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20 pages, 10942 KiB  
Article
Changes in Urban Green Spaces in the Pearl River Delta Urban Agglomeration: From the Perspectives of the Area, Spatial Configuration, and Quality
by Tianci Yao, Shengfa Li, Lixin Su and Hongou Zhang
Remote Sens. 2024, 16(23), 4369; https://doi.org/10.3390/rs16234369 - 22 Nov 2024
Viewed by 422
Abstract
Urban green spaces (UGSs) are integral to urban ecosystems, providing multiple benefits to human well-being. However, previous studies mainly focus on the quantity or quality of UGSs, with less emphasis on a comprehensive analysis. This study systematically examined the spatiotemporal UGS dynamics in [...] Read more.
Urban green spaces (UGSs) are integral to urban ecosystems, providing multiple benefits to human well-being. However, previous studies mainly focus on the quantity or quality of UGSs, with less emphasis on a comprehensive analysis. This study systematically examined the spatiotemporal UGS dynamics in the Pearl River Delta urban agglomeration (PRDUA) in China from the perspectives of the area, spatial configuration, and quality, using the high spatial resolution (30 m) Landsat-derived land-cover data and Normalized Difference Vegetation Index (NDVI) data during 1985–2021. Results showed the UGS area in both the old urban districts and expanded urban areas across all nine cities in the PRDUA has experienced a dramatic reduction from 1985 to 2021, primarily due to the conversion of cropland and forest into impervious surfaces. Spatially, the fragmentation trend of UGSs initially increased and then weakened around 2010 in nine cities, but with an inconsistent fragmentation process across different urban areas. In the old urban districts, the fragmentation was mainly due to the loss of large patches; in contrast, it was caused by the division of large patches in the expanded urban areas of most cities. The area-averaged NDVI showed a general upward trend in urban areas in nearly all cities, and the greening trend in the old urban districts was more prevalent than that in the expanded urban areas, suggesting the negative impacts of urbanization on NDVI have been balanced by the positive effects of climate change, urbanization, and greening initiatives in the PRDUA. These findings indicate that urban greening does not necessarily correspond to the improvement in UGS states. We therefore recommend incorporating the three-dimensional analytical framework into urban ecological monitoring and construction efforts to obtain a more comprehensive understanding of UGS states and support effective urban green infrastructure stewardship. Full article
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<p>The location of the PRDUA (<b>a</b>,<b>b</b>), and its land-cover maps in 1985 (<b>c</b>) and 2021 (<b>d</b>), respectively.</p>
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<p>The state and change flows of land cover in nine cities in the PRDUA from 1985 to 2021. Regarding subplot numbering, letters represent cities, and numbers indicate urban subregions.</p>
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<p>Dynamic degrees of green spaces in the expanded urban areas in nine cities in the PRDUA during 1985–2021.</p>
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<p>(<b>a</b>–<b>i</b>) The changes in landscape metrics of green spaces in nine cities in the PRDUA during 1985–2021.</p>
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<p>Box plots of trends in annual NDVI in nine cities in the PRDUA during 1986–2021. (<b>a</b>) represents green spaces with constant land-cover types during the study period, and (<b>b</b>) represents all the land-cover types, excluding permanent water bodies.</p>
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<p>Spatial patterns of trends in annual NDVI in areas with constant land-cover types in nine cities in the PRDUA during 1986–2021.</p>
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<p>Spatial patterns of trends in annual NDVI in areas with land-cover change occurring in nine cities in the PRDUA during 1986–2021.</p>
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<p>The frequency distributions of trends in annual NDVI in different city subregions where land-cover change did not occur (<b>a</b>) or occurred (<b>b</b>) during 1986–2021. O, E, and R indicate the old urban districts, expanded urban areas, and rural areas, respectively.</p>
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<p>The change in area-averaged NDVI in the PRDUA during 1986–2021 (<b>a</b>) and correlation of annual NDVI in different city subregions with the PRDUA average (<b>b</b>). The solid-colored bars represent the relationship between annual NDVI in areas with constant land-cover types and the PRDUA average, while the bars with forward slashes indicate the relationship between the areas excluding permanent water bodies and the PRDUA average. ** indicate the trends significant at <span class="html-italic">p</span> &lt; 0.01.</p>
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23 pages, 21253 KiB  
Article
Urban Flooding Disaster Risk Assessment Utilizing the MaxEnt Model and Game Theory: A Case Study of Changchun, China
by Fanfan Huang, Dan Zhu, Yichen Zhang, Jiquan Zhang, Ning Wang and Zhennan Dong
Sustainability 2024, 16(19), 8696; https://doi.org/10.3390/su16198696 - 9 Oct 2024
Viewed by 889
Abstract
This research employs the maximum entropy (MaxEnt) model alongside game theory, integrated with an extensive framework of natural disaster risk management theory, to conduct a thorough analysis of the indicator factors related to urban flooding. This study conducts an assessment of the risks [...] Read more.
This research employs the maximum entropy (MaxEnt) model alongside game theory, integrated with an extensive framework of natural disaster risk management theory, to conduct a thorough analysis of the indicator factors related to urban flooding. This study conducts an assessment of the risks associated with urban flooding disasters using Changchun city as a case study. The validation outcomes pertaining to urban flooding hotspots reveal that 88.66% of the identified flooding sites are situated within areas classified as high-risk and very high-risk. This finding is considered to be more reliable and justifiable when contrasted with the 77.73% assessment results derived from the MaxEnt model. Utilizing the methodology of exploratory spatial data analysis (ESDA), this study applies both global and local spatial autocorrelation to investigate the disparities in the spatial patterns of flood risk within Changchun. This study concludes that urban flooding occurs primarily in the city center of Changchun and shows a significant agglomeration effect. The region is economically developed, with a high concentration of buildings and a high percentage of impervious surfaces. The Receiver Operating Characteristic (ROC) curve demonstrates that the MaxEnt model achieves an accuracy of 90.3%. On this basis, the contribution of each indicator is analyzed and ranked using the MaxEnt model. The primary determinants affecting urban flooding in Changchun are identified as impervious surfaces, population density, drainage density, maximum daily precipitation, and the Normalized Difference Vegetation Index (NDVI), with respective contributions of 20.6%, 18.1%, 13.1%, 9.6%, and 8.5%. This research offers a scientific basis for solving the urban flooding problem in Changchun city, as well as a theoretical reference for early warnings for urban disaster, and is conducive to the realization of sustainable urban development. Full article
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<p>Overview map of the study area.</p>
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<p>Map of flooding hotspots in Changchun, 2017–2022.</p>
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<p>Technical flow chart of flooding disaster risk assessment in Changchun.</p>
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<p>Potential spatial drivers of urban flooding in Changchun city. (<b>a</b>) GDP, (<b>b</b>) NDVI, (<b>c</b>) proportion of impervious surfaces, (<b>d</b>) elevation, (<b>e</b>) river network density, (<b>f</b>) maximum daily rainfall, (<b>g</b>) road network density, (<b>h</b>) drainage density, (<b>i</b>) slope, (<b>j</b>) relief, and (<b>k</b>) population density.</p>
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<p>ROC curve based on the MaxEnt model.</p>
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<p>Response curves of individual spatial factors and their correlation with the likelihood of urban flooding in Changchun.</p>
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<p>Flooding risk distribution map of Changchun by the MaxEnt model.</p>
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<p>Spatial distribution of hazards for urban flooding risk assessment in Changchun.</p>
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<p>Spatial distribution of exposure for urban flooding risk assessment in Changchun.</p>
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<p>Spatial distribution of vulnerability for urban flooding risk assessment in Changchun.</p>
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<p>Spatial distribution of emergency response and recovery capability for urban flooding risk assessment in Changchun.</p>
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<p>Changchun urban flooding disaster risk assessment map.</p>
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<p>Validation of the assessment results based on flooding point data separately. (<b>a</b>) Urban flooding risk assessment in Changchun city based on comprehensive natural hazard risk management Theory. (<b>b</b>) Urban flooding risk assessment in Changchun city using MaxEnt model.</p>
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<p>Percentage of flooding points categorized by risk levels in the models.</p>
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<p>Moran’s scatterplot of urban flooding risk distribution in Changchun. (<b>a</b>) High–high clusters, (<b>b</b>) low–high clusters, (<b>c</b>) low–low clusters, (<b>d</b>) high–low clusters, (<b>f</b>) not significant, and (<b>e</b>) overall.</p>
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<p>Moran’s scatterplot of urban flooding risk distribution in Changchun. (<b>a</b>) High–high clusters, (<b>b</b>) low–high clusters, (<b>c</b>) low–low clusters, (<b>d</b>) high–low clusters, (<b>f</b>) not significant, and (<b>e</b>) overall.</p>
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<p>Localized spatial autocorrelation (LISA) clustering of urban flooding in Changchun.</p>
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21 pages, 7348 KiB  
Article
Spatiotemporal Dynamics of Urban Green Space Coverage and Its Exposed Population under Rapid Urbanization in China
by Chang Zhai, Ruoxuan Geng, Zhibin Ren, Chengcong Wang, Peng Zhang, Yujie Guo, Shengyang Hong, Wenhai Hong, Fanyue Meng and Ning Fang
Remote Sens. 2024, 16(15), 2836; https://doi.org/10.3390/rs16152836 - 2 Aug 2024
Cited by 2 | Viewed by 1421
Abstract
Urban green spaces (UGSs) provide important support for the health of urban residents and the realization of sustainable urban development. However, the spatiotemporal pattern of urban resident exposure to UGSs in cities is unclear, especially at the national scale in China. Based on [...] Read more.
Urban green spaces (UGSs) provide important support for the health of urban residents and the realization of sustainable urban development. However, the spatiotemporal pattern of urban resident exposure to UGSs in cities is unclear, especially at the national scale in China. Based on the annual 30 m resolution Normalized Difference Vegetation Index (NDVI) data of the Landsat satellite, we quantitatively analyzed the change in UGS coverage from 2000 to 2020 for 320 cities in China and combined it with population data to understand the changing patterns of urban population exposure to different UGS coverage. The results indicated that the average UGS coverage decreased from 63% to 44% from 2000 to 2020 in China, which could be divided into two stages: a rapid decline phase (2000–2014) and a progressive decline phase (2015–2020). Geographically, UGS coverage declined faster in southwestern and eastern cities than in other regions, particularly in medium-sized cities. We also found that urban pixel-based areas in cities with the highest UGS coverage (80–100%) decreased rapidly, and the proportion of the urban population exposed to the highest UGS coverage also declined significantly from 2000 to 2020. Urban pixel-based areas with low UGS coverage (20–40%) continued to expand, and there was a rapid increase in the proportion of the urban population exposed to low UGS coverage, with an increase of 146 million people from 2000 to 2020. The expansion of impervious surfaces had the most significant effect on the change in UGS coverage during different periods (2000–2020, 2000–2014, and 2015–2020). Natural factors such as precipitation, surface maximum temperature, and soil moisture also affected UGS coverage change. These findings provide insights into the impact of urbanization on the natural environment of cities, availability of UGS for residents, and sustainable urban development under rapid urbanization. Full article
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<p>The spatial distribution of China’s 320 major cities in this study.</p>
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<p>Design and framework of the study. (<b>a</b>) Extraction of UGS coverage and calculation of trend; (<b>b</b>) schematic of the model to calculate the population exposed to different UGS coverage of the city; (<b>c</b>) driving analysis.</p>
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<p>(<b>a</b>) The spatial distribution of UGS coverage in 320 major cities in China. (<b>b</b>) A plot of the spatial distribution of the rate of change of UGS coverage in 320 cities. (<b>c</b>) A histogram of the frequency distribution of the slope of change in UGS coverage. (<b>d</b>) The trend in the national average of the UGS coverage. (<b>e</b>,<b>f</b>) Indicate the trends of UGS coverage in different regions and at different city levels, respectively.</p>
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<p>(<b>a</b>) Characteristics of spatial distribution of trends in proportion of areas with different UGS coverage classes in 320 cities: lowest (<b>a</b>), low (<b>b</b>), medium (<b>c</b>), high (<b>d</b>), and highest (<b>e</b>).</p>
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<p>Trends in the proportion of the areas in each class of UGS coverage and the proportion of urban population exposure to each UGS coverage class (<b>a</b>,<b>d</b>,<b>g</b>,<b>j</b>,<b>m</b>). Comparisons are made separately in terms of geographic location (<b>b</b>,<b>e</b>,<b>h</b>,<b>k</b>,<b>n</b>) and city size (<b>c</b>,<b>f</b>,<b>i</b>,<b>l</b>,<b>o</b>).</p>
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<p>The proportion of the areas in each UGS coverage class and the proportion of the population exposed to each UGS coverage class in different regions in 2000 and 2020.</p>
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<p>The proportion of the areas in each UGS coverage class and the proportion of the population exposed to each UGS coverage class in different city levels in 2000 and 2020.</p>
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<p>Multiple linear regression and variance decomposition. “-slope” indicates the slope of the change in each factor over the entire study period (2000–2020); asterisks represent statistical significance in this regression, *: <span class="html-italic">p</span> &lt; 0.05, **: <span class="html-italic">p</span> &lt; 0.01.</p>
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<p>Multiple linear regression and variance decomposition. “-slope” indicates the slope of the change in each factor over the rapid decline phase (2000–2014); asterisks represent statistical significance in this regression, *: <span class="html-italic">p</span> &lt; 0.05, **: <span class="html-italic">p</span> &lt; 0.01.</p>
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<p>Multiple linear regression and variance decomposition. “-slope” indicates the slope of the change in each factor over the progressive decline phase (2015–2020); asterisks represent statistical significance in this regression, *: <span class="html-italic">p</span> &lt; 0.05, **: <span class="html-italic">p</span> &lt; 0.01.</p>
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14 pages, 3423 KiB  
Article
Plant Density and Health Evaluation in Green Stormwater Infrastructure Using Unmanned-Aerial-Vehicle-Based Imagery
by Jingwen Xue, Xuejun Qian, Dong Hee Kang and James G. Hunter
Appl. Sci. 2024, 14(10), 4118; https://doi.org/10.3390/app14104118 - 13 May 2024
Cited by 1 | Viewed by 1119
Abstract
Over the past few decades, there has been a notable surge in interest in green stormwater infrastructure (GSI). This trend is a result of the need to effectively address issues related to runoff, pollution, and the adverse effects of urbanization and impervious surfaces [...] Read more.
Over the past few decades, there has been a notable surge in interest in green stormwater infrastructure (GSI). This trend is a result of the need to effectively address issues related to runoff, pollution, and the adverse effects of urbanization and impervious surfaces on waterways. Concurrently, umanned aerial vehicles (UAVs) have gained prominence across applications, including photogrammetry, military applications, precision farming, agricultural land, forestry, environmental surveillance, remote-sensing, and infrastructure maintenance. Despite the widespread use of GSI and UAV technologies, there remains a glaring gap in research focused on the evaluation and maintenance of the GSIs using UAV-based imagery. This study aimed to develop an integrated framework to evaluate plant density and health within GSIs using UAV-based imagery. This integrated framework incorporated the UAV (commonly known as a drone), WebOpenDroneMap (WebDOM), ArcMap, PyCharm, and the Canopeo application. The UAV-based images of GSI components, encompassing trees, grass, soil, and unhealthy trees, as well as entire GSIs (e.g., bioretention and green roofs) within the Morgan State University (MSU) campus were collected, processed, and analyzed using this integrated framework. Results indicated that the framework yielded highly accurate predictions of plant density with a high R2 value of 95.8% and lower estimation errors of between 3.9% and 9.7%. Plant density was observed to vary between 63.63% and 75.30% in the GSIs at the MSU campus, potentially attributable to the different types of GSI, varying facility ages, and inadequate maintenance. Normalized difference vegetation index (NDVI) maps and scales of two GSIs were also generated to evaluate plant health. The NDVI and plant density results can be used to suggest where new plants can be added and to provide proper maintenance to achieve proper functions within the GSIs. This study provides a framework for evaluating plant performance within the GSIs using the collected UAV-based imagery. Full article
(This article belongs to the Section Environmental Sciences)
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<p>Schematic diagram of framework for plant density and health identification.</p>
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<p>UAV-based RGB orthophoto of GSIs within Morgan State University campus.</p>
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<p>Plant density prediction for GSI components. (<b>a</b>) Trees, (<b>b</b>) grass, (<b>c</b>) soil, and (<b>d</b>) unhealthy trees. Note: Vegetation in white pixels, and other media in black pixels in Canopeo and Pycharm results.</p>
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<p>Plant density prediction of bioretention at MSU Campus.</p>
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<p>Plant density prediction of bioretention at MSU Campus.</p>
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<p>RGB, NIR, and NDVI maps of bioretention at CBEIS. (<b>a</b>) 27 May 2021 and (<b>b</b>) 28 June 2021.</p>
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<p>Plant density prediction. (<b>a</b>) Library building (72.76%) and (<b>b</b>) green roof of business building (63.63%).</p>
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<p>RGB, NIR, and NDVI maps of GSI in MSU Tyler Hall. In each map, 6 sections were divided by sideways. Section 1, section 2, section 3 (top row, left to right) while section 4, section 5, section 6 (bottom row, left to right).</p>
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23 pages, 9608 KiB  
Article
Characterizing Land Surface Temperature (LST) through Remote Sensing Data for Small-Scale Urban Development Projects in the Gulf Cooperation Council (GCC)
by Maram Ahmed, Mohammed A. Aloshan, Wisam Mohammed, Essam Mesbah, Naser A. Alsaleh and Islam Elghonaimy
Sustainability 2024, 16(9), 3873; https://doi.org/10.3390/su16093873 - 6 May 2024
Cited by 2 | Viewed by 1806
Abstract
In the context of global climate change, there is a projected increase in land surface temperature (LST) worldwide, amplifying its impacts. This poses a particular concern for countries with hot climates, including the Kingdom of Bahrain as an example for the Gulf Cooperation [...] Read more.
In the context of global climate change, there is a projected increase in land surface temperature (LST) worldwide, amplifying its impacts. This poses a particular concern for countries with hot climates, including the Kingdom of Bahrain as an example for the Gulf Cooperation Council countries (GCC), which are countries with a hot climate. With a surge in population growth, there is a heightened demand for land to accommodate additional residential developments, creating an opportunity to investigate the influence of land use changes on LST variations. To achieve this goal, a residential development project spanning from 2013 to 2023 was undertaken. Landsat 8 OLI/TIRS remote sensing datasets were selected for four climate seasons, each set comprising images before and after development. The analysis involved extracting the LST, Normalized Difference Vegetation Index (NDVI), and Normalized Difference Built-Up Index (NDBI) on various dates, followed by correlation and regression analyses to explore their interrelationships. The results revealed a significant increase in the mean LST during spring and autumn post-development. A consistent positive association between the LST and NDBI was observed across all seasons, strengthening after development completion. Conversely, there was a pre-development negative correlation between the LST and NDVI, shifting to a positive relationship post-development. These findings empirically support the idea that small-scale residential developments contribute to notable LST increases, primarily due to expanded impervious surfaces. These insights have the potential to inform localized adaptation strategies for small-scale residential development projects, crucial for managing the impacts of rising land surface temperatures. Full article
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<p>Population in Bahrain [<a href="#B15-sustainability-16-03873" class="html-bibr">15</a>].</p>
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<p>Location of the study area. (<b>a</b>). location borders of the designated study area, (<b>b</b>). Micro location, (<b>c</b>). macro location (based on Google maps, edited by the researchers).</p>
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<p>Location of the study area. (<b>a</b>). location borders of the designated study area, (<b>b</b>). Micro location, (<b>c</b>). macro location (based on Google maps, edited by the researchers).</p>
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<p>A photo of the study area (source: author).</p>
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<p>Spatial pattern of the NDVI over the study area at (<b>a</b>) Spring 2013, (<b>b</b>) Spring 2022, (<b>c</b>) Summer 2013, (<b>d</b>) Summer 2022, (<b>e</b>) Autmn 2013, (<b>f</b>) Autmn 2022, (<b>g</b>) Winter 2014, and (<b>h</b>) Winter 2023.</p>
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<p>Seasonal variation of the land surface temperature NDVI before and after development of the study area.</p>
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<p>Spatial pattern of the NDBI over the study area at (<b>a</b>) Spring 2013, (<b>b</b>) Spring 2022, (<b>c</b>) Summer 2013, (<b>d</b>) Summer 2022, (<b>e</b>) Autmn 2013, (<b>f</b>) Autmn 2022, (<b>g</b>) Winter 2014, and (<b>h</b>) Winter 2023.</p>
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<p>Seasonal variation of the land surface temperature NDBI before and after development of the study area.</p>
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<p>Spatial pattern of the LST over the study area at (<b>A</b>) 2013, (<b>B</b>) 2022, (<b>C</b>) 2014, (<b>D</b>) 2023.</p>
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<p>Seasonal variation of the land surface temperature LST before and after development of the study area.</p>
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<p>Regression models for the NDVI and LST at (<b>a</b>) Spring 2013, (<b>b</b>) Spring 2022, (<b>c</b>) Summer 2013, (<b>d</b>) Summer 2022, (<b>e</b>) Autmn 2013, (<b>f</b>) Autmn 2022, (<b>g</b>) Winter 2014, and (<b>h</b>) Winter 2023.</p>
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<p>Regression models for the NDBI and LST at (<b>a</b>) Spring 2013, (<b>b</b>) Spring 2022, (<b>c</b>) Summer 2013, (<b>d</b>) Summer 2022, (<b>e</b>) Autmn 2013, (<b>f</b>) Autmn 2022, (<b>g</b>) Winter 2014, and (<b>h</b>) Winter 2023.</p>
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18 pages, 3511 KiB  
Article
Comparison of Random Forest and XGBoost Classifiers Using Integrated Optical and SAR Features for Mapping Urban Impervious Surface
by Zhenfeng Shao, Muhammad Nasar Ahmad and Akib Javed
Remote Sens. 2024, 16(4), 665; https://doi.org/10.3390/rs16040665 - 13 Feb 2024
Cited by 17 | Viewed by 5052
Abstract
The integration of optical and SAR datasets through ensemble machine learning models shows promising results in urban remote sensing applications. The integration of multi-sensor datasets enhances the accuracy of information extraction. This research presents a comparison of two ensemble machine learning classifiers (random [...] Read more.
The integration of optical and SAR datasets through ensemble machine learning models shows promising results in urban remote sensing applications. The integration of multi-sensor datasets enhances the accuracy of information extraction. This research presents a comparison of two ensemble machine learning classifiers (random forest and extreme gradient boost (XGBoost)) classifiers using an integration of optical and SAR features and simple layer stacking (SLS) techniques. Therefore, Sentinel-1 (SAR) and Landsat 8 (optical) datasets were used with SAR textures and enhanced modified indices to extract features for the year 2023. The classification process utilized two machine learning algorithms, random forest and XGBoost, for urban impervious surface extraction. The study focused on three significant East Asian cities with diverse urban dynamics: Jakarta, Manila, and Seoul. This research proposed a novel index called the Normalized Blue Water Index (NBWI), which distinguishes water from other features and was utilized as an optical feature. Results showed an overall accuracy of 81% for UIS classification using XGBoost and 77% with RF while classifying land use land cover into four major classes (water, vegetation, bare soil, and urban impervious). However, the proposed framework with the XGBoost classifier outperformed the RF algorithm and Dynamic World (DW) data product and comparatively showed higher classification accuracy. Still, all three results show poor separability with bare soil class compared to ground truth data. XGBoost outperformed random forest and Dynamic World in classification accuracy, highlighting its potential use in urban remote sensing applications. Full article
(This article belongs to the Topic Urban Land Use and Spatial Analysis)
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<p>Proposed framework.</p>
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<p>Selected cities from three different geographical locations.</p>
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<p>Confusion matrix: DW, RF, and XGBoost.</p>
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<p>Classified map of selected cities using DW, RF, and XGBoost. Numbers show the same area for three different datasets (DW, ESRI, ESA).</p>
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18 pages, 40104 KiB  
Article
Resilience of an Urban Coastal Ecosystem in the Caribbean: A Remote Sensing Approach in Western Puerto Rico
by Yadiel Noel Bonilla-Roman and Salvador Francisco Acuña-Guzman
Earth 2024, 5(1), 72-89; https://doi.org/10.3390/earth5010004 - 10 Feb 2024
Cited by 2 | Viewed by 1770
Abstract
Utilization of remote sensing-derived meteorological data is a valuable alternative for tropical insular territories such as Puerto Rico (PR). The study of ecosystem resilience in insular territories is an underdeveloped area of investigation. Little research has focused on studying how an ecosystem in [...] Read more.
Utilization of remote sensing-derived meteorological data is a valuable alternative for tropical insular territories such as Puerto Rico (PR). The study of ecosystem resilience in insular territories is an underdeveloped area of investigation. Little research has focused on studying how an ecosystem in PR responds to and recovers from unique meteorological events (e.g., hurricanes). This work aims to investigate how an ecosystem in Western Puerto Rico responds to extreme climate events and fluctuations, with a specific focus on evaluating its innate resilience. The Antillean islands in the Caribbean and Atlantic are vulnerable to intense weather phenomena, such as hurricanes. Due to the distinct tropical conditions inherent to this region, and the ongoing urban development of coastal areas, their ecosystems are constantly affected. Key indicators, including gross primary production (GPP), normalized difference vegetation index (NDVI), actual evapotranspiration (ET), and land surface temperature (LST), are examined to comprehend the interplay between these factors within the context of the Culebrinas River Watershed (CRW) ecosystem over the past decade during the peak of hurricane season. Data processing and analyses were performed on datasets provided by Moderate Resolution Imaging Spectroradiometer (MODIS) and Landsat 8–9 OLI TRIS, supplemented by information sourced from Puerto Rico Water and Energy Balance (PRWEB)—a dataset derived from Geostationary Operational Environmental Satellite (GOES) data. The findings revealed a complex interrelationship among atmospheric events and anthropogenic activities within the CRW, a region prone to recurrent atmospheric disruptions. NDVI and ET values from 2015 to 2019 showed the ecosystem’s capacity to recover after a prolonged drought period (2015) and Hurricanes Irma and Maria (2017). In 2015, the NDVI average was 0.79; after Hurricanes Irma and Maria in 2017, the NDVI dropped to 0.6, while in 2019, it had already increased to 0.8. Similarly, average ET values went from 3.2339 kg/m2/day in 2017 to 2.6513 kg/m2/day in 2018. Meanwhile, by 2019, the average ET was estimated to be 3.8105 kg/m2/day. Data geoprocessing of LST, NDVI, GPP, and ET, coupled with correlation analyses, revealed positive correlations among ET, NDVI, and GPP. Our results showed that areas with little anthropogenic impact displayed a more rapid and resilient restoration of the ecosystem. The spatial distribution of vegetation and impervious surfaces further highlights that areas closer to mountains have shown higher resilience while urban coastal areas have faced greater challenges in recovering from atmospheric events, thus showing the importance of preserving native vegetation, particularly mangroves, for long-term ecosystem stability. This study contributes to a deeper understanding of the dynamic interactions within urban coastal ecosystems in insular territories, emphasizing their resilience in the context of both natural atmospheric events and human activity. The insights gained from this research offer valuable guidance for managing and safeguarding ecosystems in similar regions characterized by their susceptibility to extreme weather phenomena. Full article
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<p>Land use/land cover map of Puerto Rico. The Culebrinas River Watershed (CRW) is located in the northwest region of Puerto Rico. It includes several municipalities and offers diverse ecosystem services.</p>
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<p>Spatial distribution of imperviousness within the Culebrinas River Watershed in Western Puerto Rico. The urban areas can be identified in red clusters as part of the main towns of the municipalities of Aguadilla, Aguada, Moca, and San Sebastian.</p>
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<p>Spatial distribution of NDVI estimated from MOD13Q1 between 2012 and 2022. Data for MOD17A2 (GPP) were not available for 2012 and 2022.</p>
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<p>Correlation between land surface temperature and the normalized difference vegetation index.</p>
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<p>Spatial distribution for <math display="inline"><semantics> <mrow> <msub> <mrow> <mi mathvariant="normal">L</mi> <mi mathvariant="normal">S</mi> <mi mathvariant="normal">T</mi> </mrow> <mrow> <mi>C</mi> <mi>o</mi> <mi>r</mi> <mi>r</mi> <mi>e</mi> <mi>c</mi> <mi>t</mi> <mi>e</mi> <mi>d</mi> </mrow> </msub> </mrow> </semantics></math> estimated from Landsat 8–9 OLI-TIRS between 2013 and 2022.</p>
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<p>Correlation between land surface temperature and actual evapotranspiration for 2015.</p>
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<p>Spatial distribution of ET estimated from MOD16A2 between 2012 and 2022.</p>
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<p>Correlation between normalized difference vegetation index and actual ET for 2017.</p>
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<p>Correlation between gross primary production and evapotranspiration for 2015.</p>
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<p>Spatial distribution of GPP estimated from MOD17A1; an 8-day composite with a 500 m resolution.</p>
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<p>Correlation between land surface temperature and gross primary production for 2017.</p>
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<p>Correlation between normalized difference vegetation index and gross primary production for 2017.</p>
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<p>Correlation between NDVI, LST, ET, and GPP from 2013 to 2021.</p>
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13 pages, 2575 KiB  
Article
A Study on the Evolution of Urban Underlying Surfaces and Extreme Rainfall in the Pearl River Delta
by Tianyin Xu, Zhiyong Yang, Xichao Gao and Jinjun Zhou
Water 2024, 16(2), 267; https://doi.org/10.3390/w16020267 - 12 Jan 2024
Viewed by 1225
Abstract
Problems such as the expansion of impervious areas and changes in underlying surfaces have occurred in cities due to rapid urbanization, along with an increasing probability of extreme rainfall. Based on the normalized building index (NDBI) of underlying surfaces, calculated from remote sensing [...] Read more.
Problems such as the expansion of impervious areas and changes in underlying surfaces have occurred in cities due to rapid urbanization, along with an increasing probability of extreme rainfall. Based on the normalized building index (NDBI) of underlying surfaces, calculated from remote sensing images in the Pearl River Delta from 1990 to 2020, this study determines the underlying surface changes in the Pearl River Delta. Based on the hourly rainfall data of meteorological stations in the Pearl River Delta region from 1990 to 2020, the extreme rainfall indexes are calculated to analyze the changes in extreme rainfall in the Pearl River Delta. Based on the NDBI of underlying surfaces and extreme rainfall calculated in the Pearl River Delta, the evolution of underlying surfaces and extreme rainfall is analyzed, as is the correlation between them, and the main conclusions are as follows: (1) From 1990 to 2020, the NDBI in highly urbanized areas in the Pearl River Delta was higher than that in non-highly urbanized areas. The NDBI in highly urbanized areas showed an increasing trend, and the growth rate tended to slow down; (2) From 1990 to 2020, extreme rainfall in highly urbanized areas of the Pearl River Delta was higher than in non-highly urbanized areas. Extreme rainfall in both highly urbanized areas and non-highly urbanized areas showed an increasing trend, with that in highly urbanized areas increasing faster; (3) The positive correlation between the NDBI and extreme rainfall indicators in highly urbanized areas is more significant than that in non-highly urbanized areas. Full article
(This article belongs to the Section Urban Water Management)
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<p>Study areas and meteorological stations.</p>
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<p>(<b>a</b>) Trends of NDBI in highly urbanized areas and non-highly urbanized areas; (<b>b</b>) trends of NDBI in Guangzhou and Zengcheng; (<b>c</b>) trends of NDBI in Nanhai and Gaoyao.</p>
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<p>Slopes of NDBI: (<b>a</b>) slope of NDBI between 1990 and 2020; (<b>b</b>) slope of NDBI between 1990 and 2003; (<b>c</b>) slope of NDBI between 2003 and 2020.</p>
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<p>(<b>a</b>) Trends of R99p in highly urbanized areas and non-highly urbanized areas; (<b>b</b>) trends of R95p in highly urbanized areas and non-highly urbanized areas; (<b>c</b>) trends of R99p in Guangzhou and Zengcheng; (<b>d</b>) trends of R95p in Guangzhou and Zengcheng; (<b>e</b>) trends of R99p in Nanhai and Gaoyao; (<b>f</b>) trends of R95p in Nanhai and Gaoyao.</p>
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17 pages, 9187 KiB  
Article
Automated Surface Runoff Estimation with the Spectral Unmixing of Remotely Sensed Multispectral Imagery
by Chloe Campo, Paolo Tamagnone and Guy Schumann
Remote Sens. 2024, 16(1), 136; https://doi.org/10.3390/rs16010136 - 28 Dec 2023
Viewed by 995
Abstract
This work presents a methodology for the hydrological characterization of natural and urban landscapes, focusing on accurate estimations of infiltration capacity and runoff characteristics. By combining existing methods from the literature, we created a systemic process that integrates satellite-based vegetation maps, topography, and [...] Read more.
This work presents a methodology for the hydrological characterization of natural and urban landscapes, focusing on accurate estimations of infiltration capacity and runoff characteristics. By combining existing methods from the literature, we created a systemic process that integrates satellite-based vegetation maps, topography, and soil permeability data. This process generates a detailed vegetation classification and slope-corrected composite curve number (CN) map using information at the subpixel level, which is crucial for estimating excess runoff during intense precipitation events. The algorithm designed with this methodology is automated and utilizes freely accessible multispectral imagery. Leveraging the vegetation–impervious–soil (V-I-S) model, it is assumed that land cover comprises V-I-S components at each pixel. Automated Music and spectral Separability-based Endmember Selection is employed on a generic spectral library to obtain the most relevant V-I-S endmember spectra for a particular image, which is then employed in multiple endmember spectral mixture analysis to obtain V-I-S fraction maps. The derived fractions are utilized in combination with the Normalized Difference Vegetation Index and the Modified Normalized Difference Water Index to adapt the CN map to different seasons and climatic conditions. The methodology was applied to Esch-sur-Alzette, Luxembourg, over a four-year period to validate the methodology and quantify the increase in the impervious surface area in the commune and the relationship with the runoff dynamics. This approach provides valuable insights into infiltration and runoff dynamics across diverse temporal and geographic ranges. Full article
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<p>Administrative border of Luxembourg, featuring the Esch-sur-Alzette commune in the southeast (indicated by the red rectangle).</p>
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<p>Methodology workflow.</p>
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<p>Interquartile (shaded areas) and mean reflectance (dash lines) for the V-I-S classes measured by the Sentinel-2 MSI sensor.</p>
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<p>The 2022 orthophoto of Esch-sur-Alzette, with the validation locations indicated in red. Each validation location was manually divided into vegetation, impervious, and soil portions.</p>
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<p>MESMA results in Esch-sur-Alzette over the study period showing the impervious fractional covers in 2018 (<b>left</b>) and 2022 (<b>right</b>).</p>
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<p>MESMA results in Esch-sur-Alzette over the study period showing the soil fractional covers in 2018 (<b>left</b>) and 2022 (<b>right</b>).</p>
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<p>MESMA results in Esch-sur-Alzette over the study period showing the vegetation fractional covers in 2018 (<b>left</b>) and 2022 (<b>right</b>).</p>
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<p>Runoff in the urban center of Esch-sur-Alzette in 2018 and 2022, along with the percent change in runoff during the study period.</p>
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16 pages, 15641 KiB  
Article
Evaluating Land Surface Temperature Trends and Explanatory Variables in the Miami Metropolitan Area from 2002–2021
by Alanna D. Shapiro and Weibo Liu
Geomatics 2024, 4(1), 1-16; https://doi.org/10.3390/geomatics4010001 - 25 Dec 2023
Cited by 1 | Viewed by 2982
Abstract
Physical and climatic variables such as Tree Canopy coverage, Normalized Difference Vegetation Index (NDVI), Distance to Roads, Distance to the Coast, Impervious Surface, and Precipitation can affect land surface temperature (LST). This paper examines the relationships using linear regression models and explores LST [...] Read more.
Physical and climatic variables such as Tree Canopy coverage, Normalized Difference Vegetation Index (NDVI), Distance to Roads, Distance to the Coast, Impervious Surface, and Precipitation can affect land surface temperature (LST). This paper examines the relationships using linear regression models and explores LST trends in the Miami Statistical Area (MSA) between 2002 and 2021. This study evaluates the effect of dry and wet seasons as well as day and night data on LST. A multiscale investigation is used to examine LST trends at the MSA scale, the individual county level, and at the pixel level to provide a detailed local perspective. The multiscale results are needed to understand spatiotemporal LST distributions to plan mitigation measures such as planting trees or greenery to regulate temperature and reduce the impacts of surface urban heat islands. The results indicate that LST values are rising in the MSA with a positive trend throughout the 20-year study period. The rate of change (RoC) for the wet season is smaller than for the dry season. The pixel-level analysis suggests that the RoC is primarily in rural areas and less apparent in urban areas. New development in rural areas may trigger increased RoC. This RoC relates to LST in the MSA and is different from global or regional RoC using air temperature. Results also suggest that climatic explanatory variables have different impacts during the night than they do in the daytime. For instance, the Tree Canopy variable has a positive coefficient, while during the day, the Tree Canopy variable has a negative relationship with LST. The Distance to the Coast variable changes from day to night as well. The increased granularity achieved with the multiscale analysis provides critical information needed to improve the effectiveness of potential mitigation efforts. Full article
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<p>The study area is the Miami metropolitan area.</p>
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<p>Methodology flowchart in this study.</p>
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<p>The spatial distributions of daytime and nighttime LST shown in °C during the dry and wet seasons with the urban areas overlayed (<b>a</b>) Dry Night, (<b>b</b>) Wet Night, (<b>c</b>) Dry Day, and (<b>d</b>) Wet Day.</p>
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<p>Annual LST trend analysis: (<b>a</b>) MSA, (<b>b</b>) PBC, (<b>c</b>) BC, and (<b>d</b>) MDC.</p>
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<p>Pixel-level LST trend spatial distribution showing significant pixels of <span class="html-italic">p</span>-value below 0.05 (<b>a</b>) yearly average of RoC, (<b>b</b>) dry season average of RoC, (<b>c</b>) wet season average of RoC, (<b>d</b>) yearly average of R<sup>2</sup>, (<b>e</b>) dry season average of R<sup>2</sup>, and (<b>f</b>) wet season average of R<sup>2</sup>. RoC is shown in °C/decade.</p>
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35 pages, 8026 KiB  
Article
Differential Urban Heat Vulnerability: The Tale of Three Alabama Cities
by Souleymane Fall, Kapo Coulibaly, Joseph Quansah and Gamal El Afandi
Urban Sci. 2023, 7(4), 121; https://doi.org/10.3390/urbansci7040121 - 3 Dec 2023
Viewed by 2324
Abstract
Urban heat vulnerability varies within and across cities, necessitating detailed studies to understand diverse populations’ specific vulnerabilities. This research assessed urban heat vulnerability at block group level in three Alabama cities: Birmingham, Montgomery, and Auburn-Opelika. The vulnerability index combines exposure, sensitivity, and adaptive [...] Read more.
Urban heat vulnerability varies within and across cities, necessitating detailed studies to understand diverse populations’ specific vulnerabilities. This research assessed urban heat vulnerability at block group level in three Alabama cities: Birmingham, Montgomery, and Auburn-Opelika. The vulnerability index combines exposure, sensitivity, and adaptive capacity subindices, incorporating Landsat 8 satellite-derived Land Surface Temperature (LST), demographic, and socioeconomic data using factor analysis and geospatial techniques. Results showed strong positive correlations between LST and impervious surfaces in Auburn-Opelika and Montgomery, with a moderate correlation in Birmingham. An inverse correlation between LST and Normalized Difference Vegetation Index was observed in all cities. High LST correlated with high population density, varying across cities. Birmingham and Montgomery’s central areas exhibited the highest heat exposure, influenced by imperviousness, population density, and socioeconomic factors. Auburn-Opelika had limited high heat exposure block groups, and high sensitivity did not always align with exposure. Correlations and cluster analysis were used to dissect the heat vulnerability index, revealing variations in contributing factors within and across cities. This study underscores the complex interplay of physical, social, and economic factors in urban heat vulnerability and emphasizes the need for location-specific research. Local governance, community engagement, and tailored interventions are crucial for addressing unique vulnerabilities in each urban context. Full article
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<p>Location of the Alabama cities investigated in this study and associated demographic characteristics (based on 2020 Census).</p>
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<p>Methods for LST retrieval from Landsat 8 bands.</p>
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<p>Statistical and geospatial analysis steps.</p>
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<p>Spatial distribution of LST over the cities: (<b>a</b>) Birmingham; (<b>b</b>) Montgomery; (<b>c</b>) Auburn-Opelika. Black lines denote the boundaries of block groups.</p>
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<p>Urban imperviousness (from the National Land Cover Database—NLCD, 2019) and Normalized Difference Vegetation Index (NDVI, from Landsat 8 composite [images from 2013 to 2021]): (<b>a</b>) Birmingham; (<b>b</b>) Montgomery; (<b>c</b>) Auburn-Opelika. Black lines denote the boundaries of block groups.</p>
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<p>Population density per square mile at block group level (2020 Census): (<b>a</b>) Birmingham; (<b>b</b>) Montgomery; (<b>c</b>) Auburn-Opelika.</p>
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<p>Spatial distribution of the subindices and vulnerability index scores for the City of Birmingham (Alabama) at block group level: (<b>a</b>) exposure; (<b>b</b>) sensitivity; (<b>c</b>) adaptive capacity; (<b>d</b>) vulnerability index.</p>
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<p>Spatial distribution of the subindices and vulnerability index scores for the City of Montgomery (Alabama) at block group level: (<b>a</b>) exposure; (<b>b</b>) sensitivity; (<b>c</b>) adaptive capacity; (<b>d</b>) vulnerability index.</p>
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<p>Spatial distribution of the subindices and vulnerability index scores for the Cities of Auburn and Opelika (Alabama) at block group level: (<b>a</b>) exposure; (<b>b</b>) sensitivity; (<b>c</b>) adaptive capacity; (<b>d</b>) vulnerability index.</p>
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<p>Correlation of the sensitivity subindex with its indicators: (<b>a</b>) Birmingham; (<b>b</b>) Montgomery; (<b>c</b>) Auburn-Opelika. All correlation coefficients are significant at the 5% level, except for those marked with an asterisk.</p>
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<p>Correlation of the adaptive capacity subindex with its indicators: (<b>a</b>) Birmingham; (<b>b</b>) Montgomery; (<b>c</b>) Auburn-Opelika. All correlation coefficients are significant at the 5% level, except for those marked with an asterisk.</p>
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<p>Cluster analysis for the city of Birmingham and spider diagrams representing the deconstruction of subindices associated with HH and LL clusters (clusters with higher and lower vulnerability scores): (<b>a</b>) spatial patterns of the cluster analysis; (<b>b</b>) deconstruction of the sensitivity subindex; (<b>c</b>) deconstruction of the adaptive capacity subindex. Values of indicators are scaled between 0 (lowest performance) and 100 (highest performance).</p>
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<p>Cluster analysis for the city of Montgomery and spider diagrams representing the deconstruction of subindices associated with HH and LL clusters (clusters with higher and lower vulnerability scores): (<b>a</b>) spatial patterns of the cluster analysis; (<b>b</b>) deconstruction of the sensitivity subindex; (<b>c</b>) deconstruction of the adaptive capacity subindex. Values of indicators are scaled between 0 (lowest performance) and 100 (highest performance).</p>
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<p>Cluster analysis for the cities of Auburn and Opelika and spider diagrams representing the deconstruction of subindices associated with HH and LL clusters (clusters with higher and lower vulnerability scores): (<b>a</b>) spatial patterns of the cluster analysis; (<b>b</b>) deconstruction of the sensitivity subindex; (<b>c</b>) deconstruction of the adaptive capacity subindex. Values of indicators are scaled between 0 (lowest performance) and 100 (highest performance).</p>
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<p>Example of a Montgomery block group profile. Values of the block group’s indicators are compared with the average for all the city’s other block groups.</p>
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<p>Overlay of block groups of high vulnerability (HH clusters of vulnerability) and block groups of high LST (HH clusters of LST) for (<b>a</b>) Birmingham; (<b>b</b>) Montgomery; (<b>c</b>) Auburn-Opelika. Co-occurrence is observed in Birmingham and Montgomery, but not in Auburn-Opelika.</p>
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21 pages, 23955 KiB  
Article
Assessing the Impact of Spatiotemporal Land Cover Changes on the Urban Heat Islands in Developing Cities with Landsat Data: A Case Study in Zhanjiang
by Yutian Hu, Hongye Li, Muhammad Amir Siddique and Dongyun Liu
Atmosphere 2023, 14(12), 1716; https://doi.org/10.3390/atmos14121716 - 22 Nov 2023
Cited by 2 | Viewed by 1970
Abstract
Land cover changes (LCCs) due to urbanization cause urban heat islands (UHIs), significantly affecting land surface temperature (LST) through spatiotemporal changes in compositions, parameters, and patterns. Land cover and LST have been studied in various cities; however, indicative research into heterogeneous LCC’s impact [...] Read more.
Land cover changes (LCCs) due to urbanization cause urban heat islands (UHIs), significantly affecting land surface temperature (LST) through spatiotemporal changes in compositions, parameters, and patterns. Land cover and LST have been studied in various cities; however, indicative research into heterogeneous LCC’s impact on LST in less-developed cities remains incomplete. This study analyzed new Landsat images of Zhanjiang, taken from 2004 to 2022, to determine the impact of three LCC indicators (compositions, parameters, and patterns) on LSTs. The urban thermal field variance index (UTFVI) was used to describe the distribution and variation in LST. We also quantified the cooling or warming benefits of various LCCs. The results indicate that the average temperature in the land urban heat island (SUHI) area rose to 30.6 °C. The average temperature of the SUHI was 3.32 °C higher than that of the non-SUHI area, showing the characteristic of shifting to counties and multi-core development. The LST increases by 0.37–0.67 °C with an increase of 0.1 in the normalized difference building index (NDBI), which is greater than the cooling benefit of the normalized difference of vegetation index (NDVI). The impact of landscape pattern indices on impervious surfaces and water is higher than that on vegetation and cropland, with a rising influence on impervious surfaces and a decreasing impact on water. The predominant cooling patches are vegetation and water, while large areas of impervious surface and cropland aggravate UHIs for industrial and agricultural activities. These findings are intended to guide future urban layouts and planning in less-developed cities, with thermal climate mitigation as a guiding principle. Full article
(This article belongs to the Special Issue UHI Analysis and Evaluation with Remote Sensing Data)
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<p>Study area: Zhanjiang and its geographical location (<b>a</b>–<b>c</b>).</p>
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<p>Research framework.</p>
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<p>(<b>A</b>) Land use cover changes (LUCC); (<b>B</b>) Normalized difference vegetation index (NDVI); (<b>C</b>) Normalized difference building index (NDBI).</p>
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<p>(<b>A</b>) Land surface temperature (LST); (<b>B</b>) Urban thermal field variance index (UTFVI) of Zhanjiang, 2004–2022, at 9-year intervals.</p>
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<p>Temperature statistics for SUHI and non-SUHI areas.</p>
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<p>Correlation analysis between NDVI, NDBI, and LST.</p>
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<p>Correlation analysis between landscape indices and LST. ** Sig. level <span class="html-italic">p</span> &lt; 0.01.</p>
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<p>(<b>A</b>) Temperature change caused by PLAND for each rise of 0.1; (<b>B</b>) Temperature change caused by LPI for each rise of 0.1; (<b>C</b>) Temperature change caused by DIVISION for each rise of 10.</p>
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<p>Average temperature of each land cover type in 2004, 2013, and 2022.</p>
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<p>UTFVI accounts for each land cover.</p>
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<p>UTFVI contribution over different land covers.</p>
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<p>Satellite images, land use classification, and surface temperature for typical plots from 2004 to 2022. (<b>a</b>) Lianjiang City—Qingjianling; (<b>b</b>) Xuwen County—Yugonglou Village; (<b>c</b>) Ma Zhang District—Baoshan Iron and Steel Factory; (<b>d</b>) Xuwen County—Dashuiqiao Reservoir.</p>
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20 pages, 42943 KiB  
Article
Coupling the Calibrated GlobalLand30 Data and Modified PLUS Model for Multi-Scenario Land Use Simulation and Landscape Ecological Risk Assessment
by Zongmin Wang, Mengdan Guo, Dong Zhang, Ruqi Chen, Chaofan Xi and Haibo Yang
Remote Sens. 2023, 15(21), 5186; https://doi.org/10.3390/rs15215186 - 31 Oct 2023
Cited by 7 | Viewed by 1749
Abstract
Rapid economic growth and urbanization have significantly changed the land use distribution and landscape ecological structure, which has a profound impact on the natural environment. A scientific grasp of the characteristics of land use distribution and its impact on landscape ecological risk is [...] Read more.
Rapid economic growth and urbanization have significantly changed the land use distribution and landscape ecological structure, which has a profound impact on the natural environment. A scientific grasp of the characteristics of land use distribution and its impact on landscape ecological risk is a prerequisite for sustainable urban development. This study aimed to calibrate GlobalLand30 data using the normalized difference impervious surface index (NDISI) obtained from Landsat images, thereby providing a more precise foundation for land simulation. Additionally, it sought to improve the accuracy of the patch-generating land use simulation (PLUS) through parameter sensitivity analysis. Building upon this, the research also simulates future land use in Beijing. Lastly, this study introduced an LER index to assess ecological risk in the current and future urban landscapes. The results showed that the GlobalLand30 data were calibrated and PLUS model accuracy was improved to more than 86%. The accuracy of the modified PLUS model based on a Morris sensitivity analysis was increased, and the kappa coefficients were increased by approximately 3%. The results of the multi-scenario simulation showed that under the SSP126-EP scenario, future land use in Beijing could balance urban development and ecological protection, and thus would be more suitable for sustainable development. In the other two scenarios, ecological land will be encroached by urban development. From 2000 to 2020, the degree of LER was generally lower, moderate, or higher, and the overall level of LER showed a downward trend continuing until 2100 in the SSP126-EG scenario. Future land use simulations and LER assessment under multi-scenarios could help decision makers develop multi-scale landscape protection strategies. Full article
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<p>Study area. Geographic location of Beijing, the division of the city and its four functional districts.</p>
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<p>Flowchart of land use simulation based on the PLUS Model and landscape ecological risk assessment in Beijing.</p>
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<p>Land use data before and after NDISI calibration in 2000, 2010, and 2020.</p>
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<p>Presentation of land use data by functional areas, 2000–2020: analyses based on the calibrated NDISI.</p>
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<p>Selection of the indicators with the best accuracy by combining the parameter ranges determined by the sensitivity analyses.</p>
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<p>Comparison of spatial distribution of real data and simulation results of land use pattern in 2010 and 2020 ((<b>a</b>,<b>c</b>) are calibrated GlobalLand30 data; (<b>b</b>,<b>d</b>) are the results of the PLUS simulation).</p>
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<p>Analysis of the contribution of various drivers to each land use type (“D-” indicates the closest distance to the road).</p>
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<p>Proportion of area of various land use types in Beijing in 2040, 2060, 2080 and 2100 predicted by Markov.</p>
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<p>Simulation of land use in Beijing under different scenarios based on the PLUS model.</p>
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<p>Spatial distribution of LER in 2000, 2010, and 2020. ((<b>a</b>–<b>c</b>) indicate 2000, 2010, and 2020, respectively).</p>
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<p>Spatial distribution of LER in future under different scenarios.</p>
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17 pages, 10862 KiB  
Article
Identification of Waterlogging-Prone Areas in Nanning from the Perspective of Urban Expansion
by Juan Huang, Jiangfeng Li and Zhi Huang
Sustainability 2023, 15(20), 15095; https://doi.org/10.3390/su152015095 - 20 Oct 2023
Cited by 1 | Viewed by 1253
Abstract
The objective of this study was to discern the spatial and temporal patterns of areas in Nanning that are susceptible to waterlogging, particularly during various phases of urban expansion. Furthermore, this study presents a proposal outlining strategies aimed at preventing and controlling waterlogging. [...] Read more.
The objective of this study was to discern the spatial and temporal patterns of areas in Nanning that are susceptible to waterlogging, particularly during various phases of urban expansion. Furthermore, this study presents a proposal outlining strategies aimed at preventing and controlling waterlogging. These strategies are based on the integration of the concepts of sponge city and resilient city construction. This study employed remote sensing (RS) and geographic information system (GIS) techniques to provide technical support. The supervised classification method and normalized difference index method were utilized to compare and extract impervious surfaces in Nanning from 2013 to 2020. The present investigation utilized the acquired impervious surfaces to compute the fractal dimension as a weighting factor, incorporating a digital elevation model (DEM) for the purpose of conducting a hydrological analysis in ArcGIS. Based on the findings of the study, several conclusions can be derived. The following conclusions can be drawn from the study: (1) The fractal dimension of Nanning varied over the study period, with values of 1.32, 1.41, and 1.58 in 2013, 2017, and 2020, respectively. The distribution of impervious surfaces showed a decreasing trend from the city center to the periphery. Urban planning and construction activities have significantly influenced the distribution of impervious surfaces, resulting in a progressively more complex and unstable structure. (2) From 2013 to 2020, the urban expansion fractal dimension increased from 1.32 to 1.58, indicating a decrease in the stability of impervious surfaces. The areas with higher concentrations of impervious surfaces coincided with frequent waterlogging-prone areas. Furthermore, the distribution of waterlogging-prone points transformed from a concentrated pattern to a scattered one. (3) In terms of waterlogging prevention and control strategies, the old urban areas are recommended to be transformed into sponge city projects, and the new development areas are planned, designed and implemented with the concept of “resilience”. Full article
(This article belongs to the Special Issue Land Use Change, Air Quality and Environmental Pollution Government)
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<p>Location map of Nanning in China. (<b>a</b>) Guangxi Zhuang Autonomous Region, (<b>b</b>) Nanning, (<b>c</b>) DEM and Nanning Municipal District.</p>
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<p>Waterlogging-prone area extraction flow chart.</p>
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<p>(<b>a</b>) Normalized difference index method-based extraction; (<b>b</b>) supervised taxonomy extraction.</p>
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<p>Spatial pattern of the impervious surfaces in Nanning: (<b>a</b>) 2013; (<b>b</b>) 2017; (<b>c</b>) 2020.</p>
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<p>Urban expansion fractal dimension: (<b>a</b>) 2013; (<b>b</b>) 2017; (<b>c</b>) 2020. Solid line is a double logarithmic scattering line, and dotted line represented the trend.</p>
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<p>Distribution of the waterlogging-prone areas in Nanning in (<b>a</b>) 2013, (<b>b</b>) 2017, and (<b>c</b>) 2020.</p>
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19 pages, 13062 KiB  
Article
Automatic Detection and Dynamic Analysis of Urban Heat Islands Based on Landsat Images
by Ni Na, Dandan Xu, Wen Fang, Yihan Pu, Yanqing Liu and Haobin Wang
Remote Sens. 2023, 15(16), 4006; https://doi.org/10.3390/rs15164006 - 12 Aug 2023
Cited by 5 | Viewed by 2608
Abstract
Given rapid global urban development, increases to impervious surfaces, urban population growth, building construction, and energy consumption result in the urban heat island (UHI) phenomenon. However, the spatial extent of UHIs is not clearly mapped in many UHI studies based on a remote [...] Read more.
Given rapid global urban development, increases to impervious surfaces, urban population growth, building construction, and energy consumption result in the urban heat island (UHI) phenomenon. However, the spatial extent of UHIs is not clearly mapped in many UHI studies based on a remote sensing approach. Therefore, we developed a method to extract the spatial extent of the UHI during the period from 2000 to 2021 in Nanjing, China, and explored the impact of urban two- and three-dimensional expansion on UHI spatial extent and UHI intensity. After cropland effects (i.e., bare soil) were eliminated, our proposed method combines the Getis-Ord-Gi* and the standard deviation of the normalized difference vegetation index (NDVI STD) to extract the UHI area from Landsat 5 and Landsat 8 images using land surface temperature (LST) spatial autocorrelation characteristics and the seasonal variation of vegetation. Our results show the following: (1) Bare farmland has a large influence on the extraction results of UHI—combined with the seasonal variation characteristics of NDVI STD, the impact of bare soil on UHI extraction was highly reduced, strongly improving the accuracy of UHI extraction. (2) The dynamics of the UHI area are consistent with the changes in the built-up area in Nanjing at both spatial and temporal scales, but with the increase of the urban green ratio, the UHI area of mature urban areas trends to decrease due to the cooling effect of green space. (3) The accumulation of population and GDP promote the vertical expansion of urban buildings. When the two-dimensional expansion of the city reaches saturation, the UHI intensity is primarily affected by three-dimensional urban expansion. Full article
(This article belongs to the Special Issue Application of Photogrammetry and Remote Sensing in Urban Areas)
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Figure 1

Figure 1
<p>Study area: Nanjing, China. (<b>a</b>) Administrative district map of Nanjing. The background image is a Landsat OLI image acquired on 9 October 2017, with standard false color composition (near-infrared band in red, red band in green, and green band in blue). (<b>b</b>) Land surface temperature distribution map of Nanjing on 9 October 2017.</p>
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<p>Methodology flowchart. NDVI = normalized difference vegetation index; NDVI STD = the standard deviation of normalized difference vegetation index; TIRS = thermal infrared band; NIR = near-infrared band; Red = red band; UHI = urban heat island.</p>
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<p>The extraction of urban heat island spatial distribution in Nanjing. (<b>a</b>) Land surface temperature of Nanjing on 20 May 2006; (<b>b</b>) the initial results of UHI (urban heat island) spatial extent on 20 May 2006; (<b>c</b>) the extraction of UHI spatial distribution after eliminating the effects of farmland on 20 May 2006; (<b>d</b>) land surface temperature of Nanjing on 9 October 2011; (<b>e</b>) the initial results of UHI spatial extents on 9 October 2011; (<b>f</b>) the extraction of UHI spatial distribution after eliminating the effects of farmland on 9 October 2011. The (<b>b</b>,<b>c</b>,<b>e</b>,<b>f</b>) panel backgrounds are Landsat images with standard false color composition (near-infrared band in red, red band in green, and green band in blue).</p>
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<p>Map of urban heat island (UHI) distribution. The UHI distribution in Nanjing on 10 October 2000 (<b>a</b>), 12 July 2002 (<b>b</b>), 20 May 2006 (<b>c</b>), 18 May 2011 (<b>d</b>), 9 October 2011 (<b>e</b>), 18 May 2017 (<b>f</b>), 9 October 2017 (<b>g</b>), 6 June 2018 (<b>h</b>), and 4 October 2021 (<b>i</b>). The background of panels (<b>a</b>–<b>i</b>) are Landsat images with standard false color composition (near-infrared band in red, red band in green, and green band in blue), with a spatial resolution of 30 m.</p>
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<p>(<b>a</b>) The change in urban heat island area from 2000 to 2021 in mature urban areas; (<b>b</b>) the change in urban heat island area from 2000 to 2021 in a developing urban areas.</p>
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<p>Changes in UHI area from 2000 to 2021 in Jiangning district (<b>a</b>); Pukou district (<b>b</b>); Lishui district (<b>c</b>); Gaochun district (<b>d</b>); Liuhe district (<b>e</b>).</p>
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<p>Temporal changes of air and land surface temperature in developing urban areas and mature urban areas, 2000–2021.</p>
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<p>Nanjing land cover classification map.</p>
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<p>The extraction of urban heat island (UHI) spatial distribution in Nanjing before removing farmland bare soil. (<b>a</b>) The UHI distributions of Nanjing on 3 May 2000; (<b>b</b>) 12 July 2002; (<b>c</b>) 20 May 2006; (<b>d</b>) 6 June 2018. The background of panels (<b>a</b>–<b>d</b>) are Landsat images with standard false color composition (near-infrared band in red, red band in green, and green band in blue), with a spatial resolution of 30 m.</p>
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<p>Population of each district in Nanjing (Nanjing Statistical Yearbook); mature urban area (<b>a</b>); developing urban area (<b>b</b>); Jiangning district (<b>c</b>); Pukou district (<b>d</b>); Lishui district (<b>e</b>); Gaochun district (<b>f</b>); Liuhe district (<b>g</b>).</p>
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<p>The GDP of mature and developing urban area (Nanjing Statistical Yearbook) (<b>a</b>); the completed building area of houses in Nanjing (<b>b</b>).</p>
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