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Search Results (8,603)

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Keywords = land-use and land-cover

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16 pages, 4795 KiB  
Article
Predicting the Global Distribution of Gryllus bimaculatus Under Climate Change: Implications for Biodiversity and Animal Feed Production
by Sanad H. Ragab, Shatha I. Alqurashi, Mohammad M. Aljameeli, Michael G. Tyshenko, Ahmed H. Abdelwahab and Tharwat A. Selim
Sustainability 2024, 16(23), 10278; https://doi.org/10.3390/su162310278 (registering DOI) - 24 Nov 2024
Viewed by 86
Abstract
The potential range and distribution of insects are greatly impacted by climate change. This study evaluates the potential global shifts in the range of Gryllus bimaculatus (Orthoptera: Gryllidae) under several climate change scenarios. The Global Biodiversity Information Facility provided the location data for [...] Read more.
The potential range and distribution of insects are greatly impacted by climate change. This study evaluates the potential global shifts in the range of Gryllus bimaculatus (Orthoptera: Gryllidae) under several climate change scenarios. The Global Biodiversity Information Facility provided the location data for G. bimaculatus, which included nineteen bioclimatic layers (bio01–bio19), elevation data from the WorldClim database, and land cover data. For the near future (2021–2040) and far future (2081–2100) under low (SSP1-2.6) and high (SSP5-8.5) emission scenarios, the Beijing Climate Center Climate System Model (BCC-CSM2-MR) and the Institute Pierre-Simon Laplace Coupled Model Intercomparison Project (IPSL-CM6A-LR) were used. Assessing habitat gain, loss, and stability for G. bimaculatus under potential scenarios was part of the evaluation analysis. The results showed that the main environmental parameters affecting the distribution of G. bimaculatus were mean temperature of the driest quarter, mean diurnal temperature range, isothermality, and seasonal precipitation. Since birds, small mammals, and other insectivorous insects rely on G. bimaculatus and other cricket species as their primary food supply, habitat loss necessitates management attention to the effects on the food web. The spread of G. bimaculatus as a sentinel species in the food chain and its use in animal feeds are both impacted by habitat loss and gain. Full article
(This article belongs to the Section Sustainability, Biodiversity and Conservation)
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Figure 1
<p>Global distribution of <span class="html-italic">G. bimaculatus</span> occurrence records obtained from GBIF [<a href="#B22-sustainability-16-10278" class="html-bibr">22</a>].</p>
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<p>Response curves of the predictors used in modeling <span class="html-italic">G. bimaculatus</span> distribution.</p>
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<p>The predicted potential habitat of <span class="html-italic">G. bimaculatus</span> under the current climate conditions.</p>
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<p>Displays calibration maps illustrating the changes in habitat suitability for <span class="html-italic">G. bimaculatus</span> across four future scenarios compared to the current conditions: (<b>a</b>) BCC-CSM2MR_ssp126_2021–2040, (<b>b</b>) BCC-CSM2-MR_ssp126_2081–2100, (<b>c</b>) BCC-CSM2MR_ssp585_2021–2040, and (<b>d</b>) BCC-CSM2-MR_ssp585_2081–2100.</p>
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<p>Displays calibration maps illustrating the changes in habitat suitability for <span class="html-italic">G. bimaculatus</span> across four future scenarios compared to the current conditions: (<b>a</b>) BCC-CSM2MR_ssp126_2021–2040, (<b>b</b>) BCC-CSM2-MR_ssp126_2081–2100, (<b>c</b>) BCC-CSM2MR_ssp585_2021–2040, and (<b>d</b>) BCC-CSM2-MR_ssp585_2081–2100.</p>
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<p>Illustrates calibration maps demonstrating the changes in habitat suitability for <span class="html-italic">G. bimaculatus</span> across four future scenarios compared to the current conditions using: (<b>a</b>) IPSL-CM6ALR_ssp126_2021–2040, (<b>b</b>) IPSL-CM6A-LR_ssp126_2081–2100, (<b>c</b>) IPSL-CM6ALR_ssp585_2021–2040, and (<b>d</b>) IPSL-CM6A-LR_ssp585_2081–2100.4.</p>
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<p>Illustrates calibration maps demonstrating the changes in habitat suitability for <span class="html-italic">G. bimaculatus</span> across four future scenarios compared to the current conditions using: (<b>a</b>) IPSL-CM6ALR_ssp126_2021–2040, (<b>b</b>) IPSL-CM6A-LR_ssp126_2081–2100, (<b>c</b>) IPSL-CM6ALR_ssp585_2021–2040, and (<b>d</b>) IPSL-CM6A-LR_ssp585_2081–2100.4.</p>
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24 pages, 8439 KiB  
Article
Triple Collocation-Based Uncertainty Analysis and Data Fusion of Multi-Source Evapotranspiration Data Across China
by Dayang Wang, Shaobo Liu and Dagang Wang
Atmosphere 2024, 15(12), 1410; https://doi.org/10.3390/atmos15121410 (registering DOI) - 24 Nov 2024
Viewed by 51
Abstract
Accurate estimation of evapotranspiration (ET) is critical for understanding land-atmospheric interactions. Despite the advancement in ET measurement, a single ET estimate still suffers from inherent uncertainties. Data fusion provides a viable option for improving ET estimation by leveraging the strengths of individual ET [...] Read more.
Accurate estimation of evapotranspiration (ET) is critical for understanding land-atmospheric interactions. Despite the advancement in ET measurement, a single ET estimate still suffers from inherent uncertainties. Data fusion provides a viable option for improving ET estimation by leveraging the strengths of individual ET products, especially the triple collocation (TC) method, which has a prominent advantage in not relying on the availability of “ground truth” data. In this work, we proposed a framework for uncertainty analysis and data fusion based on the extended TC (ETC) and multiple TC (MTC) variants. Three different sources of ET products, i.e., the Global Land Evaporation and Amsterdam Model (GLEAM), the fifth generation of European Reanalysis-Land (ERA5-Land), and the complementary relationship model (CR), were selected as the TC triplet. The analyses were conducted based on different climate zones and land cover types across China. Results show that ETC presents outstanding performance as most areas conform to the zero-error correlations assumption, while nearly half of the areas violate this assumption when using MTC. In addition, the ETC method derives a lower root mean square error (RMSE) and higher correlation coefficient (Corr) than the MTC one over most climate zones and land cover types. Among the ET products, GLEAM performs the best, while CR performs the worst. The merged ET estimates from both ETC and MTC methods are generally superior to the original triplets at the site scale. The findings indicate that the TC-based method could be a reliable tool for uncertainty analysis and data fusion. Full article
(This article belongs to the Section Atmospheric Techniques, Instruments, and Modeling)
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<p>The map of the study area includes (<b>a</b>) the land cover types without changes during 1982–2015, the locations of EC sites (the red circle signs), and (<b>b</b>) the four different climate zones, yellow, orange, light blue, and deep blue, represent arid, semi-arid, semi-humid, and humid regions, respectively.</p>
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<p>Framework for uncertainty analysis and data fusion of ET.</p>
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<p>Spatial distributions of the multi-year monthly averaged ET in China from (<b>a</b>) GLEAM, (<b>b</b>) ERA5-Land, and (<b>c</b>) CR during the period of 1982–2017.</p>
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<p>Spatial distributions of the RMSE of monthly ET from (<b>a</b>,<b>d</b>) GLEAM, (<b>b</b>,<b>e</b>) ERA-Land, and (<b>c</b>,<b>f</b>) CR using the ETC method (<b>a</b>–<b>c</b>) and MTC method (<b>d</b>–<b>f</b>). The ratio of the RMSE from the ETC method to that from the MTC method for the three ET products (<b>g</b>) GLEAM, (<b>h</b>) ERA5-Land and (<b>i</b>) CR. The grid cells violating the assumptions of two methods were masked out.</p>
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<p>Boxplots of the RMSE of monthly ET from three ET products under different land cover types over (<b>a</b>) arid, (<b>b</b>) semi-arid, (<b>c</b>) semi-humid, and (<b>d</b>) humid zones by using the ETC and MTC methods.</p>
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<p>Spatial distributions of the Corr of monthly ET from (<b>a</b>,<b>d</b>) GLEAM, (<b>b</b>,<b>e</b>) ERA-Land, and (<b>c</b>,<b>f</b>) CR using the ETC method (<b>a</b>–<b>c</b>) and MTC method (<b>d</b>–<b>f</b>). The ratio of the RMSE from the ETC method to that from the MTC method for the three ET products (<b>g</b>) GLEAM, (<b>h</b>) ERA5-Land and (<b>i</b>) CR. The grid cells violating the assumptions of two methods were masked out.</p>
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<p>Boxplots of the Corr of monthly ET from three ET products under different land cover types over (<b>a</b>) arid, (<b>b</b>) semi-arid, (<b>c</b>) semi-humid, and (<b>d</b>) humid zones by using the ETC and MTC methods.</p>
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<p>Spatial distributions of weights of ET from (<b>a</b>,<b>d</b>) GLEAM, (<b>b</b>,<b>e</b>) ERA-Land, and (<b>c</b>,<b>f</b>) CR using the ETC method (<b>a</b>–<b>c</b>) and MTC method (<b>d</b>–<b>f</b>), and the distributions of the best ET product based on ETC method (<b>g</b>) and MTC method (<b>h</b>).</p>
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<p>Alluvial diagram of best ET product with (<b>a</b>) ETC method and (<b>b</b>) MTC method. The black stick represents a unique type in the selected dimension (e.g., the left is ET product, the middle represents climate zone, and the right denotes land cover type), and its height indicates the proportion of the corresponding type. Curved lines of the same color are used to divide certain types, the width of which denotes the proportion.</p>
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<p>Statistical characteristics of (<b>a</b>) Bias, (<b>b</b>) Corr, (<b>c</b>) MAE, (<b>d</b>) IOA, (<b>e</b>) RMSE, (<b>f</b>) KGE, (<b>g</b>) RRMSE and (<b>h</b>) NSE from individual ET products (e.g., GLEAM, ERA5-Land and CR) and merged ET (e.g., ETC and MTC) at 11 flux tower locations during the data period.</p>
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<p>Spatial patterns of precipitation and near-surface air temperature used for generating (<b>a</b>,<b>d</b>) GLEAM, (<b>b</b>,<b>e</b>) ERA5-Land and (<b>c</b>,<b>f</b>) CR ET over China during the period of 1982–2017.</p>
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<p>Boxplots of the RMSE of monthly ET from three ET products under different land cover types over (<b>a</b>) arid zone, (<b>b</b>) semi-arid zone, (<b>c</b>) semi-humid zone, and (<b>d</b>) humid zone by using the ETC method. There is no grid cell for tundra located in semi-arid, semi-humid, or humid zones.</p>
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<p>Boxplots of the Corr of monthly ET from three ET products under different land cover types over (<b>a</b>) arid zone, (<b>b</b>) semi-arid zone, (<b>c</b>) semi-humid zone, and (<b>d</b>) humid zone by using the ETC method. There is no grid cell for tundra located in semi-arid, semi-humid, or humid zones.</p>
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18 pages, 2985 KiB  
Article
Dynamics of Zinder’s Urban Landscape: Implications for Sustainable Land Use Management and Environmental Conservation
by Kadiza Doulay Seydou, Wole Morenikeji, Abdoulaye Diouf, Kagou Dicko, Elbek Erdanaev, Ralf Loewner and Appollonia Aimiosino Okhimamhe
Sustainability 2024, 16(23), 10263; https://doi.org/10.3390/su162310263 (registering DOI) - 23 Nov 2024
Viewed by 267
Abstract
Unplanned urban expansion poses significant challenges to environmental sustainability and urban planning. This study analyzes the spatiotemporal dynamics of Zinder’s urban landscape using Landsat satellite imagery from 1988, 2000, 2011, and 2022. The study applied remote sensing (RS), geographic information system (GIS) techniques, [...] Read more.
Unplanned urban expansion poses significant challenges to environmental sustainability and urban planning. This study analyzes the spatiotemporal dynamics of Zinder’s urban landscape using Landsat satellite imagery from 1988, 2000, 2011, and 2022. The study applied remote sensing (RS), geographic information system (GIS) techniques, and urban growth models. The random forest classifier, a machine learning algorithm, was used to classify three land use/land cover categories: “vegetation”, “built-up”, and “others”. Zinder’s arid environment is characterized by sparse vegetation, which constitutes a limited but vital component of its landscape. Despite the already sparse vegetation in the area, the findings reveal a 3.5% reduction in vegetation cover between 1988 and 2022, alongside an 11.5% increase in “built-up” areas and an 8% decrease in the “others” category. This loss of already minimal vegetation raises significant concerns about environmental degradation and the exacerbation of desertification risks. Interestingly, urban expansion showed no significant correlation with population growth (r = 0.29, p > 0.5), suggesting that other factors, such as economic activities, infrastructure development, and land use policies, drive land conversion. Edge expansion emerged as the dominant growth type, with a significant directional preference (Chi-Square = 2334.41, p < 0.001) toward major roads and areas with higher accessibility to public services. These findings emphasize the need for strategic urban planning and land management policies to address the drivers of unplanned expansion. Prioritizing sustainable infrastructure development, enforcing land use regulations, and conserving natural landscapes are critical to balancing urban growth with environmental preservation, ensuring resilience and sustainability in Zinder. Full article
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<p>Location of the study area with road network.</p>
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<p>Methodological flowchart adopted for the study.</p>
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<p>Types of landscape expansion: (<b>a</b>) infilling; (<b>b</b>) edge expansion; (<b>c</b>) outlying.</p>
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<p>Classified LULC of Zinder from 1988 to 2022.</p>
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<p>(<b>a</b>) Proportion of LULC from 1988 to 2022. (<b>b</b>) Proportion of LULC area change.</p>
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<p>Urban growth types from 1988 to 2022.</p>
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<p>Proportion of urban growth type per intermittent period.</p>
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<p>Urban growth direction from 1988 to 2022 in hectares.</p>
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<p>UD by buffer zone from 1988 to 2022.</p>
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19 pages, 15297 KiB  
Article
Forecasting Urban Land Use Dynamics Through Patch-Generating Land Use Simulation and Markov Chain Integration: A Multi-Scenario Predictive Framework
by Ahmed Marey, Liangzhu (Leon) Wang, Sherif Goubran, Abhishek Gaur, Henry Lu, Sylvie Leroyer and Stephane Belair
Sustainability 2024, 16(23), 10255; https://doi.org/10.3390/su162310255 (registering DOI) - 23 Nov 2024
Viewed by 236
Abstract
Rapid urbanization and changing land use dynamics require robust tools for projecting and analyzing future land use scenarios to support sustainable urban development. This study introduces an integrated modeling framework that combines the Patch-generating Land Use Simulation (PLUS) model with Markov Chain (MC) [...] Read more.
Rapid urbanization and changing land use dynamics require robust tools for projecting and analyzing future land use scenarios to support sustainable urban development. This study introduces an integrated modeling framework that combines the Patch-generating Land Use Simulation (PLUS) model with Markov Chain (MC) analysis to simulate land use and land cover (LULC) changes for Montreal Island, Canada. This framework leverages historical data, scenario-based adjustments, and spatial drivers, providing urban planners and policymakers with a tool to evaluate the potential impacts of land use policies. Three scenarios—sustainable, industrial, and baseline—are developed to illustrate distinct pathways for Montreal’s urban development, each reflecting different policy priorities and economic emphases. The integrated MC-PLUS model achieved a high accuracy level, with an overall accuracy of 0.970 and a Kappa coefficient of 0.963 when validated against actual land use data from 2020. The findings indicate that sustainable policies foster more contiguous green spaces, enhancing ecological connectivity, while industrial-focused policies promote the clustering of commercial and industrial zones, often at the expense of green spaces. This study underscores the model’s potential as a valuable decision-support tool in urban planning, allowing for the scenario-driven exploration of LULC dynamics with high spatial precision. Future applications and enhancements could expand its relevance across diverse urban contexts globally. Full article
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<p>Markov Chain and PLUS model framework.</p>
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<p>Land use status for (<b>a</b>) 2012 and (<b>b</b>) 2020.</p>
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<p>(<b>a</b>) Simulated land use status in 2020; (<b>b</b>) current land use status in 2020; (<b>c</b>) the spatial difference between them (colored by the simulated land use type) and; (<b>d</b>) the binary spatial difference between them.</p>
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<p>The influence of driving factors’ proximity to each land use type on land use and land cover (LULC) change.</p>
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<p>Average distance to transportation points for new developments.</p>
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<p>Predicted land use in 2028 compared to observed land use in 2020 under different scenarios.</p>
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<p>Predicted land use in 2028 compared to observed land use in 2020 under different scenarios.</p>
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<p>Average patch size for different land use types under different development scenarios.</p>
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<p>Alternative land use plans.</p>
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<p>Predicted land use in 2028 under different urban plans.</p>
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<p>Land use composition through different buffer distances under each scenario.</p>
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20 pages, 10942 KiB  
Article
Changes in Urban Green Spaces in the Pearl River Delta Urban Agglomeration: From the Perspectives of the Area, Spatial Configuration, and Quality
by Tianci Yao, Shengfa Li, Lixin Su and Hongou Zhang
Remote Sens. 2024, 16(23), 4369; https://doi.org/10.3390/rs16234369 - 22 Nov 2024
Viewed by 278
Abstract
Urban green spaces (UGSs) are integral to urban ecosystems, providing multiple benefits to human well-being. However, previous studies mainly focus on the quantity or quality of UGSs, with less emphasis on a comprehensive analysis. This study systematically examined the spatiotemporal UGS dynamics in [...] Read more.
Urban green spaces (UGSs) are integral to urban ecosystems, providing multiple benefits to human well-being. However, previous studies mainly focus on the quantity or quality of UGSs, with less emphasis on a comprehensive analysis. This study systematically examined the spatiotemporal UGS dynamics in the Pearl River Delta urban agglomeration (PRDUA) in China from the perspectives of the area, spatial configuration, and quality, using the high spatial resolution (30 m) Landsat-derived land-cover data and Normalized Difference Vegetation Index (NDVI) data during 1985–2021. Results showed the UGS area in both the old urban districts and expanded urban areas across all nine cities in the PRDUA has experienced a dramatic reduction from 1985 to 2021, primarily due to the conversion of cropland and forest into impervious surfaces. Spatially, the fragmentation trend of UGSs initially increased and then weakened around 2010 in nine cities, but with an inconsistent fragmentation process across different urban areas. In the old urban districts, the fragmentation was mainly due to the loss of large patches; in contrast, it was caused by the division of large patches in the expanded urban areas of most cities. The area-averaged NDVI showed a general upward trend in urban areas in nearly all cities, and the greening trend in the old urban districts was more prevalent than that in the expanded urban areas, suggesting the negative impacts of urbanization on NDVI have been balanced by the positive effects of climate change, urbanization, and greening initiatives in the PRDUA. These findings indicate that urban greening does not necessarily correspond to the improvement in UGS states. We therefore recommend incorporating the three-dimensional analytical framework into urban ecological monitoring and construction efforts to obtain a more comprehensive understanding of UGS states and support effective urban green infrastructure stewardship. Full article
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<p>The location of the PRDUA (<b>a</b>,<b>b</b>), and its land-cover maps in 1985 (<b>c</b>) and 2021 (<b>d</b>), respectively.</p>
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<p>The state and change flows of land cover in nine cities in the PRDUA from 1985 to 2021. Regarding subplot numbering, letters represent cities, and numbers indicate urban subregions.</p>
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<p>Dynamic degrees of green spaces in the expanded urban areas in nine cities in the PRDUA during 1985–2021.</p>
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<p>(<b>a</b>–<b>i</b>) The changes in landscape metrics of green spaces in nine cities in the PRDUA during 1985–2021.</p>
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<p>Box plots of trends in annual NDVI in nine cities in the PRDUA during 1986–2021. (<b>a</b>) represents green spaces with constant land-cover types during the study period, and (<b>b</b>) represents all the land-cover types, excluding permanent water bodies.</p>
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<p>Spatial patterns of trends in annual NDVI in areas with constant land-cover types in nine cities in the PRDUA during 1986–2021.</p>
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<p>Spatial patterns of trends in annual NDVI in areas with land-cover change occurring in nine cities in the PRDUA during 1986–2021.</p>
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<p>The frequency distributions of trends in annual NDVI in different city subregions where land-cover change did not occur (<b>a</b>) or occurred (<b>b</b>) during 1986–2021. O, E, and R indicate the old urban districts, expanded urban areas, and rural areas, respectively.</p>
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<p>The change in area-averaged NDVI in the PRDUA during 1986–2021 (<b>a</b>) and correlation of annual NDVI in different city subregions with the PRDUA average (<b>b</b>). The solid-colored bars represent the relationship between annual NDVI in areas with constant land-cover types and the PRDUA average, while the bars with forward slashes indicate the relationship between the areas excluding permanent water bodies and the PRDUA average. ** indicate the trends significant at <span class="html-italic">p</span> &lt; 0.01.</p>
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30 pages, 45867 KiB  
Article
Quantitative Assessment of Future Environmental Changes in Hydrological Risk Components: Integration of Remote Sensing, Machine Learning, and Hydraulic Modeling
by Farinaz Gholami, Yue Li, Junlong Zhang and Alireza Nemati
Water 2024, 16(23), 3354; https://doi.org/10.3390/w16233354 - 22 Nov 2024
Viewed by 308
Abstract
Floods are one of the most devastating natural hazards that have intensified due to land use land cover (LULC) changes in recent years. Flood risk assessment is a crucial task for disaster management in flood-prone areas. In this study, we proposed a flood [...] Read more.
Floods are one of the most devastating natural hazards that have intensified due to land use land cover (LULC) changes in recent years. Flood risk assessment is a crucial task for disaster management in flood-prone areas. In this study, we proposed a flood risk assessment framework that combines flood vulnerability, hazard, and damages under long-term LULC changes in the Tajan watershed, northern Iran. The research analyzed historical land use change trends and predicted changes up to 2040 by employing a Geographic Information System (GIS), remote sensing, and land change modeling. The flood vulnerability map was generated using the Random Forest model, incorporating historical data from 332 flooded locations and 12 geophysical and anthropogenic flood factors under LULC change scenarios. The potential flood damage costs in residential and agricultural areas, considering long-term LULC changes, were calculated using the HEC-RAS hydraulic model and a global damage function. The results revealed that unplanned urban growth, agricultural expansion, and deforestation near the river downstream amplify flood risk in 2040. High and very high flood vulnerability areas would increase by 43% in 2040 due to human activities and LULC changes. Estimated annual flood damage for agriculture and built-up areas was projected to surge from USD 162 million to USD 376 million and USD 91 million to USD 220 million, respectively, considering 2021 and 2040 land use change scenarios in the flood-prone region. This research highlights the importance of land use planning in mitigating flood-associated risks, both in the studied area and other flood-prone regions. Full article
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<p>The location of the study area and the flooded and non-flooded points’ distribution.</p>
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<p>The conceptual framework of the methodology used in this study.</p>
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<p>Influencing flood factor maps: (<b>a</b>) slope, (<b>b</b>) aspect, (<b>c</b>) altitude, (<b>d</b>) TWI, (<b>e</b>) TPI, (<b>f</b>) TRI, (<b>g</b>) soil, (<b>h</b>) rainfall, (<b>i</b>) drainage density, (<b>j</b>) distance from river, (<b>k</b>) lithology, and (<b>l</b>) LULC.</p>
Full article ">Figure 3 Cont.
<p>Influencing flood factor maps: (<b>a</b>) slope, (<b>b</b>) aspect, (<b>c</b>) altitude, (<b>d</b>) TWI, (<b>e</b>) TPI, (<b>f</b>) TRI, (<b>g</b>) soil, (<b>h</b>) rainfall, (<b>i</b>) drainage density, (<b>j</b>) distance from river, (<b>k</b>) lithology, and (<b>l</b>) LULC.</p>
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<p>Influencing flood factor maps: (<b>a</b>) slope, (<b>b</b>) aspect, (<b>c</b>) altitude, (<b>d</b>) TWI, (<b>e</b>) TPI, (<b>f</b>) TRI, (<b>g</b>) soil, (<b>h</b>) rainfall, (<b>i</b>) drainage density, (<b>j</b>) distance from river, (<b>k</b>) lithology, and (<b>l</b>) LULC.</p>
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<p>A selected portion of the Tajan watershed for studying flood hazards and damages (<b>a</b>); images of the flood consequences in 2019 in the Tajan watershed (<b>b</b>) [<a href="#B23-water-16-03354" class="html-bibr">23</a>].</p>
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<p>The yearly maximum discharge data from 1989 to 2020 upstream and downstream of the Tajan River.</p>
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<p>Depth–damage curves adapted from [<a href="#B48-water-16-03354" class="html-bibr">48</a>].</p>
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<p>Land use land cover maps of (<b>a</b>) 2001, (<b>b</b>) 2011, and (<b>c</b>) 2021.</p>
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<p>Predicted land use land cover maps in 2040.</p>
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<p>Ranking flood influencing factors’ importance for LULC scenarios in (<b>a</b>) 2021 and (<b>b</b>) 2040.</p>
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<p>ROC-AUC curve of RF model utilizing (<b>a</b>) the training dataset and (<b>b</b>) the validation dataset based on 2021 and 2040 LULC scenarios.</p>
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<p>Flood vulnerability maps derived from RF in two scenarios: (<b>a</b>) scenario 2021 and (<b>b</b>) scenario 2040.</p>
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<p>Area of generated flood vulnerability regions: (<b>a</b>) scenario 2021; (<b>b</b>) scenario 2040.</p>
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<p>The simulated depth and inundation extent for return periods of 1000 years (<b>a</b>); the amount of each LULC class in the selected portion of the Tajan watershed from 2021 to 2040 (<b>b</b>); the simulated peak discharge and maximum depth at different return periods (<b>c</b>); the simulated food inundation extent at various return periods (<b>d</b>).</p>
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<p>Comparison of simulated and observed depths (m) at upstream and downstream stations.</p>
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<p>Flood damages estimation at various return periods under LULC scenarios: (<b>a</b>) built-up area; (<b>b</b>) agricultural land.</p>
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<p>Probability of exceedance curves: (<b>a</b>) built-up area; (<b>b</b>) agricultural land.</p>
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<p>Total expected annual damage (EAD) assessment based on LULC scenarios for agricultural land and built-up areas in 2021 and 2040.</p>
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27 pages, 3893 KiB  
Article
Seasonal Patterns of Water Chemistry into Three Boreal Rivers: Implication for Salmonid Incubation and Rearing in the Frame of Hydrological Extremes and Land Use Contexts
by Rudy Benetti, Edoardo Severini, Nerijus Nika, Natalja Čerkasova, Monia Magri and Marco Bartoli
Water 2024, 16(23), 3352; https://doi.org/10.3390/w16233352 - 22 Nov 2024
Viewed by 237
Abstract
Climate change is expected to alter the timing and intensity of precipitation and river discharge patterns, leading to hydrological extremes. Compared to forested watersheds, highly urbanized and cultivated areas are prone to sediment and nutrient loads from agricultural fields, impacting river water quality. [...] Read more.
Climate change is expected to alter the timing and intensity of precipitation and river discharge patterns, leading to hydrological extremes. Compared to forested watersheds, highly urbanized and cultivated areas are prone to sediment and nutrient loads from agricultural fields, impacting river water quality. On the other hand, prolonged low discharge periods limit the rivers’ dilution capacity, and result in hyporheic water stagnation and the accumulation of metabolic end products. Hydrological extremes may, therefore, produce severe implications for river water quality and, consequently, for aquatic life; however, this important aspect is poorly explored in the literature. In this context, three boreal streams that represent spawning and juvenile rearing habitats for anadromous salmonids were analyzed comparatively with respect to land use, anthropization level, and seasonal variability in water chemistry, during low and high discharge events. A set of chemical parameters depicting the water quality are discussed in relation to different land cover features, high discharge events, and seasonality. Finally, potential negative implications for the incubation period of salmonid embryos and juvenile rearing are outlined. Full article
(This article belongs to the Section Biodiversity and Functionality of Aquatic Ecosystems)
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<p>Map of the study area reporting the three investigated watercourses with their respective watersheds, tributaries, sampling stations, and land use concerning the 3rd level of classification from the CORINE land cover project. Dotted line delimits the Šventoji sub-basin area.</p>
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<p>Water level exceedance probability curves for the sampled period.</p>
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<p>Asymmetric biplot portraying the relationships between different land uses within the three investigated basins.</p>
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<p>PCA biplots portraying the associations among the stations (dots) of the three different basins and the environmental variables, across all the seasons and the two flood periods. Environmental variables labels refer to do: dissolved oxygen (DO, mg L<sup>−1</sup>), sat: percentage of oxygen saturation (% sat.), ph: pH, c: conductivity (EC, μS cm<sup>−1</sup>), t: temperature (T °C), nh4: ammonium N-NH<sub>4</sub><sup>+</sup>, no3: nitrate N-NO<sub>3</sub><sup>−</sup>, no2: nitrite N-NO<sub>2</sub><sup>−</sup>, po4: soluble reactive phosphorous P-PO<sub>4</sub><sup>3−</sup>, all expressed in mg L<sup>−1</sup>, alk: alkalinity (mmol L<sup>−1</sup>), tss: total suspended solids (TSS, mg L<sup>−1</sup>).</p>
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<p>Variations in the 11 environmental parameters across the three watersheds, considering each season only during the low-flow periods. <span class="html-italic">p</span> &lt; 0.05 (*), <span class="html-italic">p</span> &lt; 0.01 (**), <span class="html-italic">p</span> &lt; 0.001 (***). (<b>a</b>) dissolved oxygen (DO, mg L<sup>−1</sup>), (<b>b</b>) percentage of oxygen saturation (% saturation), (<b>c</b>) conductivity (EC, μS cm<sup>−1</sup>), (<b>d</b>) temperature (T °C), (<b>e</b>) pH, (<b>f</b>) total suspended solids (TSS, mg L<sup>−1</sup>), (<b>g</b>) alkalinity (alkalinity mmol L<sup>−1</sup>), (<b>h</b>) nitrate (N-NO<sub>3</sub><sup>−</sup>, mg L<sup>−1</sup>), (<b>i</b>) ammonium (N-NH<sub>4</sub><sup>+</sup>, mg L<sup>−1</sup>), (<b>j</b>) nitrite (N-NO<sub>2</sub><sup>−</sup>, mg L<sup>−1</sup>), (<b>k</b>) soluble reactive phosphorous (P-PO<sub>4</sub><sup>3−</sup>, mg L<sup>−1</sup>).</p>
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<p>Variations between the flooding and low-flow phases during the fall and winter seasons for the 11 environmental variables in the three watercourses. <span class="html-italic">p</span> ≤ 0.05 (*), <span class="html-italic">p</span> &lt; 0.01 (**), <span class="html-italic">p</span> &lt; 0.001 (***). (<b>a</b>) dissolved oxygen (DO, mg L<sup>−1</sup>), (<b>b</b>) percentage of oxygen saturation (% saturation), (<b>c</b>) conductivity (EC, μS cm<sup>−1</sup>), (<b>d</b>) temperature (T °C), (<b>e</b>) pH, (<b>f</b>) total suspended solids (TSS, mg L<sup>−1</sup>), (<b>g</b>) nitrate (N-NO<sub>3</sub><sup>−</sup>, mg L<sup>−1</sup>), (<b>h</b>) nitrite (N-NO<sub>2</sub><sup>−</sup>, mg L<sup>−1</sup>), (<b>i</b>) ammonium (N-NH<sub>4</sub><sup>+</sup>, mg L<sup>−1</sup>), (<b>j</b>) soluble reactive phosphorous (P-PO<sub>4</sub><sup>3−</sup>, mg L<sup>−1</sup>), (<b>k</b>) alkalinity (alkalinity mmol L<sup>−1</sup>).</p>
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17 pages, 5335 KiB  
Article
Socioeconomic Disparities in the Usage of Urban Opportunities in South Korea During the COVID-19 Pandemic: Using Land Use/Land Cover and Mobile Phone Data
by Kangjae Lee, Yoo Min Park, Yoohyung Joo, Minsoo Joo and Joon Heo
ISPRS Int. J. Geo-Inf. 2024, 13(12), 421; https://doi.org/10.3390/ijgi13120421 - 22 Nov 2024
Viewed by 308
Abstract
Severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2), the cause of coronavirus disease 19 (COVID-19), has resulted in dramatic changes in human lifestyles and the geographic distribution of populations. However, despite the unequal impact of COVID-19 across urban spaces, research on the association between [...] Read more.
Severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2), the cause of coronavirus disease 19 (COVID-19), has resulted in dramatic changes in human lifestyles and the geographic distribution of populations. However, despite the unequal impact of COVID-19 across urban spaces, research on the association between socioeconomic disparities in the usage of various types of urban amenities during the pandemic is limited. Thus, this study utilized mobile phone data and land use/land cover (LULC) data to investigate COVID-19-induced changes in the hot spots of the daytime and nighttime populations of two districts in Seoul, South Korea: Gangnam (a high-income community) and Gangbuk (a low-income community). First, the differences between Gangnam and Gangbuk in the LULC and mobile phone data, before and during the pandemic, were statistically analyzed by age. Second, the areas with significantly increased mobile phone-based populations during COVID-19 were identified using a hot spot analysis method and Welch’s t-test. This study identified that there were significant disparities in the use of green spaces during the pandemic, with a higher percentage of the mobile phone-based population in Gangnam than Gangbuk. Youths and adults in Gangnam were more likely to visit schools and enjoy physical activities in forests and open spaces during the pandemic, whereas there was no such increase in Gangbuk. The findings contribute to the understanding of the impact of COVID-19 on human behaviors and socioeconomic disparities in the quality of urban life. Full article
(This article belongs to the Special Issue HealthScape: Intersections of Health, Environment, and GIS&T)
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<p>Gangnam (Gangnam-gu and Seocho-gu) and Gangbuk (Gangbuk-gu and Seongbuk-gu) districts.</p>
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<p>Distribution of the mobile phone-based population of Seoul in April 2020 and the locations of subway stations.</p>
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<p>LULC in Gangnam and Gangbuk in 2020.</p>
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<p>Hot spots (red) of the increased population of all age groups in Gangbuk in April and August during COVID-19.</p>
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<p>Hot spots (red) of the increased population of all age groups in Gangnam in April and August during COVID-19.</p>
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26 pages, 18336 KiB  
Article
Dynamic Quantification and Characterization of Spatial Heterogeneity in Mid-Sized Urban Landscape of India
by Diksha, Varun Narayan Mishra, Deepak Kumar, Maya Kumari, Bashar Bashir, Malay Pramanik and Mohamed Zhran
Land 2024, 13(12), 1989; https://doi.org/10.3390/land13121989 - 22 Nov 2024
Viewed by 352
Abstract
Quantifying landscape features and linking them to ecological processes is a key goal of landscape ecology. Urbanization, socio-economic growth, political influences, and morphology have extended built-up and urban regions from the core to the boundaries. Population expansion and human activity in districts have [...] Read more.
Quantifying landscape features and linking them to ecological processes is a key goal of landscape ecology. Urbanization, socio-economic growth, political influences, and morphology have extended built-up and urban regions from the core to the boundaries. Population expansion and human activity in districts have increased outlying areas and living space borders, segmenting the urban area and affecting the local ecosystem. Current space-based remote sensing (RS) techniques could be used to visualize conditions and future prognoses for district growth to plan the infrastructure. The Land Use Land Cover (LULC) patterns in the Sonipat district, located within the National Capital Region (NCR), were examined using RS data from 2011 (Landsat 7) and 2021 (Sentinel-2) and analyzed on the Google Earth Engine (GEE) cloud platform. LULC datasets for both years were generated, followed by calculations of landscape metrics to evaluate changes across the study area. These metrics, computed using R software version 4.4.2, include analyses at three levels: five metrics at the patch level, five at the landscape level, and nine at the class level. This paper provides detailed insights into these landscape metrics, illustrating the extent and nature of landscape changes within the study area over the decade. Aggregation and fragmentation are observed in the study area, as the results indicate that urban, fallow, and barren areas have merged into larger, contiguous patches over time. This shows a consolidation of smaller patches into more extensive, connected land cover areas. Fragmentation is described as occurring between 2011 and 2021, especially in the cropland LULC class, where the landscape was divided into smaller, isolated patches. This means that larger, continuous land cover types were broken down into numerous smaller patches, increasing the overall patchiness and separation across the area, which might have an ecological impact. Landscape metrics and spatial-temporal monitoring of the landscape would aid the district council and planners in better planning and livelihood sustainability. Full article
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<p>Geographical location of the Sonipat district.</p>
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<p>Methodology chart.</p>
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<p>LULC map of Sonipat district, (<b>a</b>) 2011, (<b>b</b>) 2021.</p>
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<p>Percentages of the total area occupied by the LULC classes.</p>
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<p>Sample code for computing accuracy assessment in the Sonipat district.</p>
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<p>LULC classification accuracy assessment.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of a CAI, patch-level landscape metric.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of a CIRCLE, patch-level landscape metric.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of an ENN, patch-level landscape metric.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of a SHAPE, patch-level landscape metric.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of a FRAC, patch-level landscape metric.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of a CA, class-level landscape metric.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of an AI, class-level landscape metric.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of a CLUMPY, class-level landscape metric.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of an ED, class-level landscape metric.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of a DIVISION, class-level landscape metric.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of a CPLAND, class-level landscape metric.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of an NLSI, class-level landscape metric.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of a TE, class-level landscape metric.</p>
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<p>Graphical and pictorial representation of the highest and lowest values of a PAFRACE, class-level landscape metric.</p>
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<p>Pictorial representation of an AI landscape-level landscape metric.</p>
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<p>Pictorial representation of a CONTAG, landscape-level landscape metric.</p>
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<p>Pictorial representation of a DECAD, landscape-level landscape metric.</p>
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<p>Pictorial representation of an ED, landscape-level landscape metric.</p>
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<p>Pictorial representation of an ENT, landscape-level landscape metric.</p>
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<p>Graphical representation of the results of a landscape metric at landscape level.</p>
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<p>Area and perimeter changes in the class of cropland &amp; urban and Built-up from 2011 to 2021.</p>
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17 pages, 5166 KiB  
Article
Does Participatory Forest Management Reduce Deforestation and Enhance Forest Cover? A Comparative Study of Selected Forest Sites in Adaba-Dodola, Ethiopia
by Lemma Tiki, Jumanne M. Abdallah, Kristina Marquardt and Motuma Tolera
Ecologies 2024, 5(4), 647-663; https://doi.org/10.3390/ecologies5040038 - 22 Nov 2024
Viewed by 230
Abstract
Although extensive interventions are being made to protect forests, many developing countries, including Ethiopia, face persistent forest conservation challenges, particularly where local communities heavily rely on forests for their livelihoods. Recognizing the urgency of this issue, the government of Ethiopia introduced Participatory Forest [...] Read more.
Although extensive interventions are being made to protect forests, many developing countries, including Ethiopia, face persistent forest conservation challenges, particularly where local communities heavily rely on forests for their livelihoods. Recognizing the urgency of this issue, the government of Ethiopia introduced Participatory Forest Management (PFM) and devolved forest management responsibilities to enhance forest conservation. Therefore, investigating the impacts of PFM on forest covers is important. To this end, our research is based on an analysis of the land use/land cover changes (LULCCs) over the last 23 years in selected forest sites of Adaba–Dodola and their implications for the implementation of REDD+. This study examines the difference in forest cover changes between PFM and non-PFM sites within and between the study periods. Landsat images from 2000, 2012, and 2023 were analysed to detect LULCCs. Overall, the results from the comparison analysis indicate that in the period of 2000–2023, forest lands decreased by 5.22% in non-PFM sites, while they increased by 5.89% in PFM sites. On the other hand, agricultural lands experienced a notable increase of 9.64% in non-PFM sites but decreased by 1.65% in PFM sites. The increase in the forest cover is attributed to the effectiveness of PFM in halting deforestation and promoting forest conservation compared to non-PFM sites. Thus, the PFM approach is a tool for preserving forest ecosystems and mitigating the adverse effects of deforestation and forest degradation; therefore, this strategy could be used as a driving wheel for the implementation of REDD+. Full article
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<p>Map of the study area of the Adaba–Dodola forest.</p>
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<p>Flow diagram of the approach used to classify LULC of the study area.</p>
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<p>Percentage of gain or loss of each LULC in non-PFM and PFM areas during 2000–2023.</p>
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<p>Classified land use/land cover maps of sample non-PFM (<b>a</b>) and PFM (<b>b</b>) sites from Adaba during 2000–2023.</p>
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<p>Classified land use/land cover maps of sample non-PFM (<b>a</b>) and PFM (<b>b</b>) sites from Dodola during 2000–2023.</p>
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<p>Trends of LULC types in non-PFM and PFM sites from Adaba–Dodola during 2000–2023.</p>
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<p>Land use and land cover conversion matrix of non-PFM and PFM areas from 2000–2023.</p>
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<p>Major causes of forest cover changes in the Adaba–Dodola forest area.</p>
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22 pages, 16197 KiB  
Article
Accounting for Climate and Inherent Soil Quality in United Nations (UN) Land Degradation Analysis: A Case Study of the State of Arizona (USA)
by Elena A. Mikhailova, Hamdi A. Zurqani, Lili Lin, Zhenbang Hao, Christopher J. Post, Mark A. Schlautman, Gregory C. Post and George B. Shepherd
Climate 2024, 12(12), 194; https://doi.org/10.3390/cli12120194 - 21 Nov 2024
Viewed by 325
Abstract
Climate change and land degradation (LD) are some of the most critical challenges for humanity. Land degradation (LD) is the focus of the United Nations (UN) Convention to Combat Desertification (UNCCD) and the UN Sustainable Development Goal (SDG 15: Life on Land). Land [...] Read more.
Climate change and land degradation (LD) are some of the most critical challenges for humanity. Land degradation (LD) is the focus of the United Nations (UN) Convention to Combat Desertification (UNCCD) and the UN Sustainable Development Goal (SDG 15: Life on Land). Land degradation is composed of inherent and anthropogenic LD, which are both impacted by inherent soil quality (SQ) and climate. Conventional LD analysis does not take into account inherent SQ because it is not the result of land use/land cover change (LULC), which can be tracked using remote sensing platforms. Furthermore, traditional LD analysis does not link anthropogenic LD to climate change through greenhouse gas (GHG) emissions. This study uses one of the indicators for LD for SDG 15 (15.3.1: Proportion of land that is degraded over the total land area) to demonstrate how to account for inherent SQ in anthropogenic LD with corresponding GHG emissions over time using the state of Arizona (AZ) as a case study. The inherent SQ of AZ is skewed towards low SQ soils (Entisols: 29.3%, Aridisols: 49.4%), which, when combined with climate, define the inherent LD status. Currently, 8.6% of land in AZ has experienced anthropogenic LD primarily because of developments (urbanization) (42.8%) and agriculture (32.2%). All six soil orders have experienced varying degrees of anthropogenic LD. All land developments in AZ can be linked to damages from LD, with 4862.6 km2 developed, resulting in midpoint losses of 8.7 × 1010 kg of total soil carbon (TSC) and a midpoint social cost of carbon dioxide emissions (SC-CO2) of $14.7B (where B = billion = 109, USD). Arizona was not land degradation neutral (LDN) based on an increase (+9.6%) in the anthropogenic LD overall and an increase in developments (+29.5%) between 2001 and 2021. Considering ongoing climate change impacts in AZ, this increase in urbanization represents reverse climate change adaptation (RCCA) because of the increased population. The state of AZ has 82.0% of the total state area for nature-based solutions (NBS). However, this area is dominated by soils with inherently low SQ (e.g., Entisols, Aridisols, etc.), which complicates efforts for climate change adaptation. Full article
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<p>Anthropogenic land degradation (LD) can be defined as the total of the individual amounts of barren, developed, and agricultural land covers, which are directly linked to inherent soil quality (SQ) and impacted by climate (adapted from Mikhailova et al. 2024 [<a href="#B7-climate-12-00194" class="html-bibr">7</a>]).</p>
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<p>Arizona (AZ) (USA) soil map (31°20′ N to 37° N; 109°03′ W to 114°49′ W) acquired from the SSURGO soils spatial database [<a href="#B12-climate-12-00194" class="html-bibr">12</a>]. The inherent soil quality (soil suitability) of AZ is dominated by slightly weathered Entisols (29.3%) and moderately weathered Aridisols (49.4%).</p>
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<p>Flowchart of geospatial analysis used in this study. Analysis was completed using ArcGIS Pro 2.6 software. Land cover change analysis used the raster calculator to compute differences between satellite remote sensing datasets from 2001 and 2021 (Multi-Resolution Land Characteristics Consortium (MRLC) [<a href="#B25-climate-12-00194" class="html-bibr">25</a>]). The resulting change raster was converted to vector format using the raster to polygon tool and then unioned with the vector soil spatial data (SSURGO) [<a href="#B12-climate-12-00194" class="html-bibr">12</a>] using the union tool. The land cover change/soils dataset was combined with the vector administrative units using the intersect tool, which were subsequently tabulated for soil and land cover change areas.</p>
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<p>Land cover map of the state of Arizona (AZ) (USA) for 2021 (31°20′ N to 37° N; 109°03′ W to 114°49′ W) (based on data from MRLC [<a href="#B25-climate-12-00194" class="html-bibr">25</a>]).</p>
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<p>Anthropogenically degraded land proportion (%) by county for the state of Arizona (AZ) (USA) in 2021. The amount of anthropogenically degraded land was calculated as the total of degraded land from agriculture (cultivated crops and hay/pasture), from development (developed, high intensity; developed, medium intensity; developed, low intensity; developed, open space), and barren land. This figure shows the status of anthropogenic land degradation in 2021, but it is unlikely to include historical anthropogenic land degradation along with the bulk of the inherent land degradation.</p>
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<p>The proportion of land (%) that could potentially be used for nature-based solutions (NBS) by county in the state of Arizona (AZ) (USA) in 2021. Land potentially available for NBS is defined by barren land, shrub/scrub, and herbaceous land cover classes to provide potential land areas without impacting other land uses. Almost 85% of the NBS total area is composed of soils with low soil quality (SQ) (Entisols and Aridisols) that are likely not suitable for NBS despite their wide occurrence in AZ. Land availability for NBS in AZ is further limited by private land ownership.</p>
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<p>Damages from land degradation from recent land developments between 2001 and 2021 in Arizona (AZ) (USA): (<b>a</b>) soil organic carbon (SOC) loss (kg of C), (<b>b</b>) soil inorganic carbon (SIC) loss (kg of C), (<b>c</b>) total soil carbon (TSC) loss (kg of C), and (<b>d</b>) related emissions from TSC loss with midpoint “realized” social costs of soil carbon (C) (SC-CO<sub>2</sub>) based on an Environmental Protection Agency (EPA)-calculated SC-CO<sub>2</sub> of <span>$</span>46 per metric ton of CO<sub>2</sub> [<a href="#B23-climate-12-00194" class="html-bibr">23</a>]. Note: M = million = 10<sup>6</sup>, B = billion = 10<sup>9</sup>, <span>$</span> = United States dollar (USD).</p>
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<p>Damages from land degradation from the loss of potential land for soil carbon (C) sequestration from (<b>a</b>) past land developments that occurred before and up through 2021, and (<b>b</b>) recent developments between 2001 and 2021 for Arizona (AZ) (USA).</p>
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<p>Total land degradation (LD), as newly proposed, is the total of the individual amounts of inherent (“natural”) LD and anthropogenic LD (barren, developed, and agricultural land covers), which are directly linked to inherent soil quality (SQ) and impacted by climate and climate change (adapted from Mikhailova et al. 2024 [<a href="#B7-climate-12-00194" class="html-bibr">7</a>]). Anthropogenic LD generates costs associated with damages.</p>
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19 pages, 31510 KiB  
Article
Combined Effects of Forest Conservation and Population Resettlement on the Ecological Restoration of Qilian Mountain National Park
by Xi Wang, David Lopez-Carr and Liang Zhou
Land 2024, 13(12), 1983; https://doi.org/10.3390/land13121983 - 21 Nov 2024
Viewed by 311
Abstract
The combined pressures of climate change and human activities have exacerbated ecological risks in fragile and sensitive areas. Assessing the ecological restoration status of key nature reserves and developing a new conservation and development framework are fundamental for achieving ecological civilization and enhancing [...] Read more.
The combined pressures of climate change and human activities have exacerbated ecological risks in fragile and sensitive areas. Assessing the ecological restoration status of key nature reserves and developing a new conservation and development framework are fundamental for achieving ecological civilization and enhancing sustainability. As an ecological security barrier in the northwestern alpine region, Qilian Mountain National Park (QMNP), is of great significance for maintaining the sustainable ecological environment of western China. By measuring changes in ecological land use and monitoring key vegetation indicator trends in QMNP, we constructed the Regional Ecological Resilience Indicator (RERI) and proposed a new restoration and restoration framework. The results show that: (1) the ecological land restoration in QMNP was remarkable, with a total of 721.76 km2 of non-ecological land converted to ecological land, representing a 1.44% increase. Forest restoration covered 110 km2, primarily made up of previously unused land from 2000 to 2020. (2) The average NDVI value increased by 0.025. Regions showing productivity growth (NPP) accounted for 51.82% of the total area from 2000 to 2020. The four typical eco-migration zones reduced the building profile area by 47.72% between 2015 and 2019. The distribution of high Composite Vegetation Index (CFI) values overlapped with concentrated forest restoration areas, revealing two main restoration models: forest conservation and population relocation. (3) RERI calculations divided the park into three ecological zones, Priority Conservation Area (PCA), Optimization and Enhancement Area (OEA), and Concerted Development Area (CDA), leading to the proposal of an ecological restoration and development framework for QMNP, characterized by “three zones, two horizontal axes, and one vertical axis”. Our findings contribute to strengthening the ecological security barrier in northwestern China; they offer new insights for the long-term, stable improvement of the ecological environment in QMNP and in other critical protected area systems globally. Full article
(This article belongs to the Special Issue Forest Ecosystems: Protection and Restoration II)
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<p>Study area: (<b>a</b>) Location of Qilian Mountain National Park; (<b>b</b>) National Ecological Reserve surrounding QMNP; (<b>c</b>) 2020 Land Use Structure.</p>
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<p>Restoration of ecological land in QMNP and its typical localized areas.</p>
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<p>Land use transfer matrix of QMNP from 2000 to 2020.</p>
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<p>Spatial variability of woodland within QMNP and the process of CFI construction.</p>
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<p>Trends in key ecological indicators of QMNP from 2000 to 2020 and validations of remote sensing imagery.</p>
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<p>Distribution of vegetation types in QMNP and spatial–temporal changes in immigration ((<b>a</b>) Vegetation species divisions within QMNP. (<b>b</b>) Four typical WSF division areas, (<b>c</b>–<b>f</b>) Changes in building profiles due to migration between 2015–2019).</p>
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<p>RERI construction and classification of protection types.</p>
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<p>Constructing a restoration framework for QMNP.</p>
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<p>Policies and plans related to the Qilian Mountains National Park.</p>
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22 pages, 2118 KiB  
Review
Interactions Between Forest Cover and Watershed Hydrology: A Conceptual Meta-Analysis
by Mathurin François, Terencio Rebello de Aguiar, Marcelo Schramm Mielke, Alain N. Rousseau, Deborah Faria and Eduardo Mariano-Neto
Water 2024, 16(23), 3350; https://doi.org/10.3390/w16233350 - 21 Nov 2024
Viewed by 401
Abstract
The role of trees in watershed hydrology is governed by many environmental factors along with their inherent characteristics and not surprisingly has generated diverse debates in the literature. Herein, this conceptual meta-analysis provides an opportunity to propose a conceptual model for understanding the [...] Read more.
The role of trees in watershed hydrology is governed by many environmental factors along with their inherent characteristics and not surprisingly has generated diverse debates in the literature. Herein, this conceptual meta-analysis provides an opportunity to propose a conceptual model for understanding the role of trees in watershed hydrology and examine the conditions under which they can be an element that increases or decreases water supply in a watershed. To achieve this goal, this conceptual meta-analysis addressed the interaction of forest cover with climatic conditions, soil types, infiltration, siltation and erosion, water availability, and the diversity of ecological features. The novelty of the proposed conceptual model highlights that tree species and densities, climate, precipitation, type of aquifer, and topography are important factors affecting the relationships between trees and water availability. This suggests that forests can be used as a nature-based solution for conserving and managing natural resources, including water, soil, and air. To sum up, forests can reduce people’s footprint, thanks to their role in improving water and air quality, conserving soil, and other ecosystem services. The outcomes of this study should be valuable for decision-makers in understanding the types of forests that can be used in an area, following an approach of environmental sustainability and conservation aiming at restoring hydrological services, mitigating the costs of environmental services, promoting sustainable land use, managing water resources, and preserving and restoring soil water availability (SWA) when investing in reforestation for watershed hydrology, which is important for the human population and other activities. Full article
(This article belongs to the Special Issue Soil Dynamics and Water Resource Management)
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<p>Conceptual models of water mass balance of a tree canopy delineated by the upper control volume and the soil water of the underlying control volume of the porous media. In this figure, the tree canopy refers to the upper layer of a standalone tree, formed by its leaves and branches.</p>
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<p>Relationship between trees and a part of vertical water fluxes and soil water availability, illustrating differences between fast- and slow-growing forests. Fast-growing forests have a larger impact on soil water availability due to their higher transpiration rates, especially when young.</p>
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28 pages, 5794 KiB  
Article
Rehabilitated Tailing Piles in the Metropolitan Ruhr Area (Germany) Identified as Green Cooling Islands and Explained by K-Mean Cluster and Random Forest Regression Analyses
by Britta Stumpe and Bernd Marschner
Remote Sens. 2024, 16(23), 4348; https://doi.org/10.3390/rs16234348 - 21 Nov 2024
Viewed by 294
Abstract
Urban green spaces, such as parks, cemeteries, and allotment gardens provide important cooling functions for mitigating the urban heat island (UHI) effect. In the densely populated Ruhr Area (Germany), rehabilitated tailing piles (TPs), as relicts of the coal-mining history, are widespread hill-shaped landscape [...] Read more.
Urban green spaces, such as parks, cemeteries, and allotment gardens provide important cooling functions for mitigating the urban heat island (UHI) effect. In the densely populated Ruhr Area (Germany), rehabilitated tailing piles (TPs), as relicts of the coal-mining history, are widespread hill-shaped landscape forms mainly used for local recreation. Their potential role as cooling islands has never been analyzed systematically. Therefore, this study aimed at investigating the TP surface cooling potential compared to other urban green spaces (UGSs). We analyzed the factors controlling the piles’ summer land surface temperature (LST) patterns using k-mean clustering and random forest regression modeling. Generally, mean LST values of the TPs were comparable to those of other UGSs in the region. Indices describing vegetation moisture (NDMI), vitality (NDVI), and height (VH) were found to control the LST pattern of the piles during summer. The index for soil moisture (TVDI) was directly related to VH, with the highest values on the north and northeast-facing slopes and lowest on slopes with south and southeast expositions. Terrain attributes such as altitude, slope, aspect, and curvature were of minor relevance in that context, except on TPs exceeding heights of 125 m. In conclusion, we advise urban planners to maintain and improve the benefit of tailing piles as green cooling islands for UHI mitigation. As one measure, the soil’s water-holding capacity could be increased through thicker soil covers or soil additives during mine tailing rehabilitation, especially on the piles’ south and southeast expositions. Full article
(This article belongs to the Section Urban Remote Sensing)
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<p>Distribution of the tailing piles across the Ruhr Area, differentiated according to the four LST clusters (see <a href="#sec3dot2-remotesensing-16-04348" class="html-sec">Section 3.2</a>). The four named tailing piles are further characterized in Figure 6. The basemap is the NDBI (Normalized Different Built-up Index) calculated from the LANDSAT scene from 21 July 2013. The green asterisks show the locations of the weather stations (German Meteorological Service (DWD)) used for the climatic characterization of the LANDSAT 8 scenes.</p>
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<p>Flowchart of the research methodology used in this study.</p>
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<p>Histogram of the slope (°) (<b>A</b>), aspect (circular) (<b>B</b>), and vegetation height as nDSM (m) (<b>C</b>) values across all tailing piles. The dotted red lines represent the respective mean values.</p>
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<p>Histogram of the slope (°) (<b>A</b>), aspect (circular) (<b>B</b>), and vegetation height as nDSM (m) (<b>C</b>) values across all tailing piles. The dotted red lines represent the respective mean values.</p>
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<p>Histogram of the summer mean LST values (°C) across all tailing piles (<b>A</b>) and the directional distribution of the mean summer LST for all tailing piles (<b>B</b>). The red dotted line in (<b>A</b>) represents the mean LST value.</p>
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<p>Histogram of the summer mean LST values (°C) across all tailing piles (<b>A</b>) and the directional distribution of the mean summer LST for all tailing piles (<b>B</b>). The red dotted line in (<b>A</b>) represents the mean LST value.</p>
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<p>Total variance within each cluster as a function of number of clusters. The dotted line indicates the optimum cluster number as an elbow of the curve (<b>A</b>) and the visualization of cluster separation along the two main dimensions (<b>B</b>).</p>
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<p>Representative tailing piles (Kohlenhuck, Hohewardt, Tetraeder, Lohberg Nord) for the four different thermal clusters (<b>A</b>–<b>D</b>) shown as orthophotos (first column), altitude (second column), and land surface temperature (third column).</p>
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<p>Variable importance (IncNodeMSE) for the random forest regression (RFR) models based on the summer (<b>A</b>) and winter (<b>B</b>) datasets. Results are shown for the whole summer and winter datasets (all) and for datasets separated according to the tailing pile heights.</p>
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<p>Histogram of the tailing pile heights (<b>A</b>) and the variable importance (IncNodeMSE) of the aspect in RFR models differentiated according to pile heights (<b>B</b>). The dotted line indicates the threshold value of the pile height above which a distinct increase in the aspect importance in the RFR models occurs.</p>
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<p>Histogram of the tailing pile heights (<b>A</b>) and the variable importance (IncNodeMSE) of the aspect in RFR models differentiated according to pile heights (<b>B</b>). The dotted line indicates the threshold value of the pile height above which a distinct increase in the aspect importance in the RFR models occurs.</p>
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<p>Directional distribution of mean TVDI values (<b>A</b>) and vegetation heights (<b>B</b>) along the slopes of all tailing piles.</p>
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<p>Directional distribution of mean TVDI values (<b>A</b>) and vegetation heights (<b>B</b>) along the slopes of all tailing piles.</p>
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16 pages, 4269 KiB  
Article
Integrating Traditional Ecological Knowledge into Land Use and Land Cover Change Assessments, Pastoralist Communities in Northwest Inner Mongolia China
by Siru A, Bingxue Xie, Menghe Wuliji and Lisheng Zhao
Land 2024, 13(12), 1979; https://doi.org/10.3390/land13121979 - 21 Nov 2024
Viewed by 279
Abstract
Land use and land cover (LULC) changes are the primary drivers of ecosystem transformation and have substantial impacts on local livelihoods. However, most research has focused on assessing the intensity of these changes in specific regions using remotely sensed data, thus generalizing trends [...] Read more.
Land use and land cover (LULC) changes are the primary drivers of ecosystem transformation and have substantial impacts on local livelihoods. However, most research has focused on assessing the intensity of these changes in specific regions using remotely sensed data, thus generalizing trends and often overlooking the nuanced effects on local communities and their adaptive strategies. In this study, we integrated traditional ecological knowledge (TEK) with a remote sensing analysis to achieve a more comprehensive understanding of LULC changes and their social implications. Our results indicate that the grassland area in the studied region decreased significantly from 1985 to 2020, primarily due to socioeconomic development and rising temperatures, with a significant negative correlation observed between the size of the grassland area and livestock numbers. This loss of grassland has deeply affected the well-being and sustainability of pastoralist communities, whose livelihoods are intimately tied to grazing resources. A notable shift occurred around 2000; before this period, the grassland area was relatively stable, and camel populations were gradually declining. However, after 2000, grassland loss accelerated, accompanied by an increase in camel numbers. This trend reflects local herders’ adaptive strategies, as they leveraged ecological knowledge to adjust livestock composition in favor of camels, which are better suited to cope with the diminished grassland. By combining remote sensing data with TEK, we provide an integrated, longitudinal perspective on vegetation and livelihood changes. These insights are essential for shaping sustainable development policies in arid regions, where fostering ecological resilience and supporting community adaptation are critical. Full article
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<p>Location and land cover conditions of the study area in 2022.</p>
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<p>Schematic diagram of the interview process.</p>
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<p>Local people and camels (taken on October 2022 by Asiru).</p>
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<p>Chart of trends in MAT from 1985 to 2020.</p>
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<p>Pearson’s correlation matrix for climate, socioeconomic data, and land use degree index. Sample n = 32 (1985 and 1990 to 2020). MAT, mean annual temperature; MAP, mean annual precipitation; POP, population; GDP, gross domestic product; MAWS, mean annual wind speed; No. livestock, total number of livestock; LUDI, land use degree index. Numbers indicate significant positive or negative values of the corresponding correlation coefficients, as shown in the scale bar. * indicates significant correlations at <span class="html-italic">p</span> &lt; 0.05, ** indicates significant correlations at <span class="html-italic">p</span> &lt; 0.01, and *** indicates significant correlations at <span class="html-italic">p</span> &lt; 0.001 (two-sided).</p>
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