events in humid southeastern China have increased in the past half century, which is a serious concern. In this research, we used wood samples from 134 trees growing in the southeast coastal region of China (SECC) [...] Read more.
The frequency and severity of extreme hydroclimatic events in humid southeastern China have increased in the past half century, which is a serious concern. In this research, we used wood samples from 134 trees growing in the southeast coastal region of China (SECC) to reconstruct the Standardized Precipitation Evapotranspiration Index (SPEI) for the last 173 years (1843–2015 CE). Our reconstruction explained 41.6% of the variance contained in the November SPEI at a 7 month scale for the period 1957–2015. 17 extremely wet and 16 extremely dry events, 8 dry and 9 wet periods have been identified since 1843, and the most severe drought, coinciding with historical records, occurred in 1869 and 1870. The reconstruction reveals. Although the results reveal a modest upward trend in the SPEI and a predominance of extreme wet events over droughts throughout the period, the 20th century accounted for nine of the summers classified as extremely dry. Strong agreement between the current reconstruction and existing hydroclimatic reconstructions in southeastern China implied that our reconstruction exhibited high reliability. The composite anomalies of circulation during the period from May to November (MJJASON) indicate that the temporal variability in the SPEI reconstruction might be modulated by the local Hadley cell. These findings underscore the effectiveness of tree-ring-derived indices for reconstructing hydroclimatic trends in China’s humid regions and enhance our understanding of these changes within a long-term framework. Full article
(This article belongs to the Section Forest Hydrology)
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<p>(<b>Left</b>) the location of the study area in the southeast coastal region of China (SECC) on a topographic map. (<b>Right</b>) the location of the sampling sites in the study area (see <a href="#forests-15-01813-t001" class="html-table">Table 1</a>).</p>
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<p>(<b>a</b>) Regional composite tree-ring width (TRW) chronology (CTRW-1) produced by pooling all the TRW measurements from the three sites together; (<b>b</b>) the number of sampled cores included in the chronology; (<b>c</b>,<b>d</b>) expressed population signal (EPS) and running inter-series correlation (Rbar) statistics; (<b>e</b>) regional composite TRW chronology (CTRW-2) produced via principal component analysis (PCA) of the three chronologies (GS, FGY, and BSC); (<b>f</b>) regional composite TRW chronology (CTRW-3) produced by arithmetically averaging the three chronologies.</p>
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<p>The flowchart of the methodology section.</p>
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<p>(<b>a</b>) A Walter-Lieth diagram showing monthly temperature (red line) and precipitation (blue line). The annual average temperature and monthly average rainfall data (1957–2015) from the meteorological stations are located in the upper left and upper right corners, respectively. (<b>b</b>) Correlation between SPEI index at different time scales (X axis) from 1 to 24 months (Y axis) and CTRW-1 for the period 1957–2015. The highest correlation was in November after 7 months.</p>
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<p>(<b>a</b>) A comparison between actual and estimated SPEI values during 1957–2015. (<b>b</b>) The coherent spectrum of the cross-wavelet between the actual and estimated time series. (<b>c</b>) The Nov. SPEI 07 reconstruction from 1843 to 2015 for the SECC. The red line represents a 10 year low-pass filter of the annual values. The black line is the variation trend of Nov. SPEI 07. Extreme wet and dry years are represented by blue and red triangles, respectively.</p>
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<p>The split and cross-validation: (<b>a</b>,<b>b</b>) represent the time series of observed (green) and reconstructed Nov. SPEI 07 data for the calibration (red) and verification (purple) periods of the split sample procedure; (<b>c</b>) represents the time series of observed (green) and reconstructed Nov. SPEI 07 (black) data.</p>
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<p>Spatial correlations (α = 0.10) across China’s southeast region between the (<b>a</b>) non-transformed and (<b>b</b>) first-year difference CTRW-1 chronology and the SPEI for the period 1957–2015. The positions of the three tree-ring sampling points are represented by solid black circles.</p>
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<p>Comparisons of the reconstructed Nov. SPEI 07 with other hydroclimatic reconstructions. The referenced reconstructions are (<b>a</b>,<b>d</b>) May–November precipitation from GPCC v2020, (<b>b</b>,<b>e</b>) the tree-ring chronology of <span class="html-italic">Cryptomeria fortune</span> from Meihua Mountains in southeastern China [<a href="#B5-forests-15-01813" class="html-bibr">5</a>], and (<b>c</b>,<b>f</b>) the dryness/wetness index (DWI). The interannual (<b>a</b>–<b>c</b>) and decadal fluctuations (<b>d</b>–<b>f</b>) were separated using the 10-year low-pass filter.</p>
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<p>May to November (MJJASON) composite anomalies from 1981, 1982, 2005, and 2015, with (<b>a</b>) precipitation, (<b>b</b>) outgoing longwave radiation (OLR), (<b>c</b>) omega at 500 hPa, and (<b>d</b>) height-latitude cross-profiles (averaged over 110°−120° E) of omega.</p>
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19 pages, 4374 KiB  
Article
Improving Water Quality by Combined Sedimentation and Slow Sand Filtration: A Case Study in a Maasai Community, Tanzania
by Nadav Bachar, Noga Lindenstrauss, Saar David, Micha Mirkin, Noam Polani, Osher Gueta, Shaked Partush and Avner Ronen
Appl. Sci. 2024, 14(20), 9467; https://doi.org/10.3390/app14209467 - 17 Oct 2024
Viewed by 240
Abstract
Some Maasai communities in northern Tanzania face severe water quality and scarcity issues, significantly impacting the health and living conditions of the local population. To address the water quality challenges faced by one of the Maasai communities, where thousands of residents consume water [...] Read more.
Some Maasai communities in northern Tanzania face severe water quality and scarcity issues, significantly impacting the health and living conditions of the local population. To address the water quality challenges faced by one of the Maasai communities, where thousands of residents consume water with high turbidity and contaminants, a team of volunteers, primarily engineering students from Ben-Gurion University of the Negev, conducted a project in 2023. This project aimed to improve water quality through the implementation of combined sedimentation and biofilm-based slow sand filtration systems. These systems utilized mechanical filtration via sand bed percolation and biological filtration through biofilm formation, which effectively reduced turbidity and removed contaminants. The biofilm maturation significantly enhanced filtration efficiency, achieving turbidity reduction from levels exceeding 10,000 to below 5 NTU, meeting WHO standards. Comprehensive water quality assessments revealed contamination in the water sources, with elevated levels of lead (up to 11 mg/L), which pose health risks. In addition, we evaluated locally accessible materials such as chalk and limestone for coagulation and precipitation, enhancing water clarity and removing contaminants. Despite constraints that shortened the mission duration, the results provide a solid foundation for future efforts to improve water quality in the region. This study highlights the potential of low-tech biofilm-based filtration systems for sustainable water purification in resource-limited environments. It demonstrates the effectiveness of small-scale household systems and presents a development protocol optimized for local materials and water contamination characteristics. Full article
(This article belongs to the Special Issue Advances in Biofilms and Their Applications in Biotechnology)
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<p>Map of the local water sources [<a href="#B4-applsci-14-09467" class="html-bibr">4</a>].</p>
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<p>Images of local water sources for animal and human consumption: (<b>a</b>) Red Dam, mainly used to serve animals but also as a drinking water source for residents from some local villages; (<b>b</b>) Sokoru Dam (showing human consumption); (<b>c</b>) Sokoru Dam (showing animal consumption).</p>
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<p>Slow sand filter: (<b>a</b>) The sand filtration systems that were built in Tanzania; (<b>b</b>) schematic figure of the SSF: a thick layer of gravel at the bottom and a large layer of sand above it. The mechanisms the SSF uses are mechanical filtration through sand, biological filtration via biofilm development (schmutzdecke), and pathogen removal along with turbidity reduction.</p>
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<p>Measured water properties in wells and reservoirs (<b>a</b>) Well B; (<b>b</b>) local reservoirs.</p>
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<p>(<b>a</b>) Turbidity values over three days—proof of concept system (the value shown each day is the lowest recorded for that day); (<b>b</b>) water quality parameters comparison after filtration.</p>
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<p>(<b>a</b>) Comparison of turbidity values after one day (the value shown for each system is the system’s lowest recorded); (<b>b</b>) comparison of turbidity removal efficiency after one day.</p>
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<p>Turbidity values for System 3 over three days (the value shown each day is the lowest recorded for that day).</p>
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<p>(<b>a</b>) System 4—Turbidity over repetition (the value shown each day is the lowest recorded for that day); (<b>b</b>) System 5—Turbidity over repetition (the value shown each day is the lowest recorded for that day).</p>
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<p>(<b>a</b>) System 4—Turbidity over repetition (the value shown each day is the lowest recorded for that day); (<b>b</b>) System 5—Turbidity over repetition (the value shown each day is the lowest recorded for that day).</p>
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<p>Water parameters after filtration with Systems 4 and 5 (relative to Red Dam).</p>
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<p>Top view of the filter showing biofilm formation.</p>
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<p>Summary of sedimentation experiments with chalks.</p>
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<p>Water parameters after filtration with limestone (relative to Red Dam).</p>
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17 pages, 8087 KiB  
Article
Multi-Scale Analysis of Water Purification Ecosystem Service Flow in Taihu Basin for Land Management and Ecological Compensation
by Haoyang Chen and Wenbo Cai
Land 2024, 13(10), 1694; https://doi.org/10.3390/land13101694 - 16 Oct 2024
Viewed by 293
Abstract
This study investigates the spatial correlation and service flow of supply and demand for water purification ecosystem services at multiple scales (i.e., the Taihu Lake Basin, sub-basin, and county) by quantitatively assessing the supply–demand relationship of nitrogen and phosphorus and introducing the SPANS [...] Read more.
This study investigates the spatial correlation and service flow of supply and demand for water purification ecosystem services at multiple scales (i.e., the Taihu Lake Basin, sub-basin, and county) by quantitatively assessing the supply–demand relationship of nitrogen and phosphorus and introducing the SPANS algorithm to characterize the service flow paths. Through quantitative analysis, the supply–demand relationship between nitrogen and phosphorus was evaluated, and the SPANS algorithm was introduced to characterize the service flow paths. The results show that the water purification ecosystem services in the southwestern region and around Taihu Lake exhibit a good supply–demand balance, while a significant supply–demand deficit is observed in the northern and southeastern regions. Service flow analysis indicates that surplus areas are primarily concentrated in hilly and urbanized central regions, whereas deficit areas are mainly located in non-urban centers. Based on these findings, ecological compensation suggestions are proposed, including dynamic adjustment, differentiated compensation, cross-city collaboration, and guidance of social capital participation, to promote continuous improvement in water quality and sustainable development within the basin. Full article
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<p>Study area.</p>
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<p>Multi-step ecosystem-based approach.</p>
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<p>Nitrogen supply (<b>a1</b>) and demand (<b>a2</b>)/phosphorus supply (<b>b1</b>) and demand (<b>b2</b>) in the Taihu Basin in 2020.</p>
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<p>Nitrogen supply–demand differences (<b>a1</b>) and indices (<b>a2</b>)/phosphorus supply–demand differences (<b>b1</b>) and indices (<b>b2</b>) at the county level in the Taihu Basin in 2020.</p>
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<p>Nitrogen supply–demand differences (<b>a1</b>) and indices (<b>a2</b>)/phosphorus supply–demand differences (<b>b1</b>) and indices (<b>b2</b>) at the sub-basin level in the Taihu Basin in 2020.</p>
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<p>The supply and demand of nitrogen water purification ecosystem services after one (<b>a1</b>) and ten (<b>a2</b>) unit time flows. The supply and demand of phosphorus water purification ecosystem services after one (<b>b1</b>) and ten (<b>b2</b>) unit time flows.</p>
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<p>The flow path and spatial distribution of water purification services in the Taihu Basin in 2020.</p>
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63 pages, 63361 KiB  
Review
Innovative Circular Biowaste Valorisation—State of the Art and Guidance for Cities and Regions
by Miguel Ángel Suárez Valdés, José M. Soriano Disla, Elisa Gambuzzi and Gemma Castejón Martínez
Sustainability 2024, 16(20), 8963; https://doi.org/10.3390/su16208963 - 16 Oct 2024
Viewed by 278
Abstract
The management of the organic fraction of municipal solid waste (OFMSW), also called urban biowaste, and urban wastewater sludge (UWWS) represents a challenge for cities and regions, which want to adopt innovative urban bioeconomy approaches for their treatment and production of high-added-value products [...] Read more.
The management of the organic fraction of municipal solid waste (OFMSW), also called urban biowaste, and urban wastewater sludge (UWWS) represents a challenge for cities and regions, which want to adopt innovative urban bioeconomy approaches for their treatment and production of high-added-value products beyond the traditional anaerobic digestion (AD) and compost. This adoption is often restricted by the availability and maturity of technologies. The research object of this manuscript, based on the findings of EU Horizon 2020 project HOOP, is the identification of state-of-the-art circular technologies for material valorisation of OFMSW and UWWS, following a novel screening methodology based on the scale of implementation (tested at least at pilot scale). The screening resulted in 25 technologies, which have been compared and discussed under a multidisciplinary assessment approach, showing their enabling factors and challenges, their current or potential commercial status and their compatibility with the traditional technologies for urban biowaste treatment (composting and AD). The bioproducts cover market sectors such as agriculture, chemistry, nutrition, bioplastics, materials or cosmetics. Therefore, the results of this review help project promoters at city/region level to select innovative technologies for the conversion of OFMWS and UWWS into high value products. Full article
(This article belongs to the Section Waste and Recycling)
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<p>Scheme of anaerobic digestion process.</p>
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11 pages, 2132 KiB  
Article
The Single-Scattering Albedo of Black Carbon Aerosols in China
by Xiaolin Zhang and Yuanyuan Wu
Atmosphere 2024, 15(10), 1238; https://doi.org/10.3390/atmos15101238 - 16 Oct 2024
Viewed by 242
Abstract
Black carbon (BC) aerosols have attracted wide attention over the world due to their significant climate effects on local and global scales. BC extinction aerosol optical thickness (AOT), scattering AOT, and single scattering albedo (SSA) over China are systematically studied based on the [...] Read more.
Black carbon (BC) aerosols have attracted wide attention over the world due to their significant climate effects on local and global scales. BC extinction aerosol optical thickness (AOT), scattering AOT, and single scattering albedo (SSA) over China are systematically studied based on the MERRA-2 satellite reanalysis data from 1983 to 2022 in terms of the spatial, yearly, seasonal, and monthly variations. The extinction and scattering AOTs of BC show similar spatial distribution, with high values in eastern and southern China, generally as opposed to BC SSA. A decrease in BC extinction and scattering AOTs has been documented over the last decade. The mean BC extinction AOT, scattering AOT, and SSA over China are 0.0054, 0.0014, and 0.26, respectively. The BC SSA showed small variations during 1983–2022, although a high BC extinction AOT and scattering AOT have been seen in the last two decades. During different decades, the seasonal patterns of BC extinction and scattering AOTs may differ, whereas the BC SSA shows seasonal consistency. Significant monthly variations in the BC SSA are seen over four decades, which are in agreement with their seasonal patterns. The mean BC extinction AOTs are 0.037, 0.033, 0.023, and 0.0054, whereas the average BC scattering AOTs are 0.0088, 0.0082, 0.0060, and 0.0014 in the Pearl River Delta (PRD), Yangtze River Delta (YRD), Beijing–Tianjin–Hebei (BTH) region, and Tarim Basin (TB), respectively. It is interesting to see that BC SSA values in the TB region are generally higher than those over the PRD, YRD and BTH areas, whereas the reverse is true for BC extinction and scattering AOTs. This study provides references for further research on black carbon aerosols and air pollution in China. Full article
(This article belongs to the Special Issue Atmospheric Black Carbon: Monitoring and Assessment)
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<p>Locations of study areas in China. The Tarim Basin (TB, region: 36–45° N, 80–91° E), Pearl River Delta (PRD, region: 22–24° N, 112–115° E), Yangtze River Delta (YRD, region: 29–33° N, 117–122° E), and Beijing–Tianjin–Hebei region (BTH, region: 38–41° N, 114–119° E) are considered four representative regions in China in the study.</p>
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<p>Spatial distributions of the extinction AOT (<b>a</b>–<b>d</b>), scattering AOT (<b>e</b>–<b>h</b>), and SSA (<b>i</b>–<b>l</b>) of black carbon aerosols over China. Four decades, 1983–1992 (<b>a</b>,<b>e</b>,<b>i</b>), 1993–2002 (<b>b</b>,<b>f</b>,<b>j</b>), 2003–2012 (<b>c</b>,<b>g</b>,<b>k</b>) and 2013–2022 (<b>d</b>,<b>h</b>,<b>l</b>), are shown.</p>
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<p>Temporal variations in annual average BC extinction AOT (<b>a</b>), scattering AOT (<b>b</b>), and SSA (<b>c</b>) over China from 1983 to 2022. Uncertainty bars are the standard deviations related to the mean values.</p>
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<p>Seasonal average BC extinction AOT, scattering AOT, and SSA over mainland China in spring (MAM), summer (JJA), fall (SON), and winter (DJF). The results for the periods 1983–1992 (<b>a</b>,<b>e</b>,<b>i</b>), 1993–2002 (<b>b</b>,<b>f</b>,<b>j</b>), 2003–2012 (<b>c</b>,<b>g</b>,<b>k</b>), and 2013–2022 (<b>d</b>,<b>h</b>,<b>l</b>) are shown.</p>
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<p>Monthly average BC extinction AOT (<b>a</b>–<b>d</b>), scattering AOT (<b>e</b>–<b>h</b>), and SSA (<b>i</b>–<b>l</b>) over mainland China. The results for the periods 1983–1992 (<b>a</b>,<b>e</b>,<b>i</b>), 1993–2002 (<b>b</b>,<b>f</b>,<b>j</b>), 2003–2012 (<b>c</b>,<b>g</b>,<b>k</b>), and 2013–2022 (<b>d</b>,<b>h</b>,<b>l</b>) are shown.</p>
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<p>Temporal variations in annual average BC extinction AOT (<b>a</b>), scattering AOT (<b>b</b>), and SSA (<b>c</b>) over the TB, PRD, YRD, and BTH regions from 1983 to 2022.</p>
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<p>Seasonal average BC extinction AOT (<b>a</b>–<b>d</b>), scattering AOT (<b>e</b>–<b>h</b>), and SSA (<b>i</b>–<b>l</b>) in the TB, PRD, YRD, and BTH regions in spring (MAM), summer (JJA), fall (SON), and winter (DJF). Results during 1983–1992 (<b>a</b>,<b>e</b>,<b>i</b>), 1993–2002 (<b>b</b>,<b>f</b>,<b>j</b>), 2003–2012 (<b>c</b>,<b>g</b>,<b>k</b>), and 2013–2022 (<b>d</b>,<b>h</b>,<b>l</b>) are shown.</p>
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<p>Monthly average BC extinction AOT (<b>a</b>–<b>d</b>), scattering AOT (<b>e</b>–<b>h</b>), and SSA (<b>i</b>–<b>l</b>) in the TB, PRD, YRD, and BTH regions. Results in the periods of 1983–1992 (<b>a</b>,<b>e</b>,<b>i</b>), 1993–2002 (<b>b</b>,<b>f</b>,<b>j</b>), 2003–2012 (<b>c</b>,<b>g</b>,<b>k</b>), and 2013–2022 (<b>d</b>,<b>h</b>,<b>l</b>) are considered.</p>
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18 pages, 1548 KiB  
Article
Bedside Neuromodulation of Persistent Pain and Allodynia with Caloric Vestibular Stimulation
by Trung T. Ngo, Wendy N. Barsdell, Phillip C. F. Law, Carolyn A. Arnold, Michael J. Chou, Andrew K. Nunn, Douglas J. Brown, Paul B. Fitzgerald, Stephen J. Gibson and Steven M. Miller
Biomedicines 2024, 12(10), 2365; https://doi.org/10.3390/biomedicines12102365 - 16 Oct 2024
Viewed by 322
Abstract
Background: Caloric vestibular stimulation (CVS) is a well-established neurological diagnostic technique that also induces many phenomenological modulations, including reductions in phantom limb pain (PLP), spinal cord injury pain (SCIP), and central post-stroke pain. Objective: We aimed to assess in a variety of persistent [...] Read more.
Background: Caloric vestibular stimulation (CVS) is a well-established neurological diagnostic technique that also induces many phenomenological modulations, including reductions in phantom limb pain (PLP), spinal cord injury pain (SCIP), and central post-stroke pain. Objective: We aimed to assess in a variety of persistent pain (PP) conditions (i) short-term pain modulation by CVS relative to a forehead ice pack cold-arousal control procedure and (ii) the duration and repeatability of CVS modulations. The tolerability of CVS was also assessed and has been reported separately. Methods: We conducted a convenience-based non-randomised single-blinded placebo-controlled study. Thirty-eight PP patients were assessed (PLP, n = 8; SCIP, n = 12; complex regional pain syndrome, CRPS, n = 14; non-specific PP, n = 4). Patients underwent 1–3 separate-day sessions of iced-water right-ear CVS. All but four also underwent the ice pack procedure. Analyses used patient-reported numerical rating scale pain intensity (NRS-PI) scores for pain and allodynia. Results: Across all groups, NRS-PI for pain was significantly lower within 30 min post-CVS than post-ice pack (p < 0.01). Average reductions were 24.8% (CVS) and 6.4% (ice pack). CRPS appeared most responsive to CVS, while PLP and SCIP responses were less than expected from previous reports. The strongest CVS pain reductions lasted hours to over three weeks. CVS also induced substantial reductions in allodynia in three of nine allodynic CRPS patients, lasting 24 h to 1 month. As reported elsewhere, only one patient experienced emesis and CVS was widely rated by patients as a tolerable PP management intervention. Conclusions: Although these results require interpretative caution, CVS was found to modulate pain relative to an ice pack control. CVS also modulated allodynia in some cases. CVS should be examined for pain management efficacy using randomised controlled trials. Full article
(This article belongs to the Special Issue Emerging Trends in Neurostimulation and Neuromodulation Research)
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<p>Brain activity associated with caloric vestibular stimulation (CVS). Stronger and better-replicated evidence of CVS-induced brain activation and deactivation is indicated by the darker red and blue tones, respectively. CVS activates—via vestibular pathways (indicated by black arrows)—contralateral structures including the anterior cingulate cortex, insular cortex, putamen in basal ganglia and various temporoparietal areas. Several of these brain regions have been implicated in pain processing [<a href="#B33-biomedicines-12-02365" class="html-bibr">33</a>,<a href="#B34-biomedicines-12-02365" class="html-bibr">34</a>,<a href="#B35-biomedicines-12-02365" class="html-bibr">35</a>,<a href="#B36-biomedicines-12-02365" class="html-bibr">36</a>,<a href="#B37-biomedicines-12-02365" class="html-bibr">37</a>].</p>
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<p>Mean pain intensity at baseline and up to 30 min post-CVS#1 and post-ice pack intervention for all patients who underwent both conditions (N = 34). Results revealed significantly lower pain ratings compared to baseline within 30 min post-CVS than post-ice pack intervention. Error bars designate standard deviations. * Results revealed significantly lower pain ratings compared to baseline within 30 min post-CVS than post-ice pack intervention.</p>
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<p>Case illustrations of pain and allodynia modulation by CVS: (<b>A</b>) CRPS-12—a case of ≥50% short-term pain reduction following CVS that had returned to baseline by 24 h. (<b>B</b>) CRPS-13—a case of ≥30–49% short-term pain reduction following CVS that became a ≥50% reduction by 24 h, returning to baseline by 1 week. (<b>C</b>) NPP-1—a case of ≥30–49% short-term pain reduction following CVS that became a ≥50% reduction by 24 h, still evident after 1 week. (<b>D</b>) CRPS-2—a striking case of ≥50% short-term allodynia reduction following CVS, completely ameliorated allodynia by 24 h, two further CVS sessions on consecutive days keeping allodynia at low levels, repeat reduction evident after CVS#3 and allodynia reported to be still low (2/10) a month later. (<b>E</b>) CRPS-6—a case of a short-lived increase in allodynia following CVS with amelioration of allodynia by 24 h and allodynia still absent after 1 week. (<b>F</b>) CRPS-11—a case of &lt;30% allodynia reduction following CVS that became a ≥50% allodynia reduction by 24 h, returning to baseline by 1 week and a repeatable reduction after a second CVS session.</p>
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<p>Tolerability and side effects of CVS and patient willingness to repeat the intervention if it reduced their pain by 50% or more for one week or one month (figure reprinted from [<a href="#B47-biomedicines-12-02365" class="html-bibr">47</a>]). Solid bars indicate the percentage of patients (<span class="html-italic">n</span> = 25 with formal tolerability data available), while dotted lines indicate the reported intensity of CVS-induced discomfort/pain and side effects. The vast majority of patients reported that despite finding the procedure uncomfortable or painful or experiencing side effects, they were willing to repeat the intervention if it helped their pain.</p>
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13 pages, 2934 KiB  
Article
Recovery and Restructuring of Fine and Coarse Soil Fractions as Earthen Construction Materials
by Mazhar Hussain, Ines Lamrous, Antony Provost, Nathalie Leblanc, Hafida Zmamou, Daniel Levacher and Abdoulaye Kane
Sustainability 2024, 16(20), 8952; https://doi.org/10.3390/su16208952 - 16 Oct 2024
Viewed by 313
Abstract
Excessive consumption of natural resources to meet the growing demands of building and infrastructure projects has put enormous stress on these resources. On the other hand, a significant quantity of soil is excavated for development activities across the globe and is usually treated [...] Read more.
Excessive consumption of natural resources to meet the growing demands of building and infrastructure projects has put enormous stress on these resources. On the other hand, a significant quantity of soil is excavated for development activities across the globe and is usually treated as waste material. This study explores the potential of excavated soils in the Brittany region of France for its reuse as earthen construction materials. Characterization of soil recovered from building sites was carried out to classify the soils and observe their suitability for earthen construction materials. These characteristics include mainly Atterberg limits, granulometry, organic matter and optimum moisture content. Soil samples were separated into fine and coarse particles through wet sieving. The percentage of fines (particles smaller than 0.063 mm) in studied soil samples range from 28% to 65%. The methylene blue value (MBV) for Lorient, Bruz and Polama soils is 1, 1.2 and 1.2 g/100 g, and French classification (Guide de terrassements des remblais et des couches de forme; GTR) of soil samples is A1, B5 and A1, respectively. The washing of soils with lower fine content helps to recover excellent-quality sand and gravel, which are a useful and precious resource. However, residual fine particles are a waste material. In this study, three soil formulations were used for manufacturing earth blocks. These formulations include raw soil, fines and restructured soil. In restructured soil, a fine fraction of soil smaller than 0.063 mm was mixed with 15% recycled sand. Restructuring of soil fine particles helps to improve soil matrix composition and suitability for earth bricks. Compressed-earth blocks of 4 × 4 × 16 cm were manufactured at a laboratory scale for flexural strength testing by using optimum molding moisture content and compaction through Proctor normal energy. Compressive strength tests were performed on cubic blocks of size 4 × 4 × 4 cm. Mechanical testing of bricks showed that bricks with raw soil had higher resistance with a maximum of 3.4 MPa for Lorient soil. Removal of coarse particles from soil decreased the strength of bricks considerably. Restructuring of fines with recycled sand improves their granular skeleton and increases the compressive strength and durability of bricks. Full article
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<p>Brittany soil samples: Lorient (<b>a</b>), Polama (<b>b</b>) and Bruz (<b>c</b>).</p>
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<p>Wet processing of excavated soils.</p>
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<p>Raw soil (<b>a</b>), mixing soil with water (<b>b</b>), wet sieving of soil (<b>c</b>) and fine particles of soil (<b>d</b>).</p>
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<p>Samples of prismatic earth blocks.</p>
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<p>Granulometry of recycled sand.</p>
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<p>Minerology of recycled sand.</p>
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<p>Flexural and compressive strength (MPa) of earth blocks. Note: S = raw soil; F = fine soil; RS = restructured soil; Fc = compressive strength; Ft = flexural strength.</p>
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20 pages, 3024 KiB  
Article
Investigating the Spatial Pattern of White Oak (Quercus alba L.) Mortality Using Ripley’s K Function Across the Ten States of the Eastern US
by Saaruj Khadka, Hong S. He and Sougata Bardhan
Forests 2024, 15(10), 1809; https://doi.org/10.3390/f15101809 - 16 Oct 2024
Viewed by 265
Abstract
White oak mortality is a significant concern in forest ecosystems due to its impact on biodiversity and ecosystem functions. Understanding the factors influencing white oak mortality is crucial for effective forest management and conservation efforts. In this study, we aimed to investigate the [...] Read more.
White oak mortality is a significant concern in forest ecosystems due to its impact on biodiversity and ecosystem functions. Understanding the factors influencing white oak mortality is crucial for effective forest management and conservation efforts. In this study, we aimed to investigate the spatial pattern of WOM rates across the eastern US and explore the underlying processes behind the observed spatial patterns. Multicycle forest inventory and analysis data were compiled to capture all white oak plots. WOM data were selected across plot systems that utilized declining basal areas between two periods. Ripley’s K function was used to study the spatial pattern of WOM rates. Results showed clustered patterns of WOM rates at local and broad scales that may indicate stand-level competition and regional variables affecting white oaks’ dynamics across southern and northern regions. Results also indicated random patterns at broad scales, suggesting variations in topographic and hydrological conditions across the south and northern regions. However, the central region indicated both clustered and random patterns at the local scale that might be associated with inter-species competition and the possibility of environmental heterogeneity, respectively. Furthermore, uniform patterns of WOM rate at a broad scale across all regions might suggest regions with spatially homogeneous environmental factors acting on the dynamics of white oaks. This research might be helpful in identifying impacted areas of white oaks at varying scales. Future research is needed to comprehensively assess biotic and abiotic factors at various spatial scales aimed at mitigating WOM. Full article
(This article belongs to the Section Forest Inventory, Modeling and Remote Sensing)
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<p>Study area mainly showing forest covers and others across ten states of the eastern US.</p>
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<p>Our study area showing (<b>A</b>) spatial distribution of WOM rate plots and (<b>B</b>) kernel density distribution of WOM rates across different latitudes and longitudes of the eastern United States.</p>
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<p>Ripley’s K function showing clustered, random, and uniform patterns across varying scales of (<b>A</b>) southern, (<b>B</b>) central, and (<b>C</b>) northern regions WOM rates in the eastern United States.</p>
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<p>Ripley’s K function showing clustered, random, and uniform patterns across varying scales of (<b>A</b>) southern, (<b>B</b>) central, and (<b>C</b>) northern regions WOM rates in the eastern United States.</p>
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14 pages, 5326 KiB  
Article
A Circulation Study Based on the 2022 Sino–Vietnamese Joint Survey Data from the Beibu Gulf
by Zhi Zeng, Jinwen Liu, Xin Zhao, Zhijie Chen, Yanyu Chen, Bo Chen, Maochong Shi and Wei He
Water 2024, 16(20), 2943; https://doi.org/10.3390/w16202943 - 16 Oct 2024
Viewed by 200
Abstract
This study analyzed the horizontal and vertical distribution characteristics of temperature and salinity in the central and eastern regions of the Beibu Gulf, based on conductivity measurements in summer 2022, temperature, and depth (CTD) measurement data from the Sino–Vietnamese cooperative project “Demonstration Study [...] Read more.
This study analyzed the horizontal and vertical distribution characteristics of temperature and salinity in the central and eastern regions of the Beibu Gulf, based on conductivity measurements in summer 2022, temperature, and depth (CTD) measurement data from the Sino–Vietnamese cooperative project “Demonstration Study on Ecological Protection and Management in Typical Bays: Seasonal Survey of the Beibu Gulf”. Furthermore, the study utilized the computational results from the numerical Finite-Volume Coastal Ocean Model (FVCOM) to elucidate the intrinsic patterns that formed the temperature and salinity distribution characteristics in August 2022 from both thermodynamic and dynamic perspectives. The circulation in the Beibu Gulf drives external seawater to move northward from the bay mouth. During this movement, numerous upwelling areas are created by lateral Ekman transport. The formation of different scales of cyclonic and anticyclonic vortices and current convergence zones is influenced by topography, runoff, and the water flux from the Qiongzhou Strait, which are key factors in the formation of upwelling and downwelling. The surface circulation in August 2022 significantly differed from the 20-year average surface circulation, with an influx of 1.15 × 104 m3/s more water entering the Beibu Gulf compared to the multi-year average. The water flux from the Qiongzhou Strait is a critical factor affecting the circulation patterns in the Beibu Gulf. The northeastern waters of the Beibu Gulf are characterized by current convergence zones, where extensive upwelling occurs. The rich nutrient salts in these areas promote the reproduction and growth of phytoplankton and zooplankton, making this the most favorable ecological environment in the Beibu Gulf and serving as a natural reserve for fisheries, coral reefs, dugongs, and Bryde’s whales. Full article
(This article belongs to the Section Oceans and Coastal Zones)
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<p>Locations of the Sino–Vietnam joint temperature and salinity survey stations in 2022 and bathymetry map.</p>
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<p>Measured spatial distribution of temperature ((<b>top</b>), °C) and salinity (<b>bottom</b>) in the surface and bottom layers of Beibu Gulf. The dashed lines denote the data boundaries.</p>
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<p>The temperature and salinity distribution across sections.</p>
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<p>The temperature and salinity distribution across sections.</p>
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<p>(<b>a</b>) Unstructured mesh of the nested model in the Beibu Gulf and SCS and (<b>b</b>) observation stations for runoff (yellow dots), tides (blue dots), and currents (red dot, A). RR denotes Red River. PR denotes Pearl River.</p>
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<p>Simulated sea surface temperature (SST) distribution in the Beibu Gulf for August 2022.</p>
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<p>Average circulation in the Beibu Gulf in the (<b>a</b>) surface, (<b>b</b>) middle, (<b>c</b>) bottom, and (<b>d</b>) full layers in August 2022.</p>
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<p>Multi-year average (1993–2012) circulation in the Beibu Gulf in August at the (<b>a</b>) surface, (<b>b</b>) middle, and (<b>c</b>) bottom, with (<b>d</b>) vertical averaging.</p>
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<p>Multi-year average (1993–2012) of the (<b>a</b>) middle- and (<b>b</b>) bottom-layer circulation in the Beibu Gulf in February.</p>
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<p>Distribution of coral reefs in the northeastern Beibu Gulf [<a href="#B30-water-16-02943" class="html-bibr">30</a>].</p>
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