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22 pages, 14532 KiB  
Article
Assessing Vegetation Canopy Growth Variations in Northeast China
by Lijie Lu, Lingxue Yu, Xuan Li, Li Gao, Lun Bao, Xinyue Chang, Xiaohong Gao and Zhongquan Cai
Plants 2025, 14(1), 143; https://doi.org/10.3390/plants14010143 - 6 Jan 2025
Abstract
Studying climate change’s impact on vegetation canopy growth and senescence is significant for understanding and predicting vegetation dynamics. However, there is a lack of adequate research on canopy changes across the lifecycles of different vegetation types. Using GLASS LAI (leaf area index) data [...] Read more.
Studying climate change’s impact on vegetation canopy growth and senescence is significant for understanding and predicting vegetation dynamics. However, there is a lack of adequate research on canopy changes across the lifecycles of different vegetation types. Using GLASS LAI (leaf area index) data (2001–2020), we investigated canopy development (April–June), maturity (July–August), and senescence (September–October) rates in Northeast China, focusing on their responses to preseason climatic factors. We identified that early stages saw canopy development acceleration, with over 71% of areas experiencing such acceleration in April and May. As the vegetation grew, the accelerating canopy development slowed down, and the canopy reached its maturation earlier. By analyzing the partial correlation between canopy growth and preseason climatic factors, it was identified that changes in canopy growth were most significantly affected by preseason air temperature. A positive correlation was observed in the early stages, which shifted to a negative correlation during canopy maturation and senescence. Notably, the transition timing varied among different vegetation types, with grasslands (June) occurring earlier than forests (July) and farmlands (August). Additionally, grassland canopy growth showed a stronger response to precipitation than forests and farmlands, with a lagged effect of 2.50 months. Our findings improve understanding of vegetation canopy growth across different stages, holding significant importance for ecological environmental monitoring, land-use planning, and sustainable development. Full article
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Figure 1
<p>Stacked percentage chart of regions where the different trend (<span class="html-italic">p</span> &lt; 0.05) ranges in monthly LAI (leaf area index) (or VLAI: monthly LAI increments) for grasslands (<b>a</b>,<b>d</b>), forests (<b>b</b>,<b>e</b>), and farmlands (<b>c</b>,<b>f</b>) in Northeast China from 2001 to 2020. The upward and downward bars represent percentages of significant positive and negative trends, respectively.</p>
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<p>Spatial patterns of trends in monthly VLAI from 2001 to 2020 in Northeast China (with monthly designations: (<b>a</b>) = April, (<b>b</b>) = May, (<b>c</b>) = June, (<b>d</b>) = July, (<b>e</b>) = August, (<b>f</b>) = September, (<b>g</b>) = October. The regions labeled with black dots represent locations with a significant trend in VLAI (<span class="html-italic">p</span> &lt; 0.05).</p>
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<p>Spatial patterns of the partial correlation between the LAI and preseason climatic factors in Northeast China (with monthly designations: (<b>a</b>) = April, (<b>b</b>) = May, (<b>c</b>) = June, (<b>d</b>) = July, (<b>e</b>) = August, (<b>f</b>) = September, (<b>g</b>) = October and statistical chart of percentage of regions among different factors for grasslands (<b>h</b>), forests (<b>i</b>), farmlands (<b>j</b>), and three vegetation types (<b>k</b>). White bars show the fraction of insignificant, colored bars show the fraction of significant partial correlations at <span class="html-italic">p</span> &lt; 0.05. Among them, “No” indicates that the area is not significantly affected by preseason factors; “TEM”, “PRE”, and “SRAD” indicate that the area is significantly affected by a single preseason factor; “TEM + PRE”, “TEM + SRAD”, and “PRE + SRAD” indicate that the area is significantly affected by two preseason factors; “TEM + PRE + SRAD” indicates that the area is significantly affected by all three preseason factors.</p>
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<p>Spatial patterns of the partial correlation between the VLAI and preseason climatic factors in Northeast China(with monthly designations: (<b>a</b>) = April, (<b>b</b>) = May, (<b>c</b>) = June, (<b>d</b>) = July, (<b>e</b>) = August, (<b>f</b>) = September, (<b>g</b>) = October and statistical chart of percentage of regions among different factors for grasslands (<b>h</b>), forests (<b>i</b>), farmlands (<b>j</b>), and three vegetation types (<b>k</b>). White bars show the fraction of insignificant, colored bars show the fraction of significant partial correlations at <span class="html-italic">p</span> &lt; 0.05. Among them, “No” indicates that the area is not significantly affected by preseason factors; “TEM”, “PRE”, and “SRAD” indicate that the area is significantly affected by a single preseason factor; “TEM + PRE”, “TEM + SRAD”, and “PRE + SRAD” indicate that the area is significantly affected by two preseason factors; “TEM + PRE + SRAD” indicates that the area is significantly affected by all three preseason factors.</p>
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<p>Stacked percentage chart of regions where the different significant partial correlation (<span class="html-italic">p</span> &lt; 0.05) ranges between the LAI (or VLAI) and preseason PRE factors for grasslands (<b>a</b>,<b>d</b>), forests (<b>b</b>,<b>e</b>), and farmlands (<b>c</b>,<b>f</b>) in Northeast China. The upward and downward bars represent percentages of positive and negative correlations, respectively.</p>
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<p>Stacked percentage chart of regions where the different significant partial correlation (<span class="html-italic">p</span> &lt; 0.05) ranges between the LAI (or VLAI) and preseason TEM factors for grasslands (<b>a</b>,<b>d</b>), forests (<b>b</b>,<b>e</b>), and farmlands (<b>c</b>,<b>f</b>) in Northeast China. The upward and downward bars represent percentages of positive and negative correlations, respectively.</p>
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<p>Stacked percentage chart of regions where the different significant partial correlation (<span class="html-italic">p</span> &lt; 0.05) ranges between the LAI (or VLAI) and preseason SRAD factors for grasslands (<b>a</b>,<b>d</b>), forests (<b>b</b>,<b>e</b>), and farmlands (<b>c</b>,<b>f</b>) in Northeast China. The upward and downward bars represent percentages of positive and negative correlations, respectively.</p>
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<p>The length of month with the highest partial correlation coefficients between monthly LAI (or VLAI) and climate variables (PRE, TEM, and SRAD) for grasslands (<b>a</b>,<b>d</b>), forests (<b>b</b>,<b>e</b>), and farmlands (<b>c</b>,<b>f</b>).</p>
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<p>Average lagged time with the highest simple correlation coefficients between monthly LAI (or VLAI) and climate variables (PRE, TEM, and SRAD) for grasslands (<b>a</b>,<b>d</b>), forests (<b>b</b>,<b>e</b>), and farmlands (<b>c</b>,<b>f</b>).</p>
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<p>The geographic location and land use pattern across Northeast China. The legend indicates: 1 is coniferous and broad-leaved mixed forest, 2 is evergreen broad-leaved forest, 3 is deciduous broad-leaved forest, 4 is evergreen coniferous forest, 5 is deciduous coniferous forest, 6 is evergreen shrubland, 7 is deciduous shrubland, 8 is low-coverage grassland, 9 is medium-coverage grassland, 10 is high-coverage grassland, 11 is rice paddy, 12 is corn, 13 is soybean, and 14 is others.</p>
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<p>Flowchart of the partial correlation analysis method between LAI<sub>(t)</sub> (or VLAI<sub>(t)</sub>), and preseason climatic variables. In this context, if TEM(i) represents data from July 2020, TEM(i-1) represents data from June 2020, TEM(i-2) represents data from May 2020, and TEM(i-3) represents data from April 2020.</p>
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13 pages, 4958 KiB  
Technical Note
Spatiotemporal Variations in Compound Extreme Events and Their Cumulative and Lagged Effects on Vegetation in the Northern Permafrost Regions from 1982 to 2022
by Yunxia Dong, Guimin Liu, Xiaodong Wu, Lin Wang, Haiyan Xu, Sizhong Yang, Tonghua Wu, Evgeny Abakumov, Jun Zhao, Xingyuan Cui and Meiqi Shao
Remote Sens. 2025, 17(1), 169; https://doi.org/10.3390/rs17010169 - 6 Jan 2025
Abstract
The northern permafrost regions are increasingly experiencing frequent and intense extreme events, with a rise in the occurrence of compound extreme events. Many climate-related hazards in these areas are driven by such compound events, significantly affecting the stability and functionality of vegetation ecosystems. [...] Read more.
The northern permafrost regions are increasingly experiencing frequent and intense extreme events, with a rise in the occurrence of compound extreme events. Many climate-related hazards in these areas are driven by such compound events, significantly affecting the stability and functionality of vegetation ecosystems. However, the cumulative and lagged effects of compound extreme events on vegetation remain unclear, which may lead to an underestimation of their actual impacts. This study provides a comprehensive analysis of the spatiotemporal variations in compound extreme events and the vegetation response to these events in the northern permafrost regions from 1982 to 2022. The primary focus of this study is on examining the cumulative and lagged effects of compound extreme climate events on the Kernel Normalized Difference Vegetation Index (kNDVI) during the growing seasons. The results indicate that in high-latitude regions, the frequency of extreme high temperature–precipitation compound events and high temperature–drought compound events have increased in 58.0% and 67.0% of the areas, respectively. Conversely, the frequency of extreme low temperature–drought compound events and extreme low temperature–precipitation compound events has decreased in 70.6% and 57.2% of the areas, with the high temperature–drought compound events showing the fastest increase. The temporal effects of compound extreme events on kNDVI vary with vegetation type; they produce more cumulative and lagged effects compared with single extreme high-temperature events and fewer effects compared with single extreme precipitation events, with compound events significantly affecting forest and grassland ecosystems. Notably, extreme high temperature–precipitation compound events exhibit the strongest cumulative and lagged effects on vegetation, while extreme low temperature–drought compound events influence wetland and shrubland areas within the same month. This study underscores the importance of a multivariable perspective in understanding vegetation dynamics in permafrost regions. Full article
(This article belongs to the Special Issue Remote Sensing in Applied Ecology (Second Edition))
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<p>Distribution map of permafrost in the Northern Hemisphere (<b>a</b>) and vegetation type distribution map (<b>b</b>).</p>
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<p>Spatial distribution of compound extreme events in the permafrost regions from 1982 to 2022. (<b>a</b>) HP, extreme high temperature–precipitation compound event; (<b>b</b>) CD, extreme low temperature–drought compound event; (<b>c</b>) HD, extreme high temperature–drought compound event; (<b>d</b>) CP, extreme low temperature–precipitation compound event.</p>
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<p>Trends of compound extreme events in the permafrost regions from 1982 to 2022. (<b>a</b>) HP, extreme high temperature–precipitation compound event; (<b>b</b>) CD, extreme low temperature–drought compound event; (<b>c</b>) HD, extreme high temperature–drought compound event; (<b>d</b>) CP, extreme low temperature–precipitation compound event.</p>
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<p>Cumulative and lag effects of compound extreme events on kNDVI in permafrost regions from 1982 to 2022. This figure illustrates the cumulative and lag effects of compound climate indices on kNDVI across permafrost areas, categorized by the following events: (<b>a</b>) HP, extreme high temperature–precipitation compound events, (<b>b</b>) CD, extreme low temperature–drought compound events, (<b>c</b>) HD, extreme high temperature–drought compound events, and (<b>d</b>) CP, extreme low-temperature–precipitation compound events. The a represents months of lag, and the b represents months of cumulative effects. For example, “0–0” indicates no time effect, and “1–1” indicates one-month lag and one-month cumulative effects.</p>
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<p>Area proportion of cumulative and lag effects of compound extreme climate indices on kNDVI in permafrost regions from 1982 to 2022. This figure shows the distribution of area proportions for the cumulative and lag effects of various compound extreme events on kNDVI. (<b>a</b>) Forest, (<b>b</b>) wetland, (<b>c</b>) shrubbery, and (<b>d</b>) grassland. HP, extreme high temperature–precipitation compound events. CD, extreme low temperature–drought compound events. HD, extreme high temperature–drought compound events. and CP, extreme low–temperature-precipitation compound events. The a represents months of lag, and the b represents months of cumulative effects. For example, “0–0” indicates no time effect, and “1–1” indicates one-month lag and one-month cumulative effects.</p>
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21 pages, 6182 KiB  
Article
Spatiotemporal Dynamics of Drought and the Ecohydrological Response in Central Asia
by Keting Feng, Yanping Cao, Erji Du, Zengguang Zhou and Yaonan Zhang
Remote Sens. 2025, 17(1), 166; https://doi.org/10.3390/rs17010166 - 6 Jan 2025
Abstract
Due to the influences of climate change and human activities, the resources and environments of the “One Belt and One Road” initiative are facing severe challenges. Using drought indicators, this study aimed to analyze the spatiotemporal characteristics of the drought environment and the [...] Read more.
Due to the influences of climate change and human activities, the resources and environments of the “One Belt and One Road” initiative are facing severe challenges. Using drought indicators, this study aimed to analyze the spatiotemporal characteristics of the drought environment and the response of vegetation cover in the area to drought conditions. The Gravity Recovery and Climate Experiment (GRACE) drought severity index (GRACE-DSI), GRACE water storage deficit index (GRACE-WSDI) and standardized precipitation index (SPI) were calculated to measure hydrological drought. Additionally, based on GRACE and Global Land Data Assimilation System (GLDAS) data, groundwater data in Central Asia was retrieved to calculate the groundwater drought index using the GRACE Standardized Groundwater Level Index (GRACE-SGI). The findings indicate that, from 2000, Central Asia’s annual precipitation decreased at a rate of 1.80 mm/year (p < 0.1), and its annual temperature increased slightly, at a rate of 0.008 °C/year (p = 0.62). Water storage decreased significantly at a rate of −3.53 mm/year (p < 0.001) and showed an increase-decrease-increase-decrease pattern. During the study period, the aridity in Central Asia deteriorated, especially on the eastern coast of the Caspian Sea and the Aral Sea basin. After 2020, most of Central Asia experienced droughts at both the hydrological and groundwater droughts levels and of varying lengths and severity. During the growing season, there was a substantial positive association between the Normalized Difference Vegetation Index (NDVI) and drought indicators such as GRACE-DSI and GRACE-WSDI. Nonetheless, the NDVI of cultivated land and grassland distribution areas in Central Asia displayed a strong negative correlation with GRACE-SGI. This study concludes that the arid environment in Central Asia affected the growth of vegetation. The ecological system in Central Asia may be put under additional stress if drought conditions continue to worsen. This paper explores the drought characteristics in Central Asia, especially those of groundwater drought, and analyzes the response of vegetation, which is very important for the ecological and environmental protection of the region. Full article
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<p>The location of Central Asia and land cover over Central Asia in 2018 (available at <a href="https://lpdaac.usgs.gov/products/mcd12q1v006/" target="_blank">https://lpdaac.usgs.gov/products/mcd12q1v006/</a>, accessed on 12 December 2024). Central Asia includes five countries.</p>
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<p>The data processing flowchart.</p>
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<p>Annual precipitation (<b>a</b>) and air temperature (<b>c</b>) in Central Asia from 2000 and 2022; multi-year monthly average precipitation (<b>b</b>) and air temperature (<b>d</b>) in Central Asia between 2000 and 2022; multi-year average precipitation (<b>e</b>) and air temperature (<b>f</b>) in Central Asia between 2000 and 2022; and annual change trend of precipitation (<b>g</b>) and temperature (<b>h</b>). (The blank in <a href="#remotesensing-17-00166-f003" class="html-fig">Figure 3</a>e–h) represents the Caspian Sea, which is not considered in this paper).</p>
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<p>Monthly TWSA in Central Asia from April 2002 to May 2023.</p>
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<p>Spatiotemporal change trends of annual TWSA in Central Asia from 2002 to 2023. (The blank represents the Caspian Sea, which is not considered in this paper).</p>
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<p>Spatial correlation coefficients between GRACE-DSI, WSDI, SGI, and SPI during 2002–2023. <span class="html-italic">p</span> stands for the significance of linear correlation, <span class="html-italic">p</span> = 0 represents no significant correlation, and <span class="html-italic">p</span> = 1 represents significant correlation.</p>
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<p>Monthly change rate of GRACE-DSI, GRACE-WSDI, and GRACE-SGI and their MK significance test results. (<b>a</b>) Change slope of GRACE-DSI, (<b>b</b>) Significant test result of GRACE_DSI, (<b>c</b>) Change slope of GRACE-WDSI, (<b>d</b>) Significant test result of GRACE_WDSI, (<b>e</b>) Change slope of GRACE-SGI, (<b>f</b>) Significant test result of GRACE_SGI.</p>
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<p>Correlation between the GRACE drought indicators (i.e., GRACE-DSI, GRACE-WSDI, GRACE-SGI) and the MODIS NDVI during the growing season (April–September). <span class="html-italic">p</span> stands for the significance of linear correlation, <span class="html-italic">p</span> = 0 represents no significant correlation, and <span class="html-italic">p</span> = 1 represents significant correlation.</p>
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26 pages, 3308 KiB  
Article
Adaptive Cloud-Based Big Data Analytics Model for Sustainable Supply Chain Management
by Nenad Stefanovic, Milos Radenkovic, Zorica Bogdanovic, Jelena Plasic and Andrijana Gaborovic
Sustainability 2025, 17(1), 354; https://doi.org/10.3390/su17010354 - 6 Jan 2025
Viewed by 145
Abstract
Due to uncertain business climate, fierce competition, environmental challenges, regulatory requirements, and the need for responsible business operations, organizations are forced to implement sustainable supply chains. This necessitates the use of proper data analytics methods and tools to monitor economic, environmental, and social [...] Read more.
Due to uncertain business climate, fierce competition, environmental challenges, regulatory requirements, and the need for responsible business operations, organizations are forced to implement sustainable supply chains. This necessitates the use of proper data analytics methods and tools to monitor economic, environmental, and social performance, as well as to manage and optimize supply chain operations. This paper discusses issues, challenges, and the state of the art approaches in supply chain analytics and gives a systematic literature review of big data developments associated with supply chain management (SCM). Even though big data technologies promise many benefits and advantages, the prospective applications of big data technologies in sustainable SCM are still not achieved to a full extent. This necessitates work on several segments like research, the design of new models, architectures, services, and tools for big data analytics. The goal of the paper is to introduce a methodology covering the whole Business Intelligence (BI) lifecycle and a unified model for advanced supply chain big data analytics (BDA). The model is multi-layered, cloud-based, and adaptive in terms of specific big data scenarios. It comprises business process modeling, data ingestion, storage, processing, machine learning, and end-user intelligence and visualization. It enables the creation of next-generation BDA systems that improve supply chain performance and enable sustainable SCM. The proposed supply chain BDA methodology and the model have been successfully applied in practice for the purpose of supplier quality management. The solution based on the real-world dataset and the illustrative supply chain case are presented and discussed. The results demonstrate the effectiveness and applicability of the big data model for intelligent and insight-driven decision making and sustainable supply chain management. Full article
(This article belongs to the Special Issue Sustainable Enterprise Operation and Supply Chain Management)
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<p>Methodology for big data analytics.</p>
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<p>Supply chain analytics lifecycle model.</p>
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<p>Supply chain big data solution architecture.</p>
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<p>Supplier quality analysis services cube.</p>
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<p>Supplier quality dashboard page.</p>
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<p>Supplier downtime analysis dashboard.</p>
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<p>Result of natural queries.</p>
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<p>Automatically generated machine learning insights.</p>
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21 pages, 4432 KiB  
Article
MLAS: Machine Learning-Based Approach for Predicting Abiotic Stress-Responsive Genes in Chinese Cabbage
by Xiong You, Yiting Shu, Xingcheng Ni, Hengmin Lv, Jian Luo, Jianping Tao, Guanghui Bai and Shusu Feng
Horticulturae 2025, 11(1), 44; https://doi.org/10.3390/horticulturae11010044 - 6 Jan 2025
Viewed by 175
Abstract
The challenges posed by climate change have had a crucial impact on global food security, with crop yields negatively affected by abiotic and biotic stresses. Consequently, the identification of abiotic stress-responsive genes (SRGs) in crops is essential for augmenting their resilience. This study [...] Read more.
The challenges posed by climate change have had a crucial impact on global food security, with crop yields negatively affected by abiotic and biotic stresses. Consequently, the identification of abiotic stress-responsive genes (SRGs) in crops is essential for augmenting their resilience. This study presents a computational model utilizing machine learning techniques to predict genes in Chinese cabbage that respond to four abiotic stresses: cold, heat, drought, and salt. To construct this model, data from relevant studies regarding responses to these abiotic stresses were compiled, and the protein sequences encoded by abiotic SRGs were converted into numerical representations for subsequent analysis. For the selected feature set, six distinct machine learning binary classification algorithms were employed. The results demonstrate that the constructed models can effectively predict SRGs associated with the four types of abiotic stresses, with the area under the receiver operating characteristic curve (auROC) for the models being 81.42%, 87.92%, 80.85%, and 88.87%, respectively. For each type of stress, a distinct number of stress-resistant genes was predicted, and the ten genes with the highest scores were selected for further analysis. To facilitate the implementation of the proposed strategy by users, an online prediction server, has been developed. This study provides new insights into computational approaches to the identification of abiotic SRGs in Chinese cabbage as well as in other plants. Full article
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<p>Total gene counts for different stress types in Chinese cabbage.</p>
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<p>These figures illustrate the overlap of genes across different articles. In each bar chart, the horizontal axis represents the number of articles in which a specific gene is mentioned as being related to a specific abiotic stress, while the vertical axis shows the total number of genes mentioned that many times across all articles. Genes that are mentioned in only one article are excluded from these charts.</p>
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<p>Schematic workflow for model development.</p>
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<p>Discriminative motif discovery in protein sequences under various stress conditions.</p>
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<p>Scatterplot heatmaps of auROC for different machine learning algorithms and feature construction methods. In the heatmap, the color intensity indicates the performance of the models, with red representing higher auROC values and blue indicating lower auROC values.</p>
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<p>Plots of the area under the receiver operating characteristic curve (auROC) were created using CKSAAP methods with SVM-RFE for feature selection. The blue vertical line in the plot indicates the point corresponding to the number of features that maximizes the auROC value, with the corresponding optimal auROC value marked at that point.</p>
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<p>ROC curves for salt stress show evaluation results from different feature construction methods and classification algorithms. Each plot represents a different feature construction method, while the legend in each plot indicates the performance of various machine learning algorithms applied to the respective feature set, with each line color corresponding to a specific algorithm.</p>
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<p>The ROC curves for the four abiotic stresses present the assessment outcomes derived from protein sequence characteristics produced by the CKSAAP method, utilizing various classification algorithms. Each plot represents the ROC curve for the optimal CKSAAP features under a specific abiotic stress condition (cold, heat, drought, or salt). The legend in each plot indicates the performance of different machine learning algorithms applied to the selected CKSAAP features, illustrating how each classifier performed under varying stress conditions.</p>
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<p>Interface for use of MLAS.</p>
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23 pages, 28101 KiB  
Article
Quantifying Time-Lag and Time-Accumulation Effects of Climate Change and Human Activities on Vegetation Dynamics in the Yarlung Zangbo River Basin of the Tibetan Plateau
by Ning Li and Di Wang
Remote Sens. 2025, 17(1), 160; https://doi.org/10.3390/rs17010160 - 5 Jan 2025
Viewed by 369
Abstract
Vegetation, as a fundamental component of terrestrial ecosystems, plays a pivotal role in the flux of water, heat, and nutrients between the lithosphere, biosphere, and atmosphere. Assessing the impacts of climate change and human activities on vegetation dynamics is essential for maintaining the [...] Read more.
Vegetation, as a fundamental component of terrestrial ecosystems, plays a pivotal role in the flux of water, heat, and nutrients between the lithosphere, biosphere, and atmosphere. Assessing the impacts of climate change and human activities on vegetation dynamics is essential for maintaining the health and stability of fragile ecosystems, such as the Yarlung Zangbo River (YZR) basin of the Tibetan Plateau, the highest-elevation river basin in the world. Vegetation responses to climate change are inherently asymmetric, characterized by distinct temporal effects. However, these temporal effects remain poorly understood, particularly in high-altitude ecosystems. Here, we examine the spatiotemporal changes in leaf area index (LAI) and four climatic factors—air temperature, precipitation, potential evapotranspiration, and solar radiation—in the YZR basin over the period 2000–2019. We further explore the time-lag and time-accumulation impacts of these climatic factors on LAI dynamics and apply an enhanced residual trend analysis to disentangle the relative contributions of climate change and human activities. Results indicated that (1) a modest increase in annual LAI at a rate of 0.02 m2 m−2 dec−1 was detected across the YZR basin. Spatially, LAI increased in 66% of vegetated areas, with significant increases (p < 0.05) in 10% of the basin. (2) Temperature, precipitation, and potential evapotranspiration exhibited minimal time-lag (<0.5 months) but pronounced notable time-accumulation effects on LAI variations, with accumulation periods ranging from 1 to 2 months. In contrast, solar radiation demonstrated significant time-lag impacts, with an average lag period of 2.4 months, while its accumulation effects were relatively weaker. (3) Climate change and human activities contributed 0.023 ± 0.092 and –0.005 ± 0.109 m2 m−2 dec−1 to LAI changes, respectively, accounting for 60% and 40% on the observed variability. Spatially, climate change accounted for 85% of the changes in LAI in the upper YZR basin, while vegetation dynamics in the lower basin was primarily driven by human activities, contributing 63%. In the middle basin, vegetation dynamics were influenced by the combined effects of climate change and human activities. Our findings deepen insights into the drivers of vegetation dynamics and provide critical guidance for formulating adaptive management strategies in alpine ecosystems. Full article
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<p>Overview of the study area and its environmental characteristics. (<b>a</b>) Location of the YZR basin on the TP. (<b>b</b>) Elevation distribution across the basin. (<b>c</b>) Land use/cover composition. (<b>d</b>) Mean annual temperature distribution and (<b>e</b>) mean annual precipitation distribution derived from WorldClim Historical Monthly Weather Data (1980–2019) at a spatial resolution of 2.5 min (<a href="https://worldclim.org/data/monthlywth.html" target="_blank">https://worldclim.org/data/monthlywth.html</a> (accessed on 26 November 2024)).</p>
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<p>Flowchart of this study. Dotted-box indicates tools/methods used in the analysis.</p>
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<p>Spatial patterns and temporal trends of climatic factors in the YZR basin during 2000–2019. (<b>a</b>,<b>c</b>,<b>e</b>,<b>g</b>) Mean annual values of air temperature (TEM), precipitation (PRE), potential evapotranspiration (PET), and solar radiation (SRD). (<b>b</b>,<b>d</b>,<b>f</b>,<b>h</b>) Spatial distributions of the trends in TEM, PRE, PET, and SRD). Insets illustrate the frequency distribution of trends across the basin.</p>
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<p>Seasonal variations and trends of climatic factors in the YZR basin and its sub-basins from 2000 to 2019. (<b>a</b>,<b>c</b>,<b>e</b>,<b>g</b>) Seasonal mean values of air temperature (TEM), precipitation (PRE), potential evapotranspiration (PET), and solar radiation (SRD) for spring (MAM), summer (JJA), autumn (SON), and winter (DJF). (<b>b</b>,<b>d</b>,<b>f</b>,<b>h</b>) Seasonal trends of the respective climatic factors. Error bars represent the standard deviations.</p>
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<p>Spatiotemporal variations in LAI across the YZR basin during 2000–2019. (<b>a</b>) Spatial patterns of the growing season (May–September) mean LAI with an inset showing the frequency distribution of LAI values across the basin. (<b>b</b>) Temporal trend of basin-wide mean LAI, with a regression line and 95% confidence interval. (<b>c</b>) Distribution of significant (<span class="html-italic">p</span> &lt; 0.05) and insignificant greening and browning trends.</p>
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<p>Spatial patterns and proportions of optimal time-lag and time-accumulation periods for climatic factors affecting LAI dynamics in the YZR basin. (<b>a</b>,<b>c</b>,<b>e</b>,<b>g</b>) Spatial distribution of the optimal number of months for time-lag (L) and time-accumulation (A) effects for four climatic factors. (<b>b</b>,<b>d</b>,<b>f</b>,<b>h</b>) Corresponding pie charts illustrating the proportions of different time-lag and time-accumulation combinations across the basin. Color codes represent specific lag-accumulation combinations (e.g., L0A0 indicates no lag and accumulation effects, and L3A0 indicates a three-month lag with no accumulation effects).</p>
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<p>Spatial distribution LAI trends attributed to different drivers in the YZR basin over the period 2000 to 2019. (<b>a</b>–<b>d</b>) Trends of LAI components attributed to precipitation (LAI<sub>PRE</sub>), air temperature (LAI<sub>TEM</sub>), potential evapotranspiration (LAI<sub>PET</sub>), and solar radiation (LAI<sub>SRD</sub>). (<b>e</b>,<b>f</b>) Trends of LAI components driven by climate change (LAI<sub>CC</sub>) and human activities (LAI<sub>HA</sub>). Insets in each panel show the frequency distribution of trend values within the basin. Positive trends are shown in green, while negative trends are in magenta, with hatched areas indicating statistically significant trends at the <span class="html-italic">p</span> &lt; 0.05 level.</p>
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<p>Percentage contributions of climate change (CC) and human activities (HAs) to LAI changes across the YZR basin from 2000 to 2019. (<b>a</b>) Spatial distribution of the percentage contribution of CC (%), with pie charts summarizing the contributions across the entire basin (YZR) and its sub-basins (LZ, LS, NX, and PS). (<b>b</b>) Spatial distribution of the percentage contribution of HAs (%), with corresponding pie charts showing their relative impact in the YZR and its sub-basins.</p>
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<p>Comparison of model performance for LAI simulation with and without temporal effects in the YZR basin. (<b>a</b>) Spatial distribution of R<sup>2</sup> values for models without temporal effects, with a median R<sup>2</sup> of 0.81. (<b>b</b>) Spatial distribution of R<sup>2</sup> values for models with temporal effects, showing an improved median R<sup>2</sup> of 0.87. (<b>c</b>) Spatial distribution of the differences in R<sup>2</sup> between the two models. (<b>d</b>) Violin plots comparing R<sup>2</sup> values across the entire basin (YZR) and sub-basins (LZ, LS, NX, and PS).</p>
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<p>Land-use transitions in the YZR basin from 2001 to 2019. (<b>a</b>) Land use/cover maps for 2001, 2010, and 2019. The land-use classes shown in the figure were reclassified based on the MOD-IGBP classification system (<a href="#app1-remotesensing-17-00160" class="html-app">Table S4</a>). (<b>b</b>) Sankey diagram depicting overall land-use transitions in the YZR basin. (<b>c</b>–<b>f</b>) Regional Sankey diagrams for the sub-basins: LZ (<b>c</b>), LS (<b>d</b>), NX (<b>e</b>), and PS (<b>f</b>), visualizing land-use changes within each sub-region over time.</p>
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16 pages, 5234 KiB  
Article
Detection and Attribution of a Spatial Heterogeneity in the Temporal Evolution of Bulgarian River Discharge
by Natalya A. Kilifarska, Gergana I. Metodieva and Antonia Ch. Mokreva
Geosciences 2025, 15(1), 12; https://doi.org/10.3390/geosciences15010012 - 5 Jan 2025
Viewed by 299
Abstract
The hydrosphere is an element of the climate system and changes in the latter are reasonably projected over the river outflow. Climatic changes, however, are unevenly distributed over the Earth, and understanding their regional imprint on the hydrosphere is of great importance. In [...] Read more.
The hydrosphere is an element of the climate system and changes in the latter are reasonably projected over the river outflow. Climatic changes, however, are unevenly distributed over the Earth, and understanding their regional imprint on the hydrosphere is of great importance. In this study, we have conducted a statistical analysis of the monthly maximum and minimum river discharge recorded in 22 hydrological stations located on 19 of the Bulgarian rivers during the period 1993–2022. We have found that in half of the river basins, the trend of the spring maximum discharge is significantly positive (α = 0.05). In the other half of the stations, the trend is neutral. The stations with a positive trend are not randomly distributed but grouped, forming a pattern crossing the country from northwest to southeast. This pattern of trend distribution raises questions about the causes of the irregular hydrological response to the rising global near-surface temperatures. A comparison of hydrological data with some climatic variables (i.e., temperature, precipitation, and ozone at 70 hPa), combined with neural network analysis results, suggests ozone as a possible reason for the heterogeneous hydrological response. Its effect could be explained by an imposed episodic warming of the near-surface temperature due to fluctuations in the ozone density near the tropopause, which in turn favours the faster melting of ice and snow in the corresponding river basins. Full article
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<p>Location of the Bulgarian river basins used in the current study, together with the hydrological stations measuring river discharge.</p>
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<p>Maps of river discharge trends: (<b>a</b>) maximum discharge (spring); (<b>b</b>) minimum discharge (autumn) on the territory of Bulgaria, calculated by linear regression. Values higher or lower than ±0.15 [m<sup>3</sup>/s/yr] are statistically significant at α = 0.05. Stars indicate the location of hydrological stations.</p>
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<p>Spatial distribution of the correlation between modelled and measured maximum streamflow as a function of total precipitation (<b>a</b>), temperature at 2 m above the surface (<b>b</b>) and ozone at 70 hPa (<b>c</b>). maximum streamflow trends (shown in <a href="#geosciences-15-00012-f002" class="html-fig">Figure 2</a>). Stars indicate the location of the hydrological stations.</p>
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<p>Maps of near-surface temperature (top) (<b>a</b>) and total precipitation (bottom) (<b>b</b>) dynamic anomalies calculated for the period 1993–2022 (coloured shading). The spring outflow trend, shown in <a href="#geosciences-15-00012-f002" class="html-fig">Figure 2</a>, is overlaid (contours). Stars indicate the location of hydrological stations.</p>
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<p>Maps of the spring near-surface temperature (<b>a</b>) and ozone at 70 hPa (<b>b</b>) dynamic anomalies, calculated for the period 1993–2022 (coloured shading). The red contours represents the spring outflow trend, shown in <a href="#geosciences-15-00012-f002" class="html-fig">Figure 2</a>. Stars indicate the location of hydrological stations.</p>
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<p>Schematic diagram of the effect of ozone on surface temperature and late winter/early spring river discharge; GhE stands for greenhouse effect.</p>
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<p>Maps of the autumn near-surface temperature (<b>a</b>) and ozone at 70 hPa (<b>b</b>) dynamic anomalies, calculated for the period 1993–2022 (coloured shading). Stars indicate the location of hydrological stations.</p>
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<p>Time series of the monthly discharge of the Maritsa River, measured in Plovdiv, and the ozone values at 70 hPa, over Plovdiv, for the period 1993–2022.</p>
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<p>Projection of the influence of ozone at 70 hPa on the rivers discharge, determined by an artificial neural network (colour shading). The green contours indicate the statistically significant trend in river discharge (shown in <a href="#geosciences-15-00012-f002" class="html-fig">Figure 2</a>). Stars indicate the location of hydrological stations.</p>
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17 pages, 1444 KiB  
Systematic Review
Rift Valley Fever in Rwanda Is Urging for Enhancing Global Health Security Through Multisectoral One Health Strategy
by Claude Mambo Muvunyi, Jean Claude Semuto Ngabonziza, Emmanuel Edwar Siddig and Ayman Ahmed
Microorganisms 2025, 13(1), 91; https://doi.org/10.3390/microorganisms13010091 - 5 Jan 2025
Viewed by 397
Abstract
Rift Valley fever (RVF) is a devastating zoonotic mosquito-borne viral hemorrhagic fever disease that threats human and animal health and biodiversity in Africa, including in Rwanda. RVF is increasingly outbreaking in Africa, leading to devastating impacts on health, socioeconomic stability and growth, and [...] Read more.
Rift Valley fever (RVF) is a devastating zoonotic mosquito-borne viral hemorrhagic fever disease that threats human and animal health and biodiversity in Africa, including in Rwanda. RVF is increasingly outbreaking in Africa, leading to devastating impacts on health, socioeconomic stability and growth, and food insecurity in the region, particularly among livestock-dependent communi-ties. This systematic review synthesizes existing evidence on RVF’s epidemiology, transmission dynamics, and the prevention and control measures implemented in Rwanda. Our findings high-light the rapidly increasing prevalence of RVF and the expansion of its geographical distribution and host range in Rwanda. Furthermore, the review reveals gaps in local evidence, including the existence of competent vectors of RVFV and the risk factors associated with the emergence and spread of RVF in the country. This underscores the urgent need for prospective research to inform evidence-based health policymaking, strategic planning, and the development and implementation of cost-effective preventive and control measures, including diagnosis and surveillance for early detection and response. It also calls for the institutionalization of a cost-effective, multisectoral, and transdisciplinary One Health strategy for reducing the burden and risk of climate climate-sensitive and zoonotic diseases, including RVF, in the country. We recommend exploring cost-effective human and/or animal vaccination mechanisms for RVF, integrating AI-powered drones into dis-ease vectors surveillance and control, and the routine implementation of genomics-enhanced xenosurveillance to monitor changes in pathogens and vectors dynamics in order to inform poli-cymaking and guide the control interventions. Full article
(This article belongs to the Special Issue One Health Research on Infectious Diseases)
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<p>PRISMA flowchart summarizing the systematic data mining, identification and screening of records, and final inclusion of reports.</p>
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<p>Illustration of the development of the Rift Valley fever burden in Rwanda; aspects related to the integration of innovative strategies for early detection and response to outbreaks are highlighted in red boxes, and gaps in evidence and policymaking are presented in the diagonal boxes.</p>
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<p>Map of Rwanda showing the distribution of RVF infections among human and livestock populations in districts highlighted in red. Meanwhile, districts that only reported infections among livestock without the involvement of humans are highlighted in blue.</p>
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27 pages, 6682 KiB  
Review
Renewable Energy for Sustainable Development: Opportunities and Current Landscape
by Dzintra Atstāja
Energies 2025, 18(1), 196; https://doi.org/10.3390/en18010196 - 5 Jan 2025
Viewed by 329
Abstract
Energy is often described as the lifeblood of a nation’s economy, and the world energy trilemma calls for collaboration and innovative solutions at the national level. This is where Education for Sustainable Development (ESD) plays a crucial role, helping integrate the achievement of [...] Read more.
Energy is often described as the lifeblood of a nation’s economy, and the world energy trilemma calls for collaboration and innovative solutions at the national level. This is where Education for Sustainable Development (ESD) plays a crucial role, helping integrate the achievement of the United Nations Sustainable Development Goals (SDGs) while addressing the challenges posed by the energy trilemma. Europe’s strong commitment to transitioning to sustainable energy is evident in its response to geopolitical changes and climate targets. Notably, the Baltic States have taken decisive action in response to the war in Ukraine, choosing to completely halt electricity imports from Russia and Belarus. This shift was supported by increased energy imports via interconnectors from Finland, Sweden, and Poland, with electricity imports rising to 13,053 GWh—an increase of 2.6% in 2023 compared to the previous year. Latvia, which holds the highest green energy potential in the Baltic Sea region, has nevertheless lagged behind its Baltic counterparts in terms of implementation. In 2021, Latvia ranked third among European Union (EU) countries for renewable energy share in final energy consumption, with 42.1%, significantly higher than the EU average of 21.8%. However, further progress is needed to meet Latvia’s 2030 target of 14% renewable energy use in transport. The Baltic States aim to produce 98–100% of their electricity from renewable sources by 2050. The Baltic States should be regarded as a unified energy system, with a coordinated strategy for achieving sustainable energy development through collaboration and joint planning. This analysis highlights the complexities of managing energy markets amidst global and regional challenges, emphasizing the importance of well-designed public interventions to secure long-term benefits. The study concludes with a call for enhanced interagency cooperation to reform ESD and create a new interdisciplinary sector dedicated to “Sustainable Development”. Full article
(This article belongs to the Collection Renewable Energy and Energy Storage Systems)
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<p>Graphical representation of research.</p>
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<p>Keywords: “World energy trilemma” (36 documents found—period 2018–2024 in the Baltic States) [<a href="#B24-energies-18-00196" class="html-bibr">24</a>].</p>
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<p>Keywords: “World energy trilemma”, “Sustainable development”, and “Renewable energy”. (The figure shows the author’s analysis, via VOSviewer. Thirty-one documents were found—period 2018–2024 in the Baltic States).</p>
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<p>Keywords: “Sustainable development”, “renewable energy”, and “Sustainable development goals”. The figure shows the author’s analysis, via VOSviewer (223 documents were found—period 2018–2024 in the Baltic States).</p>
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<p>Keywords: “World energy trilemma” and “Renewable energy”. The figure shows the author’s analysis, via VOSviewer). Thirty-two documents were found—period 2018–2024 in the Baltic States [<a href="#B24-energies-18-00196" class="html-bibr">24</a>].</p>
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<p>Countries’ performances according to the World Energy Trilemma Index 2024 [<a href="#B31-energies-18-00196" class="html-bibr">31</a>].</p>
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<p>The “green” electricity potential of the EU countries, based on [<a href="#B47-energies-18-00196" class="html-bibr">47</a>].</p>
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<p>Offshore wind potential in Baltic States [<a href="#B48-energies-18-00196" class="html-bibr">48</a>].</p>
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<p>WindEurope Q2 2024 renewable energy performance data, based on [<a href="#B51-energies-18-00196" class="html-bibr">51</a>].</p>
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<p>Baltic countries’ performances in the World Energy Trilemma Index, and comparison across sections energy security, energy equity, and environmental sustainability, based on [<a href="#B52-energies-18-00196" class="html-bibr">52</a>].</p>
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<p>Percentage of energy derived from renewable sources, 2004–2022 (% of total final energy use), based on [<a href="#B54-energies-18-00196" class="html-bibr">54</a>].</p>
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<p>Electricity prices in Baltic countries [<a href="#B88-energies-18-00196" class="html-bibr">88</a>].</p>
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<p>The trilemma as a foundation for a new cooperation and science.</p>
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18 pages, 537 KiB  
Article
Impacts and Internal Mechanisms of High-Standard Farmland Construction on the Reduction of Agricultural Carbon Emission in China
by Shuangqiang Li, Mingyue Li, Jiaojiao Chen, Siyuan Shao and Yu Tian
Agriculture 2025, 15(1), 105; https://doi.org/10.3390/agriculture15010105 - 5 Jan 2025
Viewed by 254
Abstract
In response to climate change, the reduction of carbon emissions during agricultural production has garnered increasing global focus. This study takes high-standard farmland construction (HSFC) implemented in 2011 as the standard natural experiment and adopts the continuous differences-in-differences (DID) model to explore the [...] Read more.
In response to climate change, the reduction of carbon emissions during agricultural production has garnered increasing global focus. This study takes high-standard farmland construction (HSFC) implemented in 2011 as the standard natural experiment and adopts the continuous differences-in-differences (DID) model to explore the impact and internal mechanism of HSFC on agricultural carbon emissions based on a panel data of 31 provinces, municipalities, and autonomous regions in China from 2003 to 2021. The results show that HSFC can effectively reduce the carbon emissions in agricultural production, and the average annual reduction can reach 53.8%. The effects of HSFC on agriculture carbon emissions could be associated with reducing agricultural fossil energy consumption and reducing agricultural chemical use. Further, the heterogeneity study shows that the carbon reduction effect of HSFC was mainly reflected in non-major grain-producing areas, while there was no significant impact in major grain-producing areas. Policymakers should unswervingly continue to promote HSFC, considering their own economic and geographical conditions. This study can provide valuable information and references for developing countries similar to China to formulate policies on agricultural carbon reduction. Full article
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<p>Parallel trend test. The dashed line represents the boundary of the HSFC policy implication. Pre and Post indicate the before and after of the HSFC policy.</p>
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16 pages, 6188 KiB  
Article
Species Diversity of the Family Arecaceae: What Are the Implications of Their Biogeographical Representation? An Analysis in Amazonas, Northeastern Peru
by Freddy Miranda, José-Walter Coronel-Chugden, Jaris Veneros, Ligia García, Grobert A. Guadalupe and Erick Arellanos
Forests 2025, 16(1), 76; https://doi.org/10.3390/f16010076 - 5 Jan 2025
Viewed by 289
Abstract
The understanding of species distribution in Peru is limited, in part due to cartographic representations that traditionally use political rather than biogeographical boundaries. The objective of this study was to determine the distribution of Arecaceae species in the department of Amazonas by representing [...] Read more.
The understanding of species distribution in Peru is limited, in part due to cartographic representations that traditionally use political rather than biogeographical boundaries. The objective of this study was to determine the distribution of Arecaceae species in the department of Amazonas by representing them in biogeographical regions. To this end, geographic information systems and global databases were used to map and analyze the species in four categories: Ecosystems Map, Ecoregions Map, Peru Climate Classification Map, and Protected Natural Areas Map. Subsequently, diversity metrics were estimated, revealing high diversity in Amazonas, with 22 genera and 90 species of Arecaceae representing 51.16% and 41.28% of the records in Peru, respectively. In addition, predominant genera and species were identified, and diversity was evaluated in biogeographic units. Of a total of 336,029 records, 45 genera were found, with Geonoma and Bactris being the most representative, and of the 218 species found in total, the records that stood out the most varied according to biogeographical regions. For each Biogeographic unit by category, different responses were obtained, for example, for Index Margalef, between 0.000 (low in Agricultural Area), 7.2489 (medium in Eastern Cordillera Real Montane Forests), and 13.2636 (high in Non-protected Areas). Similarly, for the Shannon–Wiener diversity index (H¯), where values were obtained between 0.000 (low in Jalca (Andean High Grasslands), (medium in Reserved Zonez) and 3.7054 (high in Non-protected Areas). The results suggest high under-recording, evidencing gaps in knowledge and information, as analyses based on detailed studies of diversity in specific biogeographic categories in these other families, as well as future research to determine, for example, genomes and Hill numbers, will be carried out. The conclusions highlight the high correlation between the diversity metrics analyzed, confirm the theoretical validity, and allow us to recommend species richness and the Margalef Index as useful and relevant metrics due to their applicability and ease of interpretation. This study offers key information for decision makers in policies for the conservation of Arecaceae diversity and motivates us to project research of this type in other families in Peru. Full article
(This article belongs to the Section Forest Biodiversity)
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<p>Methodological outline for the analysis of family Arecaceae in Amazonas, northeastern Peru.</p>
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<p>Representation of species of the family Arecaceae in biogeographic regions in the department of Amazonas, Peru.</p>
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15 pages, 3711 KiB  
Article
Effects of Stand Structural Characteristics, Diversity, and Stability on Carbon Storage Across Different Densities in Natural Forests: A Case Study in the Xiaolong Mountains, China
by Yingdong Ma, Xiaowei Zhang, Rui Jiang, Mengduo Jiang and Jinmao Ju
Forests 2025, 16(1), 71; https://doi.org/10.3390/f16010071 - 5 Jan 2025
Viewed by 210
Abstract
The carbon storage in forest ecosystems is closely linked to biomass, and its dynamic changes are of significant importance for assessing forest structure and function, as well as their response to global climate change. Recently, the research on the influencing mechanism of forest [...] Read more.
The carbon storage in forest ecosystems is closely linked to biomass, and its dynamic changes are of significant importance for assessing forest structure and function, as well as their response to global climate change. Recently, the research on the influencing mechanism of forest carbon storage has been a hotpot in the field of forest ecology. However, it remains unclear on the relationships among stand structure, stand stability, and carbon storage. The issues needed to be answered are as follows: How are tree density, tree species diversity, stand structural characteristics, stand stability, and carbon storage correlated? Is there a direct or indirect effect between tree density, tree species diversity, stand structural characteristics, stand stability, and carbon storage? Do these factors have an impact on stand stability, and, subsequently, carbon storage? What is the crucial factor in the mechanism that influences carbon storage? Here, the natural Quercus mongolica forests in the Xiaolong Mountains were taken as the research object. Several methods, including Pearson’s correlation, the best-fitting SEM, and multiple regression, were used to examine the relationships among tree density, tree species diversity, stand structural characteristics, stand stability, and carbon storage. Our results show that there were correlations between tree density, tree species diversity, stand structural characteristics, stand stability, and carbon storage. Tree density not only directly affects stand stability but also indirectly influences it through the mediation of tree species diversity and stand structural characteristics. Meanwhile, tree density also indirectly influences carbon storage through the mediation of tree species diversity, stand structural characteristics, and stand stability. Crown volume exerts the greatest influence on stand stability, while carbon storage is mostly impacted by stand stability. Overall, the combination of tree density, tree species diversity, stand structural characteristics, and stand stability influences carbon storage (66.4%). Therefore, it is important to consider stand stability when assessing carbon sequestration potentials; furthermore, the importance of tree density, tree species composition, and stand structural characteristics should be emphasized. Our research provides a scientific basis for conservation and management decision-making in natural forests and offers novel insights as well as a scientific reference for future large-scale carbon storage investigations. Full article
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<p>Locations of the sample plot. The map of China has approval number GS(2020)4619.</p>
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<p>Conceptual model for relationships between tree density, stand structural characteristics, tree species diversity, stand stability, and carbon storage.</p>
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<p>Correlation analysis of stand factors, stability, and carbon storage. * indicates a significance level of 0.05; ** indicates a significance level of 0.01; *** indicates a significance level of 0.001. W: uniform angle index; U: neighborhood comparison; M: mingling degree; C: crowding degree; CD: crown diameter; CV: crown volume.</p>
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<p>Establishment of the best-fitting SEM. * indicates a significance level of 0.05; *** indicates a significance level of 0.001. U: neighborhood comparison; C: crowding degree; W: uniform angle index; CD: crown diameter.</p>
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<p>The direct and indirect effects of the explanatory variables (tree density, tree species diversity, stand structural characteristics, and stand stability) on the response variable (carbon storage) in the best-fitting SEM. * and *** indicate significance levels of 0.05 and 0.001, respectively. The orange pillar represents the direct effects, while the blue pillar represents the indirect effects.</p>
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<p>Multiple regression analysis of tree density, stand structural characteristics, tree species diversity, stand stability, and carbon storage. * indicates a significance level of 0.05; *** indicates a significance level of 0.001. W: uniform angle index; U: neighborhood comparison; M: mingling degree; C: crowding degree; CD: crown diameter; CV: crown volume. (<b>a</b>) indicates the results of a multiple regression analysis on stand stability, and (<b>b</b>) indicates the results of a multiple regression analysis on carbon storage.</p>
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22 pages, 1979 KiB  
Review
Methods of Capture and Transformation of Carbon Dioxide (CO2) with Macrocycles
by Edilma Sanabria, Mauricio Maldonado, Carlos Matiz, Ana C. F. Ribeiro and Miguel A. Esteso
Processes 2025, 13(1), 117; https://doi.org/10.3390/pr13010117 - 4 Jan 2025
Viewed by 671
Abstract
Rapid industrialization and the indiscriminate use of fossil fuels have generated an impact that is affecting the climate worldwide. Among the substances that are causing climate change are several gases such as carbon dioxide (CO2), methane (CH4), nitrous oxide [...] Read more.
Rapid industrialization and the indiscriminate use of fossil fuels have generated an impact that is affecting the climate worldwide. Among the substances that are causing climate change are several gases such as carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O) and sulphur hexafluoride (SF6), among others. Particularly, carbon dioxide is one of the substances that has attracted the most attention from researchers, as it is responsible for more than three quarters of greenhouse gases. Because of this, many efforts have been directed towards the capture of CO2, its separation, adsorption and transformation into products that are less harmful to the environment or that even have added value in the industry. For this purpose, the use of different types of macrocycles has been explored mainly in the last 5 years. This review seeks to present the advances that have occurred in recent years in the capture and transformation of CO2 by different methods, to finally focus on the capture and transformation through macrocycle systems such as azacompounds, heterometallic macrocycles, calixpyrrols, modified cyclodextrins and metallic porphyrins, among others. Full article
(This article belongs to the Section Environmental and Green Processes)
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<p>Forms of representations of the CO<sub>2</sub> molecule.</p>
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<p>Main methods of capturing and transforming carbon dioxide.</p>
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<p>Some macrocyclic systems used in carbon dioxide fixation.</p>
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<p>Alpha-, beta- and gamma-cyclodextrins.</p>
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<p>Structure of porphyrins and metalloporphyrins.</p>
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<p>Participation of metallo-porphyrins in CO<sub>2</sub> transformation.</p>
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<p>Structure of calixarenes, resorcinarenes and pyrogallolarenes.</p>
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<p>Participation of calixarene-type systems in CO<sub>2</sub> transformation.</p>
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<p>Synthesis gas and Fisher–Tropsch process.</p>
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25 pages, 27385 KiB  
Article
Response of Natural Forests and Grasslands in Xinjiang to Climate Change Based on Sun-Induced Chlorophyll Fluorescence
by Jinrun He, Jinglong Fan, Zhentao Lv and Shengyu Li
Remote Sens. 2025, 17(1), 152; https://doi.org/10.3390/rs17010152 - 4 Jan 2025
Viewed by 413
Abstract
In arid regions, climatic fluctuations significantly affect vegetation structure and function. Sun-induced chlorophyll fluorescence (SIF) can quantify certain physiological parameters of vegetation but has limitations in characterizing responses to climate change. This study analyzed the spatiotemporal differences in response to climate change across [...] Read more.
In arid regions, climatic fluctuations significantly affect vegetation structure and function. Sun-induced chlorophyll fluorescence (SIF) can quantify certain physiological parameters of vegetation but has limitations in characterizing responses to climate change. This study analyzed the spatiotemporal differences in response to climate change across various ecological regions and vegetation types from 2000 to 2020 in Xinjiang. According to China’s ecological zoning, R1 (Altai Mountains-Western Junggar Mountains forest-steppe) and R5 (Pamir-Kunlun Mountains-Altyn Tagh high-altitude desert grasslands) represent two ecological extremes, while R2–R4 span desert and forest-steppe ecosystems. We employed the standardized precipitation evapotranspiration index (SPEI) at different timescales to represent drought intensity and frequency in conjunction with global OCO-2 SIF products (GOSIF) and the normalized difference vegetation index (NDVI) to assess vegetation growth conditions. The results show that (1) between 2000 and 2020, the overall drought severity in Xinjiang exhibited a slight deterioration, particularly in northern regions (R1 and R2), with a gradual transition from short-term to long-term drought conditions. The R4 and R5 ecological regions in southern Xinjiang also displayed a slight deterioration trend; however, R5 remained relatively stable on the SPEI24 timescale. (2) The NDVI and SIF values across Xinjiang exhibited an upward trend. However, in densely vegetated areas (R1–R3), both NDVI and SIF declined, with a more pronounced decrease in SIF observed in natural forests. (3) Vegetation in northern Xinjiang showed a significantly stronger response to climate change than that in southern Xinjiang, with physiological parameters (SIF) being more sensitive than structural parameters (NDVI). The R1, R2, and R3 ecological regions were primarily influenced by long-term climate change, whereas the R4 and R5 regions were more affected by short-term climate change. Natural grasslands showed a significantly stronger response than forests, particularly in areas with lower vegetation cover that are more structurally impacted. This study provides an important scientific basis for ecological management and climate adaptation in Xinjiang, emphasizing the need for differentiated strategies across ecological regions to support sustainable development. Full article
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Figure 1
<p>Study area of the Xinjiang arid region in northwest China (Vegetation is classified as follows: Forest (red), high coverage grassland (HCG, &gt;50%, dark green), moderate coverage grassland (MCG, 20–50%, medium green), and low coverage grassland (LCG, 5–20%, light green). The ecological regions (R1–R5) are delineated with different hatching patterns, and meteorological stations are marked with red dots. The map was created using the standard map approved by the Ministry of Natural Resources of China (review number GS (2024) 0650). The base map provided by the Ministry of Natural Resources was used without any modifications. Similarly, all other maps in this study were created using standardized methods and remain unaltered.</p>
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<p>Technical roadmap for research of vegetation responses to climate change.</p>
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<p>Temporal variation of SPEI in Xinjiang from 2000 to 2020 (<b>a</b>) Temporal variation of SPEI at a 3-month timescale (SPEI-03). (<b>b</b>) Temporal variation of SPEI at a 6-month timescale (SPEI-06). (<b>c</b>) Temporal variation of SPEI at a 12-month timescale (SPEI-12). (<b>d</b>) Temporal variation of SPEI at a 24-month timescale (SPEI-24). Each panel shows the SPEI data series (blue) and trend line (red). Statistical values, including Z-score, <span class="html-italic">p</span>-value, and slope, are provided for each timescale to indicate the trend significance and direction.</p>
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<p>Spatial distribution of multi-year average SPEI in Xinjiang from 2000 to 2020 across different timescales. (<b>a</b>) Spatial distribution of SPEI at a 3-month timescale (SPEI-03). (<b>b</b>) Spatial distribution of SPEI at a 6-month timescale (SPEI-06). (<b>c</b>) Spatial distribution of SPEI at a 12-month timescale (SPEI-12). (<b>d</b>) Spatial distribution of SPEI at a 24-month timescale (SPEI-24). Red areas indicate drier conditions, whereas blue areas represent wetter conditions.</p>
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<p>Inter-annual variation analysis of vegetation NDVI and SIF. (<b>a</b>) Annual mean NDVI with trend line and confidence interval. The trend line (red) represents the linear trend, with the equation y = 0.0012x + 0.1276y = 0.0012x + 0.1276y = 0.0012x + 0.1276 and a correlation coefficient of 0.8929. (<b>b</b>) Annual mean SIF with trend line and confidence interval. The trend line (red) shows the linear trend, with the equation y = 0.0005x + 0.0741y = 0.0005x + 0.0741y = 0.0005x + 0.0741 and a correlation coefficient of 0.7521. Blue triangles represent observed data, and the shaded area indicates the confidence interval around the trend line.</p>
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<p>Spatial distribution of mean NDVI and SIF in Xinjiang from 2000 to 2020. (<b>a</b>) Spatial distribution of mean NDVI, representing vegetation structural conditions across Xinjiang. The color bar indicates NDVI values, with yellow to dark green representing increasing vegetation coverage from 0.0 to 1.0. (<b>b</b>) Spatial distribution of mean SIF, indicating vegetation physiological activity levels. The color bar reflects SIF values, ranging from 0.00 to 0.20 W·m<sup>−</sup><sup>2</sup>·μm<sup>−</sup><sup>1</sup>·sr<sup>−</sup><sup>1</sup>, with dark green areas showing higher fluorescence.</p>
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<p>Spatial distribution of correlation coefficients for NDVI and SIF from 2000 to 2020 in Xinjiang. (<b>a</b>) Spatial distribution of the correlation coefficient between NDVI and SPEI across pixels over the study period. (<b>b</b>) Spatial distribution of the correlation coefficient between SIF and SPEI across pixels over the study period. The color scale represents correlation values from −1 to 1, where blue areas indicate a strong positive correlation and red areas indicate a strong negative correlation. The inset bar chart shows the proportion of pixels with positive and negative correlation trends.</p>
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<p>Spatial distribution and changes in vegetation types from 2000 to 2020 in Xinjiang. (<b>a</b>) Spatial distribution of vegetation types, including forest, high-coverage grassland (HCG), moderate-coverage grassland (MCG), and low-coverage grassland (LCG). (<b>b</b>) Spatial distribution of vegetation change over the study period, identifying common, increased, and decreased areas. The bar chart inserted shows the percentage of each type.</p>
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<p>Trends in NDVI and SIF for grassland and forested areas (2000–2020). For forest areas, NDVI shows a statistically significant increasing trend (y = 0.0017x + 0.5584, Corr. = 0.569), whereas SIF displays a slight decreasing trend (y = −0.0004x + 0.1943, Corr. = −0.2389). For grassland areas, NDVI exhibits a positive trend (y = 0.0017x + 0.194, Corr. = 0.8019), with a minimal increase in SIF (y = 0.0001x + 0.0779, Corr. = 0.0712). The shaded regions indicate the confidence intervals for each regression line.</p>
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<p>Spatial distribution of maximum correlation coefficients (R<sub>max</sub>) between vegetation indices and SPEI in Xinjiang. (<b>a</b>) The spatial distribution of the maximum correlation coefficients (R<sub>max</sub>) between NDVI and SPEI across Xinjiang, with values ranging from −0.372 to 0.745, indicating varying vegetation responses to climatic changes in different ecological regions. (<b>b</b>) The spatial distribution of the maximum correlation coefficients (R<sub>max</sub>) between SIF and SPEI, with values from −0.8 to 0.9. This figure highlights the spatial variation in vegetation sensitivity to drought stress across different regions.</p>
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<p>Maximum correlation coefficients between vegetation indices and SPEI. Box plots depict the distribution of maximum correlation coefficients (R<sub>max</sub>) between NDVI and SIF with SPEI, separated by ecological regions (R1–R5) and vegetation types (Forest, HCG, MCG, and LCG). (<b>a</b>) shows NDVI correlations across ecological regions, whereas (<b>b</b>) displays SIF correlations. (<b>c</b>,<b>d</b>) present NDVI and SIF correlations, respectively, by vegetation type.</p>
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<p>Spatial distribution of the SPEI time scales corresponding to the maximum correlation coefficients between vegetation conditions represented by NDVI (<b>a</b>) and SIF (<b>b</b>) and SPEI. (<b>a</b>) NDVI and (<b>b</b>) SIF are shown with SPEI03, SPEI06, SPEI12, and SPEI24, representing the dominant timescales of vegetation response to drought. This figure illustrates the temporal dynamics of vegetation response to drought stress.</p>
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<p>Area proportion of SPEI time scales corresponding to maximum correlation coefficients between vegetation indices and SPEI across different ecological regions and vegetation types. (<b>a</b>) displays NDVI correlations by region, whereas (<b>b</b>) shows SIF correlations by region. (<b>c</b>,<b>d</b>) present NDVI and SIF correlations, respectively, by vegetation type.</p>
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16 pages, 1401 KiB  
Article
Stock Dynamics of Female Red King Crab in a Small Bay of the Barents Sea in Relation to Environmental Factors
by Alexander G. Dvoretsky and Vladimir G. Dvoretsky
Animals 2025, 15(1), 99; https://doi.org/10.3390/ani15010099 - 4 Jan 2025
Viewed by 166
Abstract
Stock–recruitment relationships depend on the total abundance of females, their fecundity, and patterns of their maturation. However, the effects of climatic conditions on the abundance, biomass, and mean weight of female red king crabs, Paralithodes camtschaticus, from the introduced population (Barents Sea) [...] Read more.
Stock–recruitment relationships depend on the total abundance of females, their fecundity, and patterns of their maturation. However, the effects of climatic conditions on the abundance, biomass, and mean weight of female red king crabs, Paralithodes camtschaticus, from the introduced population (Barents Sea) have not yet been studied. For this reason, we analyzed long-term fluctuations in stock indices and the average weight of an individual crab in a small bay of the Barents Sea and related these parameters to the dynamics of temperature conditions (temperature in January–December, mean yearly temperature, and temperature anomaly) in the sea. The average weight of a crab at age 6–9 had strong negative correlations with water temperature at lags 8 and 9, indicating faster female maturation in warm periods. Positive relationships were registered between temperature and stock indices for 15–19-year-old females at lag 4 and for 10–14-year-old females at lag 10, supporting the idea of higher survival rates of juveniles and their rapid development being a response to a pool of warm waters. Both redundancy and correlation analyses revealed seawater temperatures in June–August being the most important predictors of female abundance and biomass, indicating that favorable temperature conditions in the first 3 months of crab benthic life result in high survivorship rates for red king crabs. Full article
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<p>Near-bottom temperature fluctuations in the coastal zone of the Barents Sea (stations 1–3 of the Kola section at 50–200 m depth) in 1984–2017.</p>
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<p>Variations in female red king crab stock indices and mean weight over 2003–2017. Ab—abundance (thousand crabs), Bm—biomass (metric tons), W—weight (kg). 1—aged 6–9 years, 2—aged 10–14 years, 3—aged 15–19 years.</p>
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<p>Redundancy analysis ordination plots showing female red king crab characteristics in relation to temperature variables in Dalnezelenetskaya Bay at lag 4 (<b>a</b>), lag 8 (<b>b</b>), lag 9 (<b>c</b>), and lag 10 (<b>d</b>). T1–T12—water temperature at stations 1–3 of the Kola section at 50–200 m depth in January–December, T—averaged year water temperature, Ta—temperature anomaly. Crab indices: Bm—biomass, W—weight. Age groups: 1—aged 6–9, 2—aged 10–14, 3—aged 15–19.</p>
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