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Search Results (1,303)

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16 pages, 3338 KiB  
Article
Mixing Data Cube Architecture and Geo-Object-Oriented Time Series Segmentation for Mapping Heterogeneous Landscapes
by Michel E. D. Chaves, Lívia G. D. Soares, Gustavo H. V. Barros, Ana Letícia F. Pessoa, Ronaldo O. Elias, Ana Claudia Golzio, Katyanne V. Conceição and Flávio J. O. Morais
AgriEngineering 2025, 7(1), 19; https://doi.org/10.3390/agriengineering7010019 - 17 Jan 2025
Abstract
The conflict between environmental conservation and agricultural production highlights the need for precise land use and land cover (LULC) mapping to support agro-environmental-related policies. Satellite image time series from the Moderate Resolution Image Spectroradiometer (MODIS) sensor are essential for current LULC mapping efforts. [...] Read more.
The conflict between environmental conservation and agricultural production highlights the need for precise land use and land cover (LULC) mapping to support agro-environmental-related policies. Satellite image time series from the Moderate Resolution Image Spectroradiometer (MODIS) sensor are essential for current LULC mapping efforts. However, most approaches focus on pixel data, and studies exploring object-based spatiotemporal heterogeneity and correlation features in its time series are limited. The objective of this study is to mix the data cube architecture (analysis-ready data—ARD) and the geo-object-oriented time series segmentation via Geographic Object-Based Image Analysis (GEOBIA) to assess its performance in identifying natural vegetation and double-cropping practices over a crop season. The study area was the state of Mato Grosso, Brazil. Results indicate that, by combining GEOBIA and time series analysis (materialized by the multiresolution segmentation algorithm to derive spatiotemporal geo-objects of the MODIS data cube), representative training data collected after a quality control process, and the Support Vector Machine to classify the ARD, the overall accuracy was 0.95 and all users’ and producers’ accuracies were higher than 0.88. By considering the heterogeneity of Mato Grosso’s landscape, the results indicate the potential of the approach to provide accurate mapping. Full article
19 pages, 8430 KiB  
Article
Spatiotemporal Variation of Water Use Efficiency and Its Responses to Climate Change in the Yellow River Basin from 1982 to 2018
by Jie Li, Fen Qin, Yingping Wang, Xiuyan Zhao, Mengxiao Yu, Songjia Chen, Jun Jiang, Linhua Wang and Junhua Yan
Remote Sens. 2025, 17(2), 316; https://doi.org/10.3390/rs17020316 - 17 Jan 2025
Viewed by 167
Abstract
The ecosystem water use efficiency (WUE) plays a critical role in many aspects of the global carbon cycle, water management, and ecological services. However, the response mechanisms and driving processes of WUE need to be further studied. This research was conducted based on [...] Read more.
The ecosystem water use efficiency (WUE) plays a critical role in many aspects of the global carbon cycle, water management, and ecological services. However, the response mechanisms and driving processes of WUE need to be further studied. This research was conducted based on Gross Primary Productivity (GPP), Evapotranspiration (ET), meteorological station data, and land use/cover data, and the methods of Ensemble Empirical Mode Decomposition (EEMD), trend variation analysis, the Mann–Kendall Significant Test (M-K test), and Partial Correlation Analysis (PCA) methods. Our study revealed the spatio-temporal trend of WUE and its influencing mechanism in the Yellow River Basin (YRB) and compared the differences in WUE change before and after the implementation of the Returned Farmland to Forestry and Grassland Project in 2000. The results show that (1) the WUE of the YRB showed a significant increase trend at a rate of 0.56 × 10−2 gC·kg−1·H2O·a−1 (p < 0.05) from 1982 to 2018. The area showing a significant increase in WUE (47.07%, Slope > 0, p < 0.05) was higher than the area with a significant decrease (14.64%, Slope < 0, p < 0.05). The region of significant increase in WUE in 2000–2018 (45.35%, Slope > 0, p < 0.05) was higher than that of 1982–2000 (8.23%, Slope > 0, p < 0.05), which was 37.12% higher in comparison. (2) Forest WUE (1.267 gC·kg−1·H2O) > Cropland WUE (0.972 gC·kg−1·H2O) > Grassland WUE (0.805 gC·kg−1·H2O) under different land cover types. Forest ecosystem WUE has the highest rate of increase (0.79 × 10−2 gC·kg−1·H2O·a−1) from 2000 to 2018. Forest ecosystem WUE increased by 0.082 gC·kg−1·H2O after 2000. (3) precipitation (37.98%, R > 0, p < 0.05) and SM (10.30%, R > 0, p < 0.05) are the main climatic factors affecting WUE in the YRB. A total of 70.39% of the WUE exhibited an increasing trend, which is mainly attributed to the simultaneous increase in GPP and ET, and the rate of increasing GPP is higher than the rate of increasing ET. This study could provide a scientific reference for policy decision-making on the terrestrial carbon cycle and biodiversity conservation. Full article
(This article belongs to the Special Issue Remote Sensing for Terrestrial Hydrologic Variables)
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<p>Study area, vegetation type, basin boundary, and elevation.</p>
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<p>Temporal trends of WUE in 1982–2018. (<b>a</b>) Annual; (<b>b</b>) Grow.</p>
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<p>Spatial variation characteristics of WUE in the YRB. (<b>a</b>) Annual WUE in 1982–2018; (<b>b</b>) Annual WUE in 1982–2000; (<b>c</b>) Annual WUE in 2000–2018; (<b>d</b>) Grow WUE in 1982–2018; (<b>e</b>) Annual WUE in 1982–2000; (<b>f</b>) Annual WUE in 2000–2018.</p>
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<p>Spatial characteristics of significant variation trend of the WUE in different time periods.</p>
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<p>Variation in WUE in different land cover types.</p>
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<p>The trends of WUE for different ecosystem types in the YRB. (<b>a</b>) Farmland; (<b>b</b>) Forest; (<b>c</b>) Grassland; (<b>d</b>) Other.</p>
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<p>Spatial distribution of partial correlation coefficient between WUE and climate factors in the YRB from 1982 to 2018. (<b>a</b>) WUE and temperature; (<b>b</b>) WUE and precipitation; (<b>c</b>) WUE and vapor pressure deficit; (<b>d</b>) WUE and soil moisture.</p>
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<p>Spatial distribution of partial correlation coefficient between WUE and climate factors in the YRB from 1982 to 2018 (significance test <span class="html-italic">p</span> &lt; 0.05). (<b>a</b>) WUE and temperature; (<b>b</b>) WUE and precipitation; (<b>c</b>) WUE and vapor pressure deficit; (<b>d</b>) WUE and soil moisture.</p>
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<p>WUE changes in response to GPP and ET across different time periods.</p>
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<p>WUE significant changes in response to GPP significant changes and ET significant changes across different time periods (significant test <span class="html-italic">p</span> &lt; 0.05).</p>
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14 pages, 2358 KiB  
Article
Evaluation of Energy Potential in a Landfill Through the Integration of a Biogas–Solar Photovoltaic System
by Héctor Alfredo López-Aguilar, Guadalupe Kennedy Puentes, Luis Armando Lozoya Márquez, Oscar Chávez Acosta, Humberto Alejandro Monreal Romero, Claudia López Meléndez and Antonino Pérez-Hernández
Urban Sci. 2025, 9(1), 17; https://doi.org/10.3390/urbansci9010017 - 14 Jan 2025
Viewed by 645
Abstract
The integration of biogas and photovoltaic solar energy systems in sanitary landfills represents a promising strategy for sustainable energy generation and efficient urban waste management. This study evaluates the potential for biogas and photovoltaic energy production in two cells of the Municipal Landfill [...] Read more.
The integration of biogas and photovoltaic solar energy systems in sanitary landfills represents a promising strategy for sustainable energy generation and efficient urban waste management. This study evaluates the potential for biogas and photovoltaic energy production in two cells of the Municipal Landfill of Chihuahua, Mexico. Using the LandGEM and MMB models (Landfill Gas Emission Model and the Mexican Biogas Model), biogas generation was estimated by considering the composition of the landfill gas and the characteristics of the cover in each cell, revealing notable differences due to their operational periods and waste deposition. Photovoltaic simulations, conducted with the HelioScope software 2020, evaluated spatial configurations and solar radiation data. The generation potential for 2025 was simulated using predictive models, yielding results between 25.48 and 26.08 MW for the biogas–photovoltaic system, depending on the orientation of the panels and the optimization of the coverage. The novelty of this work lies in the combined evaluation of biogas and photovoltaic potential within a single landfill site, integrating advanced modeling tools to optimize system design. By demonstrating the feasibility and benefits of this hybrid system, the study contributes to clean energy solutions, environmental mitigation, and improved waste management strategies. Our findings emphasize the importance of site-specific management practices and predictive modeling to enhance renewable energy production and reduce greenhouse gas emissions, supporting sustainable urban development initiatives. Full article
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<p>Metropolitan Landfill of Chihuahua (28°41′58.3″ N 106°02′16.0″ W) and biogas sampling points [own research].</p>
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<p>Projections of biogas (methane 50% in m<sup>3</sup>/h) generation (solid line) and recovery (dotted line) in Cell 1 of the Metropolitan Landfill calculated using the MMB [own research].</p>
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<p>Proposed system for the photovoltaic system in Cell 1 [own research].</p>
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<p>Projections of biogas (methane 50% in m<sup>3</sup>/h) generation (solid line) and recovery (dotted line) in Cell 2 of the Metropolitan Landfill calculated using the MMB [own research].</p>
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<p>Proposed system for the photovoltaic system in Cell 2 [own research].</p>
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19 pages, 3300 KiB  
Article
Impact of Spatial Evolution of Cropland Pattern on Cropland Suitability in Black Soil Region of Northeast China, 1990–2020
by Long Kang and Kening Wu
Agronomy 2025, 15(1), 172; https://doi.org/10.3390/agronomy15010172 - 12 Jan 2025
Viewed by 513
Abstract
Agricultural land resources are essential for food production, and thus it is vital to examine the spatiotemporal changes in these resources and their impacts on land suitability to optimize resource allocation. In this study, we investigated the spatial evolution of cropland resources through [...] Read more.
Agricultural land resources are essential for food production, and thus it is vital to examine the spatiotemporal changes in these resources and their impacts on land suitability to optimize resource allocation. In this study, we investigated the spatial evolution of cropland resources through land use change analysis by utilizing four periods of land use data from 1990 to 2020 in the black soil region of northeast China (BSRNC). Employing niche theory, we developed a cultivability evaluation model tailored to the BSRNC, which was used to assess the impact of the spatial changes in cropland patterns over the past 30 years on land suitability. Our key findings are as follows: (1) Cropland resources have generally tended to expand in the BSRNC, with an increase of 7.16 × 103 km2 in the cultivated area and a northeastward shift in the cropland center by 52.94 km, indicating significant changes in the spatial configuration of the land. (2) The region’s cultivable land resources were substantial, covering 694.06 × 103 km2, or 55.78% of the total area, with notable spatial variability, influenced by the regional climate and topography. (3) The land cultivability has slightly improved, as shown by a 0.10 increase in the cultivability index, but a significant declining trend in the cultivability of cropland was observed after 2000. Our findings provide valuable insights to help accurately assess land productivity in the BSRNC and facilitate the sustainable use and conservation of black soil. Full article
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<p>Location (<b>a</b>), administrative subdivisions (<b>b</b>), and soil types (<b>c</b>) in the black soil region of northeast China (BSRNC).</p>
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<p>Spatial changes in cropland gravity center.</p>
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<p>Hotspots for cropland change from 1990 to 2020.</p>
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<p>Spatial distribution of cultivable land in the BSRNC.</p>
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<p>Relationships between actual crop yields and simulated cultivability scores for different cities in the BSRNC.</p>
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<p>Suitability of cropland resources in the BSRNC (<b>a</b>) and changes in single-factor suitability (<b>b</b>).</p>
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<p>Cropland cultivation levels across years (<b>a</b>) and factors contributing to unsuitability for cultivation in the BSRNC (<b>b</b>).</p>
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<p>Spatial distribution of cropland reserves in the BSRNC (<b>a</b>) and coupling of reserves with current land use across various cultivability levels (<b>b</b>).</p>
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25 pages, 28841 KiB  
Article
Applying the Dempster–Shafer Fusion Theory to Combine Independent Land-Use Maps: A Case Study on the Mapping of Oil Palm Plantations in Sumatra, Indonesia
by Carl Bethuel, Damien Arvor, Thomas Corpetti, Julia Hélie, Adrià Descals, David Gaveau, Cécile Chéron-Bessou, Jérémie Gignoux and Samuel Corgne
Remote Sens. 2025, 17(2), 234; https://doi.org/10.3390/rs17020234 - 10 Jan 2025
Viewed by 452
Abstract
The remote sensing community benefits from new sensors and easier access to Earth Observation data to frequently released new land-cover maps. The propagation of such independent and heterogeneous products offers promising perspectives for various scientific domains and for the implementation and monitoring of [...] Read more.
The remote sensing community benefits from new sensors and easier access to Earth Observation data to frequently released new land-cover maps. The propagation of such independent and heterogeneous products offers promising perspectives for various scientific domains and for the implementation and monitoring of land-use policies. Yet, it may also confuse the end-users when it comes to identifying the most appropriate product to address their requirements. Data fusion methods can help to combine competing and/or complementary maps in order to capitalize on their strengths while overcoming their limitations. We assessed the potential of the Dempster–Shafer Theory (DST) to enhance oil palm mapping in Sumatra (Indonesia) by combining four land-cover maps, hereafter named DESCALS, IIASA, XU, and MAPBIOMAS, according to the first author’s name or the research group that published it. The application of DST relied on four steps: (1) a discernment framework, (2) the assignment of mass functions, (3) the DST fusion rule, and (4) the DST decision rule. Our results showed that the DST decision map achieved significantly higher accuracy (Kappa = 0.78) than the most accurate input product (Kappa = 0.724). The best result was reached by considering the probabilities of pixels to belong to the OP class associated with DESCALS map. In addition, the belief (i.e., confidence) and conflict (i.e., uncertainty) maps produced by DST evidenced that industrial plantations were detected with higher confidence than smallholder plantations. Consequently, Kappa values computed locally were lower in areas dominated by smallholder plantations. Combining land-use products with DST contributes to producing state-of-the-art maps and continuous information for enhanced land-cover analysis. Full article
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<p>Location of the study area, Sumatra island (Indonesia), and illustration of different types of oil palm plantations as seen from very-high-resolution remote sensing image (© Google Earth).</p>
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<p>Presentation of the reference (GAVEAU [<a href="#B44-remotesensing-17-00234" class="html-bibr">44</a>]) and input land-use maps at Sumatra-scale (<b>A</b>) and tile-scale, considering a tile dominated by industrial plantations (<b>B</b>) and a tile dominated by smallholder plantations (<b>C</b>).</p>
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<p>A flowchart of the methodology, including input sources, stages of DST fusion process, outputs, and validation approach.</p>
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<p>The discernment framework is composed of the empty set ∅, the oil palm class <math display="inline"><semantics> <msub> <mi>θ</mi> <mrow> <mi>O</mi> <mi>P</mi> </mrow> </msub> </semantics></math>, the no oil palm class <math display="inline"><semantics> <msub> <mi>θ</mi> <mrow> <mi>N</mi> <mi>O</mi> <mi>P</mi> </mrow> </msub> </semantics></math>, and the union of OP and NOP <math display="inline"><semantics> <mrow> <msub> <mi>θ</mi> <mrow> <mi>O</mi> <mi>P</mi> </mrow> </msub> <mo>∪</mo> <msub> <mi>θ</mi> <mrow> <mi>N</mi> <mi>O</mi> <mi>P</mi> </mrow> </msub> </mrow> </semantics></math>, representing the uncertainty.</p>
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<p>Mass functions assignment with an application to DESCALS map.</p>
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<p>The distribution of Kappa values at the tile scale for the <math display="inline"><semantics> <mrow> <mi>D</mi> <mi>S</mi> <msub> <mi>T</mi> <mrow> <mi>P</mi> <mi>r</mi> <mi>o</mi> <mi>b</mi> <msub> <mi>a</mi> <mi>D</mi> </msub> </mrow> </msub> </mrow> </semantics></math> fused map.</p>
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<p>Belief, conflict, and DST decision maps resulting from the application of the Dempster–Shafer theory at (<b>A</b>) the Sumatra scale and for two tiles characterized by the predominance of (<b>B</b>) industrial OP plantations and (<b>C</b>) smallholder OP plantations.</p>
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<p>Distribution of reference points according to their land-use class for (<b>A</b>) values of belief between input sources and (<b>B</b>) values of conflict in each hypothesis.</p>
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<p>The distribution of Kappa values according to the landscape composition metric (i.e., ratio between smallholder and industrial plantations) at tile-scale. Letters <span class="html-italic">a</span> and <span class="html-italic">b</span> produced by CLD method indicate statistically significant different distributions.</p>
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26 pages, 6157 KiB  
Article
Assessing the Impact of Climate Change on the Landscape Stability in the Mediterranean World Heritage Site Based on Multi-Sourced Remote Sensing Data: A Case Study of the Causses and Cévennes, France
by Mingzhuo Zhu, Daoye Zhu, Min Huang, Daohong Gong, Shun Li, Yu Xia, Hui Lin and Orhan Altan
Remote Sens. 2025, 17(2), 203; https://doi.org/10.3390/rs17020203 - 8 Jan 2025
Viewed by 405
Abstract
Global climate fluctuations pose challenges not only to natural environments but also to the conservation and transmission of human cultural and historical heritage. World Heritage Sites are pivotal regions for studying climate change impacts and devising adaptation strategies, with remote sensing technology showcasing [...] Read more.
Global climate fluctuations pose challenges not only to natural environments but also to the conservation and transmission of human cultural and historical heritage. World Heritage Sites are pivotal regions for studying climate change impacts and devising adaptation strategies, with remote sensing technology showcasing significant utility in monitoring these impacts, especially in the Mediterranean region’s diverse and sensitive climate context. Although existing work has begun to explore the role of remote sensing in monitoring the effects of climate change, detailed analysis of the spatial distribution and temporal trends of landscape stability remains limited. Leveraging remote sensing data and its derived products, this study assessed climate change impacts on the Causses and Cévennes Heritage Site, a typical Mediterranean heritage landscape. Specifically, this study utilized remote sensing data to analyze the trends in various climatic factors from 1985 to 2020. The landscape stability model was developed utilizing land cover information and landscape indicators to explore the landscape stability and its distribution features within the study area. Finally, we adopted the Geographical Detector to quantify the extent to which climatic factors influence the landscape stability’s spatial distribution across different periods. The results demonstrated that (1) the climate showed a warming and drying pattern during the study period, with distinct climate characteristics in different zones. (2) The dominance of woodland decreased (area proportion dropped from 76% to 66.5%); transitions primarily occurred among woodland, cropland, shrubland, and grasslands; landscape fragmentation intensified; and development towards diversification and uniformity was observed. (3) Significant spatiotemporal differences in landscape stability within the heritage site were noted, with an overall downward trend. (4) Precipitation had a high contribution rate in factor detection, with the interactive enhancement effects between temperature and precipitation being the most prominent. The present study delivers a thorough examination of how climate change affects the Causses and Cévennes Heritage Landscape, reveals its vulnerabilities, and offers crucial information for sustainable conservation efforts. Moreover, the results offer guidance for the preservation of similar Mediterranean heritage sites and contribute to the advancement and deepening of global heritage conservation initiatives. Full article
(This article belongs to the Section Environmental Remote Sensing)
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<p>Location (<b>a</b>), topography (<b>b</b>), and climatic zones (<b>c</b>) of the Causses and Cévennes World Heritage Site (Cf: temperate oceanic; Cs: Mediterranean; Df: temperate continental).</p>
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<p>Research framework.</p>
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<p>The annual cycle of temperature and precipitation in the heritage site (1985–2020).</p>
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<p>Temporal dynamics of climate factors in the heritage site from 1985 to 2020; (<b>a</b>) temperature, (<b>b</b>) precipitation, (<b>c</b>) potential evaporation, and (<b>d</b>) relative humidity.</p>
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<p>Spatial distribution of landscape types across different time periods in the Causses and Cévennes World Heritage Site; (<b>a</b>) 1985, (<b>b</b>) 2010, and (<b>c</b>) 2020.</p>
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<p>Landscape-type transition trajectory map of the heritage site, 1985–2020 (in km<sup>2</sup>).</p>
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<p>Spatial distribution of landscape-type transitions in the heritage site; (<b>a</b>) 1985–2010 and (<b>b</b>) 2010–2020.</p>
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<p>Changes in landscape indices.</p>
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<p>Spatial distribution of landscape stability in the heritage site from 1985 to 2020; (<b>a</b>) 1985, (<b>b</b>) 2010, and (<b>c</b>) 2020.</p>
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<p>Spatial dynamics of landscape stability from 1985 to 2020; (<b>a</b>) 1985–2010, (<b>b</b>) 2010–2020, and (<b>c</b>) 1985–2020.</p>
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<p>Contribution of climatic factors to the spatial divergence of landscape stability in the heritage site. (TMP, temperature; PRE, precipitation; RH, relative humidity; PET, potential evaporation).</p>
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<p>Climate trends and sub-regional variations in the heritage site (1985–2020); (<b>a</b>) temperature, (<b>b</b>) precipitation, (<b>c</b>) potential evaporation, (<b>d</b>) relative humidity.</p>
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18 pages, 7044 KiB  
Article
Assessing Dominant Production Systems in the Eastern Amazon Forest
by Lívia Caroline César Dias, Neil Damas de Oliveira-Junior, Juliana Santos da Mota, Erison Carlos dos Santos Monteiro, Silvana Amaral, André Luis Regolin, Naíssa Batista da Luz, Luciana Soler and Cláudio Aparecido de Almeida
Forests 2025, 16(1), 89; https://doi.org/10.3390/f16010089 - 8 Jan 2025
Viewed by 394
Abstract
The expansion of agricultural frontiers in the Amazon region poses a significant threat to forest conservation and biodiversity persistence. This study focuses on Pará state, Brazil, aiming to identify and characterize the predominant production systems by combining remote sensing data and landscape structure [...] Read more.
The expansion of agricultural frontiers in the Amazon region poses a significant threat to forest conservation and biodiversity persistence. This study focuses on Pará state, Brazil, aiming to identify and characterize the predominant production systems by combining remote sensing data and landscape structure metrics. A rule-based classification tree algorithm is applied to classify hexagonal cells based on land cover, deforestation patterns, and distance from dairy facilities. The results reveal three dominant production systems: Natural Region, Non-Intensive Beef, and Initial Front, with livestock production being prominent. The analysis indicates that there is a correlation between the productive area and deforestation, emphasizing the role of agriculture as a driver of forest loss. Moreover, road networks significantly influence production system spatial distribution, highlighting the importance of infrastructure in land use dynamics. The Shannon diversity index reveals that areas with production systems exhibit greater diversity in land use and land cover classes, reflecting a wider range of modifications. In contrast, natural vegetation areas show lower Shannon values, suggesting that these areas are more intact and are less affected by human activities. These findings underscore the urgent need for sustainable development policies that will mitigate threats to forest resilience and biodiversity in Pará state. Full article
(This article belongs to the Special Issue Monitoring Forest Change Dynamic with Remote Sensing)
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<p>Location map of the state of Pará, highlighting its position in Brazil and the predominance of the Amazon biome, and the road network overlaid on the state’s boundaries.</p>
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<p>Rule-based tree illustrating data classification based on deforestation, percentage cover of agriculture, pasture, silviculture, and secondary vegetation and dairy location information. The diagram categorizes areas into various production systems, including Natural, Agricultural, cattle raising, Silviculture, and Mixed-Economy systems, with further subdivisions such as Natural Region, Initial Front, Strict Agriculture, and different types of Intensified and Non-intensified production zones. The color scheme in the diagram applies to the subdomains and is as follows: NR (Green), IF (Light green), SA (Cyan), DA (Orange), CA (Light pink), IBM (Violet), IB (Dark red), NIBM (Blue), NIB (Olive green), TPZ (Gray), MTPZ (Light brown), SDA (Yellow) and MER (Light purple). Descriptions of each subdomain are provided in <a href="#sec2dot2-forests-16-00089" class="html-sec">Section 2.2</a> above. The colors were selected to enhance the clarity of the thematic map, enabling easy differentiation of the subdomains.</p>
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<p>Map illustrating the spatial distribution of agricultural production systems in Pará, categorizing the state into distinct systems such as Natural Region, Initial Front, Strict Agriculture, and various types of cattle raising, Silviculture, and Mixed-Economy zones. The map reflects the complexity and diversity of land use within the state, providing a comprehensive overview of production distribution.</p>
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<p>Bar chart representing the percentage occupied by each agricultural production system in Pará, corresponding to the systems illustrated on the map. The colors in the chart match those in the map, indicating the distribution of Natural Region (NR), Non-intensified Beef (NIB), Initial Front (IF), Small Diversified Agriculture (SDA), Intensified Beef (IB), Coexistence Agriculture (CA), Mixed Economy Region (MER), Non-intensified Beef + Milk (NIBM), Dominance Agriculture (DA), Intensified Beef + Milk (IBM), Mixed Tree Plantation Zone (MTPZ), Tree Plantation Zone (TPZ), and Strict Agriculture (SA).</p>
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<p>Scatter plot showing the positive correlation between productive area and deforestation in km. The linear regression line (red) indicates that as the productive area increases, deforestation rates also rise (<span class="html-italic">r</span> = 1, <span class="html-italic">p</span> &lt; 2 × 10<sup>−16</sup>, R<sup>2</sup> = 0.99). This result suggests that regions with larger productive areas are associated with higher levels of deforestation, supporting the notion that agricultural expansion often leads to significant environmental degradation.</p>
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<p>Map of Pará State illustrating the Shannon Diversity Index of Land Use and Land Cover (LULC) classes for each hexagon, overlaid with the classification of agricultural production systems. The index values range from low diversity (blue) to high diversity (red). Higher Shannon Diversity Index values, indicated by warmer colors (yellow to red), are often found in regions associated with more complex agricultural systems, such as Coexistence Agriculture and Mixed-Economy Regions. Conversely, areas dominated by a single production system, like Intensive Beef or Tree Plantation Zones, tend to exhibit lower diversity (blue areas). This spatial relationship highlights how agricultural practices influence the heterogeneity of land use across the state.</p>
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<p>Bar chart showing the average Shannon diversity index values for different production system classes in Pará. The chart highlights that production systems such as DA (Dominant Agriculture), CA (Coexistence Agriculture), and NIBM (Non-Intensive Beef and Milk) exhibit higher average diversity values, indicating more heterogeneous landscapes. In contrast, natural vegetation systems, such as NR (Natural Region) and IF (Initial Front), have lower diversity values, reflecting more homogeneous land cover. The colors in the chart match those in the classification map (<a href="#forests-16-00089-f003" class="html-fig">Figure 3</a>), indicating the Production Systems.</p>
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<p>Classification of production systems by domain, subdomain, and description: This chart categorizes different production systems into the following categories: Natural Domain, Agriculture Subdomain, cattle raising Subdomain, Tree Plantation Subdomain, and Mixed-Economy Subdomain. Each system is described based on the percentage of production activity and specific criteria related to deforestation polygons, agriculture, and vegetation cover.</p>
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30 pages, 60239 KiB  
Article
Retrieval and Evaluation of Global Surface Albedo Based on AVHRR GAC Data of the Last 40 Years
by Shaopeng Li, Xiongxin Xiao, Christoph Neuhaus and Stefan Wunderle
Remote Sens. 2025, 17(1), 117; https://doi.org/10.3390/rs17010117 - 1 Jan 2025
Viewed by 552
Abstract
In this study, the global land surface albedo namely GAC43 was retrieved for the years 1979 to 2020 using Advanced Very High Resolution Radiometer (AVHRR) global area coverage (GAC) data onboard National Oceanic and Atmospheric Administration (NOAA) and Meteorological Operational (MetOp) satellites. We [...] Read more.
In this study, the global land surface albedo namely GAC43 was retrieved for the years 1979 to 2020 using Advanced Very High Resolution Radiometer (AVHRR) global area coverage (GAC) data onboard National Oceanic and Atmospheric Administration (NOAA) and Meteorological Operational (MetOp) satellites. We provide a comprehensive retrieval process of the GAC43 albedo, followed by a comprehensive assessment against in situ measurements and three widely used satellite-based albedo products, the third edition of the CM SAF cLoud, Albedo and surface RAdiation (CLARA-A3), the Copernicus Climate Change Service (C3S) albedo product, and MODIS BRDF/albedo product (MCD43). Our quantitative evaluations indicate that GAC43 demonstrates the best stability, with a linear trend of ±0.002 per decade at nearly all pseudo invariant calibration sites (PICS) from 1982 to 2020. In contrast, CLARA-A3 exhibits significant noise before the 2000s due to the limited availability of observations, while C3S shows substantial biases during the same period due to imperfect sensors intercalibrations. Extensive validation at globally distributed homogeneous sites shows that GAC43 has comparable accuracy to C3S, with an overall RMSE of approximately 0.03, but a smaller positive bias of 0.012. Comparatively, MCD43C3 shows the lowest RMSE (~0.023) and minimal bias, while CLARA-A3 displays the highest RMSE (~0.042) and bias (0.02). Furthermore, GAC43, CLARA-A3, and C3S exhibit overestimation in forests, with positive biases exceeding 0.023 and RMSEs of at least 0.028. In contrast, MCD43C3 shows negligible bias and a smaller RMSE of 0.015. For grasslands and shrublands, GAC43 and MCD43C3 demonstrate comparable estimation uncertainties of approximately 0.023, with close positive biases near 0.09, whereas C3S and CLARA-A3 exhibit higher RMSEs and biases exceeding 0.032 and 0.022, respectively. All four albedo products show significant RMSEs around 0.035 over croplands but achieve the highest estimation accuracy better than 0.020 over deserts. It is worth noting that significant biases are typically attributed to insufficient spatial representativeness of the measurement sites. Globally, GAC43 and C3S exhibit similar spatial distribution patterns across most land surface conditions, including an overestimation compared to MCD43C3 and an underestimation compared to CLARA-A3 in forested areas. In addition, GAC43, C3S, and CLARA-A3 estimate higher albedo values than MCD43C3 in low-vegetation regions, such as croplands, grasslands, savannas, and woody savannas. Besides the fact that the new GAC43 product shows the best stability covering the last 40 years, one has to consider the higher proportion of backup inversions before 2000. Overall, GAC43 offers a promising long-term and consistent albedo with good accuracy for future studies such as global climate change, energy balance, and land management policy. Full article
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<p>Local solar times and solar zenith angles of equator observations for all AVHRR-carrying NOAA and MetOp satellites used to generate GAC43 albedo products as shown in (<b>a</b>,<b>b</b>), respectively. SZA &gt; 90° indicates night conditions.</p>
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<p>Globally distributed sites with homogeneous characteristics and corresponding land cover types defined by the IGBP from the MCD12C1 product. Purple squares located in the desert are used to evaluate temporal stability, while other sites are utilized for direct validations.</p>
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<p>Flowchart for this study.</p>
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<p>The performance of full inversion and full and backup inversion at various IGBP land cover types.</p>
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<p>The performance of the GAC43 albedo with full inversions at various land cover types, where panels (<b>a</b>–<b>h</b>) represent the land cover types of BSV, CRO, DBF, EBF, ENF, GRA, OSH and WSA, respectively. In the plots, the red solid line represents the 1:1 line, and the green dotted line and purple solid lines represent the limits of deviation ±0.02 and ±0.04, respectively.</p>
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<p>Google Earth <sup>TM</sup> images were used to visually illustrate the heterogeneity surrounding selected homogeneous sites representing various land cover types: (<b>a</b>) EBF, (<b>b</b>) BSV, (<b>c</b>) CRO and (<b>d</b>) GRA, as defined by the MCD12C1 IGBP classification. The red circle in each image denotes a radius of 2.5 km.</p>
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<p>Inter-comparison performance among four satellite-based albedo products. The top four subfigures (<b>a</b>–<b>d</b>) show the accuracy of all available matching samples between in situ measurements and estimated albedo values derived from satellite products, while the bottom four subfigures (<b>e</b>–<b>h</b>) give the performance of that using same samples.</p>
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<p>The performance of four satellite-based albedo products using same samples across various land surface types, evaluated in terms of (<b>a</b>) RMSE and (<b>b</b>) bias, respectively. The <span class="html-italic">x</span>-axis represents the land cover type classified as forest, grassland or shrublands, cropland, and desert, and corresponding available samples.</p>
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<p>The temporal performance of four satellite-based albedo products related to in situ measurements, and each subplot represents one case of different land cover surface, including (<b>a</b>) EBF, (<b>b</b>) ENF, (<b>c</b>) DBF, (<b>d</b>) GRA, and (<b>e</b>) CRO, respectively. The grey shaded areas depict situations with snow cover.</p>
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<p>Spatial distributions of GAC43 BSA in July 2013 are shown in subgraph (<b>a</b>), with corresponding differences from (<b>b</b>) CLARA-A3, (<b>c</b>) C3S, and (<b>d</b>) MCD43C3 in the same month, respectively.</p>
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<p>Percentage difference in BSA values between (<b>a</b>) GAC43 and CLARA-A3, (<b>b</b>) GAC43 and C3S, and (<b>c</b>) GAC43 and MCD43C3 in July 2013.</p>
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<p>The scattering plots between GAC43 BSA and (<b>a</b>) CLARA-A3 BSA, (<b>b</b>) C3S BSA, and (<b>c</b>) MCD43C3 BSA using all snow-free monthly pixels in July 2013, where the red lines indicate 1:1.</p>
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<p>The monthly BSA for the four satellite-based products across various land cover types in July 2013, where panels (<b>a</b>–<b>i</b>) represent the land cover types of CRO, DBF, DNF, EBF, ENF, GRA, MF, SAV and WSA, respectively. In the plots, the bottom values of each albedo product are the median of all corresponding land cover estimates. The top values match available samples.</p>
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<p>Monthly BSA from GAC43, MCD43C3, C3S, and CALRA-A3 at three randomly selected PICS sites: (<b>a</b>) Arabia 2, 20.19°N, 51.63°E; (<b>b</b>) Libya 3, 23.22°N, 23.23°E; and (<b>c</b>) Sudan 1, 22.11°N, 28.11°E, all characterized by BSV land surfaces as defined by IGBP.</p>
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<p>Box plots of the slope per decade for GAC43, CLARA-A3, C3S, and MCD43C3 at all PICS sites, where (<b>a</b>–<b>d</b>) represent the corresponding statistics during 1982–1990, 1991–2000, 2001–2010 and 2011–2020, respectively, and three dashed grey lines represent the 75%, 50%, and 25% quantiles. Red dotted lines indicate the horizontal line where slope is 0.</p>
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<p>Percentage of full inversions for the years 2004, 2008, 2012, and 2016 based on GAC43 (<b>top</b>) and MCD43A3 (<b>bottom</b>).</p>
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<p>Percentage of full inversions of GAC43 at various continents from 1979 to 2020.</p>
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<p>Spatial distributions of GAC43 BSA in July 2004 are shown in subgraph (<b>a</b>), with corresponding differences from (<b>b</b>) CLARA-A3, (<b>c</b>) C3S, and (<b>d</b>) MCD43C3 in the same month, respectively.</p>
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<p>Spatial distributions of GAC43 BSA in July 2008 are shown in subgraph (<b>a</b>), with corresponding differences from (<b>b</b>) CLARA-A3, (<b>c</b>) C3S, and (<b>d</b>) MCD43C3 in the same month, respectively.</p>
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<p>Spatial distributions of GAC43 BSA in July 2012 are shown in subgraph (<b>a</b>), with corresponding differences from (<b>b</b>) CLARA-A3, (<b>c</b>) C3S, and (<b>d</b>) MCD43C3 in the same month, respectively.</p>
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<p>Spatial distributions of GAC43 BSA in July 2016 are shown in subgraph (<b>a</b>), with corresponding differences from (<b>b</b>) CLARA-A3, (<b>c</b>) C3S, and (<b>d</b>) MCD43C3 in the same month, respectively.</p>
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<p>Percentages of full inversions for the years between 1979 and 2020 based on GAC43 data record.</p>
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18 pages, 5858 KiB  
Article
Automatic Multi-Temporal Land Cover Mapping with Medium Spatial Resolution Using the Model Migration Method
by Ruijun Chen, Xidong Chen and Yu Ren
Remote Sens. 2025, 17(1), 37; https://doi.org/10.3390/rs17010037 - 26 Dec 2024
Viewed by 391
Abstract
Accurate land cover mapping plays a critical role in enhancing our understanding of Earth’s energy balance, carbon cycle, and ecosystem dynamics. However, existing methods for producing multi-epoch land cover products still heavily depend on manual intervention, limiting their efficiency and scalability. This study [...] Read more.
Accurate land cover mapping plays a critical role in enhancing our understanding of Earth’s energy balance, carbon cycle, and ecosystem dynamics. However, existing methods for producing multi-epoch land cover products still heavily depend on manual intervention, limiting their efficiency and scalability. This study introduces an automated approach for multi-epoch land cover mapping using remote sensing imagery and the model migration strategy. Landsat ETM+ and OLI images with a 30 m resolution were utilized as the primary data sources. An automatic training sample extraction method based on prior multi-source land cover products was first utilized. Then, based on the generated training dataset and a random forest classifier, local adaptive land cover classification models of the reference year were developed. Finally, by migrating the classification model to the target epoch, multi-epoch land cover products were generated. Yuli County in Xinjiang and Linxi County in Inner Mongolia were used as test cases. The classification models were first generated in 2020 and then migrated to 2010 to test the effectiveness of automated land cover classification over multiple years. Our mapping results show high accuracy in both regions, with Yuli County achieving 92.52% in 2020 and 88.33% in 2010, and Linxi County achieving 90.28% in 2020 and 85.28% in 2010. These results demonstrate the reliability of our proposed automated land cover mapping strategy. Additionally, the uncertainty analysis of the model migration strategy indicated that land cover types such as water bodies, wetlands, and impervious surfaces, which exhibit significant spectral changes over time, were the least suitable for model migration. Our results can offer valuable insights for medium-resolution, multi-epoch land cover mapping, which could facilitate more efficient and accurate environmental assessments. Full article
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<p>The location of Yuli County area, Xinjiang and Linxi County area, Inner Mongolia. The background images of Yuli and Linxi are RGB composites of Landsat 8 OLI images from 2020.</p>
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<p>Flowchart for rapid mapping of multi-year medium-resolution land cover products.</p>
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<p>Land cover mapping results of two years in Yuli County and Linxi County area. (<b>a</b>) the RGB image of Yuli in 2020; (<b>b</b>) the land cover map of Yuli in 2020; (<b>c</b>) the RGB image of Yuli in 2010; (<b>d</b>) the land cover mapof Yuli in 2010; (<b>e</b>) the RGB image of Linxi in 2020; (<b>f</b>) the land cover mapof of Linxi in 2020; (<b>g</b>) the RGB image of Linxi in 2010; (<b>h</b>) the land cover map of Linxi in 2010.</p>
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<p>Percentages of land cover types in 2010 and 2020. (<b>a</b>) Yuli County; (<b>b</b>) Linxi County.</p>
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<p>Spectral differences for land cover classes from 2020 to 2010 in Yuli and Linxi County areas. Noted: B1, B2, B3, B4, B5, and B6 represent Blue, Green, Red, NIR, SWIR1, and SWIR2 bands, respectively; P25_2020, P50_2020, P75_2020 represent the 25th, 50th, and 75th quantile composites in 2020, respectively; P25_2010, P50_2010, P75_2010 represent the 25th, 50th, and 75th quantile composites in 2010, respectively.</p>
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<p>Cross-comparison of the mapping results of our study, GlobeLand30 and CLCD in the Yuli and Linxi County areas: (I) Mapping results of Yuli in 2020; (II) Mapping results of Yuli in 2010; (III) Mapping results of Linxi in 2020; (IV) Mapping results of Linxi in 2010. (Note: a and b are the magnified area of the RGB image.)</p>
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<p>Cross-comparison of the mapping results of our study, GlobeLand30 and CLCD in the Yuli and Linxi County areas: (I) Mapping results of Yuli in 2020; (II) Mapping results of Yuli in 2010; (III) Mapping results of Linxi in 2020; (IV) Mapping results of Linxi in 2010. (Note: a and b are the magnified area of the RGB image.)</p>
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17 pages, 4641 KiB  
Technical Note
Evaluating Remote Sensing Metrics for Land Surface Phenology in Peatlands
by Michal Antala, Anshu Rastogi, Marcin Stróżecki, Mar Albert-Saiz, Subhajit Bandopadhyay and Radosław Juszczak
Remote Sens. 2025, 17(1), 32; https://doi.org/10.3390/rs17010032 - 26 Dec 2024
Viewed by 331
Abstract
Vegetation phenology is an important indicator of climate change and ecosystem productivity. However, the monitoring of vegetation generative phenology through remote sensing techniques does not allow for species-specific retrieval in mixed ecosystems; hence, land surface phenology (LSP) is used instead of traditional plant [...] Read more.
Vegetation phenology is an important indicator of climate change and ecosystem productivity. However, the monitoring of vegetation generative phenology through remote sensing techniques does not allow for species-specific retrieval in mixed ecosystems; hence, land surface phenology (LSP) is used instead of traditional plant phenology based on plant organ emergence and development observations. Despite the estimated timing of the LSP parameters being dependent on the vegetation index (VI) used, inadequate attention was paid to the evaluation of the commonly used VIs for LSP of different vegetation covers. We used two years of data from the experimental site in central European peatland, where plots of two peatland vegetation communities are under a climate manipulation experiment. We assessed the accuracy of LSP retrieval by simple remote sensing metrics against LSP derived from gross primary production and canopy chlorophyll content time series. The product of Near-Infrared Reflectance of Vegetation and Photosynthetically Active Radiation (NIRvP) and Green Chromatic Coordinates (GCC) was identified as the best-performing remote sensing metrics for peatland physiological and structural phenology, respectively. Our results suggest that the changes in the physiological phenology due to increased temperature are more prominent than the changes in the structural phenology. This may mean that despite a rather accurate assessment of the structural LSP of peatland by remote sensing, the changes in the functioning of the ecosystem can be underestimated by simple VIs. This ground-based phenological study on peatlands provides the base for more accurate monitoring of interannual variation of carbon sink strength through remote sensing. Full article
(This article belongs to the Section Environmental Remote Sensing)
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<p>The location of the Rzecin peatland in Poland and the location and experimental design of the CL and CR sites and their plots (part of the figure was adapted from Górecki et al. [<a href="#B31-remotesensing-17-00032" class="html-bibr">31</a>], CC BY-NC-ND license).</p>
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<p>Correlation coefficient (R) for the linear model between gross primary production-derived (<b>A</b>) or canopy chlorophyll content-derived (<b>B</b>) phenological parameters and the phenological parameters derived from different reflectance-based parameters. All observations, regardless of site, treatment, and year, were analyzed together (n = 72). The stars of a particular color indicate a significant correlation at alpha = 0.05. CCC—Canopy Chlorophyll Content, EVI—Enhanced Vegetation Index, ExG—Excess Green, GCC—Green Chromatic Coordinates, LAI—Leaf Area Index, MTCI—MERRIS Terrestrial Chlorophyll Index, NDVI—Normalized Difference Vegetation Index, NIRv—Near-Infrared Reflectance of Vegetation, PAR—Photosynthetically Active Radiation, PPI—Plant Phenology Index, CCCP—CCC*PAR, EVIP—EVI*PAR, ExGP—ExG*PAR, GCCP—GCC*PAR, LAIP—LAI*PAR, MTCIP—MTCI*PAR, NDVIP—NDVI*PAR, NIRvP—NIRv*PAR, PPIP—PPI*PAR.</p>
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<p>The mean absolute error of chosen remote sensing metrics-derived gross primary production-based (<b>A</b>) and canopy chlorophyll content-based (<b>B</b>) start of the season (SoS), peak of the season (PoS), end of the season (EoS), and the general performance calculated as the mean of SoS, PoS, and EoS (mean). Different letters within the cells of the same parameter (SoS, PoS, Eos, or mean) denote significantly different performances at alpha = 0.05, as found by the Conover test. Green names of metrics denote the simple vegetation indices. CCC—Canopy Chlorophyll Content, EVI—Enhanced Vegetation Index, ExG—Excess Green, GCC—Green Chromatic Coordinates, LAI—Leaf Area Index, MTCI—MERRIS Terrestrial Chlorophyll Index, NDVI—Normalized Difference Vegetation Index, NIRv—Near-Infrared Reflectance of Vegetation, PAR—Photosynthetically Active Radiation, PPI—Plant Phenology Index, CCCP—CCC*PAR, EVIP—EVI*PAR, ExGP—ExG*PAR, GCCP—GCC*PAR, LAIP—LAI*PAR, MTCIP—MTCI*PAR, NDVIP—NDVI*PAR, NIRvP—NIRv*PAR, PPIP—PPI*PAR.</p>
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21 pages, 10301 KiB  
Article
Integrated Approach to Understanding Perceived Importance and Changes in Watershed Ecosystem Services (WESs): Insights from Central Nepal
by Nabin Dhungana, Chun-Hung Lee, Samjhana Adhikari, Bishal Kumar Rayamajhi, Udit Chandra Aryal and Pramod Ghimire
Sustainability 2025, 17(1), 62; https://doi.org/10.3390/su17010062 - 26 Dec 2024
Viewed by 705
Abstract
With environmental changes, sustaining watershed ecosystem services requires understanding community perceptions and preferences. Integrated approaches considering community perceptions, climate change, and land use cover change are crucial. We address a study gap by combining climate change and land use cover change data with [...] Read more.
With environmental changes, sustaining watershed ecosystem services requires understanding community perceptions and preferences. Integrated approaches considering community perceptions, climate change, and land use cover change are crucial. We address a study gap by combining climate change and land use cover change data with an analysis of community perceptions to evaluate the watershed ecosystem services situation in Nepal’s Khageri Khola Watershed. Data from in-depth stakeholder interviews (n = 16), household perception surveys (n = 440), and participant observations (n = 5) were supplemented by meteorological and land use cover change data. Descriptive analysis, index value calculation, Spearman’s Rho correlation, and chi-square statistics were used to understand linkages between socio-demographics, climate change perceptions, watershed ecosystem services importance, and changes in watershed ecosystem services supply. The Mann–Kendall test, Sen’s slope calculation, and land use cover change analysis considered temperature, precipitation, and land use. Among watershed ecosystem services, communities prioritized drinking water as the most important and biodiversity support as the least important. Watershed ecosystem services exhibited decreasing trends, with soil fertility and productivity notably high (89%) and natural hazard control low (41%). Significant alignment existed between community perceptions and local climate indicators, unlike the incongruity found with land use cover changes, especially regarding water bodies. Socio-demographic factors influenced community perceptions. Policy recommendations include analyzing watershed-level community demand and preferences, integrating community perceptions with climate change and land use cover change data in decision making, engaging communities, equitable sharing of the benefits generated by watershed ecosystem services, and considering socio-demographic and topographic diversity in tailoring management strategies. Full article
(This article belongs to the Special Issue Advances in Ecosystem Services and Urban Sustainability, 2nd Edition)
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<p>Study watershed in Chitwan District, Central Nepal, showing watershed boundaries, rivers, irrigation canals, forest corridors, buffer zone, local government areas, and land use. Note: OWL represent other wooded land.</p>
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<p>Methodological framework for identifying key WESs, importance, and trends for management and policy inputs.</p>
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<p>Stacked bar chart showing the rank index values of WESs across socio-demographic groups, with higher values indicating greater importance. The figure idea is adopted from [<a href="#B22-sustainability-17-00062" class="html-bibr">22</a>].</p>
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<p>Respondents’ perceptions of local climate change indicators.</p>
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<p>Bar chart showing total annual precipitation (in mm), and trend line showing mean temperature (in °C) at stations near the watershed from 1980 to 2023, along with Sen’s slope equation.</p>
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<p>Respondents’ perceptions of WES supply trends over the past decade.</p>
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<p>Percentage change in watershed land use/land cover per category from 2000 to 2019.</p>
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<p>Map showing watershed land use/land cover changes (gain or loss) across seven categories from 2000 to 2019.</p>
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<p>Watershed land use maps from 2000 (<b>a</b>) and 2019 (<b>b</b>).</p>
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24 pages, 4808 KiB  
Article
Climate Variability and Adaptation Strategies in a Pastoralist Area of the Eastern Bale Zone: The Case of Sawena District, Ethiopia
by Mesfin Bekele Gebbisa and Zsuzsanna Bacsi
Appl. Sci. 2025, 15(1), 69; https://doi.org/10.3390/app15010069 - 25 Dec 2024
Viewed by 437
Abstract
This study was conducted in Sawena district, located in the Eastern Bale Zone of Ethiopia, with the aim of analyzing climate variability and identifying adaptation strategies. Secondary data covering the period from 1984 to 2023 were utilized, along with structured and unstructured questionnaires. [...] Read more.
This study was conducted in Sawena district, located in the Eastern Bale Zone of Ethiopia, with the aim of analyzing climate variability and identifying adaptation strategies. Secondary data covering the period from 1984 to 2023 were utilized, along with structured and unstructured questionnaires. Primary data were gathered from 350 pastoralist households across six kebeles through a household survey. This study used the Mann–Kendall test, Sen’s slope estimator, the coefficient of variation, descriptive statistics, and a multivariate probit model to analyze climate variability and adaptation strategies. The Mann–Kendall test, Sen’s slope estimator, and coefficient of variation analysis results showed significant rainfall increases in September, October, and November, with high winter variability and an upward autumn trend. Temperature analysis revealed consistent warming, with the greatest increases in September (0.049 °C/year) and summer (0.038 °C/year), and an annual mean rise of 0.034 °C per year, indicating climate shifts affecting pastoralist and agro-pastoral livelihood strategies and water resources that lead the area toward vulnerability. The descriptive results indicated that pastoralist households have adopted various adaptation strategies: 45.1% participate in seasonal livestock migration, 26.3% rely on productive safety net programs, 19% pursue livelihood diversification, and 9.7% engage in agroforestry. Multivariate analysis indicates that education, age, credit access, livestock ownership, asset value, and media exposure influence these strategies. The findings highlight the importance of policies to enhance climate resilience through diversification, sustainable land management, and improved access to resources like credit and markets, alongside strengthened education and targeted extension services. Full article
(This article belongs to the Special Issue Potential Impacts and Risks of Climate Change on Agriculture)
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<p>Map of the study area. Source: authors’ own construction.</p>
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<p>Trend of winter season rainfall.</p>
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<p>Trend of spring season rainfall.</p>
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<p>Trend of Summer season rainfall.</p>
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<p>Trend of autumn season rainfall.</p>
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<p>Trend of annual rainfall in Sawena district.</p>
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<p>Trend of winter season temperature.</p>
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<p>Trend of mean annual temperature.</p>
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<p>The most common adaptation and coping strategies of households in Sawena district. Source: authors’ own computation.</p>
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18 pages, 2787 KiB  
Article
Correlation Between Flying Insect Diversity and Environmental Factors in Various Land Use Types in Paseh District, Sumedang Regency, West Java
by Susanti Withaningsih, Bilhaq Fahmi Ilmi and Parikesit Parikesit
Diversity 2025, 17(1), 2; https://doi.org/10.3390/d17010002 - 24 Dec 2024
Viewed by 333
Abstract
Indonesia is known for its incredible diversity of insects. Being ectothermic, insects are influenced by environmental factors. The relationship between insect diversity and the environment can be understood using multivariate analysis. The Paseh District in Sumedang Regency has various land uses, including gardens, [...] Read more.
Indonesia is known for its incredible diversity of insects. Being ectothermic, insects are influenced by environmental factors. The relationship between insect diversity and the environment can be understood using multivariate analysis. The Paseh District in Sumedang Regency has various land uses, including gardens, rice fields, and plantations. Changes in land use due to the construction of the Cisumdawu Toll Road can impact environmental factors, such as soil quality, microclimate, and water availability, which are critical for sustaining diverse insect communities. Similarly, changes in vegetation cover can alter temperature and humidity levels, impacting terrestrial insects adapted to specific climatic conditions. This study aims to gather information on the relationship between insect diversity and environmental factors in different land use types in the Paseh District. A preliminary survey was carried out to record land use types and determine sampling locations. An intensive survey was done to collect and identify flying insect samples, as well as to measure the environmental factors. The results were analyzed using the Shannon–Wiener Diversity Index (H’), Evenness Index (E’), Simpson’s Diversity Index (C), and Canonical Correspondence Analysis (CCA). The study found 115 species of flying insects, with mixed gardens having the highest diversity. The CCA results showed that temperature strongly and positively correlated with insect diversity across all land uses, while wind speed correlated positively with insect diversity in gardens. Altitude correlated negatively with insect diversity in mixed gardens but positively in rice fields. Humidity had a strong positive correlation with insect diversity in other land uses. This research is important for understanding how land use types and environmental factors influence flying insect diversity, which is crucial for conserving biodiversity and maintaining essential ecosystem services such as pollination and pest control. Its impact lies in providing scientific data to guide sustainable land management practices, support agricultural productivity, and inform policies for biodiversity conservation in the Paseh District and similar regions. Full article
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<p>Map of research locations and sample points for data collection in Paseh District, Sumedang Regency.</p>
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<p>Insect H’ index values in various land uses in Paseh District, Sumedang Regency.</p>
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<p>Bar chart of E’ index for several land uses in Paseh District, Sumedang Regency.</p>
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<p>Bar chart of C index for several land uses in Paseh District, Sumedang Regency.</p>
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<p>Diagram of (<b>a</b>) temperature; (<b>b</b>) relative humidity; (<b>c</b>) light intensity; (<b>d</b>) wind speed; (<b>e</b>) altitude in each land use type.</p>
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<p>CCA graph for all land uses in Paseh District.</p>
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<p>(<b>a</b>) CCA graph on garden land use; (<b>b</b>) CCA graph in mixed garden land use; (<b>c</b>) CCA graph in rice field land use; (<b>d</b>) CCA graphics in other land uses.</p>
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16 pages, 8606 KiB  
Article
Annual Cropping Intensity Dynamics in China from 2001 to 2023
by Jie Ren, Yang Shao and Yufei Wang
Remote Sens. 2024, 16(24), 4801; https://doi.org/10.3390/rs16244801 - 23 Dec 2024
Viewed by 436
Abstract
Spatial and temporal information about cropping patterns of single and multiple crops is important for monitoring crop production and land-use intensity. We used time-series MODIS NDVI 8-day composite data to develop annual cropping pattern products at a 250 m spatial resolution for China, [...] Read more.
Spatial and temporal information about cropping patterns of single and multiple crops is important for monitoring crop production and land-use intensity. We used time-series MODIS NDVI 8-day composite data to develop annual cropping pattern products at a 250 m spatial resolution for China, covering the period from 2001 to 2023. To address the potential impacts of varying parameters in both data pre-processing and the peak detection algorithm on the accuracy of cropping pattern mapping, we employed a grid-search method to fine-tune these parameters. This process focused on optimizing the Savitzky–Golay smoothing window size and the peak width parameters using a calibration dataset. The results highlighted that an optimal combination of a five to seven MODIS composite window size in Savitzky–Golay smoothing and a peak width of four MODIS composites achieved good overall mapping accuracy. Pixel-wise accuracy assessments were conducted for the selected mapping years of 2001, 2011, and 2021. Overall accuracies were between 89.7% and 92.0%, with F1 scores ranging from 0.921 to 0.943. Nationally, this study observed a fluctuating trend in multiple cropping percentages, with a notable increase after 2013, suggesting shifts toward more intensive agricultural practices in recent years. At a finer spatial scale, the combination of Mann–Kendall and Sen’s slope analyses revealed that approximately 12.9% of 3 km analytical windows exhibited significant changes in cropping intensity. We observed spatial clusters of increasing and decreasing crop intensity trends across provinces such as Hebei, Shandong, Shaanxi, and Gansu. This study underscores the importance of data smoothing and peak detection methods in analyzing high temporal resolution remote sensing data. The generation of annual single/multiple cropping pattern maps at a 250 m spatial resolution enhances our comprehension of agricultural dynamics through time and across different regions. Full article
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<p>MODIS tiles (represented by dashed-line polygons) spanning horizontal zones 23 to 29 and vertical zones three to seven. Cropland distribution at a 250 m resolution. The 10 m land cover map products were employed to determine the percentage of croplands.</p>
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<p>Illustration of time-series NDVI data in 2023 for single crop (<b>a</b>) and double crop (<b>b</b>). Peak width at half-prominence is highlighted in red.</p>
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<p>Data and workflow for cropping intensity mapping.</p>
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<p>Comparison of F1 scores across different peak detection methods, examining the impact of various Savitzky–Golay (SG) smoothing combinations, SG window sizes, and peak width parameters.</p>
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<p>MODIS-derived map of single and multiple cropping patterns for the year 2023. The subplots show the details of the cropping intensity within major agricultural regions in China and their locations are indicated by red dots: (<b>a</b>) Northeast China Plain, (<b>b</b>) Qinghai-Tibet Plateau, (<b>c</b>) North China Plain, (<b>d</b>) Yangtze Plain, and (<b>e</b>) Southern China. Only the 2023 map is presented here for simplicity.</p>
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<p>The percentages of multiple crops within all cropland from the year 2001 to 2023.</p>
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<p>Slope coefficient (change rate) of cropping intensity trend model (2001–2023). Note only 3 km windows showing significant (<span class="html-italic">p</span> &lt; 0.05) upward/downward trends based on the Mann–Kendall test were used for trend model development.</p>
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<p>NDVI time series from 2001 to 2023 for two selected 3 km analytical windows: (<b>a</b>) areas transitioning from multiple to single cropping practices, and (<b>b</b>) areas transitioning from single to multiple cropping practices. NDVI values were averaged for all cropland pixels within each 3 km window for every MODIS composite.</p>
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23 pages, 12453 KiB  
Article
Soil Salinity Detection and Mapping by Multi-Temporal Landsat Data: Zaghouan Case Study (Tunisia)
by Karem Saad, Amjad Kallel, Fabio Castaldi and Thouraya Sahli Chahed
Remote Sens. 2024, 16(24), 4761; https://doi.org/10.3390/rs16244761 - 20 Dec 2024
Viewed by 519
Abstract
Soil salinity is considered one of the biggest constraints to crop production, particularly in arid and semi-arid regions affected by recurrent and long periods of drought, where high salinity levels severely impact plant stress and consequently agricultural production. Climate change accelerates soil salinization, [...] Read more.
Soil salinity is considered one of the biggest constraints to crop production, particularly in arid and semi-arid regions affected by recurrent and long periods of drought, where high salinity levels severely impact plant stress and consequently agricultural production. Climate change accelerates soil salinization, driven by factors such as soil conditions, land use/land cover changes, and water deficits, over extensive spatial and temporal scales. Continuous monitoring of areas at risk of salinization plays a critical role in supporting effective land management and enhancing agricultural production. For these purposes, this work aims to propose a spatiotemporal method for monitoring soil salinization using spectral indices derived from Earth observation data. The proposed approach was tested in the Zaghouan Region in northeastern Tunisia, a region where soils are characterized by alarming levels of salinization. To address this concern, remote sensing techniques were applied for the analysis of satellite imagery generated from Landsat 5, Landsat 8, and Landsat 9 missions. A comprehensive field survey complemented this approach, involving the collection of 229 geo-referenced soil samples. These samples were representative of distinct soil salinity classes, including non-saline, slightly saline, moderately saline, strongly saline, and very strongly saline soils. Soil salinity modeling using Landsat-8 OLI data revealed that the SI-5 index provided the most accurate predictions, with an R2 of 0.67 and an RMSE of 0.12 dS/m. By 2023, 42.3% of the study area was classified as strongly or very strongly saline, indicating a significant increase in salinity over time. This rise in salinity corresponds to notable land use and land cover (LULC) changes, as 55.9% of the study area experienced LULC shifts between 2000 and 2023. A decline in vegetation cover coincided with increasing salinity, showing an inverse relationship between these factors. Additionally, the results highlight the complex interplay among these variables demonstrating that soil salinity levels are significantly impacted by climate change indicators, with a negative correlation between precipitation and salinity (r = −0.85, p < 0.001). Recognizing the interconnections between soil salinity, LULC changes, and climate variables is essential for developing comprehensive strategies, such as targeted irrigation practices and land suitability assessments. Earth observation and remote sensing play a critical role in enabling more sustainable and effective soil management in response to both human activities and climate-induced changes. Full article
(This article belongs to the Section Environmental Remote Sensing)
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<p>Flowchart of the overall methodology.</p>
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<p>A map of the study area and field sample point distribution.</p>
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<p>Average monthly precipitation and temperature recorded between 2000 and 2023 with linear trend lines for temperature (in red) and rainfall (in blue). (Source: Regional Commissary for Agriculture Development of Zaghouan, 2023).</p>
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<p>Method of collecting a composite soil sample from five subsamples (<b>a</b>), and storing it in a plastic bag with an identification number (<b>b</b>).</p>
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<p>Soil preparation and analysis in the laboratory.</p>
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<p>Flowchart of the Methodology for Soil Salinity Mapping and Prediction.</p>
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<p>LULC change dynamics between 2000 and 2023.</p>
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<p>Five soil SIs maps obtained from Landsat-8 OLI using linear regression.</p>
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<p>Correlation between SI values and observed EC values using SIs derived from Landsat 8 bands for the year 2021: (<b>a</b>) Linear regression model using SI-1; (<b>b</b>) Linear regression model using SI-2; (<b>c</b>) Linear regression model using SI-3; (<b>d</b>) Linear regression model using SI-4; and (<b>e</b>) Linear regression model using SI-5.</p>
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<p>Maps of spatiotemporal variability of soil salinity levels observed for the years 2000, 2004, 2008, 2012, 2016, 2020, and 2023.</p>
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<p>Long-term trends in Salt-affected soils, Vegetation, and Bare land areas.</p>
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<p>Relationship between areas affected by soil salinity and average annual precipitation in mm per year between 2000 and 2023.</p>
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<p>Scatterplot between areas affected by soil salinity and precipitation over the study area between 2000 and 2023 (<span class="html-italic">p</span> ˂ 0.05).</p>
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