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21 pages, 2766 KiB  
Article
A Quantitative Approach to Evaluating Multi-Event Resilience in Oil Pipeline Incidents
by Labiba N. Asha, Nita Yodo and Ying Huang
CivilEng 2025, 6(1), 1; https://doi.org/10.3390/civileng6010001 (registering DOI) - 28 Dec 2024
Viewed by 189
Abstract
This study introduces a quantitative approach to evaluating the resilience of oil pipeline systems against various natural and physical disruptions. Resilience is increasingly essential in critical infrastructure to ensure continuous operations and minimize disruption impacts. However, existing quantitative methods often need specific time-dependent [...] Read more.
This study introduces a quantitative approach to evaluating the resilience of oil pipeline systems against various natural and physical disruptions. Resilience is increasingly essential in critical infrastructure to ensure continuous operations and minimize disruption impacts. However, existing quantitative methods often need specific time-dependent data, making measuring resilience in pipeline infrastructure challenging. To address this gap, this paper proposed a comprehensive framework by integrating the existing incident database with key features of assessing failure probabilities based on historical events and developing multi-event resilience indicators based on system performance under various disruptions. The methodology employs event tree analysis to quantify the probabilities of multiple failure scenarios and their impact on pipeline operations and recovery efforts. The practical application of the proposed approach was demonstrated using real-world oil pipeline incident data from across the United States, covering the period from 2010 to 2022. The focus was on multiple event scenarios involving pipeline disruptions, followed by shutdowns, examining how these events collectively impact pipeline resilience. The results indicate that corrosion failure, equipment failure, and natural hazard damage significantly impact oil pipeline resilience. Corrosion and equipment failures affect resilience primarily due to their frequency, while natural hazard damage, despite its lower occurrence rate, is more unpredictable and often requires more frequent shutdowns. Understanding these failure causes and their impacts is essential for enhancing the resilience and sustainable operation of oil pipeline systems. Full article
(This article belongs to the Collection Recent Advances and Development in Civil Engineering)
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<p>A visual representation of the quantitative resilience framework integrated with existing incident reporting infrastructure.</p>
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<p>Ranking failure causes based on the frequency and probability of occurrence during the 2010–2022 oil pipeline incident period.</p>
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<p>Event tree analysis of multiple intermediate events following an initiating event.</p>
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<p>Incident count of subsequent events during the 2010–2022 oil pipeline study period.</p>
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<p>Counts of failure consequences for Scenarios 1 through 4 during the 2010–2022 oil pipeline incident period.</p>
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<p>Resilience analysis results for all failure cause categories.</p>
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27 pages, 999 KiB  
Article
Measuring the Impacts of Argentina’s Presidential Election Process in 2023 on the Stock Market Performance Using a Dynamic Event Study Methodology
by Eduardo Enrique Sandoval Álamos, Claudio René Molina Mac-Kay and Erwin Octavio Taipe Aquino
Risks 2025, 13(1), 1; https://doi.org/10.3390/risks13010001 - 27 Dec 2024
Viewed by 237
Abstract
This study measured the individual and conjoint effects of Argentina’s primaries and first- and second-voting presidential election results, as well as their post-election comparative effects, on the stock market performance of its most relevant economic sectors. Within four different estimation methods, the state-space [...] Read more.
This study measured the individual and conjoint effects of Argentina’s primaries and first- and second-voting presidential election results, as well as their post-election comparative effects, on the stock market performance of its most relevant economic sectors. Within four different estimation methods, the state-space specification outperformed the rest. The findings suggest that investors can under/overreact compared to post-election sectors performance, the public services sector being the exception. Therefore, those investors who anticipated the election results by liquidating positions in companies in the materials sector and investing more in companies in the energy and other industrial sectors achieved a superior performance. Full article
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<p>Types of political risk of most concern to investors in developing economies by percentage. Source: Adapted from WIPR <a href="#B48-risks-13-00001" class="html-bibr">World Bank</a> (<a href="#B48-risks-13-00001" class="html-bibr">2013</a>).</p>
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<p>Data and Argentine presidential election process.</p>
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<p>Significant sector market betas and country risk sensitiveness. Source: own elaboration.</p>
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24 pages, 3114 KiB  
Article
Risk Perception in the Nigua River Basin: Key Determinants and Policy Implications
by Casimiro Maldonado-Santana, Antonio Torres-Valle, Carol Franco-Billini and Ulises Javier Jauregui-Haza
Water 2025, 17(1), 45; https://doi.org/10.3390/w17010045 - 27 Dec 2024
Viewed by 326
Abstract
The Nigua River basin in the Dominican Republic is a critical hydrographic area facing significant environmental challenges, including deforestation, soil erosion and pollution from mining and agricultural activities. This study explores the role of risk perception among local residents in shaping policies for [...] Read more.
The Nigua River basin in the Dominican Republic is a critical hydrographic area facing significant environmental challenges, including deforestation, soil erosion and pollution from mining and agricultural activities. This study explores the role of risk perception among local residents in shaping policies for the basin’s sustainable management. The research aims to identify the factors influencing risk perception and propose actionable strategies to improve environmental governance in the region. A “perceived risk profile” methodology was applied, using survey data from 1223 basin residents. The analysis identified key variables that influence risk perception, including demographic factors such as education, gender, and place of residence. The findings reveal that risk underestimation correlates with low awareness of risks, uncertainty about the origins of disasters, fatalism toward natural events, and low trust in institutions. In contrast, risk over-estimation is linked to infrequent risk communication, heightened catastrophism and a strong emphasis on the benefits of environmental protection. The study also highlights significant regional differences in risk perception, with residents of the lower basin exhibiting higher perceptions of risk due to cumulative pollution and frequent disaster impacts. Based on these insights, the study recommends targeted strategies to bridge risk perception gaps, including tailored risk communication, community-based environmental education and stronger institutional trust-building initiatives, all aimed at fostering more effective and inclusive environmental governance in the Nigua basin. Full article
(This article belongs to the Section Water Resources Management, Policy and Governance)
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<p>Geographic location of the Nigua hydrographic basin, Dominican Republic.</p>
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<p>Algorithm for risk perception study.</p>
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<p>Locations where the surveys were carried out (See <a href="#water-17-00045-t0A2" class="html-table">Table A2</a> in the <a href="#app1-water-17-00045" class="html-app">Appendix A</a>).</p>
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<p>Distribution of respondents according to place of residence and work in the Nigua basin.</p>
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<p>Perceived risk profile. (FAMI—Familiarity of the subject with the risk situation, UNDER—Risk understanding, UNCE—Uncertainty, WILL—Willfulness, INVO—Personal Involvement, CONT—Controllability, CATA—Catastrophic potential, HIST—Past history of disasters or dangers, IMME—Immediacy of consequences, REVE—Reversibility of consequences, PANI—Panic, R-IB—Risk-inequality benefit, BENE—Expected benefits of exposure, INST—Trust in institutions, PRES—Role of the press or broadcast media). The dimensionless risk perception scale (Y axis) indicates: 1–risk underestimation; 2–adequate estimation of the risk; 3–risk overestimation.</p>
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<p>Comparison of risk perception by sex. (FAMI—Familiarity of the subject with the risk situation, UNDER—Risk understanding, UNCE—Uncertainty, WILL—Willfulness, INVO-Personal Involvement, CONT—Controllability, CATA—Catastrophic potential, HIST—Past history of disasters or dangers, IMME—Immediacy of consequences, REVE-Reversibility of consequences, PANI—Panic, R-IB—Risk-inequality benefit, BENE—Expected benefits of exposure, INST—Trust in institutions, PRES—Role of the press or broadcast media). The dimensionless risk perception scale (Y axis) indicates: 1–risk underestimation; 2–adequate estimation of the risk; 3–risk overestimation.</p>
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<p>Comparison of risk perception by age. (FAMI—Familiarity of the subject with the risk situation, UNDER—Risk understanding, UNCE—Uncertainty, WILL—Willfulness, INVO—Personal Involvement, CONT—Controllability, CATA—Catastrophic potential, HIST—- Past history of disasters or dangers, IMME—Immediacy of consequences, REVE—Reversibility of consequences, PANI—Panic, R-IB—Risk-inequality benefit, BENE—Expected benefits of exposure, INST—Trust in institutions, PRES—Role of the press or broadcast media). The dimensionless risk perception scale (Y axis) indicates: 1–risk underestimation; 2–adequate estimation of the risk; 3–risk overestimation.</p>
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<p>Comparison of risk perception by place of residence. (FAMI—Familiarity of the subject with the risk situation, UNDER—Risk understanding, UNCE—Uncertainty, WILL—Willfulness, INVO—Personal Involvement, CONT—Controllability, CATA—Catastrophic potential, HIST—Past history of disasters or dangers, IMME—Immediacy of consequences, REVE—Reversibility of consequences, PANI—Panic, R-IB—Risk-inequality benefit, BENE—Expected benefits of exposure, INST—Trust in institutions, PRES—Role of the press or broadcast media). The dimensionless risk perception scale (Y axis) indicates: 1–risk underestimation; 2–adequate estimation of the risk; 3–risk overestimation.</p>
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<p>Comparison of risk perception by education. (FAMI—Familiarity of the subject with the risk situation, UNDER—Risk understanding, UNCE—Uncertainty, WILL—Willfulness, INVO—Personal Involvement, CONT—Controllability, CATA—Catastrophic potential, HIST—Past history of disasters or dangers, IMME—Immediacy of consequences, REVE—Reversibility of consequences, PANI—Panic, R-IB—Risk-inequality benefit, BENE—Expected benefits of exposure, INST—Trust in institutions, PRES—Role of the press or broadcast media). The dimensionless risk perception scale (Y axis) indicates: 1–risk underestimation; 2–adequate estimation of the risk; 3–risk overestimation.</p>
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24 pages, 17593 KiB  
Article
Simplified Multi-Hazard Assessment to Foster Resilience for Sustainable Energy Infrastructure on Santa Cruz Island, Galapagos
by Ana Gabriela Haro-Baez, Eduardo Posso, Santiago Rojas and Diego Arcos-Aviles
Sustainability 2025, 17(1), 106; https://doi.org/10.3390/su17010106 - 27 Dec 2024
Viewed by 514
Abstract
This study analyzes the clean energy infrastructure resilience on Santa Cruz Island, located in the Galapagos archipelago, facing identified multi-natural hazard scenarios such as earthquakes, tsunamis, volcanic eruptions, and extreme weather events. Although Santa Cruz Island has a relatively modern energy infrastructure, its [...] Read more.
This study analyzes the clean energy infrastructure resilience on Santa Cruz Island, located in the Galapagos archipelago, facing identified multi-natural hazard scenarios such as earthquakes, tsunamis, volcanic eruptions, and extreme weather events. Although Santa Cruz Island has a relatively modern energy infrastructure, its geographic location and lack of clear emergency management actions would significantly affect its performance. Risk assessment components, such as exposure and vulnerability, are also analyzed, highlighting the need for strategic interventions to ensure the continuity of energy supply and other essential services. Proved methodologies are used to propose action plans, including structural and non-structural solutions and simulations based on disaster scenarios. As a result, a series of strategies are revealed to strengthen the response and adaptation capacity of both critical infrastructure and the local community. These strategies hold the potential to ensure the island’s long-term energy security and sustainability, reducing its carbon footprint and instilling hope for a resilient future. Full article
(This article belongs to the Section Hazards and Sustainability)
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<p>Geographical map of Galapagos Islands.</p>
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<p>Manuscript structure flowchart.</p>
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<p>Multi-hazard map.</p>
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<p>Puerto Ayora power distribution lines.</p>
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<p>Bellavista power distribution lines.</p>
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<p>Baltra Island power distribution lines.</p>
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<p>Multi-hazard map of Puerto Ayora.</p>
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<p>Bellavista multi-hazard map.</p>
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<p>Multi-hazard map of Baltra Island.</p>
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<p>Vulnerability map of Puerto Ayora.</p>
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<p>Bellavista vulnerability map.</p>
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<p>Baltra Island vulnerability map.</p>
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<p>General risk map by area.</p>
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<p>Electrical structure risk map—Puerto Ayora.</p>
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<p>Electrical structure risk map—Baltra Island.</p>
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35 pages, 2379 KiB  
Communication
Seasonal Analysis and Risk Management Strategies for Credit Guarantee Funds: A Case Study from Republic of Korea
by Juryon Paik and Kwangho Ko
Stats 2025, 8(1), 2; https://doi.org/10.3390/stats8010002 - 26 Dec 2024
Viewed by 264
Abstract
This study investigates the prediction of small and medium-sized enterprise (SME) default rates in Republic of Korea by comparing the performance of three prominent time-series forecasting models: ARIMA, SARIMA, and Prophet. The research utilizes a comprehensive dataset provided by the Korea Credit Guarantee [...] Read more.
This study investigates the prediction of small and medium-sized enterprise (SME) default rates in Republic of Korea by comparing the performance of three prominent time-series forecasting models: ARIMA, SARIMA, and Prophet. The research utilizes a comprehensive dataset provided by the Korea Credit Guarantee Fund (KODIT), which covers regional and monthly default rates from January 2012 to December 2023, spanning 12 years. By focusing on Republic of Korea’s 17 major cities, the study aims to identify regional and seasonal patterns in default rates, highlighting the critical role that regional economic conditions and seasonality play in risk management. The proposed methodology includes an exploratory analysis of default rate trends and seasonal patterns, followed by a comparative evaluation of ARIMA, SARIMA, and Prophet models. ARIMA serves as a baseline model for capturing non-seasonal trends, while SARIMA incorporates seasonal components to handle recurring patterns. Prophet is uniquely suited for dynamic datasets, offering the ability to include external factors such as holidays or economic shocks. This work distinguishes itself from others by combining these three models to provide a comprehensive approach to regional and seasonal default risk forecasting, offering insights specific to Republic of Korea’s economic landscape. Each model is evaluated based on its ability to capture trends, seasonality, and irregularities in the data. The ARIMA model shows strong performance in stable economic environments, while SARIMA proves effective in modeling seasonal patterns. The Prophet model, however, demonstrates superior flexibility in handling irregular trends and external events, making it the most accurate model for predicting default rates across varied economic regions. The study concludes that Prophet’s adaptability to irregularities and external factors positions it as the most suitable model for dynamic economic conditions. These findings emphasize the importance of region-specific and seasonal factors in tailoring risk forecasting models. Future research will validate these predictions by comparing forecasted default rates with actual data from 2024, providing actionable insights into the long-term effectiveness of the proposed methods. This comparison aims to refine the models further, ensuring robust financial stability and enhanced SME support strategies for institutions like KODIT. Full article
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<p>Monthly Average Default Rates across 17 regions in Republic of Korea (2012–2023). The graph highlights seasonal patterns in default rates, with most regions showing a decrease from May to June, except for Sejong, which exhibits an anomalous increase during this period.</p>
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<p>Yearly Average Default Rates across 17 regions in Republic of Korea (2012–2023). The graph shows a general decline in default rates until 2022, followed by a sharp increase in 2023, particularly in Sejong, Gwangju, and Jeonnam, likely reflecting the delayed economic impacts of the COVID-19 pandemic.</p>
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<p>Seasonal Decomposition of Sejong Default Rates (2015–2023). The graph shows significant seasonal fluctuations, particularly around mid-year, which aligns with the unique spike in default rates observed during May and June.</p>
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<p>Seasonal Decomposition of Gwangju Default Rates (2012–2023). The seasonal component is pronounced, with an upward trend in recent years, reflecting the sharp increase in default rates in 2023.</p>
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<p>Seasonal Decomposition of Jeonnam Default Rates (2012–2023). The analysis reveals a strong seasonal influence alongside a significant upward trend in recent years, contributing to the region’s increased default risk.</p>
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<p>Seasonal Decomposition of Seoul Default Rates (2012–2023). While the seasonal component is present, the overall stability in trends reflects the region’s robust economic activities.</p>
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<p>Seasonal Decomposition of Gyeonggi Default Rates (2012–2023). The graph shows consistent seasonal patterns, with less pronounced fluctuations, indicating relative stability in default rates.</p>
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<p>ACF and PACF plots for selected regions: (<b>a</b>) Gangwon, (<b>b</b>) Gyeonggi, (<b>c</b>) Sejong, and (<b>d</b>) Jeju. These plots help determine the ARIMA model parameters <span class="html-italic">p</span> and <span class="html-italic">q</span> for each region.</p>
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<p>Prophet component analysis for Seoul with weekends and holidays considered. The model effectively captures seasonal patterns and trends, providing insights into the impact of these factors on default rates. (Black dot: actual observed data, blue line: predicted trend, blue shaded area: 95% uncertainty interval).</p>
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<p>Prophet component analysis for Sejong with weekends and holidays considered. The model captures unique regional patterns, reflecting local economic and administrative cycles that influence default rates. (Black dot: actual observed data, blue line: predicted trend, blue shaded area: 95% uncertainty interval).</p>
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<p>Prophet component analysis for Gwangju with weekends and holidays considered. The model highlights strong seasonal patterns, showcasing its effectiveness in capturing region-specific trends. (Black dot: actual observed data, blue line: predicted trend, blue shaded area: 95% uncertainty interval).</p>
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<p>Component Analysis of Prophet Model for Seoul: Trend, Holiday Effects, and Yearly Seasonality.</p>
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<p>Component Analysis of Prophet Model for Sejong: Trend, Holiday Effects, and Yearly Seasonality.</p>
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<p>Component Analysis of Prophet Model for Gwangju: Trend, Holiday Effects, and Yearly Seasonality.</p>
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<p>ARIMA Model Forecasts for Monthly Default Rates in Selected Regions (January 2024–December 2024). The forecasts for most regions show stable, flat predictions with minimal variation, indicating the ARIMA model’s tendency to revert to a mean level in the absence of strong linear trends.</p>
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<p>SARIMA Model Forecasts for Monthly Default Rates in Selected Regions (January 2024–December 2024). The forecasts incorporate seasonal components, providing more dynamic predictions that reflect the periodic patterns observed in the historical data.</p>
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<p>Prophet model forecasts without considering weekends and holidays for 17 regions in Republic of Korea. The model captures general trends and seasonality but shows limitations in regions with irregular patterns such as Sejong and Jeju.</p>
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<p>Prophet model forecasts with weekends and holidays considered for 17 regions in Republic of Korea. The inclusion of weekends and holidays improves forecast accuracy, especially in regions like Seoul and Sejong, where these factors significantly impact default rates.</p>
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19 pages, 3801 KiB  
Article
Cold Front Identification Using the DETR Model with Satellite Cloud Imagery
by Yujing Qin, Qian Liu and Chuhan Lu
Remote Sens. 2025, 17(1), 36; https://doi.org/10.3390/rs17010036 - 26 Dec 2024
Viewed by 279
Abstract
The cloud system characteristics within satellite cloud imagery play a crucial role in the meteorological operational analysis of cold fronts, and integrating satellite cloud imagery into automated frontal identification schemes can provide valuable insights for accurately determining the position and morphology of cold [...] Read more.
The cloud system characteristics within satellite cloud imagery play a crucial role in the meteorological operational analysis of cold fronts, and integrating satellite cloud imagery into automated frontal identification schemes can provide valuable insights for accurately determining the position and morphology of cold fronts. This study introduces Cloud-DETR, a deep learning identification method that uses the DETR model with satellite cloud imagery, to identify cold fronts from extensive datasets. In the Cloud-DETR method, preprocessed satellite cloud imagery is used to generate training images, which are then put into the DETR model for cold front identification, achieving excellent results. The alignment between the Cloud-DETR cold fronts and weather systems during continuous periods and extreme weather events is assessed. The Cloud-DETR method exhibits high accuracy in both the position and morphology of cold fronts, ensuring stable identification performance. The high matching rate between the Cloud-DETR cold fronts and the manually identified ones in the test set, image dataset and labels from 2017 is verified. This indicates that the Cloud-DETR method can provide an accurate cold fronts dataset. The cold fronts dataset from 2005 to 2023 was obtained using the Cloud-DETR method. It was found that over the past 18 years, the frequency of cold fronts displays distinct seasonal patterns, with the highest occurrences observed during winter, particularly along the mid-latitude storm tracks extending from the east coast of East Asia to the Northwest Pacific. The methodology and findings presented in this study could help advance further research on the characteristics of cold front cloud systems based on long-term datasets. Full article
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<p>The general workflow of the Cloud-DETR method (the red dotted box indicates the preprocessing of infrared cloud images based on the U-Net and partition processing scheme; the blue dotted box indicates the object detection step and the segmentation step of DETR).</p>
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<p>Preprocessing of infrared satellite cloud image at 12:00 UTC on 15 May 2022: (<b>a</b>) FY-2G infrared brightness temperature (shaded, K); (<b>b</b>) the cloud area initially segmented by the U-Net model in the first step (shaded in red); (<b>c</b>) labeling results of individual cloud areas in the second step; (<b>d</b>) the partition processing result.</p>
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<p>Generating of cold front labels at 12:00 UTC on 9 November 2017: (<b>a</b>) manually generated cold fronts (blue lines), cold advection at 850 hPa (shaded, 10<sup>−4</sup> K/s) and temperature at 850 hPa (contours, K); (<b>b</b>) manually generated cold fronts (blue lines), sea-level pressure (contours, hPa) and surface 10 m wind (arrows, m/s); (<b>c</b>–<b>e</b>) thickened cold front labels.</p>
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<p>Cold fronts identified by the Cloud-DETR method at 12:00 UTC on 7 May 2022: (<b>a</b>) FY-2G infrared brightness temperature (shaded, K); (<b>b</b>) cloud image after preprocessing; (<b>c</b>) Cloud-DETR cold front (blue lines), cold advection at 850 hPa (shaded, 10<sup>−4</sup> K/s) and temperature at 850 hPa (contours, K); (<b>d</b>) Cloud-DETR cold front (blue lines), sea-level pressure (contours, hPa) and surface (10 m) wind (arrows, m/s).</p>
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<p>Cold fronts identified by the Cloud-DETR method (blue lines) from 00:00 UTC on 9 October 2022 to 12:00 UTC on 10 October 2022: (<b>a</b>–<b>d</b>) FY-2G infrared brightness temperature (shaded, K); (<b>e</b>–<b>h</b>) cold advection at 850 hPa (shaded, 10<sup>−4</sup> K/s), temperature at 850 hPa (red contours, K) and surface 10 m wind (arrows, m/s); (<b>i</b>–<b>l</b>) 12-h accumulated precipitation (shaded, mm) and sea-level pressure (black contours, hPa).</p>
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<p>Cold fronts identified by the Cloud-DETR method (blue lines) and two-step method (red lines) at 12:00 UTC on 18 September 2017: (<b>a</b>) FY-2G infrared brightness temperature (shaded, K); (<b>b</b>) cold advection at 850 hPa (shaded, 10<sup>−4</sup> K/s) and temperature at 850 hPa (red contours, K); (<b>c</b>) sea-level pressure (black contours, hPa) and surface (10 m) wind (arrows, m/s).</p>
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<p>Cold fronts identified by the Cloud-DETR method (blue lines) from 12:00 UTC on 14 March 2021, to 12:00 UTC on 15 March 2021: (<b>a</b>–<b>d</b>) FY-2G infrared brightness temperature (shaded, K); (<b>e</b>–<b>h</b>) PM<sub>10</sub> (shaded, μg·m<sup>−3</sup>).</p>
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<p>From 12:00 UTC on 14 March 2021 to 12:00 UTC on 15 March 2021: (<b>a</b>–<b>c</b>) geopotential height (contours, dagpm) and wind with speed higher than 30 m/s (shaded, m/s) at 200 hPa; (<b>d</b>–<b>f</b>) geopotential height (black solid contours, dagpm) and temperature (red dotted contours, K) at 500 hPa; (<b>g</b>–<b>i</b>) geopotential height (contours, dagpm) and wind (arrows, m/s, the wind speed in the shaded area is higher than 12 m/s) at 700 hPa; (<b>j</b>–<b>l</b>) Cloud-DETR cold front (blue lines), sea-level pressure (black contours, hPa) and surface 10 m wind (arrows, m/s).</p>
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<p>The proportion of cold fronts occurrence (shaded, %) and sea-level pressure (contours, hPa) in (<b>a</b>) winter, (<b>b</b>) spring, (<b>c</b>) summer, and (<b>d</b>) autumn from 2005 to 2023.</p>
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30 pages, 4743 KiB  
Article
Rapid Landslide Detection Following an Extreme Rainfall Event Using Remote Sensing Indices, Synthetic Aperture Radar Imagery, and Probabilistic Methods
by Aikaterini-Alexandra Chrysafi, Paraskevas Tsangaratos, Ioanna Ilia and Wei Chen
Land 2025, 14(1), 21; https://doi.org/10.3390/land14010021 - 26 Dec 2024
Viewed by 311
Abstract
The rapid detection of landslide phenomena that may be triggered by extreme rainfall events is a critical point concerning timely response and the implementation of mitigation measures. The main goal of the present study is to identify susceptible areas by estimating changes in [...] Read more.
The rapid detection of landslide phenomena that may be triggered by extreme rainfall events is a critical point concerning timely response and the implementation of mitigation measures. The main goal of the present study is to identify susceptible areas by estimating changes in the Normalized Difference Vegetation Index (NDVI), Normalized Difference Moisture Index (NDMI), Bare Soil Index (BSI), and Synthetic Aperture Radar (SAR) amplitude ratio before and after extreme rainfall events. The developed methodology was utilized in a case study of Storm Daniel, which struck central Greece in September 2023, with a focus on the Mount Pelion region on the Pelion Peninsula. Using Google Earth Engine, we processed satellite imagery to calculate these indices, enabling the assessment of vegetation health, soil moisture, and exposed soil areas, which are key indicators of landslide activity. The methodology integrates these indices with a Weight of Evidence (WofE) model, previously developed to identify regions of high and very high landslide susceptibility based on morphological parameters like slope, aspect, plan and profile curvature, and stream power index. Pre- and post-event imagery was analyzed to detect changes in the indices, and the results were then masked to focus only on high and very high susceptibility areas characterized by the WofE model. The outcomes of the study indicate significant changes in NDVI, NDMI, BSI values, and SAR amplitude ratio within the masked areas, suggesting locations where landslides were likely to have occurred due to the extreme rainfall event. This rapid detection technique provides essential data for emergency services and disaster management teams, enabling them to prioritize areas for immediate response and recovery efforts. Full article
(This article belongs to the Special Issue Remote Sensing Application in Landslide Detection and Assessment)
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<p>Flowchart of the developed methodology.</p>
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<p>Study area and historical landslides (training and test subsets).</p>
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<p>Geological map, adopted by [<a href="#B92-land-14-00021" class="html-bibr">92</a>].</p>
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<p>(<b>a</b>) Hourly accumulated precipitation 4 September 2023; (<b>b</b>) hourly accumulated precipitation 5 September 2023; (<b>c</b>) hourly accumulated precipitation 6 September 2023; (<b>d</b>) hourly accumulated precipitation 7 September 2023; (<b>e</b>) hourly accumulated precipitation 8 September 2023; (<b>f</b>) hourly accumulated precipitation 9 September 2023.</p>
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<p>(<b>a</b>) Hourly accumulated precipitation 4 September 2023; (<b>b</b>) hourly accumulated precipitation 5 September 2023; (<b>c</b>) hourly accumulated precipitation 6 September 2023; (<b>d</b>) hourly accumulated precipitation 7 September 2023; (<b>e</b>) hourly accumulated precipitation 8 September 2023; (<b>f</b>) hourly accumulated precipitation 9 September 2023.</p>
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<p>Landslide susceptibility map based on WofE model.</p>
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<p>(<b>a</b>) Spatial distribution of NDVI change; (<b>b</b>) spatial distribution of NDMI change; (<b>c</b>) spatial distribution of BSI change; and (<b>d</b>) spatial distribution of SAR amplitude change.</p>
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<p>(<b>a</b>) The Rapid Landslide Detection Potential map; (<b>b</b>) Rapid Landslide Detection Potential–WofE map along a 50 m buffer zone road network.</p>
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<p>Sensitivity, 100-specificity, and ROC curves for the test dataset of RLD, RLD-Slope, and RLD-WofE models.</p>
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<p>Field surveys—ground truth evidence—high and very high susceptibility zones.</p>
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<p>Field surveys—ground truth evidence—high and very high susceptibility zones.</p>
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43 pages, 19726 KiB  
Article
Badges of (Dis-)Honour: Manifesting the ‘Conquest’ of Uluṟu via Wearable Material Culture
by Dirk H. R. Spennemann and Sharnie Hurford
Heritage 2025, 8(1), 8; https://doi.org/10.3390/heritage8010008 - 26 Dec 2024
Viewed by 327
Abstract
Set in a wide open plain, the monolith of Uluṟu (‘Ayers Rock’) has become an internationally recognizable symbol for the Australian outback, currently attracting hundreds of thousands of tourists each year. Promoted since the 1950s as an exotic tourist destination, one of the [...] Read more.
Set in a wide open plain, the monolith of Uluṟu (‘Ayers Rock’) has become an internationally recognizable symbol for the Australian outback, currently attracting hundreds of thousands of tourists each year. Promoted since the 1950s as an exotic tourist destination, one of the major activities has been the ‘conquest’ of Uluṟu by completing the steep climb to the top. Always disapproved by the Aṉangu, the Indigenous Australian community of the area, and actively discouraged since 1990, the climb became an extremely contentious issue in the final two years before it was permanently closed to tourists on 26 October 2019. Given that climbing Uluṟu as a tourist activity has become an event of the past, this paper will examine the nature, materiality, and potential heritage value of the portable material culture associated with the climb. The background to the history of climbing Uluṟu in the context of European invasion (‘exploration’), the nature of tourism at Uluṟu and the role climbing played in this, as well as the management decisions that led to the closure of the climb can be grouped into four thematic periods: the beginnings of settler colonialist ascents (1873–1950), the ‘heroic’ age of Uluṟu tourism (1950–1958), lodges in a National Park (1958–1985), and joint management and the eventual closure of the climb (1985–2019). Based on a description of the material culture associated with the climb, particularly badges, patches and certificates, and drawing on the methodologies of historic and material culture studies, this paper will discuss the various interpretations of climbing Uluṟu and how the portable material culture reflects or exemplifies climbing as a conquest and heroic deed, as a spiritual ritual, and as a violation of cultural rights. After examining the materiality of the wearable material culture, we conclude by exploring which of these portable items are culturally significant and which, if any, should be curated in public collections. Full article
(This article belongs to the Section Cultural Heritage)
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<p>The first photograph of a person standing on top of Uluṟu. Constable William McKinnon next to the cairn, February 1932 [<a href="#B40-heritage-08-00008" class="html-bibr">40</a>].</p>
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<p>A tourist camp at the base of Uluṟu, with Ken Tuit’s 4 × 4 and a Bond’s Tours bus (in the background), 1952. Photo by Kevin Harris (of Bond Tours) (State Library of South Australia, B 70782/69).</p>
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<p>A women’s tour group ascending Uluṟu in 1957 [<a href="#B79-heritage-08-00008" class="html-bibr">79</a>].</p>
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<p>The climb at Uluṟu in the late 1950s or early 1960s prior to the installation of the safety chain. Note the Pioneer Tours bus and Len Tuit’s VW-combi bus at the base (photograph by Valerie Lhuede, Plastichrome postcard).</p>
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<p>Bus groups and individual travelers climbing Uluṟu in 1973 [<a href="#B4-heritage-08-00008" class="html-bibr">4</a>]. The line of <span class="html-italic">minga</span> streaming up the spur is readily discernible.</p>
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<p>Certificate issued by Alice Springs Tours for the completed ascent of Uluṟu, dated 11 September 1962. (<b>A</b>) Recto showing climber’s name and data; (<b>B</b>) verso listing fellow climbers.</p>
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<p>Development of visitor numbers to Uluṟu, 1958 to 2023 (in financial years, July–June) [<a href="#B65-heritage-08-00008" class="html-bibr">65</a>,<a href="#B69-heritage-08-00008" class="html-bibr">69</a>,<a href="#B78-heritage-08-00008" class="html-bibr">78</a>,<a href="#B118-heritage-08-00008" class="html-bibr">118</a>,<a href="#B119-heritage-08-00008" class="html-bibr">119</a>,<a href="#B120-heritage-08-00008" class="html-bibr">120</a>,<a href="#B121-heritage-08-00008" class="html-bibr">121</a>,<a href="#B122-heritage-08-00008" class="html-bibr">122</a>,<a href="#B123-heritage-08-00008" class="html-bibr">123</a>,<a href="#B124-heritage-08-00008" class="html-bibr">124</a>,<a href="#B125-heritage-08-00008" class="html-bibr">125</a>,<a href="#B126-heritage-08-00008" class="html-bibr">126</a>,<a href="#B127-heritage-08-00008" class="html-bibr">127</a>,<a href="#B128-heritage-08-00008" class="html-bibr">128</a>,<a href="#B129-heritage-08-00008" class="html-bibr">129</a>,<a href="#B130-heritage-08-00008" class="html-bibr">130</a>,<a href="#B131-heritage-08-00008" class="html-bibr">131</a>]. 1—Yulara Resort opened; 2—Handed back to the Aṉangu community; 3—World Heritage listing; 4—Asian economic downturn; 5—Sydney Olympic Games; 6—Global financial crisis; 7—Climbing ban announced; 8—Climbing ban took effect; 9—COVID-19.</p>
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<p>The percentage of visitors also climbing (dots) or intending to climb Uluṟu (circles), 1950–2019 [<a href="#B79-heritage-08-00008" class="html-bibr">79</a>,<a href="#B98-heritage-08-00008" class="html-bibr">98</a>,<a href="#B108-heritage-08-00008" class="html-bibr">108</a>,<a href="#B132-heritage-08-00008" class="html-bibr">132</a>,<a href="#B133-heritage-08-00008" class="html-bibr">133</a>,<a href="#B135-heritage-08-00008" class="html-bibr">135</a>,<a href="#B136-heritage-08-00008" class="html-bibr">136</a>,<a href="#B137-heritage-08-00008" class="html-bibr">137</a>,<a href="#B138-heritage-08-00008" class="html-bibr">138</a>,<a href="#B139-heritage-08-00008" class="html-bibr">139</a>,<a href="#B140-heritage-08-00008" class="html-bibr">140</a>,<a href="#B141-heritage-08-00008" class="html-bibr">141</a>,<a href="#B142-heritage-08-00008" class="html-bibr">142</a>,<a href="#B143-heritage-08-00008" class="html-bibr">143</a>,<a href="#B144-heritage-08-00008" class="html-bibr">144</a>,<a href="#B145-heritage-08-00008" class="html-bibr">145</a>,<a href="#B146-heritage-08-00008" class="html-bibr">146</a>]. Dashed lines: (1) the first formal acknowledgment of the inappropriateness of the climb in a management plan; (2) planned closure of the climb announced. The regression line refers to visitors climbing.</p>
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<p>Enamel metal badges with the text “I climbed Ayers Rock”, possibly issued by the Alice Springs Tours. (<b>A</b>) Enamel metal lapel pin; (<b>B</b>) enamel metal badge.</p>
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<p>Enamel metal badges produced by tour companies and accommodation providers.</p>
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<p>Metal badges issued by souvenir merchants.</p>
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<p>Examples of cloth patches issued by souvenir merchants.</p>
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<p>Examples of adhesive decals issued by souvenir merchants.</p>
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<p>Lou A. Borgelt atop of the cairn, flanked by Tiger Tjalkalyirri and Mick Mitjenkeri, 30 June 1946. Out of respect, the faces of the two Aṉangu men have been blurred. Screengrab [<a href="#B187-heritage-08-00008" class="html-bibr">187</a>].</p>
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<p>Early signage at the base of the climb makes no reference to the Aṉangu community, let alone their wishes that Uluṟu should not be climbed (Photos by Rick Horn, 24 May 1984 via Flickr).</p>
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<p>Final appearance of signage at the base of the climb making reference to the Aṉangu community and their wishes that Uluṟu should not be climbed (Photo by Vince Basile, 25 October 2019 via Flickr).</p>
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<p>A solitary example of culturally responsive messaging (postcard, Baker Souvenirs) [<a href="#B208-heritage-08-00008" class="html-bibr">208</a>].</p>
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<p>Ontological relationships of the badges issued by tour operators.</p>
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<p>Ontological relationships of the badges sold by souvenir merchants pre handover.</p>
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<p>Ontological relationships of badges with the text “I have climbed Ayers Rock” sold by souvenir merchants after handover.</p>
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<p>Ontological relationships of badges with the text “I didn’t climb Ayers Rock” sold by souvenir merchants after handover.</p>
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<p>Ontological relationships of the badges with the text “I didn’t climb Ayers Rock” accompanied by a deck chair as sold by souvenir merchants after handover.</p>
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<p>Tea towel expounding ‘ocker’ reasons why the purchaser chose not to climb Uluṟu [<a href="#B164-heritage-08-00008" class="html-bibr">164</a>].</p>
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<p>Ontological relationships of the patches with the text ‘I tried to climb Ayers Rock’ sold by souvenir merchants after handover.</p>
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<p>Ontological relationships of certificates issued by tour operators.</p>
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70 pages, 7977 KiB  
Article
A Martingale-Free Introduction to Conditional Gaussian Nonlinear Systems
by Marios Andreou and Nan Chen
Entropy 2025, 27(1), 2; https://doi.org/10.3390/e27010002 - 24 Dec 2024
Viewed by 169
Abstract
The conditional Gaussian nonlinear system (CGNS) is a broad class of nonlinear stochastic dynamical systems. Given the trajectories for a subset of state variables, the remaining follow a Gaussian distribution. Despite the conditionally linear structure, the CGNS exhibits strong nonlinearity, thus capturing many [...] Read more.
The conditional Gaussian nonlinear system (CGNS) is a broad class of nonlinear stochastic dynamical systems. Given the trajectories for a subset of state variables, the remaining follow a Gaussian distribution. Despite the conditionally linear structure, the CGNS exhibits strong nonlinearity, thus capturing many non-Gaussian characteristics observed in nature through its joint and marginal distributions. Desirably, it enjoys closed analytic formulae for the time evolution of its conditional Gaussian statistics, which facilitate the study of data assimilation and other related topics. In this paper, we develop a martingale-free approach to improve the understanding of CGNSs. This methodology provides a tractable approach to proving the time evolution of the conditional statistics by deriving results through time discretization schemes, with the continuous-time regime obtained via a formal limiting process as the discretization time-step vanishes. This discretized approach further allows for developing analytic formulae for optimal posterior sampling of unobserved state variables with correlated noise. These tools are particularly valuable for studying extreme events and intermittency and apply to high-dimensional systems. Moreover, the approach improves the understanding of different sampling methods in characterizing uncertainty. The effectiveness of the framework is demonstrated through a physics-constrained, triad-interaction climate model with cubic nonlinearity and state-dependent cross-interacting noise. Full article
(This article belongs to the Section Information Theory, Probability and Statistics)
19 pages, 1780 KiB  
Article
The Contribution of Extreme Event Communication to Climate Change Mitigation: Outrage and Blame Discourse in Twitter Conversation on Severe Fires
by Ángela Alonso Jurnet and Ainara Larrondo Ureta
Journal. Media 2025, 6(1), 1; https://doi.org/10.3390/journalmedia6010001 - 24 Dec 2024
Viewed by 285
Abstract
Risk communication from the perspective of Extreme Event Attribution (EEA), which assesses the extent to which climate change influences various extreme weather events, has significant potential for climate change communication due to its ability to make the phenomenon more relatable to citizens. This [...] Read more.
Risk communication from the perspective of Extreme Event Attribution (EEA), which assesses the extent to which climate change influences various extreme weather events, has significant potential for climate change communication due to its ability to make the phenomenon more relatable to citizens. This study examines the digital conversation generated following the wave of wildfires in Spain in 2022, which was declared the worst year of the 21st century in terms of hectares burned. By using the Social Network Analysis (SNA) methodology, 145,081 tweets were analyzed to construct a mention network, capturing the digital clusters formed around this discussion and highlighting the predominant tones in the debate. The findings reveal that the conversation predominantly adopted a tone of outrage and assigned responsibility. This research study offers a renewed perspective on risk communication, highlighting significant challenges faced by environmental activism on social media and underscoring the need to improve communication strategies to increase awareness and mobilization around climate change. Full article
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<p>Network graph and digital clusters. Source: own creation through Gephi software.</p>
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17 pages, 3460 KiB  
Article
Research on Flood Storage and Disaster Mitigation Countermeasures for Floods in China’s Dongting Lake Area Based on Hydrological Model of Jingjiang–Dongting Lake
by Wengang Zhao, Weizhi Ji, Jiahu Wang, Jieyu Jiang, Wen Song, Zaiai Wang, Huizhu Lv, Hanyou Lu and Xiaoqun Liu
Water 2025, 17(1), 1; https://doi.org/10.3390/w17010001 - 24 Dec 2024
Viewed by 266
Abstract
China’s Dongting Lake area is intertwined with rivers and lakes and possesses many water systems. As such, it is one of the most complicated areas in the Yangtze River Basin, in terms of the complexity of its flood control. Over time, siltation and [...] Read more.
China’s Dongting Lake area is intertwined with rivers and lakes and possesses many water systems. As such, it is one of the most complicated areas in the Yangtze River Basin, in terms of the complexity of its flood control. Over time, siltation and reclamation in the lake area have greatly weakened the river discharge capacity of the lake area, and whether it can endure extreme floods remains an open question. As there is no effective scenario simulation model for the lake area, this study constructs a hydrological model for the Jingjiang–Dongting Lake system and verifies the model using data from 11 typical floods occurring from 1954 to 2020. The parameters derived from 2020 data reflect the latest hydrological relationship between the lake and the river, while meteorological data from 1954 and 1998 are used as inputs for various scenarios with the aim of evaluating the flood pressure of the lake area, using the water levels at the Chengglingji and Luoshan stations as indicators. The preliminary results demonstrate that the operation of the upstream Three Gorges Dam and flood storage areas cannot completely offset the flood pressure faced by the lake area. Therefore, the reinforcement and raising of embankments should be carried out, in order to cope with potential extreme flood events. The methodology and results of this study have reference value for policy formation, flood control, and assessment and dispatching in similar areas. Full article
(This article belongs to the Special Issue Advances in Ecohydrology in Arid Inland River Basins)
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<p>Map of the study area’s location.</p>
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<p>Flowchart of the CREST Model. (PE: rainfall minus evapotranspiration capacity; IM: impermeability factor; Ec: canopy evaporation; Th: thresholds for delineation of slopes and channels; other symbols are customary in hydrological modelling).</p>
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<p>Correlations between water levels at Hankou and Lianhuatang stations before and after the operation of the Three Gorges Dam.</p>
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<p>Relationships between the highest water levels at various control stations and the warning and control water levels during high flood years.</p>
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<p>Comparisons of simulated and observed water levels and flow rates for typical years at Luoshan station.</p>
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<p>Comparisons of simulated and observed water levels and flow rates for typical years at Luoshan station.</p>
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24 pages, 7431 KiB  
Article
Cyclone Classification over the South Atlantic Ocean in Centenary Reanalysis
by Eduardo Traversi de Cai Conrado, Rosmeri Porfírio da Rocha, Michelle Simões Reboita and Andressa Andrade Cardoso
Atmosphere 2024, 15(12), 1533; https://doi.org/10.3390/atmos15121533 - 21 Dec 2024
Viewed by 455
Abstract
Since the beginning of the satellite era, only three tropical cyclones have been recorded over the South Atlantic Ocean. To investigate the potential occurrence of such systems since the 1900s, ERA20C, a centennial reanalysis, was utilised. This study first evaluates the performance of [...] Read more.
Since the beginning of the satellite era, only three tropical cyclones have been recorded over the South Atlantic Ocean. To investigate the potential occurrence of such systems since the 1900s, ERA20C, a centennial reanalysis, was utilised. This study first evaluates the performance of ERA20C in reproducing the climatology of all cyclone types over the southwestern South Atlantic Ocean by comparing it with a modern reanalysis (ERA5) for the period 1979–2010. Despite its simpler construction, ERA20C is able to reproduce key climatological features, such as frequency, location, seasonality, intensity, and thermal structure of cyclones similar to ERA5. Then, the Cyclone Phase Space (CPS) methodology was applied to determine the thermal structure at each time step for every cyclone between 1900 and 2010 in ERA20C. The cyclones were then categorised into different types (extratropical, subtropical, and tropical), and systems exhibiting a warm core at their initial time step were classified as tropical cyclogenesis. Between 1900 and 2010, 96 cases of tropical cyclogenesis were identified over the South Atlantic. Additionally, throughout the lifetime of all cyclones, a total of 1838 time steps exhibited a tropical structure, indicating that cyclones can acquire a warm core at different stages of their lifecycle. The coasts of southeastern and southern sectors of northeast Brazil emerged as the most favourable for cyclones with tropical structures during their lifecycle. The findings of this study highlight the occurrence of tropical cyclones in the South Atlantic prior to the satellite era, providing a foundation for future research into the physical mechanisms that enabled these events. Full article
(This article belongs to the Special Issue Cyclones: Types and Phase Transitions)
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<p>Tracking domain (black large box) and areas used in the study: entire South Atlantic Ocean (green box) and main cyclogenetic regions of eastern South America coast (SEB: Southeast/South Brazil, URU: Uruguay and extreme south Brazil, and ARG: Argentina).</p>
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<p>(<b>a</b>) CPS thresholds used for the cyclone’s classification following the criteria: C01 [<a href="#B39-atmosphere-15-01533" class="html-bibr">39</a>], C02 [<a href="#B11-atmosphere-15-01533" class="html-bibr">11</a>], and C03 [<a href="#B34-atmosphere-15-01533" class="html-bibr">34</a>]; (<b>b</b>) CPS quadrants delimiting the cyclone phase, B versus <math display="inline"><semantics> <mrow> <mo>−</mo> <mrow> <mo>|</mo> <mrow> <msubsup> <mi>V</mi> <mi>T</mi> <mi>L</mi> </msubsup> </mrow> <mo>|</mo> </mrow> </mrow> </semantics></math> (<b>left</b>) and <math display="inline"><semantics> <mrow> <mo>−</mo> <mrow> <mo>|</mo> <mrow> <msubsup> <mi>V</mi> <mi>T</mi> <mi>L</mi> </msubsup> </mrow> <mo>|</mo> </mrow> </mrow> </semantics></math> versus <math display="inline"><semantics> <mrow> <mo>−</mo> <mrow> <mo>|</mo> <mrow> <msubsup> <mi>V</mi> <mi>T</mi> <mi>U</mi> </msubsup> </mrow> <mo>|</mo> </mrow> </mrow> </semantics></math> (<b>right</b>) to C01, C02 e C03 criteria.</p>
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<p>Mean annual density of cyclogenesis for the common period 1979–2010: (<b>a</b>) ERA20C and (<b>b</b>) ERA5. Density unit: number of cyclones by area (km<sup>2</sup>) ×10<sup>5</sup> per year.</p>
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<p>Mean annual density of cyclone’s trajectory with genesis in the subdomains for the common period 1979–2010 for: (<b>a</b>,<b>d</b>) SEB, (<b>b</b>,<b>e</b>) URU, and (<b>c</b>,<b>f</b>) ARG for ERA20C (<b>left column</b>) and ERA5 (<b>right column</b>). Density unit: number of cyclones by area (km<sup>2</sup>) ×10<sup>5</sup> per year.</p>
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<p>Cyclogenesis annual cycle (events/month) in ERA20C (red line) and ERA5 (blue line) in the common period (1979–2010) for: (<b>a</b>) SEB, (<b>b</b>) URU, (<b>c</b>) ARG, and (<b>d</b>) the South Atlantic (green box in <a href="#atmosphere-15-01533-f001" class="html-fig">Figure 1</a>). The numbers on the right bottom side of the panels indicate annual mean and standard deviation, while the right side boxes present the seasonal mean for ERA20C (red) and ERA5 (blue).</p>
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<p>Histograms of the relative vorticity (×10<sup>−5</sup> s<sup>−1</sup>) at cyclogenesis for the common period (1979–2010) for ERA20C (red) and ERA5 (blue) in subdomains: (<b>a</b>) SEB, (<b>b</b>) URU, (<b>c</b>) ARG, and (<b>d</b>) South Atlantic (green box in <a href="#atmosphere-15-01533-f001" class="html-fig">Figure 1</a>).</p>
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<p>Time series of the annual frequency of cyclogenesis (events year-1) in ERA5 (1979–2010; blue) and ERA20C (1900–2010; red) in subdomains: (<b>a</b>) SEB, (<b>b</b>) URU, (<b>c</b>) ARG, and (<b>d</b>) Atlantic (green box in <a href="#atmosphere-15-01533-f001" class="html-fig">Figure 1</a>); r is the Pearson correlation calculated between ERA20C and ERA5 for the period 1979–2010.</p>
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<p>Distribution of CPS parameters for each 6-h time step across the cyclone’s lifecycle for South Atlantic: The left column shows B vs. <math display="inline"><semantics> <mrow> <mo>−</mo> <mrow> <mo>|</mo> <mrow> <msubsup> <mi>V</mi> <mi>T</mi> <mi>L</mi> </msubsup> </mrow> <mo>|</mo> </mrow> </mrow> </semantics></math> diagrams and the right column <math display="inline"><semantics> <mrow> <mo>−</mo> <mrow> <mo>|</mo> <mrow> <msubsup> <mi>V</mi> <mi>T</mi> <mi>U</mi> </msubsup> </mrow> <mo>|</mo> </mrow> </mrow> </semantics></math> vs. <math display="inline"><semantics> <mrow> <mo>−</mo> <mrow> <mo>|</mo> <mrow> <msubsup> <mi>V</mi> <mi>T</mi> <mi>L</mi> </msubsup> </mrow> <mo>|</mo> </mrow> </mrow> </semantics></math> diagrams. (<b>a</b>,<b>b</b>) ERA20C (1900–2010), (<b>c</b>,<b>d</b>) ERA20C (1979–2010), and (<b>e</b>,<b>f</b>) ERA5 (1979–2010). Dotted lines indicate significant values based in C01, C02 and C03 thresholds: <math display="inline"><semantics> <mrow> <mi>B</mi> <mo>=</mo> <mn>10</mn> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <mo>−</mo> <mrow> <mo>|</mo> <mrow> <msubsup> <mi>V</mi> <mi>T</mi> <mi>L</mi> </msubsup> </mrow> <mo>|</mo> </mrow> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <mo>−</mo> <mrow> <mo>|</mo> <mrow> <msubsup> <mi>V</mi> <mi>T</mi> <mi>U</mi> </msubsup> </mrow> <mo>|</mo> </mrow> <mo>=</mo> <mn>0</mn> </mrow> </semantics></math>. I–IV refers to the quadrant order, from first to fourth.</p>
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<p>Similar to <a href="#atmosphere-15-01533-f008" class="html-fig">Figure 8</a>, but only for the cyclogenesis time step.</p>
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<p>Annual cycle of the cyclogenesis types over the South Atlantic (extratropical in blue, subtropical in orange, tropical in red, and others in grey) for the long (ERA20C from 1900 to 2010) and common period (1979–2010) of ERA20C and ERA5. The types were separated with the thresholds: C01 (<b>left panel</b>) and C02–C03 (<b>right panel</b>).</p>
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<p>(<b>a</b>) Spatial distribution of all types of cyclogenesis (extratropical in blue, subtropical in orange, tropical in red, and others in grey) and separated for (<b>b</b>) subtropical and (<b>c</b>) tropical (<b>right panel</b>) cyclogenesis. The cyclogenesis types were classified considering the criteria C01, C02, and C03.</p>
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<p>Annual frequency of the time steps with extratropical (<b>a</b>,<b>b</b>), subtropical (<b>c</b>,<b>d</b>), and tropical (<b>e</b>,<b>f</b>) phases (<b>left panel</b>) and the same just for cyclogenesis (<b>right panel</b>) in the South Atlantic for ERA20C (red) and ERA5 (blue). “R” is the slope of the trend lines: ERA20C (1900–2010) is represented in red, ERA20C (1979–2010) in green, and ERA5 (1979–2010) in blue. “MK” is the Mann-Kendall test at a 95% confidence level, and the colours green and red indicate, respectively, statistically significant and non-significant trends.</p>
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<p>CPS for Hurricane Catarina over the South Atlantic Ocean in March 2004: for (<b>a</b>,<b>b</b>) ERA20C (<b>left panel</b>) and (<b>d</b>,<b>e</b>) ERA5 (<b>right panel</b>); (<b>c</b>,<b>f</b>) depict the hurricane tracking, with the colors indicating the phases of the system: extratropical in blue, subtropical in orange, tropical in red and “other” in gray. In these same panels “SC” and “RS” indicate, respectively, Santa Catarina and Rio Grande do Sul states, where Hurricane Catarina had landfall.</p>
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<p>Hurricane Catarina: atmospheric fields for ERA20C (upper panels) and ERA5 (lower panels): (<b>a</b>–<b>d</b>) mean sea level pressure (hPa—black contour), zonal wind at 200 hPa (m s<sup>−1</sup>; shaded), and Catarina position limited by black square, and (<b>e</b>–<b>h</b>) vertical cross sections of cyclonic relative vorticity (×10<sup>−5</sup> s<sup>−1</sup>; shaded) considering the central latitude of Catarina.</p>
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15 pages, 1951 KiB  
Article
The Proteomics of T-Cell and Early T-Cell Precursor (ETP) Acute Lymphocytic Leukemia: Prognostic Patterns in Adult and Pediatric-ETP ALL
by Fieke W. Hoff, Lourdes Sriraja, Yihua Qiu, Gaye N. Jenkins, David T. Teachey, Brent Wood, Meenakshi Devidas, Shaina Shockley, Mignon L. Loh, Evangelia Petsalaki, Steven M. Kornblau and Terzah M. Horton
Cancers 2024, 16(24), 4241; https://doi.org/10.3390/cancers16244241 - 19 Dec 2024
Viewed by 529
Abstract
Background. The 5-year overall survival (OS) rates of T-cell lymphocytic leukemia (T-ALL) are better for children (>90%) compared to adults (~57%). The early T-cell precursor (ETP) T-ALL subtype is prognostically unfavorable in adults, but less significant in pediatric T-ALL, and the diagnosis and [...] Read more.
Background. The 5-year overall survival (OS) rates of T-cell lymphocytic leukemia (T-ALL) are better for children (>90%) compared to adults (~57%). The early T-cell precursor (ETP) T-ALL subtype is prognostically unfavorable in adults, but less significant in pediatric T-ALL, and the diagnosis and prognosis of “near”-ETP is controversial. We compared protein and RNA expression patterns in pediatric and adult T-ALL to identify prognostic subgroups, and to further characterize ETP and near-ETP T-ALL in both age groups. Methods. Protein expression was assessed using RPPA methodology for 321 target proteins in 361 T-ALL patient samples from 292 pediatrics and 69 adults, including 103 ETP-ALL. RNA-sequencing was performed on 81 pediatric T-ALL samples. Results. We identified recurrent protein expression patterns that classified patients into ten protein expression signatures using the “MetaGalaxy” analysis. In adults, Cox regression analysis identified two risk-groups associated with OS (p = 0.0002) and complete remission duration (p < 0.001). Cluster analysis of adults and pediatric-ETP patients identified three ETP-clusters strongly associated with age. Pediatric ETP-patients with a pediatric-dominant expression profile were associated with a shorter OS (p = 0.04) and event-free survival (p = 0.05) compared to pediatric ETP-patients with an ETP expression profile that was also identified in adults. Conclusion. Our study demonstrates that proteomics are predictive of outcome in adult T-ALL and that we can identify a small subset of pediatric ETP with an inferior outcome. The observation that there are age-specific patterns supports the idea that the origin of T-ALL in most pediatric and adult patients is different, while overlapping patterns suggests that there are some with a common pathophysiology. Proteomics could enhance risk stratification in both pediatric and adults with T-ALL. Full article
(This article belongs to the Section Molecular Cancer Biology)
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<p>Meta-Galaxy analysis. A large binary matrix representing the 361 patients (columns) and 125 protein clusters (PC) (rows, <a href="#app1-cancers-16-04241" class="html-app">Supplemental Table S3</a>). A blue pixel indicates the presence of a given PC in that patient. Block clustering analysis identified the presence of 13 protein constellations (horizontally) that formed 10 protein expression signatures (vertically). Annotations are included at the top for each individual patient. Age (class): adult (navy blue), pediatric (pink); age (subclass): age (≤1 year, navy blue), pediatric (2–17 years, yellow), adolescents and young adults (pink), adult (30+ years, green); ETP phenotype: ETP (navy blue), near-ETP (light blue), non-ETP (yellow).</p>
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<p>Regression analysis identified 2 protein clusters associated with clinical outcomes in adult T-ALL in the training set (n = 33). (<b>A</b>) Heatmap showing relative protein expression levels of 15 proteins significantly associated with complete remission (CR) duration in the training set (n = 33). (<b>B</b>) Prognostic risk score calculated for each individual patient. Patients were divided into a low-risk protein cluster (LR-PC) and a high-risk protein cluster (HR-PC) based on the median risk score. (<b>C</b>) Time-dependent receiver operator characteristic (ROC) analysis. (<b>D</b>) Overall survival and CR duration stratified for patients in the low-risk (red) and the high-risk (navy blue) protein cluster.</p>
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<p>(<b>A</b>) Heatmap showing 14 proteins that were most strongly associated with the three protein clusters based on differential expression analysis. Protein expression levels are shown relative to normal, ranging from low (blue) to normal (green) to high (red). (<b>B</b>) Overall survival (upper) and event-free survival (lower) analysis for the AALL1231 patients that clustered into the pediatric-dominant (ETP-P; pink) and the adult/pediatric mixed protein clusters (ETP-MX; green). Non-ETP patients (red) were shown as a reference.</p>
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<p>(<b>A</b>) RNA UMAP cluster analysis assignments of pediatric transcriptome data (n = 81). (<b>B</b>) Sankey plot of RPPA protein UMAP clusters and RNA-Seq UMAP clusters (<b>C</b>) Cluster-specific enrichment scores for the top representative pathways using Hallmark gene sets of upregulated and downregulated genes. The <span class="html-italic">x</span>-axis represents the normalized enrichment score (NES) from the FGSEA analysis, where NES &lt; 0 indicates downregulated pathways, and NES &gt; 0 indicates upregulated pathways.</p>
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<p>Gene expression profiling comparing near-ETP/ETP to non-ETP T-ALL. (<b>A</b>) Volcano plot displaying differentially expressed genes between near-ETP/ETP and non-ETP patient samples. Genes shown in red have an FDR <span class="html-italic">p</span>-value &lt; 0.05 and an absolute log2 fold change greater than 2.5, blue points indicate genes with an FDR <span class="html-italic">p</span>-value &lt; 0.05 and an absolute log2 change less than 2.5, and green and grey points represent non-significant genes. (<b>B</b>) Heatmap showing differential gene expression with a log2FC cut-off greater than 1.5. fold difference between variance stabilizing transformation normalized RNA expression counts in near-ETP/ETP and non-ETP T-ALL. (<b>C</b>) The FGSEA enrichment scores for pathways upregulated in the near-ETP/ETP are shown in blue, while those shown in yellow are down-regulated. (<b>D</b>) Transcription factor activities and transcription factors between near-ETP/ETP and non-ETP. TF activity estimates are based on the normalized gene counts (<span class="html-italic">y</span>-axis).</p>
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29 pages, 5568 KiB  
Article
Geomatics Innovation and Simulation for Landslide Risk Management: The Use of Cellular Automata and Random Forest Automation
by Vincenzo Barrile, Luigi Bibbò, Giuliana Bilotta, Giuseppe M. Meduri and Emanuela Genovese
Appl. Sci. 2024, 14(24), 11853; https://doi.org/10.3390/app142411853 - 18 Dec 2024
Viewed by 460
Abstract
Landslides are among the most serious and frequent environmental disasters, involving the fall of large masses of rock and soil that can significantly impact human structures and inhabited areas. Anticipating these events is crucial to reduce risks through real-time monitoring of areas at [...] Read more.
Landslides are among the most serious and frequent environmental disasters, involving the fall of large masses of rock and soil that can significantly impact human structures and inhabited areas. Anticipating these events is crucial to reduce risks through real-time monitoring of areas at risk during extreme weather events, such as heavy rains, allowing for early warnings. This study aims to develop a methodology to enhance the prediction of landslide susceptibility, creating a more reliable system for early identification of risk areas. Our project involves creating a model capable of quickly predicting the susceptibility index of specific areas in response to extreme weather events. We represent the terrain using cellular automata and implement a random forest model to analyze and learn from weather patterns. Providing data with high spatial accuracy is vital to identify vulnerable areas and implement preventive measures. The proposed method offers an early warning mechanism by comparing the predicted susceptibility index with the current one, allowing for the issuance of alarms for the entire observed area. This early warning mechanism can be integrated into existing emergency protocols to improve the response to natural disasters. We applied this method to the area of Prunella, a small village in the municipality of Melito di Porto Salvo, known for numerous historical landslides. This approach provides an early warning mechanism, allowing for alarms to be issued for the entire observed area, and it can be integrated into existing emergency protocols to enhance disaster response. Full article
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<p>Grid search cross-validation results.</p>
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<p>SELU activation function.</p>
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<p>SNN network architecture.</p>
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<p>Flowchart of the proposed methodology.</p>
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<p>Map of Prunella land use.</p>
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<p>Geological map.</p>
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<p>Lithological map.</p>
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<p>Random forest confusion matrix.</p>
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<p>Self-normalizing neural network confusion matrix.</p>
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<p>Random forest’s ROC curve.</p>
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<p>Self-normalizing neural network’s ROC curve.</p>
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<p>Percentage of areas at high and low risk.</p>
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<p>Landslide susceptibility prediction.</p>
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<p>Susceptibility map.</p>
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17 pages, 3492 KiB  
Article
Conservation Implications of Population Structure and Dynamics in Medicinal Arbor Albizia odoratissima on Hainan Island, China
by Yong Yang, Xinran Ke, Qiaomiao Ji, Tao Lang, Zongrui Lai and Yali Guan
Forests 2024, 15(12), 2227; https://doi.org/10.3390/f15122227 - 17 Dec 2024
Viewed by 428
Abstract
Albizia odoratissima Benth is a perennial evergreen tree valued for its medicinal properties and is indigenous to the mountainous regions of southwestern China. The population status of A. odoratissima has been sparsely studied. This study systematically evaluated the population structure and dynamics of [...] Read more.
Albizia odoratissima Benth is a perennial evergreen tree valued for its medicinal properties and is indigenous to the mountainous regions of southwestern China. The population status of A. odoratissima has been sparsely studied. This study systematically evaluated the population structure and dynamics of A. odoratissima in the central mountainous region of Hainan Island, China, with the objective of informing the development of sustainable conservation strategies for the ecological restoration of its natural populations. Using the methodologies of population ecology, including the development of static life tables, population survival curves, population dynamics analysis, and time-series predictions, the results indicated that the populations of A. odoratissima on Hainan Island were geographically isolated into three groups. The age class distribution revealed that young, middle-aged, and mature individuals accounted for 5.73%, 74.94%, and 19.33%, respectively, suggesting a declining trend in the population. Moreover, the A. odoratissima population on Hainan Island was highly sensitive to anthropogenic disturbances, with significant increases in mortality rates observed at both the juvenile and mature stages. These results were likely due to the intraspecific and interspecific competitions, as well as external factors including human-induced disturbances, climate variability, and extreme weather events, which might potentially lead to the species’ future endangerment. Based on the current status of the A. odoratissima population, we develop adaptive management and forbid anthropogenic deforestation, conserving in situ and expanding populations, protecting ex situ germplasm resources, and replanting artificially, in order to manage the long-term conservation and management of A. odoratissima. Full article
(This article belongs to the Special Issue Advances in Forest Medicinal Resources: Evaluation and Diversity)
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<p>The geographical scope of this study focusing on the forests of <span class="html-italic">A. odoratissima</span> located in the central mountainous region of Hainan Island, China: ① Bawang Hill; ② Jianfeng Hill; ③ Limu Hill; ④ Yingge Hill; ⑤ Wuzhi Hill; ⑥ Maorui District; and ⑦ Sanya District.</p>
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<p>The distribution of DBH classes in <span class="html-italic">A. odoratissima</span> populations from (<b>a</b>) the western region (Bawang Hill and Jianfeng Hill), (<b>b</b>) the central region (Limu Hill, Yingge Hill, and Wuzhi Hill), and (<b>c</b>) the southern region (Maorui District and Sanya District) in the central mountainous region of Hainan Island, China.</p>
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<p>Curves of the mortality (red lines) and vanishing rates (blue lines) of <span class="html-italic">A. odoratissima</span> populations in the central mountainous region of Hainan Island, China. The mortality and vanishing rates of <span class="html-italic">A. odoratissima</span> population were shown in (<b>a</b>) the western region (Bawang Hill and Jianfeng Hill), (<b>b</b>) the middle region (Limu Hill, Yingge Hill, and Wuzhi Hill), and (<b>c</b>) the southern region (Maorui District and Sanya District), respectively.</p>
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<p>Curves of the survival rate functions (red lines) and the cumulative mortality rate functions (blue lines) of <span class="html-italic">A. odoratissima</span> populations in the central mountainous region of Hainan Island, China. The survival rate functions and the cumulative mortality rate functions of <span class="html-italic">A. odoratissima</span> population were shown in (<b>a</b>) the western region (Bawang Hill and Jianfeng Hill), (<b>b</b>) the middle region (Limu Hill, Yingge Hill, and Wuzhi Hill), and (<b>c</b>) the southern region (Maorui District and Sanya District), respectively.</p>
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<p>Curves of the mortality density functions (red lines) and the hazard rate functions (blue lines) of <span class="html-italic">A. odoratissima</span> populations in the central mountainous region of Hainan Island, China. The mortality density functions and the hazard rate functions of <span class="html-italic">A. odoratissima</span> population were shown in (<b>a</b>) the western region (Bawang Hill and Jianfeng Hill), (<b>b</b>) the middle region (Limu Hill, Yingge Hill, and Wuzhi Hill), and (<b>c</b>) the southern region (Maorui District and Sanya District), respectively.</p>
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<p>Time-series predictions of <span class="html-italic">A. odoratissima</span> populations in the central mountainous region of Hainan Island, China. M2 (green circles), M4 (red circles), and M6 (blue circles) are number distributions in the predicted II, IV, and VI age classes of <span class="html-italic">A. odoratissima</span> populations. The time-series predictions of <span class="html-italic">A. odoratissima</span> populations were shown in (<b>a</b>) the western region (Bawang Hill and Jianfeng Hill), (<b>b</b>) the middle region (Limu Hill, Yingge Hill, and Wuzhi Hill), and (<b>c</b>) the southern region (Maorui District and Sanya District), respectively.</p>
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