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Search Results (4,564)

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Keywords = land use/cover change

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21 pages, 5767 KiB  
Article
Spatiotemporal Analysis of Open Biomass Burning in Guangxi Province, China, from 2012 to 2023 Based on VIIRS
by Xinjie He, Qiting Huang, Dewei Yang, Yingpin Yang, Guoxue Xie, Shaoe Yang, Cunsui Liang and Zelin Qin
Fire 2024, 7(10), 370; https://doi.org/10.3390/fire7100370 (registering DOI) - 18 Oct 2024
Abstract
Open biomass burning has significant adverse effects on regional air quality, climate change, and human health. Extensive open biomass burning is detected in most regions of China, and capturing the characteristics of open biomass burning and understanding its influencing factors are important prerequisites [...] Read more.
Open biomass burning has significant adverse effects on regional air quality, climate change, and human health. Extensive open biomass burning is detected in most regions of China, and capturing the characteristics of open biomass burning and understanding its influencing factors are important prerequisites for regulating open biomass burning. The characteristics of open biomass burning have been widely investigated at the national scale, with regional studies often focusing on northeast China, but few studies have examined regional discrepancies in spatiotemporal variations over a long timescale in Guangxi province. In this study, we used the Visible Infrared Imaging Radiometer Suite (VIIRS) 375 m active fire product (VNP14IMG), combined with land cover data and high-resolution remote sensing images, to extract open biomass burning (crop residue burning and forest fire) fire points in Guangxi province from 2012 to 2023. We explored the spatial density distribution and temporal variation of open biomass burning using spatial analysis methods and statistical methods, respectively. Furthermore, we analyzed the driving forces of open biomass burning in Guangxi province from natural (topography, climate, and plant schedule), policy, and social (crop production and cultural customs) perspectives. The results show that open biomass burning is concentrated in the central, eastern, and southern parts of the study area, where there are frequent agricultural activities and abundant forests. At the city level, the highest numbers of fire points were found in Baise, Yulin, Wuzhou, and Nanning. The open biomass burning fire points exhibited large annual variation, with high levels from 2013 to 2015 and a remarkable decrease from 2016 to 2020 under strict control measures; however, inconsistent enforcement led to a significant rebound in fire points from 2021 to 2023. Forest fires are the predominant type of open biomass burning in the region, with forest fires and crop residue burning accounting for 76.82% and 23.18% of the total, respectively. The peak period for crop residue burning occurs in the winter, influenced mainly by topography, planting schedules, crop production, and policies, while forest fires predominantly occur in the winter and spring, primarily influenced by topography, climate, and cultural customs. The results indicate that identifying the driving forces behind spatiotemporal variations is essential for the effective management of open biomass burning. Full article
(This article belongs to the Special Issue Vegetation Fires and Biomass Burning in Asia)
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<p>Population density distribution of Guangxi Province.</p>
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<p>Distribution of elevation and geographical location in Guangxi Province.</p>
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<p>S-NPP satellite orbit diagram.</p>
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<p>Methodology of this research.</p>
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<p>Land cover in Guangxi in 2020.</p>
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<p>Spatial distribution of open biomass burning fire points in Guangxi from 2012 to 2023.</p>
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<p>Percentage of fire points in different regions of Guangxi.</p>
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<p>Spatial distribution of crop fire point density in Guangxi from 2012 to 2023.</p>
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<p>Spatial distribution of forest fire point density in Guangxi from 2012 to 2023.</p>
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<p>Inter-annual variation of fire points in Guangxi from 2012 to 2023.</p>
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<p>The number of fire points in Guangxi from 2012 to 2023 and their corresponding FRP.</p>
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<p>Inter-month changes of crop fire points in Guangxi from 2012 to 2023.</p>
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<p>Inter-month changes of forest fire points in Guangxi from 2012 to 2023.</p>
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<p>Distribution of open biomass burning fire points in different topographies in Guangxi from 2012 to 2023.</p>
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<p>(<b>a</b>) Correlation between annual forest fire points and the average number of consecutive days with temperatures above the mean during 2012–2023; (<b>b</b>) Correlation between monthly forest fire points and the average number of consecutive days with light rain during 2012–2023.</p>
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<p>Planting and harvesting time of major crops in Guangxi.</p>
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<p>Correlation between crop fire points and crop production during 2012–2023: (<b>a</b>) The data include Chongzuo; (<b>b</b>) The data exclude Chongzuo.</p>
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26 pages, 3651 KiB  
Article
Land Use, Travel Patterns and Gender in Barcelona: A Sequence Analysis Approach
by Lídia Montero, Lucía Mejía-Dorantes and Jaume Barceló
Sustainability 2024, 16(20), 9004; https://doi.org/10.3390/su16209004 - 17 Oct 2024
Viewed by 289
Abstract
Transport systems are essential for the path toward sustainable urbanisation and the transition to more sustainable living. Recently, European cities have undergone substantial changes, and suburbanisation is posing new challenges. Suburban areas are often more affordable in terms of housing, but these neighbourhoods [...] Read more.
Transport systems are essential for the path toward sustainable urbanisation and the transition to more sustainable living. Recently, European cities have undergone substantial changes, and suburbanisation is posing new challenges. Suburban areas are often more affordable in terms of housing, but these neighbourhoods tend to be car-oriented. This leads to higher commuter costs, immobility, transport and time poverty, pollution, higher accident rates and a lack of social interactions. To offer sustainable mobility options to citizens, we must comprehensively understand, together with their individual characteristics, their specific mobility practices and the built environment where they live. This study is centred on the Barcelona Metropolitan Region, which has a public transport network that covers its entire area. The aim of this study is to examine the relationships between travel behaviour, transport mode use, individual characteristics and built environment characteristics in the place of residence using detailed information sources. Herein, we used data from the 2018 to 2021 annual travel survey conducted in the Barcelona region, together with land use and sociodemographic information. Our findings suggest that transport policies have encouraged sustainable mobility practices, particularly in the centre of Barcelona. Despite the positive results, considerable disparities exist between the inner and outer city, with a notable decline in sustainable mobility practices in the latter, due to the uneven distribution of basic services and uneven provision of public transport, together with lower density areas. Our results demonstrate that this uneven distribution reduces the available sequence profiles of inhabitants. In conclusion, the promotion of sustainable mobility policies necessitates further advances in transport, city and land-use planning that consider equity, gender, the socioeconomic profiles of citizens and mixed urban planning. Full article
(This article belongs to the Section Sustainable Transportation)
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<p>Metropolitan Region of Barcelona: “Crowns” and TAZ-EMEF.</p>
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<p>Principal component analysis (base analysis): (<b>left</b>) dimensions 1 and 2; and dimensions 3 and 4 (<b>right</b>).</p>
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<p>Base analysis: spatial clustering of the TAZs.</p>
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<p>PCA (full analysis): Contributions to the first to fourth dimensions in the PCA and variable projections: (left) dimensions 1–2; (right) dimensions 3–4.</p>
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<p>Full analysis: spatial clustering of the TAZs.</p>
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<p>PCA results by year. Data sources: 2018 to 2021 EMEF surveys, land-use and built-environment data.</p>
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<p>Percentages of the transport modes used by zone and gender. Data source: EMEF data, 2018 to 2021.</p>
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<p>(<b>upper</b>) Number of public transport stops by zone; (<b>middle</b>) extra travel time required when taking public transport to Barcelona’s CBD according to zone; (<b>lower</b>) transport mode shared by gender and number of public transport stops (with the <span class="html-italic">y</span>-axis as the discretised number of stops by zone).</p>
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<p>(<b>upper</b>) Number of public transport stops by zone; (<b>middle</b>) extra travel time required when taking public transport to Barcelona’s CBD according to zone; (<b>lower</b>) transport mode shared by gender and number of public transport stops (with the <span class="html-italic">y</span>-axis as the discretised number of stops by zone).</p>
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<p>Optimal spatial clustering according to the base analysis variables.</p>
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<p>State distribution of the activity sequences subclusters in spatial group III by gender ((<b>top</b>)—men; (<b>bottom</b>)—women). All years are based on EMEF survey data.</p>
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<p>State distribution of the activity sequences subclusters in spatial group III by gender ((<b>top</b>)—men; (<b>bottom</b>)—women). All years are based on EMEF survey data.</p>
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<p>Percentage of SA subclusters for spatial group I.</p>
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<p>Percentage of SA subclusters for spatial group II.</p>
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<p>Percentage of SA subclusters for spatial group III.</p>
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20 pages, 12196 KiB  
Article
Peatland Transformation: Land Cover Changes and Driving Factors in the Kampar Peninsula (1990–2020)
by Dian Novarina, Jatna Supriatna, Iman Santoso and Mahawan Karuniasa
Land 2024, 13(10), 1699; https://doi.org/10.3390/land13101699 - 17 Oct 2024
Viewed by 177
Abstract
The Kampar Peninsula, spanning approximately 735,091 hectares, is critical for its carbon reserves and biodiversity, including the endangered Sumatran tiger. However, nearly half of the 4 million hectares of peat swamp in the region is deforested, drained, decomposing, or burning, largely due to [...] Read more.
The Kampar Peninsula, spanning approximately 735,091 hectares, is critical for its carbon reserves and biodiversity, including the endangered Sumatran tiger. However, nearly half of the 4 million hectares of peat swamp in the region is deforested, drained, decomposing, or burning, largely due to settlements and development projects. This research employs a mixed-method approach, using quantitative spatial analysis of Landsat imagery from 1990 to 2020 based on the Spectral Mixture Analysis (SMA) model to detect forest disturbances and classify land cover changes, utilizing the Normalized Difference Fraction Index (NDFI). Ground truthing validates the image interpretation with field conditions. Additionally, qualitative analysis through interviews and regulatory review examines spatial change trends, context, and driving factors. The result showed, over 30 years, that natural forest in the Kampar Peninsula decreased significantly from 723,895.30 hectares in 1990 to 433,395.20 hectares in 2020. The primary factors driving land use changes include the construction of access roads by oil companies in 1975, leading to extensive deforestation, and government policies during the New Order period that issued forest exploitation concessions and promoted transmigration programs, resulting in widespread establishment of oil palm and acacia plantations. Full article
(This article belongs to the Section Land Systems and Global Change)
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<p>Map of the research area in the Kampar Peninsula, Riau Province.</p>
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<p>Flow chart of selecting and processing data from Landsat imagery.</p>
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<p>Distribution map of ground check data.</p>
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<p>Four classification clusters for identifying land use conditions: (<b>A</b>) Cluster A, consisting of oil and gas industry buildings, and industrial forest plantations—pulp and paper; (<b>B</b>) Cluster B, consisting of residential buildings; (<b>C</b>) oil palm plantation cluster; and (<b>D</b>) acacia industrial forest plantation cluster.</p>
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<p>NDFI change overview (<b>a1</b>) NDFI change map between 1990 and 1993, (<b>a2</b>) NDFI change map between 1998 and 2000, (<b>a3</b>) NDFI change map between 2000 and 2003, (<b>a4</b>) NDFI change map between 2008 and 2010, (<b>a5</b>) NDFI change map between 2010 and 2013, (<b>a6</b>) NDFI change map between 2018 and 2020; (<b>b1</b>) Landsat image 1993, (<b>b2</b>) Landsat image 2000, (<b>b3</b>) Landsat image 2003, (<b>b4</b>) Landsat image 2010, (<b>b5</b>) Landsat image 2013, (<b>b6</b>) Landsat image 2020.</p>
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<p>NDFI change overview (<b>a1</b>) NDFI change map between 1990 and 1993, (<b>a2</b>) NDFI change map between 1998 and 2000, (<b>a3</b>) NDFI change map between 2000 and 2003, (<b>a4</b>) NDFI change map between 2008 and 2010, (<b>a5</b>) NDFI change map between 2010 and 2013, (<b>a6</b>) NDFI change map between 2018 and 2020; (<b>b1</b>) Landsat image 1993, (<b>b2</b>) Landsat image 2000, (<b>b3</b>) Landsat image 2003, (<b>b4</b>) Landsat image 2010, (<b>b5</b>) Landsat image 2013, (<b>b6</b>) Landsat image 2020.</p>
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<p>Land use classification map of 2020 with ground check data.</p>
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<p>Natural forest cover change trend in Kampar Peninsula (1990–2020).</p>
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<p>Land use change map indicating the transition from natural forest to non-forest areas from 1990 to 2020. (<b>a</b>) Changes occurred between 1990 and 1995, and (<b>b</b>) between 2016 and 2020.</p>
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<p>NDFI change detection (1990–1993) in the Mempura Village area on the banks of the Siak River: 1. Benteng Ulu Dock, 2. Tomb of the 2nd Sultan of Siak (<b>a</b>) NDFI change map (1990–1993); (<b>b</b>) Landsat image (1993).</p>
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<p>NDFI change detection (1990–1993) in the Mempura Village area on the banks of the Siak River: (1) Benteng Ulu Dock, (2) Tomb of the 2nd Sultan of Siak, (3) Dayun Village, (4) oil road built 1975–1982, (5) Idris Oil Well, and (6) boundaries of Zamrud National Park (<b>a</b>) NDFI change map (1990–1993); (<b>b</b>) Landsat image (1993).</p>
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<p>NDFI change detection results (1990–1993): Land cover changes occurred at locations a1, a2, and b2 in 1993 (red). Locations b1, Kerinci (8), and Translok (7) experienced previous land cover changes, showing no visual changes (white) and regrowth (light blue). (<b>a</b>) NDFI change map (1990–1993); (<b>b</b>) Landsat image (1993).</p>
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<p>NDFI change detection results (2000–2003): Continued land cover changes and acacia expansion at locations a1 and a2. Location a3 shows land cover changes related to the acacia HTI industry, including a jet runway at location a4. Locations b1 and b2 indicate oil palm plantation expansion. (<b>a</b>) NDFI change map (2000–2003); (<b>b</b>) Landsat image (2003).</p>
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22 pages, 17884 KiB  
Article
Assessment of Carbon Stock and Sequestration Dynamics in Response to Land Use and Land Cover Changes in a Tropical Landscape
by Dipankar Bera, Nilanjana Das Chatterjee, Santanu Dinda, Subrata Ghosh, Vivek Dhiman, Bashar Bashir, Beata Calka and Mohamed Zhran
Land 2024, 13(10), 1689; https://doi.org/10.3390/land13101689 - 16 Oct 2024
Viewed by 319
Abstract
Quantitative analysis of LULC changes and their effects on carbon stock and sequestration is important for mitigating climate change. Therefore, this study examines carbon stock and sequestration in relation to LULC changes using the Land Change Modeler (LCM) and Ecosystem Services Modeler (ESM) [...] Read more.
Quantitative analysis of LULC changes and their effects on carbon stock and sequestration is important for mitigating climate change. Therefore, this study examines carbon stock and sequestration in relation to LULC changes using the Land Change Modeler (LCM) and Ecosystem Services Modeler (ESM) in tropical dry deciduous forests of West Bengal, India. The LULC for 2006, 2014, and 2021 were classified using Google Earth Engine (GEE), while LULC changes and predictions were analyzed using LCM. Carbon stock and sequestration for present and future scenarios were estimated using ESM. The highest carbon was stored in forest land (124.167 Mg/ha), and storage outside the forest declined to 13.541 Mg/ha for agricultural land and 0–8.123 Mg/ha for other lands. Carbon stock and economic value decreased from 2006 to 2021, and are likely to decrease further in the future. Forest land is likely to contribute to 94% of future carbon loss in the study region, primarily due to its conversion into agricultural land. The implementation of multiple-species plantations, securing tenure rights, proper management practices, and the strengthening of forest-related policies can enhance carbon stock and sequestration. These spatial-temporal insights will aid in management strategies, and the methodology can be applied to broader contexts. Full article
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<p>Location of the study area.</p>
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<p>Methodological flow chart for LULC prediction. LULC: land use land cover; MLP-NN: Multi-Layer Perceptron Neural Network.</p>
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<p>Static variables: assuming that these variables remain constant over time.</p>
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<p>Dynamic variables: assuming that these variables change over time. (<b>A</b>) Distance from forest land (meters); (<b>B</b>) distance from agriculture land (meters); (<b>C</b>) distance from water body (meters); (<b>D</b>) distance from built-up land (meters); (<b>E</b>) distance from barren land (meters); (<b>F</b>) population (number/sq.m).</p>
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<p>Constrained areas that are not expected to change in the future.</p>
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<p>Classified and predicted LULC maps for the year 2021.</p>
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<p>Classified LULC maps for the years 2006, 2014, and 2021, and predicted LULC map for the year 2030.</p>
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<p>Dominant transitions or changes from 2006 to 2021.</p>
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<p>Carbon stock and sequestration in Mg/ha. (<b>A</b>) Carbon stock 2006; (<b>B</b>) carbon stock 2021; (<b>C</b>) carbon stock 2030; (<b>D</b>) carbon sequestration from 2006 to 2021; (<b>E</b>) carbon sequestration from 2021 to 2030. FL: forest land; AL: agricultural land; BUL: built-up land; BL: barren land; WB: water body.</p>
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15 pages, 6543 KiB  
Article
Spatiotemporal Dynamics and Driving Factors of Vegetation Greenness in Typical Tourist Region: A Case Study of Hainan Island, China
by Jianchao Guo, Lin Zhang, Shi Qi and Jiadong Chen
Land 2024, 13(10), 1687; https://doi.org/10.3390/land13101687 (registering DOI) - 16 Oct 2024
Viewed by 250
Abstract
Vegetation greenness has been one of the most widely utilized indicators to assess the vegetation growth status for the better ecological environment. However, in typical tourist regions, the impact of the geographical environment, socioeconomic development, and tourism development on vegetation greenness changes is [...] Read more.
Vegetation greenness has been one of the most widely utilized indicators to assess the vegetation growth status for the better ecological environment. However, in typical tourist regions, the impact of the geographical environment, socioeconomic development, and tourism development on vegetation greenness changes is still a challenge. To address this challenge, we used the Google Earth Engine (GEE) cloud platform combined with a series of Landsat remote sensing images to calculate the fractional vegetation cover (FVC) which can be used as an indicator to characterize the spatiotemporal evolution of vegetation greenness in Hainan Island from 2000 to 2020. Furthermore, we employed geographic detector and structural equation models to quantify the relative importance and explanatory power of the geographical environment, socioeconomic development, and tourism development on vegetation greenness changes and to clarify the interaction of mechanisms of various factors in Haikou and Sanya. The results show that the annual growth rate of the FVC in Hainan Island was 0.0025/a. In terms of spatial distribution, the trend of the FVC changes was mainly characterized by non-significant and extremely significant improvement, accounting for 35.34% and 29.38% of the study area. Future vegetation greenness was dominated by weak counter-persistent increase and weak persistent increase. The geographical environmental factors were the main factors affecting vegetation greenness in Haikou, followed by the socioeconomic and the tourism development factors, while the geographical environmental factors also dominate in Sanya, followed by the tourism development factors and finally the socioeconomic factors. Specifically, the spatial distribution of vegetation greenness was primarily influenced by land use types, elevation, slope, and travel services. Geographical environmental factors could indirectly affect changes in socioeconomic and tourism development, thereby indirectly affecting the spatial distribution of vegetation greenness. These findings can provide some significant implications to guide the ecological environmental protection for sustainable development in Hainan Island in China. Full article
(This article belongs to the Section Land Environmental and Policy Impact Assessment)
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<p>Map of the administrative divisions of the study area.</p>
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<p>Interannual trend of FVC in Hainan Island from 2000 to 2020.</p>
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<p>Spatial distribution of annual mean FVC (<b>a</b>) and spatial distribution of significant change in FVC (<b>b</b>) in Hainan Island from 2000 to 2020.</p>
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<p>Spatial distribution of FVC stability (<b>a</b>) and spatial distribution of FVC Hurst index (<b>b</b>) in Hainan Island.</p>
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<p>Persistence of FVC (<b>a</b>) and prediction of future FVC change trend (<b>b</b>) in Hainan Island.</p>
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<p>Factor detection results of FVC changes in Haikou.</p>
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<p>Factor detection results of FVC changes in Sanya.</p>
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<p>Direct and indirect effects of geographical environment, socioeconomic development, and tourism development on FVC in Haikou. Notes: red represents a significant negative impact, green represents a significant positive impact, and the dashed line represents a non-significant impact. * denotes a significant relationship (<span class="html-italic">p</span> &lt; 0.05), ** denotes a very significant relationship (<span class="html-italic">p</span> &lt; 0.01).</p>
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<p>Direct and indirect effects of geographical environment, socioeconomic development, and tourism development on FVC in Sanya. Notes: red represents a significant negative impact, green represents a significant positive impact, and the dashed line represents a non-significant impact. * denotes a significant relationship (<span class="html-italic">p</span> &lt; 0.05), ** denotes a very significant relationship (<span class="html-italic">p</span> &lt; 0.01).</p>
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18 pages, 3814 KiB  
Article
Assessing the Cooling Potential of Vegetation in a Central European Rural Landscape: A Local Study
by Tereza Pohanková and Vilém Pechanec
Land 2024, 13(10), 1685; https://doi.org/10.3390/land13101685 (registering DOI) - 16 Oct 2024
Viewed by 209
Abstract
This study investigates the cooling potential of vegetation in rural landscapes of the Czech Republic to mitigate heat-related issues. Using remote sensing, the Cooling Capacity Index (CCI) is assessed to measure green spaces’ ability to lower air temperatures using evapotranspiration and [...] Read more.
This study investigates the cooling potential of vegetation in rural landscapes of the Czech Republic to mitigate heat-related issues. Using remote sensing, the Cooling Capacity Index (CCI) is assessed to measure green spaces’ ability to lower air temperatures using evapotranspiration and shading. Landsat 8/9 and meteorological data are utilised, with CCI calculated based on vegetation cover, albedo, and evapotranspiration. Our results demonstrate significant variations in cooling capacity across different land use types. Forests exhibited the highest cooling potential, while urban areas, characterised by heat-absorbing materials, displayed the least. We analysed temporal and spatial variations in cooling capacity using various visualisation tools and validated the results against the InVEST software (v3.14.0). This study highlights the effectiveness of remote sensing in quantifying ecosystem functions, particularly the cooling services provided by vegetation. Our findings emphasise the crucial role of vegetation in mitigating urban heat islands and addressing climate change. This research provides valuable insights for developing climate change adaptation strategies in rural landscapes. Full article
(This article belongs to the Special Issue Dynamics of Urbanization and Ecosystem Services Provision II)
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<p>Study area—town Černovice.</p>
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<p>Workflow of our calculation <span class="html-italic">CCI</span>.</p>
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<p>Visualisation development of Cooling Capacity Index during the analysed period.</p>
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<p>Cooling Capacity values progress through imagining dates.</p>
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<p>Land surface temperature values progress through imagining dates.</p>
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<p>Visualisation development of land surface temperature during the analysed period.</p>
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21 pages, 3364 KiB  
Article
Integrated Geospatial and Analytical Hierarchy Process Approach for Assessing Sustainable Management of Groundwater Recharge Potential in Barind Tract
by Md. Zahed Hossain, Sajal Kumar Adhikary, Hrithik Nath, Abdulla Al Kafy, Hamad Ahmed Altuwaijri and Muhammad Tauhidur Rahman
Water 2024, 16(20), 2918; https://doi.org/10.3390/w16202918 - 14 Oct 2024
Viewed by 642
Abstract
Groundwater depletion in Bangladesh’s Barind tract poses significant challenges for sustainable water management. This study aims to delineate groundwater recharge potential zones in this region using an integrated geospatial and Analytical Hierarchy Process (AHP) approach. The methodology combines remote-sensing data with GIS analysis, [...] Read more.
Groundwater depletion in Bangladesh’s Barind tract poses significant challenges for sustainable water management. This study aims to delineate groundwater recharge potential zones in this region using an integrated geospatial and Analytical Hierarchy Process (AHP) approach. The methodology combines remote-sensing data with GIS analysis, considering seven factors influencing groundwater recharge: rainfall, soil type, geology, slope, lineament density, land use/land cover, and drainage density. The AHP method was employed to assess the variability of groundwater recharge potential within the 7586 km2 study area. Thematic maps of relevant factors were processed using ArcGIS software. Results indicate that 9.23% (700.22 km2), 47.68% (3617.13 km2), 37.12% (2816.13 km2), and 5.97% (452.70 km2) of the study area exhibit poor, moderate, good, and very good recharge potential, respectively. The annual recharge volume is estimated at 2554 × 106 m3/year, constituting 22.7% of the total precipitation volume (11,227 × 106 m3/year). Analysis of individual factors revealed that geology has the highest influence (33.57%) on recharge potential, followed by land use/land cover (17.74%), soil type (17.25%), and rainfall (12.25%). The consistency ratio of the pairwise comparison matrix was 0.0904, indicating acceptable reliability of the AHP results. The spatial distribution of recharge zones shows a concentration of poor recharge potential in areas with low rainfall (1200–1400 mm/year) and high slope (6–40%). Conversely, very good recharge potential is associated with high rainfall zones (1800–2200 mm/year) and areas with favorable geology (sedimentary deposits). This study provides a quantitative framework for assessing groundwater recharge potential in the Barind tract. The resulting maps and data offer valuable insights for policymakers and water resource managers to develop targeted groundwater management strategies. These findings have significant implications for sustainable water resource management in the region, particularly in addressing challenges related to agricultural water demand and climate change adaptation. Full article
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<p>Description of study area.</p>
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<p>Methodological flowchart for GW RP derivation.</p>
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<p>Schematic of overlay operation.</p>
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<p>Derived (<b>A</b>) rainfall distribution, (<b>B</b>) slope, (<b>C</b>) geology, (<b>D</b>) drainage density, (<b>E</b>) LULC, (<b>F</b>) lineament density, (<b>G</b>) soil type map of the study area.</p>
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<p>GW potential based on the AHP map.</p>
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23 pages, 48646 KiB  
Article
Land Subsidence Detection Using SBAS- and Stacking-InSAR with Zonal Statistics and Topographic Correlations in Lakhra Coal Mines, Pakistan
by Tariq Ashraf, Fang Yin, Lei Liu and Qunjia Zhang
Remote Sens. 2024, 16(20), 3815; https://doi.org/10.3390/rs16203815 - 14 Oct 2024
Viewed by 435
Abstract
The adverse combination of excessive mining practices and the resulting land subsidence is a significant obstacle to the sustainable growth and stability of regions associated with mining activities. The Lakhra coal mines, which contain some of Pakistan’s largest coal deposits, have been overlooked [...] Read more.
The adverse combination of excessive mining practices and the resulting land subsidence is a significant obstacle to the sustainable growth and stability of regions associated with mining activities. The Lakhra coal mines, which contain some of Pakistan’s largest coal deposits, have been overlooked in land subsidence monitoring, indicating a considerable oversight in the region. Subsidence in mining areas can be spotted early when using Interferometric Synthetic Aperture Radar (InSAR), which can precisely monitor ground changes over time. This study is the first to employ the Small Baseline Subset (SBAS)-InSAR and stacking-InSAR techniques to identify land subsidence at the Lakhra coal mines. This research offers critical insights into subsidence mechanisms in the study area, which has never been previously investigated for ground deformation monitoring, by utilizing 150 Sentinel-1A (ascending) images obtained between January 2018 and September 2023. A total of 102 deformation spots were identified using SBAS-InSAR, while stacking-InSAR detected 73 deformation locations. The most extensive cumulative subsidence in the Lakhra coal mine was −114 mm, according to SBAS-InSAR, with a standard deviation of 6.63 mm. In comparison, a subsidence rate of −19 mm/year was reported using stacking-InSAR with a standard deviation of 1.17 mm/year. The rangeland covered 88.8% of the total area and exhibited the most significant deformation values, as determined by stacking and SBAS-InSAR techniques. Linear regression showed that there was not a strong correlation between subsidence and topographic factors. As detected by optical remote sensing data, the subsidence locations were near or above the mines in the research area, indicating that widespread mining in Lakhra coal mines was the cause of subsidence. Our findings suggest that SAR interferometric time series analysis is helpful for proactively identifying and controlling subsidence difficulties in mining regions by closely monitoring activities, hence reducing negative consequences on operations and the environment. Full article
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<p>Location of the Study Area Lakhra Mines. (<b>A</b>) Top left corner shapefile of Pakistan and area showing Sindh province where Lakhra mines are located. (<b>B</b>) Area of Interest zoomed view.</p>
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<p>(<b>A</b>) Digital Elevation Model of the Study Area. (<b>B</b>) Land Cover Map.</p>
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<p>SBAS- and Stacking-InSAR Workflow.</p>
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<p>Interferogram Network and Average Spatial Coherence.</p>
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<p>(<b>A</b>) Stacking-InSAR Results. (<b>B</b>,<b>C</b>) Magnified View and Profile Plot, Respectively.</p>
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<p>(<b>A</b>,<b>B</b>) Magnified view of (Stacking) deformation in Upper and Lower Lakhra overlaid on satellite imagery, respectively.</p>
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<p>Enlarged Google Earth Image of the Upper (<b>left side</b>) and Lower Lakhra (<b>right side</b>).</p>
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<p>SBAS-InSAR Results. (<b>A</b>) Displacement Rates in Lakhra Coal Mines. (<b>B</b>,<b>C</b>) Magnified View and Profile Plot, Respectively.</p>
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<p>(<b>A</b>,<b>B</b>) Magnified View of SBAS Accumulative Deformation in the Upper and Lower Lakhra Overlaid on Satellite Imagery, Respectively.</p>
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<p>SBAS-InSAR Time Series (2018–2023).</p>
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<p>Terrain Factors and SBAS-InSAR Deformation Distribution. (<b>A</b>–<b>C</b>) Connection of aspect, slope, and elevation with land deformation, respectively.</p>
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<p>SBAS- and Stacking-InSAR Standard Deviation Plot.</p>
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<p>SBAS-InSAR Time-Series Plot of 10 Locations from Upper (<b>A</b>) and Lower (<b>B</b>) Lakhra Mines.</p>
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<p>Expansion of Mines and Subsidence in the Lower Lakhra in 2018–2023. (<b>A</b>,<b>B</b>) Google Earth images of mines from 2018–2023 (<b>C</b>,<b>D</b>) subsidence observed during 2018–2023.</p>
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<p>Shaft Mining in Lakhra Coal Mines. Source: Mineral Transformation Plan Vision 2025, Government of Pakistan.</p>
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<p>Coal Production in Pakistan. Source: BP Statistical Review 2022 and Pakistan Energy Yearbook 2022.</p>
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23 pages, 16985 KiB  
Article
Analysis of Spatiotemporal Predictions and Drivers of Carbon Storage in the Pearl River Delta Urban Agglomeration via the PLUS-InVEST-GeoDetector Model
by Jinghang Cai, Hui Chi, Nan Lu, Jin Bian, Hanqing Chen, Junkeng Yu and Suqin Yang
Energies 2024, 17(20), 5093; https://doi.org/10.3390/en17205093 - 14 Oct 2024
Viewed by 401
Abstract
Land use and land cover change (LUCC) significantly influences the dynamics of carbon storage in thin terrestrial ecosystems. Investigating the interplay between land use alterations and carbon sequestration is crucial for refining regional land use configurations, sustaining the regional carbon balance, and augmenting [...] Read more.
Land use and land cover change (LUCC) significantly influences the dynamics of carbon storage in thin terrestrial ecosystems. Investigating the interplay between land use alterations and carbon sequestration is crucial for refining regional land use configurations, sustaining the regional carbon balance, and augmenting regional carbon storage. Using land use data from the Pearl River Delta Urban Agglomeration (PRDUA) from 2010 to 2020, this study employed PLUS-InVEST models to analyze the spatiotemporal dynamics of land use and carbon storage. Projections for the years 2030, 2040, and 2050 were performed under three distinct developmental scenarios, namely, natural development (ND), city priority development (CPD), and ecological protection development (EPD), to forecast changes in land use and carbon storage. The geographic detector model was leveraged to dissect the determinants of the spatial and temporal variability of carbon storage, offering pertinent recommendations. The results showed that (1) during 2010–2020, the carbon storage in the PRDUA showed a decreasing trend, with a total decrease of 9.52 × 106 Mg, and the spatial distribution of carbon density in the urban agglomeration was imbalanced and showed an overall trend in increasing from the center to the periphery. (2) Clear differences in carbon storage were observed among the three development scenarios of the PRDUA between 2030 and 2050. Only the EPD scenario achieved an increase in carbon storage of 1.10 × 106 Mg, and it was the scenario with the greatest potential for carbon sequestration. (3) Among the drivers of the evolution of spatial land use patterns, population, the normalized difference vegetation index (NDVI), and distance to the railway had the greatest influence on LUCC. (4) The annual average temperature, annual average rainfall, and GDP exerted a significant influence on the spatiotemporal dynamics of carbon storage in the PRDUA, and the interactions between the 15 drivers and changes in carbon storage predominantly manifested as nonlinear and double-factor enhancements. The results provide a theoretical basis for future spatial planning and achieving carbon neutrality in the PRDUA. Full article
(This article belongs to the Special Issue Energy Transitions: Low-Carbon Pathways for Sustainability)
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<p>Research framework.</p>
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<p>Location of the study area.</p>
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<p>Drivers of LUCC in the PRDUA.</p>
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<p>Distribution of land use types and a Sankey diagram of mutual conversion.</p>
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<p>Distribution of carbon storage and areas where carbon storage changed.</p>
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<p>Distribution of land use types under the multi-scenario simulations in 2030–2050.</p>
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<p>Interconversion of land use types under the multi-scenario simulation in 2030–2050.</p>
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<p>Map of high and low carbon storage distribution areas and their refinement under a multi-scenario simulation (a1, a4, a7, b1, b4, b7, c1, c4, c7 represent the same area; a2, a5, a8, b2, b5, b8, c2, c5, c8 represent the same area; a3, a6, a9, b3, b6, b9, c3, c6, c9 represent the same area).</p>
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<p>Distribution area of carbon storage changes under multi-scenario simulation.</p>
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<p>Contribution of the 15 drivers to the land use types.</p>
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<p>Average values of the 15 drivers for the main land types influencing LUCC.</p>
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<p>Dominant interactive factors of carbon storage changes in 2020 (X1 is distance to railway, X2 is annual average rainfall, X3 is slope, X4 is soi1, X5 is distance to the secondary trunk road, X6 is annual average temperature, X7 is aspect of slope, X8 is sistance to city center, X9 is distance to expressway, X10 is distance to trunk road, X11 is DEM, X12 is GDP, X13 is NDVI, X14 is population, X15 is distance to river).</p>
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14 pages, 6760 KiB  
Article
Integrating Machine Learning, Land Cover, and Hydrological Modeling to Contribute Parameters for Climate Impacts on Water Resource Management
by Joonghyeok Heo, Jeongho Lee, Yunjung Hyun and Joonkyu Park
Sustainability 2024, 16(20), 8805; https://doi.org/10.3390/su16208805 - 11 Oct 2024
Viewed by 567
Abstract
The purpose of this study is to establish basic policies for managing the impacts of climate change on water resources using the integration of machine learning and land cover modeling. We predicted future changes in land cover within the water management and assessed [...] Read more.
The purpose of this study is to establish basic policies for managing the impacts of climate change on water resources using the integration of machine learning and land cover modeling. We predicted future changes in land cover within the water management and assessed its vulnerability to climate change. After confirming this vulnerability, we considered measures to improve climate resilience and presented future water resource parameters. We reviewed the finances available to promote climate projects, noting the major river management funds. The future project will serve as a stepping stone to promote climate resilience projects addressing water resource challenges exacerbated by future climate change. The study examined the results of analyzing changes in land cover maps due to climate change and assessed vulnerability in water management areas until 2050. According to the analysis results, the regulations for our study areas were set lower than those for other water management zones, resulting in a high rate of urbanization. Therefore, the climate resilience project in the water management area should be implemented first, despite the need for a long-term view in adapting to climate change. Full article
(This article belongs to the Section Sustainable Water Management)
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<p>A perceptron expressed in a formula.</p>
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<p>Multi-Layer Perception (MLP) neural network diagram in our study.</p>
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<p>Transition potential analysis between different land use types: (<b>a</b>) bare area urbanization, (<b>b</b>) forest urbanization, (<b>c</b>) forest farmland, (<b>d</b>) farmland urbanization.</p>
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<p>Comparison between (<b>a</b>) the actual land cover map and (<b>b</b>) the LCM model result.</p>
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<p>ROC analysis result.</p>
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<p>Historical land cover maps for (<b>a</b>) 1990 and (<b>b</b>) 2000.</p>
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<p>Water supply management area subjected to the analysis.</p>
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<p>Input data for land cover transition potential analysis using MLP.</p>
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<p>Land-use changes in 2050 for (<b>a</b>) Han River, (<b>b</b>) Geum River, (<b>c</b>) Seomjin River area, and (<b>d</b>) Nakdong River area.</p>
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<p>Predicted water balance distribution in 2050 for (<b>a</b>) Han River, (<b>b</b>) Geum River, (<b>c</b>) Seomjin River area, and (<b>d</b>) Nakdong River area.</p>
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26 pages, 5700 KiB  
Article
Remote Sensing-Based Drought Monitoring in Iran’s Sistan and Balouchestan Province
by Kamal Omidvar, Masoume Nabavizadeh, Iman Rousta and Haraldur Olafsson
Atmosphere 2024, 15(10), 1211; https://doi.org/10.3390/atmos15101211 - 10 Oct 2024
Viewed by 265
Abstract
Drought is a natural phenomenon that has adverse effects on agriculture, the economy, and human well-being. The primary objective of this research was to comprehensively understand the drought conditions in Sistan and Balouchestan Province from 2002 to 2017 from two perspectives: vegetation cover [...] Read more.
Drought is a natural phenomenon that has adverse effects on agriculture, the economy, and human well-being. The primary objective of this research was to comprehensively understand the drought conditions in Sistan and Balouchestan Province from 2002 to 2017 from two perspectives: vegetation cover and hydrology. To achieve this goal, the study utilized MODIS satellite data in the first part to monitor vegetation cover as an indicator of agricultural drought. In the second part, GRACE satellite data were employed to analyze changes in groundwater resources as an indicator of hydrological drought. To assess vegetation drought, four indices were used: Vegetation Health Index (VHI), Vegetation Drought Index (VDI), Visible Infrared Drought Index (VSDI), and Temperature Vegetation Drought Index (TVDI). To validate vegetation drought indices, they were compared with Global Land Data Assimilation System (GLDAS) precipitation data. The vegetation indices showed a strong, statistically significant correlation with GLDAS precipitation data in most regions of the province. Among all indices, the VHI showed the highest correlation with precipitation (moderate (0.3–0.7) in 51.7% and strong (≥0.7) in 45.82% of lands). The output of vegetation indices revealed that the study province has experienced widespread drought in recent years. The results showed that the southern and central regions of the province have faced more severe drought classes. In the second part of this research, hydrological drought monitoring was conducted in fifty third-order sub-basins located within the study province using the Total Water Storage (TWS) deficit, Drought Severity, and Total Storage Deficit Index )TSDI Index). Annual average calculations of the TWS deficit over the period from April 2012 to 2016 indicated a substantial depletion of groundwater reserves in the province, amounting to a cumulative loss of 12.2 km3 Analysis results indicate that drought severity continuously increased in all study basins until the end of the study period. Studies have shown that all the studied basins are facing severe and prolonged water scarcity. Among the 50 studied basins, the Rahmatabad basin, located in the semi-arid northern regions of the province, has experienced the most severe drought. This basin has experienced five drought events, particularly one lasting 89 consecutive months and causing a reduction of more than 665.99 km3. of water in month 1, placing it in a critical condition. On the other hand, the Niskoofan Chabahar basin, located in the tropical southern part of the province near the Sea of Oman, has experienced the lowest reduction in water volume with 10 drought events and a decrease of approximately 111.214 km3. in month 1. However, even this basin has not been spared from prolonged droughts. Analysis of drought index graphs across different severity classes confirmed that all watersheds experienced drought conditions, particularly in the later years of this period. Data analysis revealed a severe water crisis in the province. Urgent and coordinated actions are needed to address this challenge. Transitioning to drought-resistant crops, enhancing irrigation efficiency, and securing water rights are essential steps towards a sustainable future. Full article
(This article belongs to the Section Meteorology)
18 pages, 3599 KiB  
Article
Rapid Appraisal of Wildlife Corridor Viability with Geospatial Modelling and Field Data: Lessons from Makuyuni, Tanzania
by Emmanuel H. Lyimo, Gabriel Mayengo, Kwaslema M. Hariohay, Joseph Holler, Alex Kisingo, David J. Castico, Niwaeli E. Kimambo, Justin Lucas, Emanuel H. Martin and Damian Nguma
Land 2024, 13(10), 1647; https://doi.org/10.3390/land13101647 - 9 Oct 2024
Viewed by 659
Abstract
Connectivity between protected areas is necessary to prevent habitat fragmentation. Biodiverse countries like Tanzania craft legislation to promote habitat connectivity via the creation of ecological corridors, but their viability for wildlife often remains unknown. We therefore develop a scalable and replicable approach to [...] Read more.
Connectivity between protected areas is necessary to prevent habitat fragmentation. Biodiverse countries like Tanzania craft legislation to promote habitat connectivity via the creation of ecological corridors, but their viability for wildlife often remains unknown. We therefore develop a scalable and replicable approach to assess and monitor multispecies corridor viability using geospatial modeling and field data. We apply and test the approach in the Makuyuni study area: an unprotected ecological corridor connecting Tarangire National Park to Essmingor mountain, Makuyuni Wildlife Park and Mto Wa Mbu Game Controlled Area. We analyzed the viability of Makuyuni as an ecological corridor by creating and validating a geospatial least-cost corridor model with field observations of wildlife and livestock. We created the model from publicly available spatial datasets augmented with manual digitization of pastoral homesteads (bomas). The least-cost corridor model identified two likely pathways for wildlife, confirmed and validated with field observations. Locations with low least-cost values were significantly correlated with more wildlife observations (Spearman’s rho = −0.448, p = 0.002). Our findings suggest that Makuyuni is a viable ecological corridor threatened by development and land use change. Our methodology presents a replicable approach for both monitoring Makuyuni and assessing corridor viability more generally. The incorporation of manually digitized homesteads (bomas) and field-based livestock observations makes corridor assessment more robust by taking into account pastoral land uses that are often missing in land cover maps. Integration of geospatial analysis and field observations is key for the robust identification of corridors for habitat connectivity. Full article
(This article belongs to the Section Landscape Ecology)
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<p>Makuyuni study site, survey transects (lines numbered with transect ID), and nearby conservation areas [<a href="#B43-land-13-01647" class="html-bibr">43</a>].</p>
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<p>Conceptual workflow for least-cost corridor model and validation. <a href="#sec2dot2dot1-land-13-01647" class="html-sec">Section 2.2.1</a>, <a href="#sec2dot2dot2-land-13-01647" class="html-sec">Section 2.2.2</a>, <a href="#sec2dot3dot1-land-13-01647" class="html-sec">Section 2.3.1</a> and <a href="#sec2dot3dot2-land-13-01647" class="html-sec">Section 2.3.2</a>.</p>
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<p>Map of the Makuyuni study area showing inputs for the least-cost corridor model, as listed in <a href="#land-13-01647-t001" class="html-table">Table 1</a>.</p>
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<p>Modeled least-cost corridors that are locations with low cost of movement (blue) relative to the rest of the study area. Overlaid are “observed corridors,” generated by digitizing regions with high wildlife counts in field surveys. The most western “observed corridor” measures 7065 ha, while the most eastern one measures 7552 ha.</p>
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<p>Wildlife density based on total count of individuals of all wildlife species encountered during the field transect survey (kernel diameter = 300 m). Numbered lines indicate survey transects.</p>
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<p>Livestock density based on total count of individual livestock (sheep, goats, cows, donkeys) encountered during the field transect survey (kernel diameter = 300 m). Numbered lines indicate survey transects.</p>
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<p>QGIS graphic model for the least-cost wildlife corridor analysis.</p>
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<p>Sample land cover types across the Tarangire–Manyara ecosystem. Photographs are illustrative of flora and fauna of the ecosystem and do not all originate from the Makuyuni study area. Credit: Salum Mpapa.</p>
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22 pages, 11903 KiB  
Article
Remote Sensing Mapping and Analysis of Spatiotemporal Patterns of Land Use and Cover Change in the Helong Region of the Loess Plateau Region (1986–2020)
by Jingyu Li, Yangbo Chen, Yu Gu, Meiying Wang and Yanjun Zhao
Remote Sens. 2024, 16(19), 3738; https://doi.org/10.3390/rs16193738 - 8 Oct 2024
Viewed by 550
Abstract
Land use and cover change (LUCC) is directly linked to the sustainability of ecosystems and the long-term well-being of human society. The Helong Region in the Loess Plateau has become one of the areas most severely affected by soil and water erosion in [...] Read more.
Land use and cover change (LUCC) is directly linked to the sustainability of ecosystems and the long-term well-being of human society. The Helong Region in the Loess Plateau has become one of the areas most severely affected by soil and water erosion in China due to its unique geographical location and ecological environment. The long-term construction of terraces and orchards is one of the important measures for this region to combat soil erosion. Despite the important role that terraces and orchards play in this region, current studies on their extraction and understanding remain limited. For this reason, this study designed a land use classification system, including terraces and orchards, to reveal the patterns of LUCC and the effectiveness of ecological restoration projects in the area. Based on this system, this study utilized the Random Forest classification algorithm to create an annual land use and cover (LUC) dataset for the Helong Region that covers eight periods from 1986 to 2020, with a spatial resolution of 30 m. The validation results showed that the maps achieved an average overall accuracy of 87.54% and an average Kappa coefficient of 76.94%. This demonstrates the feasibility of the proposed design and land coverage mapping method in the study area. This study found that, from 1986 to 2020, there was a continuous increase in forest and grassland areas, a significant reduction in cropland and bare land areas, and a notable rise in impervious surface areas. We emphasized that the continuous growth of terraces and orchards was an important LUCC trend in the region. This growth was primarily attributed to the conversion of grasslands, croplands, and forests. This transformation not only reduced soil erosion but also enhanced economic efficiency. The products and insights provided in this study help us better understand the complexities of ecological recovery and land management. Full article
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<p>Location of Helong Region.</p>
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<p>Workflow of this study.</p>
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<p>Number of Landsat scenes used in the GEE image synthesis.</p>
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<p>Anomaly screening and repair of Landsat data (<b>a</b>) filling missing data (<b>b</b>) repairing Landsat 7 image gaps.</p>
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<p>Distribution of the training sample polygons at different times and in different categories.</p>
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<p>Validation of the spatial distribution of the sample set.</p>
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<p>Temporal distribution of area changes for various LUC types in the Helong Region (the proportion of change on the right axis is relative to the area change ratio with respect to the base year (1986)).</p>
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<p>Spatial distribution of LUC change rates in the Helong Region. (Through linear regression, we calculated the area ratio change rates for each category within each grid (0.1°) from 1986 to 2020, and the spatial distributions of the area ratio changes that were found to be significant (<span class="html-italic">p</span> &lt; 0.05) are displayed. In the figure, gray grids represent results with insignificant changes or changes below 0.1% per year (−0.1 to 0.1)).</p>
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<p>Spatial and temporal distributions of forests, grasslands, and croplands transformed into terraces and orchards.</p>
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<p>Heat map of the transitions of LUC types in two adjacent periods.</p>
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<p>Comparison of the accuracy of HL-LUC, FROM-GLC, CLC-FCS30, and ESA CCI-LC.</p>
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<p>Comparison of HL-LUC-2015 with the three other datasets.</p>
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21 pages, 13152 KiB  
Article
Analysis of Spatial and Temporal Trends of Vegetation Cover Evolution and Its Driving Forces from 2000 to 2020—A Case Study of the WuShen Counties in the Maowusu Sandland
by Zeyu Zhao, Xiaomin Liu, Tingxi Liu, Yingjie Wu, Wenjuan Wang, Yun Tian and Laichen Fu
Forests 2024, 15(10), 1762; https://doi.org/10.3390/f15101762 - 8 Oct 2024
Viewed by 413
Abstract
The WuShen counties in the hinterland of the Maowusu Sandland are located in the “ecological stress zone” of the forest–steppe desert, with low vegetation cover, a strong ecosystem sensitivity, and poor stability under the influence of human activities. Therefore, it is important to [...] Read more.
The WuShen counties in the hinterland of the Maowusu Sandland are located in the “ecological stress zone” of the forest–steppe desert, with low vegetation cover, a strong ecosystem sensitivity, and poor stability under the influence of human activities. Therefore, it is important to study and analyze the changes in vegetation growth in this region for the purpose of objectively evaluating the effectiveness of desertification control in China’s agricultural and pastoral intertwined zones, and formulating corresponding measures in a timely manner. In this paper, the spatial and temporal variations in the vegetation NDVI in the WuShen counties of the Maowusu Sandland and their response relationships with driving factors were investigated by using a trend test, center of gravity transfer model, partial correlation calculation, and residual analysis, and by using the MOD13A3 vegetation NDVI time series data from 2000 to 2020, as well as the precipitation, temperature, and potential evapotranspiration data from the same period. The results showed the following: ① The regional vegetation NDVI did not fluctuate significantly with latitude and longitude, and the NDVI varied between 0.227 and 0.375 over the 21-year period, with a mean increase of 0.13 for the region as a whole and an increase of 0.61 for the region of greatest change. Of the area, 86.83% experienced a highly significant increase, and the trend in increase around rivers and towns was higher than that in the northwestern inland flow area, with the overall performance of “low in the west and high in the east”. ② Only 2.07% of the vegetation NDVI center of gravity did not shift, and the response with climate factors was mainly characterized by having consistent or opposite center of gravity changes with precipitation and potential evapotranspiration. ③ Human activities have been the dominant factor in the vegetation NDVI change, with 75.89 percent of the area positively impacted by human activities, and human activities in the southwest inhibiting the improvement of vegetation in the area. The impact of human activities on the unchanged land type area is increasing, most obviously in the farmland area, and the impact of human activities on the changed land type area is gradually decreasing in the area where the farmland becomes impervious. The vegetation in the area above 1300 m above sea level is degraded by the environment and human activities. The research results can provide scientific support for the implementation of ecological fine management and the formulation of corresponding ecological restoration and desertification control measures in the Maowusu Sandland. At the same time, it is expected to serve as a baseline for other studies on the evolution of vegetation in agro-pastoral zones. Full article
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<p>Overview of the study area.</p>
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<p>Temporal variation characteristics of NDVI and driver factors. (<b>a</b>). Characterization of trends with longitude. (<b>b</b>). Characterization of trends with latitude. (<b>c</b>). NDVI and interannual variability of climate factors.</p>
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<p>Temporal variation characteristics of NDVI and driver factors. (<b>a</b>). Characterization of trends with longitude. (<b>b</b>). Characterization of trends with latitude. (<b>c</b>). NDVI and interannual variability of climate factors.</p>
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<p>Spatial and temporal trends of NDVI and driving factors. (<b>a</b>). Trends in NDVI. (<b>b</b>). NDVI trend test. (<b>c</b>). Precipitation test statistics. (<b>d</b>). Temperature test statistics. (<b>e</b>). PET test statistics.</p>
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<p>Spatial and temporal trends of NDVI and driving factors. (<b>a</b>). Trends in NDVI. (<b>b</b>). NDVI trend test. (<b>c</b>). Precipitation test statistics. (<b>d</b>). Temperature test statistics. (<b>e</b>). PET test statistics.</p>
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<p>NDVI and driver gravity shift characteristics. (<b>a</b>). NDVI center of gravity shift. (<b>b</b>). Shift in precipitation center of gravity. (<b>c</b>). Shift in the center of gravity of average temperature. (<b>d</b>). PET center of gravity shift.</p>
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<p>Center of gravity shift responses between NDVI and driver factors. (<b>a</b>). NDVI and precipitation response. (<b>b</b>). NDVI and temperature response. (<b>c</b>). NDVI and PET response. (<b>d</b>). Precipitation and temperature response. (<b>e</b>). Precipitation and PET response. (<b>f</b>). Temperature and PET response.</p>
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<p>Partial correlation analysis between NDVI and driving factors. (<b>a</b>). NDVI and precipitation bias. (<b>b</b>). NDVI and temperature bias. (<b>c</b>). NDVI and PET bias. (<b>d</b>). NDVI and precipitation <span class="html-italic">t</span>-test. (<b>e</b>). NDVI and temperature <span class="html-italic">t</span>-test. (<b>f</b>). NDVI and PET <span class="html-italic">t</span>-test.</p>
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<p>Response relationship between NDVI and driver factors. (<b>a</b>). Residual trend analysis. (<b>b</b>). Relative role of climate change. (<b>c</b>). Relative role of human activities. (<b>d</b>). Dominant factors.</p>
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<p>Changes in land-use types from 2000 to 2020.</p>
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<p>Response of vegetation to driving factors in different land-use regions.</p>
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<p>Response of vegetation at different elevations to driving factors.</p>
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19 pages, 24334 KiB  
Article
A 40-Year Time Series of Land Surface Emissivity Derived from AVHRR Sensors: A Fennoscandian Perspective
by Mira Barben, Stefan Wunderle and Sonia Dupuis
Remote Sens. 2024, 16(19), 3686; https://doi.org/10.3390/rs16193686 - 2 Oct 2024
Viewed by 424
Abstract
Accurate land surface temperature (LST) retrieval depends on precise knowledge of the land surface emissivity (LSE). Neglecting or inaccurately estimating the emissivity introduces substantial errors and uncertainty in LST measurements. The emissivity, which varies across different surfaces and land uses, reflects material composition [...] Read more.
Accurate land surface temperature (LST) retrieval depends on precise knowledge of the land surface emissivity (LSE). Neglecting or inaccurately estimating the emissivity introduces substantial errors and uncertainty in LST measurements. The emissivity, which varies across different surfaces and land uses, reflects material composition and surface roughness. Satellite data offer a robust means to determine LSE at large scales. This study utilises the Normalised Difference Vegetation Index Threshold Method (NDVITHM) to produce a novel emissivity dataset spanning the last 40 years, specifically tailored for the Fennoscandian region, including Norway, Sweden, and Finland. Leveraging the long and continuous data series from the Advanced Very High Resolution Radiometer (AVHRR) sensors aboard the NOAA and MetOp satellites, an emissivity dataset is generated for 1981–2022. This dataset incorporates snow-cover information, enabling the creation of annual emissivity time series that account for winter conditions. LSE time series were extracted for six 15 × 15 km study sites and compared against the Moderate Resolution Imaging Spectroradiometer (MODIS) MOD11A2 LSE product. The intercomparison reveals that, while both datasets generally align, significant seasonal differences exist. These disparities are attributable to differences in spectral response functions and temporal resolutions, as well as the method considering fixed values employed to calculate the emissivity. This study presents, for the first time, a 40-year time series of the emissivity for AVHRR channels 4 and 5 in Fennoscandia, highlighting the seasonal variability, land-cover influences, and wavelength-dependent emissivity differences. This dataset provides a valuable resource for future research on long-term land surface temperature and emissivity (LST&E) trends, as well as land-cover changes in the region, particularly with the use of Sentinel-3 data and upcoming missions such as EUMETSAT’s MetOp Second Generation, scheduled for launch in 2025. Full article
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Graphical abstract

Graphical abstract
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<p>Spectral emissivities of different land-cover classes, as recorded in the ECOSTRESS spectral library [<a href="#B41-remotesensing-16-03686" class="html-bibr">41</a>,<a href="#B42-remotesensing-16-03686" class="html-bibr">42</a>].</p>
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<p>The study area across Norway, Sweden, and Finland, showing the six chosen study sites (15 × 15 km each). The abbreviations indicating the study sites stand for Low Vegetation (LV) or Forest (F) and South (S), Mid-Latitude (ML), or North (N). The base map is the ESA CCI Land-Cover Dataset [<a href="#B43-remotesensing-16-03686" class="html-bibr">43</a>].</p>
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<p>Schematic workflow showing the AVHRR data preparation, emissivity dataset calculation process, and incorporated auxiliary data.</p>
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<p>Overview of the availability of AVHRR data since 1981 in the local archive. The data used for this study are indicated in blue-grey, while the data excluded from the analysis due to quality or processing issues are indicated in orange.</p>
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<p>The 40-year time series of monthly mean land surface emissivities for the 15 × 15 km low-vegetation southern (LVS) study site.</p>
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<p>Mean annual cycle of LSE for channel 4, including the confidence interval (1 <math display="inline"><semantics> <mi>σ</mi> </semantics></math>), for the 40-year period for the 15 × 15 km low-vegetation southern (LVS) study site.</p>
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<p>(<b>a</b>) Land cover (ESA CCI; see <a href="#remotesensing-16-03686-f002" class="html-fig">Figure 2</a> for details) and emissivity differences (Ch5–Ch4) derived from the monthly mean emissivity values over the 40-year period (1981–2022) for an area of 1° × 1° around the FN site in February (<b>b</b>) and July (<b>c</b>).</p>
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<p>(<b>a</b>) Land cover (ESA CCI; see <a href="#remotesensing-16-03686-f002" class="html-fig">Figure 2</a> for details) and emissivity differences (Ch5–Ch4) derived from the monthly mean emissivity values over the 40-year period (1981–2022) for an area of 1° × 1° around the FS site in February (<b>b</b>) and July (<b>c</b>).</p>
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<p>Comparison of the AVHRR LAC LSE dataset and the MODIS MOD11A2 LSE dataset for the low-vegetation southern (LVS) study site (2015–2022).</p>
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