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24 pages, 18018 KiB  
Article
Analysis of Land Surface Performance Differences and Uncertainty in Multiple Versions of MODIS LST Products
by Ruoyi Zhao, Wenping Yu, Xiangyi Deng, Yajun Huang, Wen Yang and Wei Zhou
Remote Sens. 2024, 16(22), 4255; https://doi.org/10.3390/rs16224255 - 15 Nov 2024
Viewed by 62
Abstract
Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature (LST) products are essential data sources for global and regional climate change research. Currently, several versions of the MODIS LST product have been released, yet the performance differences and uncertainties they introduce in land surface [...] Read more.
Moderate Resolution Imaging Spectroradiometer (MODIS) Land Surface Temperature (LST) products are essential data sources for global and regional climate change research. Currently, several versions of the MODIS LST product have been released, yet the performance differences and uncertainties they introduce in land surface studies remain insufficiently addressed. To bridge this gap, this study focuses on four distinct versions of the LST product: MxD11A1 Collection 5 (C5), Collection 6 (C6), Collection 6.1 (C6.1), and MxD21A1 Collection 6.1 (MxD21). The spatial resolution of all product generations is 1 km, and the temporal resolution is 0.5 days. This study provides a comprehensive analysis of the errors arising from different generations of these products in various land surface process studies. The error assessment includes cross-comparisons between product versions and evaluations of the absolute errors generated. Absolute errors in evaluation data were collected from 13 surface sites within the Heihe Watershed Allied Telemetry Experimental Research (HiWATER) project during the period 2013–2018. Cross-validation results show that the largest difference between C5 and C6.1 occurs over bare land, with an RMSE of approximately 1.45 K, while there is no significant change between C6 and C6.1. MOD21 shows considerable variation compared to C6.1 at night across different land cover types, with RMSE over cropland exceeding 2 K. The temperature difference between MOD21 and C6.1 is more pronounced at night (2.01 K) than during the day (0.30 K). Validation results based on temperature indicate that C5 has greater uncertainty compared to C6, especially over bare land, where errors are 2.06 K and 1.06 K, respectively. Furthermore, MxD21 demonstrates significant day–night performance discrepancies, with an average bias of 0.10 K at night, while daytime errors over bare land can reach 2 K, potentially influenced by atmospheric conditions. Based on the research in this paper, it is possible to clarify the performance of different versions of MODIS products, reflecting the appropriateness of their past applications; on the other hand, it is recommended to prioritize the use of the MxD11A1 C6 and C6.1 products for monitoring and applications in bare soil areas to ensure higher accuracy. Furthermore, for day and night monitoring, it may be beneficial to alternate between the MxD11A1 and MxD21A1 products to fully leverage their respective advantages and enhance overall monitoring effectiveness. Full article
(This article belongs to the Special Issue Remote Sensing for Land Surface Temperature and Related Applications)
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<p>The study area and the site locations in the Heihe River Basin.</p>
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<p>Scatter plot of the correlation between MOD11A1 C5, MOD11A1 C6, and MOD21A1 C6.1 with MOD11A1 C6.1 LST during the daytime (<b>a</b>–<b>c</b>) and nighttime (<b>d</b>–<b>f</b>).</p>
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<p><b>The</b> BIAS and RMSE of different land surface covers MOD11A1 C5, MOD11A1 C6, and MOD21A1 C6.1 with respect to MOD11A1 C6.1 LST during the daytime (<b>a</b>,<b>b</b>) and nighttime (<b>c</b>,<b>d</b>).</p>
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<p>Boxplot of monthly scale temperature differences between MOD11A1 C5, MOD11A1 C6, and MOD21A1 C6.1 compared to MOD11A1 C6.1 LST during the daytime (<b>a</b>–<b>c</b>) and nighttime (<b>d</b>–<b>f</b>).</p>
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<p>Line graphs of the different land surface covers of MOD11A1 C5, MOD11A1 C6, and MOD21A1 C6.1 temperature differences compared to MOD11A1 C6.1 LST across four seasons during the daytime.</p>
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<p>Line graphs of the different land surface covers of MOD11A1 C5, MOD11A1 C6, and MOD21A1 C6.1 temperature differences compared to MOD11A1 C6.1 LST across four seasons during the nighttime.</p>
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<p>Comparison of emissivity between different land surface covers in C5 and C6.1 (<b>a</b>: Emissivity in MODIS b31, <b>b</b>: Emissivity in MODIS b32, <b>c</b>: Emissivity mean, <b>d</b>: Emissivity difference).</p>
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<p>The annual mean differences for 2013, daytime: (<b>a</b>) C5-C6.1, (<b>b</b>) C6-C6.1, (<b>c</b>) MOD21-C6.1; nighttime: (<b>d</b>) C5-C6.1, (<b>e</b>) C6-C6.1, (<b>f</b>) MOD21-C6.1.</p>
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<p>The temperature difference distribution map for MODIS LST products on the 282nd day, daytime: (<b>a</b>) C5-C6.1, (<b>b</b>) C6-C6.1, (<b>c</b>) MOD21-C6.1; nighttime: (<b>d</b>) C5-C6.1, (<b>e</b>) C6-C6.1, (<b>f</b>) MOD21-C6.1.</p>
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<p>Line graphs of different land surface cover temperature differences from 2013 to 2018 for MOD11A1 C6 and MOD21A1 C6.1 compared to MOD11A1 C6.1 during daytime.</p>
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<p>Line graphs of different land surface cover temperature differences from 2013 to 2018 for MOD11A1 C6 and MOD21A1 C6.1 compared to MOD11A1 C6.1 during nighttime.</p>
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<p>Line plot of monthly average BIASs for MOD11 C6, C6.1, and MOD21 for 2013–2018 during daytime.</p>
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<p>Line plot of monthly average BIASs for MOD11 C6, C6.1, and MOD21 for 2013–2018 during nighttime.</p>
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<p>Line plot of monthly average BIASs for MYD11 C6, C6.1, and MYD21 for 2013–2018 during daytime.</p>
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<p>Line plot of monthly average BIASs for MYD11 C6, C6.1, and MYD21 for 2013–2018 during nighttime.</p>
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30 pages, 9808 KiB  
Article
Multi-Criteria Analysis for Geospatialization of Potential Areas for Water Reuse in Irrigated Agriculture in Hydrographic Regions
by Ana Paula Pereira Carvalho, Ana Claudia Pereira Carvalho, Mirian Yasmine Krauspenhar Niz, Fabrício Rossi, Giovana Tommaso and Tamara Maria Gomes
Agronomy 2024, 14(11), 2689; https://doi.org/10.3390/agronomy14112689 - 15 Nov 2024
Viewed by 191
Abstract
As the climate crisis progresses, droughts and the seasonal availability of fresh water are becoming increasingly common in different regions of the world. One solution to tackle this problem is the reuse of treated wastewater in agriculture. This study was carried out in [...] Read more.
As the climate crisis progresses, droughts and the seasonal availability of fresh water are becoming increasingly common in different regions of the world. One solution to tackle this problem is the reuse of treated wastewater in agriculture. This study was carried out in two significant hydrographic regions located in the southeast of Brazil (Mogi Guaçu River Water Management Unit—UGRHI-09 and Piracicaba River Basin—PRB) that have notable differences in terms of land use and land cover. The aim of this study was to carry out a multi-criteria analysis of a set of environmental attributes in order to classify the areas under study according to their levels of soil suitability and runoff potential. The integrated analysis made it possible to geospatialize prospective regions for reuse, under two specified conditions. In the UGRHI-09, condition 1 corresponds to 3373.24 km2, while condition 2 comprises 286.07 km2, located mainly in the north-western and central-eastern portions of the unit. In the PRB, condition 1 was also more expressive in occupational terms, corresponding to 1447.83 km2; and condition 2 was perceptible in 53.11 km2, predominantly in the central region of the basin. The physical characteristics of the areas studied were decisive in delimiting the areas suitable for the reuse of treated wastewater. Full article
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<p>Location of study areas. Land use and land cover maps of UGRHI-09 (<b>A</b>) and PRB (<b>B</b>). Source: Adapted from [<a href="#B45-agronomy-14-02689" class="html-bibr">45</a>,<a href="#B46-agronomy-14-02689" class="html-bibr">46</a>].</p>
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<p>Methodological steps developed in the study. * So: soils (type, texture and thickness). It is worth noting that the PRB runoff levels were mapped by [<a href="#B47-agronomy-14-02689" class="html-bibr">47</a>].</p>
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<p>Slope chart of UGRHI-09 (<b>a</b>) and PRB (<b>b</b>).</p>
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<p>Elevation map of UGRHI-09 (<b>a</b>) and PRB (<b>b</b>).</p>
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<p>Soil maps of UGRHI-09 (<b>a</b>) and PRB (<b>b</b>).</p>
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<p>Drainage density map of UGRHI-09 (<b>a</b>) and PRB (<b>b</b>) [<a href="#B47-agronomy-14-02689" class="html-bibr">47</a>].</p>
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<p>Geology map of UGRHI-09 (<b>a</b>) and PRB (<b>b</b>).</p>
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<p>Depth of groundwater level map of UGRHI-09 (<b>a</b>) and PRB (<b>b</b>).</p>
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<p>Drainage network map of UGRHI-09 (<b>a</b>) and PRB (<b>b</b>); distance to stream map of UGRHI-09 (<b>c</b>) and PRB (<b>d</b>).</p>
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<p>Random Consistency Index values considering the order of the matrix.</p>
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<p>Normalized matrices considering the environmental attributes of the LSC and the SRPC.</p>
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<p>Final weights of environmental attributes used to prepare interpretative cartographic products.</p>
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<p>Descriptions of potential areas for the reuse of treated wastewater from agro-industrial sources in irrigation.</p>
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<p>Map of inapt areas at UGRHI-09 (<b>a</b>) and PRB (<b>b</b>).</p>
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<p>UGRHI-09 Land Suitability Chart (<b>a</b>), PRB Land Suitability Chart (<b>b</b>), UGRHI-09 Surface Runoff Potential Chart (<b>c</b>), and PRB Surface Runoff Potential Chart (<b>d</b>).</p>
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<p>Decadal average rainfall (2013 to 2022) (<b>a</b>), decadal average actual evapotranspiration (2013 to 2022) (<b>b</b>), and the difference between the decadal average rainfall and the decadal average actual evapotranspiration (<b>c</b>).</p>
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<p>Potential areas in UGRHI-09 (<b>a</b>) and PRB (<b>b</b>) for adopting the practice of reusing treated wastewater from agro-industries.</p>
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26 pages, 13283 KiB  
Article
Reconstruction of 30 m Land Cover in the Qilian Mountains from 1980 to 1990 Based on Super-Resolution Generative Adversarial Networks
by Xiaoya Wang, Bo Zhong, Kai Ao, Bailin Du, Longfei Hu, He Cai, Yang Qiao, Junjun Wu, Aixia Yang, Shanlong Wu and Qinhuo Liu
Remote Sens. 2024, 16(22), 4252; https://doi.org/10.3390/rs16224252 - 14 Nov 2024
Viewed by 327
Abstract
Long time series of annual land cover with fine spatio-temporal resolutions play a crucial role in studying environmental climate change, biophysical modeling, carbon cycling models, and land management. Despite a strong consistency exhibited by several publicly available medium to fine resolution global land [...] Read more.
Long time series of annual land cover with fine spatio-temporal resolutions play a crucial role in studying environmental climate change, biophysical modeling, carbon cycling models, and land management. Despite a strong consistency exhibited by several publicly available medium to fine resolution global land cover datasets, significant discrepancies exist at the regional scale; moreover, only every 5/10 year land cover were available. Consequently, high-quality annual land cover datasets before 2000 are unavailable in China. In this study, we proposed a deep learning-based method by integrating multiple remote sensing data from different platforms with historical high spatial resolution land cover datasets (CNLUCC) to derive the 30 m annual land cover maps from 1980 to 1990 for Qilian Mountain. First, the super-resolution generative adversarial network models for upscaling the 5.5 km AVHRR NDVI to 250 m were established by employing the AVHRR and MODIS NDVI data with the same year as input, and the early time series AVHRR NDVI data were subsequently upscaled to 250 m through the above models. Second, the breaks for the additive seasonal and trend (BFAST) change detection algorithm was applied to the upscaled time series NDVI data to detect the change time of different land cover types. Third, the CNLUCC data in 1980 and 1990 were updated to annual land cover datasets from 1980 to 1990 and the annual mapping results provided insights into the dynamic processes of urbanization, deforestation, water bodies, and farmland from 1980 to 1990. Finally, comprehensive analysis and validation were carried out for evaluation and an overall accuracy of 77.26% for the land cover product in 1986 was achieved. Full article
(This article belongs to the Special Issue Surface Radiative Transfer: Modeling, Inversion, and Applications)
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<p>The location of major river basins in the Qilian Mountains (<b>left</b>) and the visualization of geographical characteristics including color composite from remote sensing image (<b>right</b>).</p>
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<p>Multiple satellite images’ time range and availability.</p>
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<p>Preprocessing rendering. (<b>a</b>) Quality check and cloud mask; (<b>b</b>) fill in missing values by temporal filter; (<b>c</b>) fill in missing values by spatial filter.</p>
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<p>Workflow of the annual land cover mapping process.</p>
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<p>The process of making SR model training dataset (LR-HR image pairs). (<b>a</b>) Creating a square grid; (<b>b</b>) creating centroids of the grids.</p>
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<p>The examples of training dataset (LR-HR image pairs). (<b>a</b>) Gobi; (<b>b</b>) Lake; (<b>c</b>) Forest; (<b>d</b>) River.</p>
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<p>The architecture of generator and discriminator network.</p>
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<p>Minibatch statistic layer.</p>
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<p>Example of change pixels for 3 × 3 grids (C: Cropland, F: Forest, G: Grassland, W: Water body, B: Built-up land, and U: Unused land).</p>
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<p>Breakpoint test (example for one pixel).</p>
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<p>The location of Jiayuguan City and Suzhou District (indicated by the red line) and the Heihe River Basin (indicated by the blue line).</p>
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<p>Annual land cover maps from 1980 to 1990.</p>
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<p>Annual land cover maps from 1980 to 1990.</p>
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<p>The expansion of built-up in the study area.</p>
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<p>June 1986 NDVI super-resolution results (The left column (<b>a</b>,<b>c</b>,<b>e</b>) displays the results of SR NDVI data in the Qilian Mountains from original resolution to 1 km and further to 250 m; the right column (<b>b</b>,<b>d</b>,<b>f</b>) shows enlarged details of the black box area and (<b>g</b>,<b>h</b>) show 30 m SR data and resampled data, respectively).</p>
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<p>June 1986 NDVI super-resolution results (The left column (<b>a</b>,<b>c</b>,<b>e</b>) displays the results of SR NDVI data in the Qilian Mountains from original resolution to 1 km and further to 250 m; the right column (<b>b</b>,<b>d</b>,<b>f</b>) shows enlarged details of the black box area and (<b>g</b>,<b>h</b>) show 30 m SR data and resampled data, respectively).</p>
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<p>The spatial distribution of validation samples in 1986.</p>
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<p>Confusion matrix for our land cover map (<b>left</b>) and CLUD-A (<b>right</b>) in 1986.</p>
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<p>Spatial distribution of 1000 random sample points.</p>
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<p>Area change in different land cover classes from 1995 to 2005. The fluctuations for each land cover type are enlarged using the different ranges of y-axis.</p>
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<p>Visual comparison of the detected change years (the first column) with the images from Google Earth and Landsat (the second and third column). The highlighted areas with blue shapes were the change regions. (<b>a</b>) Change from unused land to water body, (<b>b</b>) the conversion from unused land to urban area, (<b>c</b>) change from unused land to cropland.</p>
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<p>Deviation of detected change years from the change samples.</p>
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24 pages, 12186 KiB  
Article
Green Infrastructure Mapping in Almeria Province (Spain) Using Geographical Information Systems and Multi-Criteria Evaluation
by Álvaro Navas González, Richard J. Hewitt and Javier Martínez-Vega
Land 2024, 13(11), 1916; https://doi.org/10.3390/land13111916 - 14 Nov 2024
Viewed by 252
Abstract
Green infrastructure (GI) is increasingly prioritised in landscape policy and planning due to its potential to benefit ecosystems and enhance wildlife conservation. However, due to the uneven distribution of protected areas (PAs) and the fragmentation of habitats more generally, multi-level policy strategies are [...] Read more.
Green infrastructure (GI) is increasingly prioritised in landscape policy and planning due to its potential to benefit ecosystems and enhance wildlife conservation. However, due to the uneven distribution of protected areas (PAs) and the fragmentation of habitats more generally, multi-level policy strategies are needed to create an integrated GI network bridging national, regional and local scales. In the province of Almeria, southeastern Spain, protected areas are mainly threatened by two land use/land cover changes. On the one hand, there is the advance of intensive greenhouse agriculture, which, between 1984 and 2007, increased in surface area by more than 58%. On the other hand, there is the growth of artificial surfaces, including urban areas (+64%), construction sites (+194%) and road infrastructures (+135%). To address this challenge, we present a proposal for green infrastructure deployment in the province of Almeria. We combine Geographic Information Systems (GISs) and multi-criteria evaluation (MCE) techniques to identify and evaluate suitability for key elements to be included in GI in two key ways. First, we identify the most suitable areas to form part of the GI in order to address vulnerability to degradation and fragmentation. Second, we propose 15 ecological corridors connecting the 35 protected areas of the province that act as core areas. The proposed GI network would extend along the western coast of the province and occupy the valleys of the main rivers. The river Almanzora plays a leading role. Due to its remoteness from the coast and its climatic conditions, it has not attracted intensive greenhouse agriculture and urban development, the main drivers of the transformation and fragmentation of traditional land uses. Around 50% of the area occupied by the proposed corridors would be located in places of medium and high suitability for the movement of species between core areas. Full article
(This article belongs to the Special Issue Managing Urban Green Infrastructure and Ecosystem Services)
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<p>Location of the province of Almeria. Distribution and categorisation of its protected areas, comprising the RENPA network. SAC = Special Area of Conservation; SCI = Site of Community Importance.</p>
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<p>Research methods workflow.</p>
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<p>Factor maps: (<b>a</b>) slope; (<b>b</b>) aspect; (<b>c</b>) proximity to forest areas; (<b>d</b>) road safety; (<b>e</b>) Habitats of Community Interest; (<b>f</b>) proximity to linear corridors; (<b>g</b>) accessibility from urban areas; (<b>h</b>) land use and land cover fragmentation.</p>
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<p>Green infrastructure restricted area map.</p>
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<p>Suitability map for green infrastructure in the province of Almería.</p>
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<p>Proposal for ecological corridors in the province of Almeria.</p>
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<p>Results of overlay analysis between ecological corridors and suitability for GI. Each bar corresponds to an ecological corridor identified in the connectivity analysis, ordered by surface area from left to right along the <span class="html-italic">x</span>-axis from largest to smallest.</p>
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18 pages, 12063 KiB  
Article
Deformation Monitoring and Analysis of Beichuan National Earthquake Ruins Museum Based on Time Series InSAR Processing
by Jing Fan, Weihong Wang, Jialun Cai, Zhouhang Wu, Xiaomeng Wang, Hui Feng, Yitong Yao, Hongyao Xiang and Xinlong Luo
Remote Sens. 2024, 16(22), 4249; https://doi.org/10.3390/rs16224249 - 14 Nov 2024
Viewed by 251
Abstract
Since the Wenchuan earthquake in 2008, Old Beichuan County-town has experienced significant subsidence due to the disruption of the geological environment and the concurrent increase in precipitation. The ongoing land surface deformation poses a threat to the preservation and utilization of the Beichuan [...] Read more.
Since the Wenchuan earthquake in 2008, Old Beichuan County-town has experienced significant subsidence due to the disruption of the geological environment and the concurrent increase in precipitation. The ongoing land surface deformation poses a threat to the preservation and utilization of the Beichuan National Earthquake Ruins Museum (BNERM), as well as to the safety of urban residents’ lives. However, the evolutionary characteristics of surface deformation in these areas remain largely unexplored. Here, we focused on the BNERM control zone and employed the small-baseline subset interferometric synthetic aperture radar (SBAS-InSAR) technique to accurately measure land surface deformation and its spatiotemporal changes. Subsequently, we integrated this data with land cover types and precipitation to investigate the driving factors of deformation. The results indicate a slight overall elevation increase in the study area from June 2015 to May 2023, with deformation rates varying between −35.2 mm/year and 22.9 mm/year. Additionally, four unstable slopes were identified within the BNERM control zone. Our analysis indicates that surface deformation in the study area is closely linked to changes in land cover types and precipitation, exhibiting a seasonal cumulative pattern, and active geological activity may also be a cause of deformation. This study provides invaluable insights into the surface deformation characteristics of the BNERM and can serve as a scientific foundation for the protection of earthquake ruins, risk assessment, early warning, and disaster prevention measures. Full article
(This article belongs to the Section Remote Sensing in Geology, Geomorphology and Hydrology)
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<p>Overview of the study area. (<b>a</b>) BNERM Control Zone and SAR satellite imagery coverage. (<b>b</b>) The extent of the study area (from Google Earth on 6 September 2020), where RJP for Renjiaping Earthquake Memorial Museum and a comprehensive Service Area, OBC for Earthquake Ruins Protection Area of Old Beichuan, TJS for Tangjiashan Secondary Hazard Demonstration and Natural Recovery Area. (<b>c</b>) The current status of the BNERM.</p>
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<p>The main framework and flow chart of the methodology.</p>
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<p>(<b>a</b>) The location of the reference point. (<b>b</b>) The time series of the reference point. (<b>c</b>) Interference baseline map.</p>
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<p>(<b>a</b>) The deformation rate in the LOS direction of the study area and (<b>b</b>–<b>d</b>) correspond to the deformation rate maps of RJP, OBC, and TJS, respectively.</p>
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<p>(<b>a</b>–<b>c</b>) are the selected feature points of RJP, OBC, and TJS. (<b>d</b>,<b>e</b>) are the unstable slope boundaries of the feature points B3 and C3. (<b>f</b>,<b>g</b>) are the current status of the collapse in Jingjiashan and landslides in Wangjiyan.</p>
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<p>Time series cumulative variogram of feature points. (<b>a</b>–<b>c</b>) correspond to A1, B1, C1, which are the feature points in P1 region; (<b>d</b>–<b>f</b>) correspond to A2, B2, C2, which are the feature points in OBC region; (<b>g</b>–<b>i</b>) correspond to A3, B3, C3, which are the feature points in TJS region.</p>
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<p>(<b>a</b>) Cumulative displacement map. (<b>b</b>) RMSE distribution of cumulative deformation in the study area.</p>
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<p>RMSE distribution of cumulative deformation.</p>
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<p>(<b>a</b>) 2017 Land Use Types in the Study Area. (<b>b</b>) 2023 Land Use Types in the Study Area.</p>
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<p>(<b>a</b>) Map of land cover type changes in the deformed area between 2017 and 2023. (<b>b</b>) Map of land cover types changes in the deformed area that changed between 2017 and 2023.</p>
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<p>(<b>a</b>) Surface deformation rate of Renjiaping Earthquake Memorial Museum and comprehensive service area, and RJP stands for Renjiaping Earthquake Memorial Museum and a comprehensive Service Area. (<b>b</b>) The optical images of the area in 2015. (<b>c</b>) The optical images of the area in 2020.</p>
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<p>Precipitation and time series cumulative deformation trends. (<b>a</b>) is the Renjiaping Earthquake Memorial Museum and comprehensive Service Area. (<b>b</b>) is the Earthquake Ruins Protection Area of Old Beichuan, and (<b>c</b>) is the Tangjiashan Secondary Hazard Demonstration and Natural Recovery Area. (<b>d</b>) is the average of the study area.</p>
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<p>Distribution of faults in the vicinity of the study area and the seismotectonic context (the yellow ball indicates large and small earthquakes that occurred after the 12 May 2008 earthquake and between 17 June 2015, and the red ball indicates earthquakes that occurred between 18 June 2015 and 31 May 2023).</p>
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21 pages, 7459 KiB  
Article
Deep Learning for Urban Tree Canopy Coverage Analysis: A Comparison and Case Study
by Grayson R. Morgan, Danny Zlotnick, Luke North, Cade Smith and Lane Stevenson
Geomatics 2024, 4(4), 412-432; https://doi.org/10.3390/geomatics4040022 - 14 Nov 2024
Viewed by 202
Abstract
Urban tree canopy (UTC) coverage, or area, is an important metric for monitoring changes in UTC over large areas within a municipality. Several methods have been used to obtain these data, but remote sensing image classification is one of the fastest and most [...] Read more.
Urban tree canopy (UTC) coverage, or area, is an important metric for monitoring changes in UTC over large areas within a municipality. Several methods have been used to obtain these data, but remote sensing image classification is one of the fastest and most reliable over large areas. However, most studies have tested only one or two classification methods to accomplish this while using costly satellite imagery or LiDAR data. This study seeks to compare three urban tree canopy cover classifiers by testing a deep learning U-Net convolutional neural network (CNN), support vector machine learning classifier (SVM) and a random forests machine learning classifier (RF) on cost-free 2012 aerial imagery over a small southern USA city and midsize, growing southern USA city. The results of the experiment are then used to decide the best classifier and apply it to more recent aerial imagery to determine canopy changes over a 10-year period. The changes are subsequently compared visually and statistically with recent urban heat maps derived from thermal Landsat 9 satellite data to compare the means of temperatures within areas of UTC loss and no change. The U-Net CNN classifier proved to provide the best overall accuracy for both cities (89.8% and 91.4%), while also requiring the most training and classification time. When compared spatially with city heat maps, city periphery regions were most impacted by substantial changes in UTC area as cities grow and the outer regions get warmer. Furthermore, areas of UTC loss had higher temperatures than those areas with no canopy change. The broader impacts of this study reach the urban forestry managers at the local, state/province, and national levels as they seek to provide data-driven decisions for policy makers. Full article
(This article belongs to the Topic Geocomputation and Artificial Intelligence for Mapping)
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<p>Study areas (<b>A</b>) Georgetown TX and (<b>B</b>) Laurel MS within the United States of America.</p>
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<p>Land surface temperature (LST) maps for Georgetown (<b>A</b>) and Laurel (<b>B</b>) and the quality assessment overlay in pink. The pink colors indicate regions where the uncertainty is higher.</p>
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<p>A general workflow of the experiment and case study.</p>
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<p>Training and validation samples used for classification and accuracy assessment of the 2012 NAIP images (water included for map purpose only).</p>
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<p>Comparison of the original NAIP image (<b>A</b>), the RF classifier results (<b>B</b>), SVM classifier results (<b>C</b>), and the U-Net classifier results (<b>D</b>) for Laurel, MS. Light green represents grass, dark green is urban tree canopy, and yellow is urban and other classes combined.</p>
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<p>Comparison of the original NAIP image (<b>A</b>), the RF classifier results (<b>B</b>), SVM classifier results (<b>C</b>), and the U-Net classifier results (<b>D</b>) for Georgetown, TX. Light green represents grass, dark green is urban tree canopy, and yellow is urban and other classes combined.</p>
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<p>Canopy changes (in blue) overlaid on the heat maps for Georgetown (<b>A</b>) and Laurel (<b>B</b>).</p>
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<p>Laurel Mississippi example of tree canopy loss or change using the 2012 NAIP image (<b>A</b>), 2023 NAIP image (<b>B</b>), heat map (<b>C</b>), and heat map showing detected canopy loss (<b>D</b>).</p>
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<p>Georgetown, TX first example of tree canopy loss or change using the 2012 NAIP image (<b>A</b>), 2023 NAIP image (<b>B</b>), heat map (<b>C</b>), and heat map showing detected canopy loss (<b>D</b>).</p>
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<p>Georgetown, TX second example of tree canopy loss or change using the 2012 NAIP image (<b>A</b>), 2023 NAIP image (<b>B</b>), heat map (<b>C</b>), and heat map showing detected canopy loss (<b>D</b>).</p>
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31 pages, 9887 KiB  
Article
Deforestation and Forest Degradation Detection in the Brazilian Amazon: A Comparative Analysis of Two Areas and Their Conservation Units
by Danielle Nogueira Lopes and Satoshi Tsuyuki
Appl. Sci. 2024, 14(22), 10504; https://doi.org/10.3390/app142210504 - 14 Nov 2024
Viewed by 326
Abstract
This study analyzed land use and land cover (LULC) changes to identify the levels of deforestation and forest degradation in two locations in the Amazon rainforest and their conservation units. Using Sentinel-2 satellite imagery and object-based image classification, yearly LULC maps were created [...] Read more.
This study analyzed land use and land cover (LULC) changes to identify the levels of deforestation and forest degradation in two locations in the Amazon rainforest and their conservation units. Using Sentinel-2 satellite imagery and object-based image classification, yearly LULC maps were created from 2018 to 2023. Disturbances were then quantified by Primary Forest conversions. This study revealed a gain of around 22,362 ha in Secondary Forest areas in Manaus and 29,088 ha in Agriculture/Pastureland in Porto Velho within the study period. Differing yearly rates of deforestation and degradation were detected between the areas, with agriculture/pastureland expansion being observed as the primary driver of forest loss. State and federal units showed the largest conversion of primary to Secondary Forest, while state units experienced the most conversion to non-forest areas. Sustainable use units and buffer zones were particularly impacted by these disturbances. These findings suggest that factors beyond environmental policies contribute to these outcomes, highlighting the importance of understanding local contexts. Comparing areas with varying degradation levels provides insights into the effectiveness of restoration and conservation efforts. Full article
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<p>Location of (<b>a</b>) Brazilian Legal Amazon (BLA) inside Brazil; (<b>b</b>) Types of conservation units inside the BLA states territory; (<b>c</b>) Manaus city and its conservation units; (<b>d</b>) Porto Velho district and its conservation units.</p>
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<p>Location of (<b>a</b>) Brazilian Legal Amazon (BLA) inside Brazil; (<b>b</b>) Types of conservation units inside the BLA states territory; (<b>c</b>) Manaus city and its conservation units; (<b>d</b>) Porto Velho district and its conservation units.</p>
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<p>Deforestation and forest degradation yearly rate in the two study sites in all years.</p>
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<p>Maps representing areas of deforestation and forest degradation in consecutive years within the study sites: (<b>a</b>) Deforestation and (<b>b</b>) forest degradation in Manaus, and (<b>c</b>) deforestation, and (<b>d</b>) forest degradation in Porto Velho.</p>
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<p>Maps representing areas of deforestation and forest degradation in consecutive years within the study sites: (<b>a</b>) Deforestation and (<b>b</b>) forest degradation in Manaus, and (<b>c</b>) deforestation, and (<b>d</b>) forest degradation in Porto Velho.</p>
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<p>Total areas of deforestation and forest degradation inside Conservation Units in both study sites per administrative types. Each management type (full protection and sustainable use) belonging to the (<b>a</b>) Federal Level; (<b>b</b>) State Level; and (<b>c</b>) Local Level.</p>
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<p>Total area of deforestation and forest degradation inside buffer zones around conservation units in both study sites per administrative types. Buffers zones of each management type (full protection and sustainable use) belonging to the (<b>a</b>) Federal Level; (<b>b</b>) State Level; and (<b>c</b>) Local Level.</p>
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<p>Relative Feature Importance in percentage derived from the Random Forest model used to create LULC maps of Porto Velho for all years: (<b>a</b>) 2018; (<b>b</b>) 2019; (<b>c</b>) 2020; (<b>d</b>) 2021; (<b>e</b>) 2022; and (<b>f</b>) 2023.</p>
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<p>Relative Feature Importance in percentage derived from the Random Forest model used to create LULC maps of Manaus for all years: (<b>a</b>) 2018; (<b>b</b>) 2019; (<b>c</b>) 2020; (<b>d</b>) 2021; (<b>e</b>) 2022; and (<b>f</b>) 2023.</p>
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<p>LULC maps of Manaus, resulting from the Random Forest model for all years: (<b>a</b>) 2018; (<b>b</b>) 2019; (<b>c</b>) 2020; (<b>d</b>) 2021; (<b>e</b>) 2022; and (<b>f</b>) 2023.</p>
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<p>LULC maps of Porto Velho, resulting from the Random Forest model for all years: (<b>a</b>) 2018; (<b>b</b>) 2019; (<b>c</b>) 2020; (<b>d</b>) 2021; (<b>e</b>) 2022; and (<b>f</b>) 2023.</p>
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23 pages, 25453 KiB  
Article
The Trend of Coal Mining-Disturbed CDR AVHRR NDVI (1982–2022) in a Plain Agricultural Region—A Case Study on Yongcheng Coal Mine and Its Buffers in China
by Jingyang Lu, Chao Ma, Zhenzhen Cui, Wensi Ma and Tingting Li
Agriculture 2024, 14(11), 2051; https://doi.org/10.3390/agriculture14112051 - 14 Nov 2024
Viewed by 213
Abstract
The destruction of arable land caused by coal mining in coal grain compound areas is a major bottleneck restricting grain production increase. The spatiotemporal correlation between the decline in cultivated land quality and crop growth deterioration due to mining subsidence still needs to [...] Read more.
The destruction of arable land caused by coal mining in coal grain compound areas is a major bottleneck restricting grain production increase. The spatiotemporal correlation between the decline in cultivated land quality and crop growth deterioration due to mining subsidence still needs to be clarified. This study employed the CDR AVHRR NDVI dataset and applied correlation and trend analysis methods to extract vegetation cover information from 1982 to 2022. It also explored the relationships between vegetation cover and temperature and precipitation. The study found the following: (1) Over the past 41 years, the NDVI in the study area showed a significant upward trend. Specifically, the average annual NDVI growth rate in the mining area was 51.85%, while the corresponding growth rates for the 10 km buffer area, 20 km buffer area, and check area (CK) were 65.91%, 65.86%, and 68.09%, respectively. The start of the growing season (SOS) for winter wheat in the mining area and control area advanced by 49 ± 1.5 days and 65 ± 1.5 days, respectively, while the length of the growing season (LOS) extended by 59 ± 1.5 days and 72 ± 1.5 days, respectively. For summer maize, the SOS advanced by 11 ± 1.5 days and 15 ± 1.5 days, respectively, and the LOS extended by 17 ± 1.5 days and 19 ± 1.5 days, respectively. The study area exhibited a significant positive correlation between the NDVI and temperature. Specifically, the correlation coefficient for the mining area was 0.6865 (p < 0.01); for the 10 km buffer zone, it was 0.5937 (p < 0.01), for the 20 km buffer zone, it was 0.6775 (p < 0.01), and for the control check area (CK), it was 0.6591 (p < 0.01). The results of this study can provide data support for the collaborative rehabilitation of and source reduction in coal grain compound areas, as well as for the restoration of damaged farmland. Full article
(This article belongs to the Section Digital Agriculture)
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<p>Geographical location of the study sites and typical surface damage. Note: (<b>a</b>,<b>b</b>): Globeland30 land-use map (<a href="https://www.webmap.cn/commres.do?method=globeIndex" target="_blank">https://www.webmap.cn/commres.do?method=globeIndex</a>, accessed on 10 May 2023); (<b>c</b>): farmland subsidence; (<b>d</b>): farmland cracks; (<b>e</b>): underground coal mining.</p>
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<p>The trend of intra-annual variation in the NDVI.</p>
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<p>The analytic geometry of the Gaussian multimodal fitting of the average NDVI.</p>
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<p>A shading map of the half-monthly mean NDVI in the double-crop cultivation area.</p>
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<p>The characteristics of vegetation phenology in the experimental areas.</p>
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<p>The trend of the annual average NDVI over 41 years: (<b>a</b>–<b>d</b>): Annual avergae of NDVI; (<b>e</b>–<b>h</b>): Yearly NDVI changes; (<b>i</b>–<b>l</b>): Percentage of yearly NDVI changes.</p>
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<p>Spatial distribution of the trend in the annual average NDVI over 41 years.</p>
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<p>The trends of the annual average temperature and precipitation.</p>
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<p>Correlation coefficients and significance tests between annual average NDVI and both annual average temperature and annual total precipitation.</p>
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<p>Time series NDVI and residual NDVI in different areas: (<b>a</b>) mining area; (<b>b</b>) 10 km buffer; (<b>c</b>) 20 km buffer.</p>
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<p>PKU GIMMS NDVI vs. CDR AVHRR NDVI: (<b>a</b>–<b>d</b>): Annual average of NDVI; (<b>e</b>–<b>h</b>): Yearly NDVI changes.</p>
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<p>Comparison of half-monthly PKU GIMMS NDVI and CDR AVHRR NDVI.</p>
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<p>Geographical location and basic information of four mining areas.</p>
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13 pages, 2987 KiB  
Article
Evaluation of the Hydrological Response to Land Use Change Scenarios in Urban and Non-Urban Mountain Basins in Ecuador
by Diego Mejía-Veintimilla, Pablo Ochoa-Cueva and Juan Arteaga-Marín
Land 2024, 13(11), 1907; https://doi.org/10.3390/land13111907 - 14 Nov 2024
Viewed by 223
Abstract
Land cover is a crucial factor in controlling rainfall–runoff processes in mountain basins. However, various anthropogenic activities, such as converting natural vegetation to agricultural or urban areas, can affect this cover, thereby increasing the risk of flooding in cities. This study evaluates the [...] Read more.
Land cover is a crucial factor in controlling rainfall–runoff processes in mountain basins. However, various anthropogenic activities, such as converting natural vegetation to agricultural or urban areas, can affect this cover, thereby increasing the risk of flooding in cities. This study evaluates the hydrological behavior of two mountain basins in Loja, Ecuador, under varying land use scenarios. El Carmen small basin (B1), located outside the urban perimeter, and Las Pavas small basin (B2), within the urban area, were modeled using HEC-HMS 4.3 software. The results highlight the significant influence of vegetation degradation and restoration on hydrological processes. In degraded vegetation scenarios, peak flows increase due to reduced soil infiltration capacity, while baseflows decrease. Conversely, the conserved and restored vegetation scenarios show lower peak flows and higher baseflows, which are attributed to enhanced evapotranspiration, interception, and soil water storage. The study underscores the importance of ecosystem management and restoration in mitigating extreme hydrological events and improving water resilience. These findings provide a foundation for decision-making in urban planning and basin management, emphasizing the need for comprehensive and multidisciplinary approaches to develop effective public policies. Full article
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<p>Location map and average monthly distribution of temperature and precipitation of the study area.</p>
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<p>Selected precipitation events and hydrographs for hydrological modeling of the B1.</p>
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<p>Current and future hypothetical land cover scenarios. (<b>a</b>,<b>b</b>) El Carmen (B1). (<b>c</b>,<b>d</b>) Las Pavas (B2).</p>
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<p>Gauged and simulated flows under the LULC scenarios for basins B1 and B2.</p>
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<p>Box plot for scenario-specific flow rates.</p>
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18 pages, 3490 KiB  
Article
MFMamba: A Mamba-Based Multi-Modal Fusion Network for Semantic Segmentation of Remote Sensing Images
by Yan Wang, Li Cao and He Deng
Sensors 2024, 24(22), 7266; https://doi.org/10.3390/s24227266 - 13 Nov 2024
Viewed by 453
Abstract
Semantic segmentation of remote sensing images is a fundamental task in computer vision, holding substantial relevance in applications such as land cover surveys, environmental protection, and urban building planning. In recent years, multi-modal fusion-based models have garnered considerable attention, exhibiting superior segmentation performance [...] Read more.
Semantic segmentation of remote sensing images is a fundamental task in computer vision, holding substantial relevance in applications such as land cover surveys, environmental protection, and urban building planning. In recent years, multi-modal fusion-based models have garnered considerable attention, exhibiting superior segmentation performance when compared with traditional single-modal techniques. Nonetheless, the majority of these multi-modal models, which rely on Convolutional Neural Networks (CNNs) or Vision Transformers (ViTs) for feature fusion, face limitations in terms of remote modeling capabilities or computational complexity. This paper presents a novel Mamba-based multi-modal fusion network called MFMamba for semantic segmentation of remote sensing images. Specifically, the network employs a dual-branch encoding structure, consisting of a CNN-based main encoder for extracting local features from high-resolution remote sensing images (HRRSIs) and of a Mamba-based auxiliary encoder for capturing global features on its corresponding digital surface model (DSM). To capitalize on the distinct attributes of the multi-modal remote sensing data from both branches, a feature fusion block (FFB) is designed to synergistically enhance and integrate the features extracted from the dual-branch structure at each stage. Extensive experiments on the Vaihingen and the Potsdam datasets have verified the effectiveness and superiority of MFMamba in semantic segmentation of remote sensing images. Compared with state-of-the-art methods, MFMamba achieves higher overall accuracy (OA) and a higher mean F1 score (mF1) and mean intersection over union (mIoU), while maintaining low computational complexity. Full article
(This article belongs to the Section Remote Sensors)
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<p>The overall architecture of our proposed MFMamba.</p>
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<p>(<b>a</b>) The detailed architecture of a VSS block. (<b>b</b>) The visualization of an SS2D unit.</p>
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<p>(<b>a</b>) The overall architecture of an FFB. (<b>b</b>) The structure of an MCKA unit. (<b>c</b>) The structure of an EAA unit.</p>
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<p>(<b>a</b>) The structure of a GLTB. (<b>b</b>) The structure of an FRH.</p>
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<p>Samples (<b>a</b>,<b>b</b>) are 256 × 256 from Vaihingen and (<b>c</b>,<b>d</b>) are 256 × 256 from Potsdam. The first row shows the orthophotos with three channels (NIRRG for Vaihingen and RGB for Potsdam). The second and third rows show the corresponding depth information and semantic labels in pixel-wise mapping.</p>
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<p>Visualization of the segmentation results from different methods on the Vaihingen dataset. (<b>a</b>) NIRRG images, (<b>b</b>) DSM, (<b>c</b>) Ground Truth, (<b>d</b>) CMFNet, (<b>e</b>) ABCNet, (<b>f</b>) TransUNet, (<b>g</b>) UNetFormer, (<b>h</b>) MAResU-Net, (<b>i</b>) CMTFNet, (<b>j</b>) RS3Mamba, and (<b>k</b>) the proposed MFMamba. Two purple boxes are added to each subfigure to highlight the differences.</p>
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<p>Visualization of the segmentation results from different methods on the Potsdam dataset. (<b>a</b>) RGB images, (<b>b</b>) DSM, (<b>c</b>) Ground Truth, (<b>d</b>) CMFNet, (<b>e</b>) ABCNet, (<b>f</b>) TransUNet, (<b>g</b>) UNetFormer, (<b>h</b>) MAResU-Net, (<b>i</b>) CMTFNet, (<b>j</b>) RS3Mamba, and (<b>k</b>) the proposed MFMamba. Two purple boxes are added to each subfigure to highlight the differences.</p>
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16 pages, 7870 KiB  
Article
Analyzing the Contribution of Urban Land Uses to the Formation of Urban Heat Islands in Urmia City
by Raziyeh Teimouri and Pooran Karbasi
Urban Sci. 2024, 8(4), 208; https://doi.org/10.3390/urbansci8040208 - 13 Nov 2024
Viewed by 467
Abstract
An Urban Heat Island (UHI) is an important variable in climate and environmental studies. Nowadays, population growth and urbanization development are the most important factors affecting the temperature increase in urban areas, which cause the creation of heat islands in urban areas. (1) [...] Read more.
An Urban Heat Island (UHI) is an important variable in climate and environmental studies. Nowadays, population growth and urbanization development are the most important factors affecting the temperature increase in urban areas, which cause the creation of heat islands in urban areas. (1) Background: This study explores the influence of major land uses on the creation of Urban Heat Islands in Urmia city, Iran. (2) Methods: To achieve the aim of this study, Landsat satellite data including Landsat 5 and 8 imageries from the time periods of 1990 and 2023 were used. With the series of data processing and analyses on vegetation cover and land surface temperature, the impact of main land uses on the creation of Urban Heat Islands and the intensification of their effects have been investigated. (3) Results: The analysis reveals that barren lands consistently exhibit the highest temperature, while garden lands show the lowest temperature across both periods. In addition, the spatial distribution of Urban Heat Islands demonstrates a clustered pattern throughout the study period, with hot spots mainly located in the northwestern and southwestern areas. (4) Conclusions: This study’s findings can be helpful for urban policymakers and planners to develop practical strategies to mitigate UHIs and improve climate resilience in cities. Full article
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<p>Case study location.</p>
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<p>The process of preparing maps for evaluating UHIs.</p>
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<p>Land use in Urmia city in 1990 and 2023.</p>
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<p>UHIs in Urmia city, TM sensor, thermal band 6 in 1990.</p>
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<p>UHIs in Urmia city, TIRS sensor, thermal band 10, year 2023.</p>
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<p>Moran’s index for 1990.</p>
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<p>Moran’s index for 2023.</p>
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<p>Hot and cold spots index for 1990.</p>
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<p>Hot and cold spots index for 2023.</p>
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26 pages, 11851 KiB  
Article
Development and Evaluation of Machine Learning Models for Air-to-Land Temperature Conversion Using the Newly Established Kunlun Mountain Gradient Observation System
by Yongkang Li, Qing He, Yongqiang Liu, Amina Maituerdi, Yang Yan and Jiao Tan
Land 2024, 13(11), 1903; https://doi.org/10.3390/land13111903 - 13 Nov 2024
Viewed by 258
Abstract
Mountainous land types are characterized by a scarcity of observational data, particularly in remote areas such as the Kunlun Mountains, where conventional Automatic Weather Stations (AWSs) typically do not record land surface temperature (LST) data. This study aims to develop and evaluate models [...] Read more.
Mountainous land types are characterized by a scarcity of observational data, particularly in remote areas such as the Kunlun Mountains, where conventional Automatic Weather Stations (AWSs) typically do not record land surface temperature (LST) data. This study aims to develop and evaluate models for converting air temperature (TA) to LST using newly established meteorological station data from the Kunlun Mountain Gradient Observation System, thereby providing time-continuous LST data for AWSs. We constructed a conceptual model to explore the relationship between 1.5 m TA and LST and instantiated it using three machine learning algorithms: Support Vector Machine (SVR), Convolutional Neural Network (CNN), and CatBoost. The results demonstrated that the CatBoost algorithm outperformed the others under complex terrain and climatic conditions, achieving a coefficient of determination (R2) of 0.997 and the lowest root mean square error (RMSE) of 0.627 °C, indicating superior robustness and accuracy. Consequently, CatBoost was selected as the optimal model. Additionally, this study analyzed the spatiotemporal distribution characteristics of cloud cover in the Kunlun Mountain region using the MOD11A1 product and assessed the uncertainties introduced by the 8-day average compositing method of the MOD11A2 product. The results revealed significant discrepancies between the monthly average LST derived from polar-orbiting satellites and the hourly composite monthly LST measured on-site or under ideal cloud-free conditions. These differences were particularly pronounced in high-altitude regions (4000 m and above), with the greatest differences occurring in winter, reaching up to 10.2 °C. These findings emphasize the importance of hourly LST calculations based on AWSs for accurately assessing the spatiotemporal characteristics of LST in the Kunlun Mountains, thus providing more precise spatiotemporal support for remote sensing applications in high-altitude regions. Full article
(This article belongs to the Section Land Innovations – Data and Machine Learning)
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<p>Overview of study area.</p>
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<p>Flowchart of data processing steps. Note: The red text section represents the Derivative Data constructed based on the conceptual model proposed in this article.</p>
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<p>Comparison of 10-fold cross-validation of three machine learning algorithms for whether <span class="html-italic">at_diff_up</span> participates or not. (<b>a</b>) is a box plot of RMSE against the Pearson correlation coefficient, (<b>b</b>) is the box plot of significance test probability p against the Pearson correlation coefficient. Note: The feature variable denoted by <b><span class="html-italic">at_diff_up</span></b> represents the difference between the current hourly 1.5 m atmospheric temperature and the corresponding value from the preceding hour.</p>
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<p>Importance box graph of Catboost, the corresponding optimal parameters based on the grid search, and the model validation accuracy metric. Note: ** represents significance through a <span class="html-italic">p</span> &lt; 0.01 correlation test.</p>
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<p>Comparison of Supersite-based measured LST with Catboost-simulated LST across the Kunlun Mountain Vertical Gradient. Note: The elevations of Yeyike, Kalasai, Akesusai, Khunjerab, and Wolonggang are 2275 m, 3013 m, 3934.7 m, 4700 m, and 5896 m, respectively.</p>
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<p>Comparison of Supersite-based measured LST with Catboost-simulated LST across the Kunlun Mountain Vertical Gradient. Note: The elevations of Yeyike, Kalasai, Akesusai, Khunjerab, and Wolonggang are 2275 m, 3013 m, 3934.7 m, 4700 m, and 5896 m, respectively.</p>
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<p>Comparison of Supersite-based measured LST with Catboost-simulated LST across the Kunlun Mountain Vertical Gradient. Note: The elevations of Yeyike, Kalasai, Akesusai, Khunjerab, and Wolonggang are 2275 m, 3013 m, 3934.7 m, 4700 m, and 5896 m, respectively.</p>
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<p>Accuracy evaluation of the CatBoost model across different seasons at five supersites. Panels (<b>a</b>,<b>b</b>) represent the coefficient of determination and the root mean square error of the CatBoost model, respectively.</p>
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<p>Cross-validated Taylor diagrams of Suomi NPP’s VIIRS LST versus Catboost-simulated LST for spring, summer, autumn, winter, daytime, nighttime, and yearly comparisons.</p>
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<p>Cross-validated Taylor diagrams of Terra and Aqua MODIS LST versus Catboost-simulated LST for spring, summer, autumn, winter, daytime, nighttime, and yearly comparisons.</p>
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<p>Spatial distribution of MOD11A1 data availability under cloud influence from 2000 to 2023. Note: (<b>a</b>–<b>g</b>) represent the spatial distribution of data availability for spring, summer, autumn, winter, daytime, nighttime, and the entire year, respectively. (<b>h</b>) represents the spatial distribution of elevation.</p>
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<p>Spatial distribution of MOD11A1 data availability under cloud influence from 2000 to 2023. Note: (<b>a</b>–<b>g</b>) represent the spatial distribution of data availability for spring, summer, autumn, winter, daytime, nighttime, and the entire year, respectively. (<b>h</b>) represents the spatial distribution of elevation.</p>
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<p>Time series comparison of four datasets—8-Day Composite MOD11A2 LST, Site LST in Terra Scan Time, Site LST No Clouds, and Site LST 24h—based on observations from Kunlun Mountain Gradient Stations. Note: (<b>a</b>) Yeyike station represents the 2000 m gradient, (<b>b</b>) Kalasai represents the 3000 m gradient, (<b>c</b>) Akesuaai represents the 4000 m gradient, (<b>d</b>) Khunjurab represents the 5000 m gradient, and (<b>e</b>) Wolonggang represents the 6000 m gradient.</p>
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<p>Time series comparison of four datasets—8-Day Composite MOD11A2 LST, Site LST in Terra Scan Time, Site LST No Clouds, and Site LST 24h—based on observations from Kunlun Mountain Gradient Stations. Note: (<b>a</b>) Yeyike station represents the 2000 m gradient, (<b>b</b>) Kalasai represents the 3000 m gradient, (<b>c</b>) Akesuaai represents the 4000 m gradient, (<b>d</b>) Khunjurab represents the 5000 m gradient, and (<b>e</b>) Wolonggang represents the 6000 m gradient.</p>
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<p>Comparative analysis of time series data from four distinct datasets—derived from monthly composite MOD11A2 LST and site-specific LST measurements at the Kunlun Mountain Gradient LST Observatory. The datasets include MOD11A2 LST, Site LST in Terra Scan Time, Site LST No Clouds, and Site LST 24h. Note: (<b>a</b>) Yeyike station represents the 2000 m gradient, (<b>b</b>) Kalasai represents the 3000 m gradient, (<b>c</b>) Akesuaai represents the 4000 m gradient, (<b>d</b>) Khunjurab represents the 5000 m gradient, and (<b>e</b>) Wolonggang represents the 6000 m gradient.</p>
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15 pages, 4301 KiB  
Article
Spatial Distribution of Burned Areas from 1986 to 2023 Using Cloud Computing: A Case Study in Amazonas (Peru)
by Elgar Barboza, Efrain Y. Turpo, Aqil Tariq, Rolando Salas López, Samuel Pizarro, Jhon A. Zabaleta-Santisteban, Angel J. Medina-Medina, Katerin M. Tuesta-Trauco, Manuel Oliva-Cruz and Héctor V. Vásquez
Fire 2024, 7(11), 413; https://doi.org/10.3390/fire7110413 - 13 Nov 2024
Viewed by 478
Abstract
Wildfire represents a significant threat to ecosystems and communities in the Department of Amazonas, Peru, causing losses in biodiversity and land degradation and affecting socioeconomic security. The objective of this study was to analyze the spatial and temporal distribution of burned areas (BAs) [...] Read more.
Wildfire represents a significant threat to ecosystems and communities in the Department of Amazonas, Peru, causing losses in biodiversity and land degradation and affecting socioeconomic security. The objective of this study was to analyze the spatial and temporal distribution of burned areas (BAs) from 1986 to 2023 to identify recurrence patterns and their impact on different types of land use and land cover (LULC). Landsat 5, 7, and 8 satellite images, processed by Google Earth Engine (GEE) using a decision tree approach, were used to map and quantify the affected areas. The results showed that the BAs were mainly concentrated in the provinces of Utcubamba, Luya, and Rodríguez de Mendoza, with a total of 1208.85 km2 burned in 38 years. The most affected land covers were pasture/grassland (38.25%), natural cover (forest, dry forest, and shrubland) (29.55%) and agricultural areas (14.74%). Fires were most frequent between June and November, with the highest peaks in September and August. This study provides crucial evidence for the implementation of sustainable management strategies, fire prevention, and restoration of degraded areas, contributing to the protection and resilience of Amazonian ecosystems against future wildfire threats. Full article
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<p>The Department of Amazonas is located in South America.</p>
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<p>Process of obtaining historical cartography (1986–2023) through cloud computing for the Department of Amazonas.</p>
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<p>Classification of fires in Amazonas on 13 October 2022, (<b>a</b>) SWIR2, NIR, and Red combination, (<b>b</b>) burned area by decision tree classification.</p>
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<p>(<b>a</b>) Mapping of burned areas for Amazonas between 1986 and 2023; (<b>b</b>) cumulative burned areas between 1986 and 2023; (<b>c</b>) annual burned areas between 1986 and 2023; and (<b>d</b>) burned area patterns by month.</p>
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<p>(<b>a</b>) Spatial distribution of fire frequency between 1986 and 2023 in Amazonas, and (<b>b</b>) area burned and proportion of area burned by frequency class.</p>
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<p>(<b>a</b>,<b>b</b>) Spatial distribution of accumulated burned area by LULC type and (<b>c</b>) percentage of accumulated burned area by ecoregion.</p>
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19 pages, 16510 KiB  
Article
Mapping Crop Types for Beekeepers Using Sentinel-2 Satellite Image Time Series: Five Essential Crops in the Pollination Services
by Navid Mahdizadeh Gharakhanlou, Liliana Perez and Nico Coallier
Remote Sens. 2024, 16(22), 4225; https://doi.org/10.3390/rs16224225 - 13 Nov 2024
Viewed by 282
Abstract
Driven by the widespread adoption of deep learning (DL) in crop mapping with satellite image time series (SITS), this study was motivated by the recent success of temporal attention-based approaches in crop mapping. To meet the needs of beekeepers, this study aimed to [...] Read more.
Driven by the widespread adoption of deep learning (DL) in crop mapping with satellite image time series (SITS), this study was motivated by the recent success of temporal attention-based approaches in crop mapping. To meet the needs of beekeepers, this study aimed to develop DL-based classification models for mapping five essential crops in pollination services in Quebec province, Canada, by using Sentinel-2 SITS. Due to the challenging task of crop mapping using SITS, this study employed three DL-based models, namely one-dimensional temporal convolutional neural networks (CNNs) (1DTempCNNs), one-dimensional spectral CNNs (1DSpecCNNs), and long short-term memory (LSTM). Accordingly, this study aimed to capture expert-free temporal and spectral features, specifically targeting temporal features using 1DTempCNN and LSTM models, and spectral features using the 1DSpecCNN model. Our findings indicated that the LSTM model (macro-averaged recall of 0.80, precision of 0.80, F1-score of 0.80, and ROC of 0.89) outperformed both 1DTempCNNs (macro-averaged recall of 0.73, precision of 0.74, F1-score of 0.73, and ROC of 0.85) and 1DSpecCNNs (macro-averaged recall of 0.78, precision of 0.77, F1-score of 0.77, and ROC of 0.88) models, underscoring its effectiveness in capturing temporal features and highlighting its suitability for crop mapping using Sentinel-2 SITS. Furthermore, applying one-dimensional convolution (Conv1D) across the spectral domain demonstrated greater potential in distinguishing land covers and crop types than applying it across the temporal domain. This study contributes to providing insights into the capabilities and limitations of various DL-based classification models for crop mapping using Sentinel-2 SITS. Full article
(This article belongs to the Section AI Remote Sensing)
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<p>The flowchart of the research methodology.</p>
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<p>Geographic location of the study area with a true-color median composite of Sentinel-2 satellite imagery generated for 1–10 April 2021.</p>
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<p>The macro-average of the F1-score for the 100 designed architectures on the validation dataset for (<b>a</b>) 1DTempCNN, (<b>b</b>) 1DSpecCNN, and (<b>c</b>) LSTM models.</p>
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<p>The macro-average of the F1-score for the 100 designed architectures on the validation dataset for (<b>a</b>) 1DTempCNN, (<b>b</b>) 1DSpecCNN, and (<b>c</b>) LSTM models.</p>
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<p>The 1DTempCNN architecture with optimal performance.</p>
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<p>The 1DSpecCNN architecture with optimal performance.</p>
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<p>The LSTM architecture with optimal performance.</p>
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<p>(<b>a</b>) The ground reference map; and (<b>b</b>) the LSTM-provided map of land cover and crop type across the entire study area.</p>
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<p>Confusion matrix of the top-performing DL model (i.e., LSTM) in predicting land cover and crop type on the test dataset.</p>
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18 pages, 10457 KiB  
Article
Integrating Remote Sensing and GIS-Based Map Analysis in Determining Spread of Built-Ups and Land-Use Dynamics of Terrain of Onitsha Metropolis, Anambra State, Nigeria
by Romanus Udegbunam Ayadiuno and Dominic Chukwuka Ndulue
Land 2024, 13(11), 1896; https://doi.org/10.3390/land13111896 - 13 Nov 2024
Viewed by 264
Abstract
Land scarcity in most cases hampers development and encourages the misuse of land. The suitability of land must be considered before appropriating or allocating land for any use. Land supports the livelihood of every being on the Earth and therefore determines survival, success, [...] Read more.
Land scarcity in most cases hampers development and encourages the misuse of land. The suitability of land must be considered before appropriating or allocating land for any use. Land supports the livelihood of every being on the Earth and therefore determines survival, success, and sustainability (sustainable living). This study aimed at integrating remote sensing and GIS-based analysis to determine the rate at which built-up areas have spread across the terrain of Onitsha Metropolis, Anambra State, Nigeria, and the dynamics of other land uses. This research involved both primary and secondary data. The primary data included measurements, direct field observations, and key informant interviews to understand people’s perceptions of the land use in the area. The secondary data included satellite images of the area obtained from USGS and analyzed using ArcGIS 10.2 for variations in the terrain of the Onitsha Metropolis; to determine the land use and land cover change (LULCC) of the Onitsha Metropolis over 40 years, published and unpublished articles and books were also consulted. The geological analysis of the study showed that the area of the Ogwashi/Asaba formation is 318.57 km2; the areas of the Nanka sands and Bende-Ameke are 423.07 km2 and 259.42 km2, respectively. The Nanka sands and Bende-Ameke formations are best suited for engineering construction purposes, while the Ogwashi/Asaba formation is suitable for agriculture and should be designated as a buffer zone or park. However, due to the unavailability of land as a result of the growing population and the proximity of the area to the city center, the area is being encroached upon, and a large area (about 30.40%) has been converted to built-up areas as of 2022. Forecast analysis showed that if the trend continues, 158.28 km2 (49.68%) of the alluvium soils of the Ogwashi/Asaba formation will be covered with buildings by 2072. The geology and the terrain of the Onitsha Metropolis determine the soil characteristics and the land use suitability; mapping the geological formations and overlaying these with the land use and land cover change of the area revealed the extent of the encroachment on the Ogwashi/Asaba formation, which must be discouraged. Full article
(This article belongs to the Section Urban Contexts and Urban-Rural Interactions)
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<p>Anambra State with the Study Location. <b>Source:</b> USGS, processed by the author (2023).</p>
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<p>Soil types of the different geologic formations in Onitsha Metropolis. (<b>A</b>) Bende-Ameke, (<b>B</b>) Nanka Sands, and (<b>C</b>) Ogwashi/Asaba formations.</p>
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<p>Elevation map of Onitsha Metropolis. <b>Source:</b> USGS, processed by the author (2023).</p>
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<p>Geologic map formations of Onitsha Metropolis. <b>Source:</b> USGS, processed by the author (2023).</p>
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<p>Chart representing the sizes of the geologic formations of Onitsha Metropolis.</p>
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<p>LULCC map of Onitsha Metropolis in 1982. <b>Source:</b> USGS, processed by the author (2023).</p>
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<p>LULCC map of Onitsha Metropolis in 1992. <b>Source:</b> USGS, processed by the author (2023).</p>
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<p>LULCC map of Onitsha Metropolis in 2002. <b>Source:</b> USGS, processed by the author (2023).</p>
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<p>LULCC map of Onitsha Metropolis in 2012. <b>Source:</b> USGS, processed by the author (2023).</p>
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<p>LULCC map of Onitsha Metropolis in 2022. <b>Source:</b> USGS, processed by the author (2023).</p>
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<p>Land use percentage change in 1982, 1992, 2002, 2012, and 2022.</p>
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<p>Map overlay of the geology and LULCC of Onitsha Metropolis (1982). <b>Source:</b> USGS, processed by the author (2023).</p>
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<p>Map overlay of the geology and LULCC of Onitsha Metropolis (1992). <b>Source:</b> USGS, processed by the author (2023).</p>
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<p>Map overlay of the geology and LULCC of Onitsha Metropolis (2002). <b>Source:</b> USGS, processed by the author (2023).</p>
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<p>Map overlay of the geology and LULCC of Onitsha Metropolis (2012). <b>Source:</b> USGS, processed by the author (2023).</p>
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<p>Map overlay of the geology and LULCC of Onitsha Metropolis (2022). <b>Source:</b> USGS, processed by the author (2023).</p>
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<p>Chart representing the encroached size of the Ogwashi/Asaba formation by built-ups.</p>
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<p>The forecast of built-up encroachment on the Ogwashi/Asaba formation in 40 years.</p>
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<p>Diagrammatical Flowchart Representing the GIS Analysis Methods for the Geomorphological and LULCC Maps.</p>
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