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15 pages, 3730 KiB  
Article
A Study on Dust Storm Pollution and Source Identification in Northwestern China
by Hongfei Meng, Feiteng Wang, Guangzu Bai and Huilin Li
Toxics 2025, 13(1), 33; https://doi.org/10.3390/toxics13010033 - 3 Jan 2025
Viewed by 699
Abstract
In April 2023, a major dust storm event in Lanzhou attracted widespread attention. This study provides a comprehensive analysis of the causes, progression, and dust sources of this event using multiple data sources and methods. Backward trajectory analysis using the HYSPLIT model was [...] Read more.
In April 2023, a major dust storm event in Lanzhou attracted widespread attention. This study provides a comprehensive analysis of the causes, progression, and dust sources of this event using multiple data sources and methods. Backward trajectory analysis using the HYSPLIT model was employed to trace the origins of the dust, while FY-2H satellite data provided high-resolution dust distribution patterns. Additionally, the MAIAC AOD product was used to analyze Aerosol Optical Depth, and concentration-weighted trajectory (CWT) analysis was used to identify key dust source regions. The study found that PM10 played a dominant role in the storm, and the AOD values during the storm in Lanzhou were significantly higher than the annual average, highlighting the severe impact on regional air quality. Key meteorological conditions influencing the storm’s occurrence were analyzed, including the formation and eastward movement of a high-potential ridge, convection driven by diurnal temperature variations, and surface temperature increases coupled with decreased relative humidity, which together promoted the generation and development of dust. Backward trajectory and dust distribution analyses revealed that the dust primarily originated from Central Asia, western Mongolia, Xinjiang, and Gansu. From the 19th to the 21st, the dust distribution showed similarities between day and night, with a noticeable increase in dust concentration from night to day due to strong vertical atmospheric mixing. To mitigate the impacts of future dust storms, this study highlights both short-term and long-term strategies, including enhanced monitoring systems, public health advisories, and vegetation restoration in key source regions. Strengthening regional and international cooperation for transboundary dust management is also emphasized as critical for sustainable mitigation efforts. These findings are significant for understanding and predicting the causes, characteristics, and environmental impacts of dust storms in Lanzhou and the Northwestern region. Full article
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Figure 1
<p>Location of the study area and site distribution map.</p>
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<p>Mean spatial distribution of AOD in Lanzhou from 17 to 23 April 2023.</p>
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<p>Temporal variation in pollutants (PM<sub>10</sub> [µg/m<sup>3</sup>], PM<sub>2.5</sub> [µg/m<sup>3</sup>], CO [mg/m<sup>3</sup>], O<sub>3</sub> [µg/m<sup>3</sup>], SO<sub>2</sub> [µg/m<sup>3</sup>], NO<sub>2</sub> [µg/m<sup>3</sup>]) at six monitoring stations in Lanzhou (LLBG: Lan Lian Bin Guan; JYG: Jiao Yu Gang; BHGY: Bai He Gong Yuan; TLSJY: Tie Lu She Ji Yuan; SWZPS: Sheng Wu Zhi Pin Suo; HP: He Ping) from 17 to 23 April 2023.</p>
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<p>Backward trajectories of atmospheric pollutants from 17 to 23 April 2023: (<b>a</b>) overall cluster distribution, (<b>b</b>) trajectory directions for 17 to 18 April, (<b>c</b>) trajectory directions for 19 to 21 April (dust storm phase), and (<b>d</b>) trajectory directions for 22 to 23 April.</p>
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<p>Concentration-weighted trajectory (CWT) analysis of PM<sub>2.5</sub> and PM<sub>10</sub> during 19–21 April 2023: (<b>a</b>) PM<sub>2.5</sub> contribution from source regions and (<b>b</b>) PM<sub>10</sub> contribution from source regions. Black dots in the figure represent the location of Lanzhou City.</p>
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<p>Temperature and 500 hPa geopotential height field (<b>a</b>–<b>c</b>) and relative humidity and wind field ((<b>d</b>–<b>f</b>), White arrows indicate wind speed and direction) from the 19th to the 21st. Black dots in the figure represent the location of Lanzhou City.</p>
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<p>Sand and dust distribution maps from the night of the 19th to the 21st (<b>a</b>,<b>c</b>,<b>e</b>) and during the day (<b>b</b>,<b>d</b>,<b>f</b>). Black dots in the figure represent the location of Lanzhou City.</p>
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20 pages, 7358 KiB  
Article
Research on the Estimation of Air Pollution Models with Machine Learning in Urban Sustainable Development Based on Remote Sensing
by Wenqian Chen, Na Zhang, Xuesong Bai and Xiaoyi Cao
Sustainability 2024, 16(24), 10949; https://doi.org/10.3390/su162410949 - 13 Dec 2024
Viewed by 640
Abstract
Air quality is directly related to people’s health and quality of life and has a profound impact on the sustainable development of cities. Good air quality is the foundation of sustainable development. To solve the current problem of air quality for sustainable development, [...] Read more.
Air quality is directly related to people’s health and quality of life and has a profound impact on the sustainable development of cities. Good air quality is the foundation of sustainable development. To solve the current problem of air quality for sustainable development, we used high-resolution (1 km) satellite-retrieved aerosol optical depth (AOD), meteorological, nighttime light and vegetation data to develop a spatiotemporal convolution feature random forest (SCRF) model to predict the PM2.5 concentration in Shandong from 2016 to 2019. We evaluated the performance of the SCRF model and compared the results of other models, including neural network (BPNN), gradient boosting (GBDT), and random forest (RF) models. The results show that compared with the other models, the improved SCRF model performs best. The coefficient of determination (R2) and root mean square error (RMSE) are 0.83 and 9.87 µg/m3, respectively. Moreover, we discovered that the characteristic variables AOD and air temperature (TEM) data improved the accuracy of the model in Shandong Province. The annual average PM2.5 concentrations in Shandong Province from 2016 to 2019 were 74.44 µg/m3, 65.01 µg/m3, 58.32 µg/m3, and 59 µg/m3, respectively. The spatial distribution of air pollution increases from northeastern and southeastern to western Shandong inland. In general, our research has significant implications for the sustainable development of various cities in Shandong Province. Full article
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<p>Overview of the study area and distribution map of PM<sub>2.5</sub> stations (AOD data on 26 December 2018).</p>
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<p>Schematic diagram of the SCRF model.</p>
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<p>Histogram and descriptive statistics of the independent model variables (mean, median and standard deviation).</p>
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<p>Average PM<sub>2.5</sub> concentrations at ground monitoring stations in Shandong Province.</p>
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<p>Heatmap and Pearson correlation coefficient histogram of the correlation analysis between the PM<sub>2.5</sub> concentration and other characteristic variables: (<b>a</b>) Correlation analysis heatmap; (<b>b</b>) Pearson correlation coefficient histogram.</p>
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<p>Changes in overall R<sup>2</sup> and RMSE with the number of decision trees from 2016 to 2019.</p>
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<p>Model-based feature importance ranking.</p>
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<p>Fitting diagram of the annual PM<sub>2.5</sub> concentrations predicted by the RF (<b>a</b>–<b>d</b>) and SCRF (<b>e</b>–<b>h</b>) models in Shandong Province from 2016 to 2019.</p>
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<p>Fitting diagram of the seasonal PM<sub>2.5</sub> concentrations predicted by the RF (<b>a</b>–<b>d</b>) and SCRF (<b>e</b>–<b>h</b>) models in Shandong Province from 2016 to 2019.</p>
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<p>Annual average PM<sub>2.5</sub> concentration in Shandong Province from 2016 to 2019.</p>
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<p>Seasonal average PM<sub>2.5</sub> concentrations in spring, summer, autumn and winter in Shandong Province from 2016 to 2019.</p>
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<p>Average total concentration of PM<sub>2.5</sub> in spring, summer, autumn and winter in Shandong Province from 2016 to 2019.</p>
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17 pages, 3410 KiB  
Article
The Aerosol Optical Depth Retrieval from Wide-Swath Imaging of DaQi-1 over Beijing
by Zhongting Wang, Ruijie Zhang, Ruizhi Chen and Hui Chen
Atmosphere 2024, 15(12), 1476; https://doi.org/10.3390/atmos15121476 - 10 Dec 2024
Viewed by 624
Abstract
The Wide-Swath Imaging (WSI) sensor is a Chinese satellite launched in 2022, capable of providing data at resolutions ranging from 75 to 600 m for monitoring aerosols, fire points, and dust, among other uses. In this study, we developed a Dark Dense Vegetation [...] Read more.
The Wide-Swath Imaging (WSI) sensor is a Chinese satellite launched in 2022, capable of providing data at resolutions ranging from 75 to 600 m for monitoring aerosols, fire points, and dust, among other uses. In this study, we developed a Dark Dense Vegetation method to retrieve the Aerosol Optical Depth (AOD) quickly from WSI 600 m data. First, after splitting into three types according to the Normalized Difference Vegetation Index (NDVI), we calculated the empirical parameters of land reflectance between the red (0.65 μm) and blue (0.47 μm) channels using Moderate Resolution Imaging Spectroradiometer (MODIS) reflectance products over the Beijing area. Second, the decrease in the NDVI was simulated and analyzed under different AODs and solar zenith angles, and we introduced an iterative inversion approach to account for it. The simulation retrievals demonstrated that the iterative inversion produced accurate results after less than four iterations. Thirdly, we utilized the atmospherically corrected NDVI for dark target identification and output the AOD result. Finally, retrieval experiments were conducted using WSI 600 m data collected over Beijing in 2023. The retrieved AOD images highlighted two air pollution events occurring during 3–8 March and 27–31 October 2023. The inversion results in 2023 showed a strong correlation with Aerosol Robotic Network station data (the correlation coefficient was greater than 0.9). Our method exhibited greater accuracy than the MODIS aerosol product, though it was less accurate than the Multi-Angle Implementation of Atmospheric Correction product. Full article
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<p>Filter response functions of WSI and MODIS in the channels which range from 380 nm to 900 nm.</p>
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<p>Flow chart of AOD retrieval method for WSI.</p>
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<p>The percentage histogram of pixel count over the Beijing area: (<b>a</b>) is surface reflectance in blue, green, red and NIR channels, and (<b>b</b>) is NDVI.</p>
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<p>The comparison of surface reflectance between red and blue: (<b>a</b>) is low vegetation, (<b>b</b>) is medium vegetation, (<b>c</b>) is high vegetation, and (<b>d</b>) is all of the vegetation. Dashed line represents the linear fitting line. The color represents the percentage of pixel numbers.</p>
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<p>The decreased NDVI under different AODs. The left is SZA = 21 degrees (<b>a</b>,<b>c</b>,<b>e</b>), while the right is SZA = 63 degrees (<b>b</b>,<b>d</b>,<b>f</b>). The top is low vegetation (<b>a</b>,<b>b</b>), the middle is medium vegetation (<b>c</b>,<b>d</b>), and the bottom is high vegetation (<b>e</b>,<b>f</b>).</p>
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<p>The maximum number of iterations changing with AOD and errors from measurements: (<b>a</b>) is low vegetation, (<b>b</b>) is medium vegetation, and (<b>c</b>) is high vegetation.</p>
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<p>Daily PM<sub>2.5</sub> concentration on 3–8 March 2023.</p>
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<p>WSI AOD images during a pollution event on 3–8 March 2023.</p>
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<p>Daily PM<sub>2.5</sub> concentration on 27–31 October 2023.</p>
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<p>WSI AOD images during a pollution event on 27–31 October 2023. (<b>a</b>) is October 27, (<b>b</b>) is October 28, (<b>c</b>) is October 29, (<b>d</b>) is October 30, and (<b>e</b>) is October 31.</p>
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<p>WSI AOD images during a pollution event on 27–31 October 2023. (<b>a</b>) is October 27, (<b>b</b>) is October 28, (<b>c</b>) is October 29, (<b>d</b>) is October 30, and (<b>e</b>) is October 31.</p>
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<p>AOD in 2023 over AERONET Beijing station. The yellow is AERONET, the green is WSI, the red is MYD04, and the black is MAIAC.</p>
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<p>AOD validation of WSI (<b>a</b>) MAIAC, (<b>b</b>) and MYD04, (<b>c</b>) with AERONET data. N represents the number of matched pixels. (<b>d</b>) All matched points, where the green is WSI, the red is MYD04, and the black is MAIAC.</p>
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<p>AOD validation of WSI (<b>a</b>) MAIAC, (<b>b</b>) and MYD04, (<b>c</b>) with AERONET data. N represents the number of matched pixels. (<b>d</b>) All matched points, where the green is WSI, the red is MYD04, and the black is MAIAC.</p>
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20 pages, 7713 KiB  
Article
Dynamics of Aboveground Carbon Across Karst Terrestrial Ecosystems in China from 2015 to 2021
by Jinan Shi, Ling Yu, Hongqian Fang, Ke Zhang, Jean-Pierre Wigneron, Xiaojun Li, Tianxiang Cui, Can Liu, Yue Jiao and Dacheng Wang
Forests 2024, 15(12), 2143; https://doi.org/10.3390/f15122143 - 5 Dec 2024
Viewed by 562
Abstract
Over the past half-century, environmental degradation and human disturbances have threatened the aboveground biomass carbon (AGC) in China’s karst ecosystems. However, recent ecological programs have led to environmental improvements, leaving it unclear whether China’s karst ecosystems act as an AGC sink or AGC [...] Read more.
Over the past half-century, environmental degradation and human disturbances have threatened the aboveground biomass carbon (AGC) in China’s karst ecosystems. However, recent ecological programs have led to environmental improvements, leaving it unclear whether China’s karst ecosystems act as an AGC sink or AGC source. In this study, we utilized L-band vegetation optical depth to quantify the dynamics of AGC across the karst regions of China from 2015 to 2021. We observed an increase in AGC density of 0.73 Mg C ha−1 yr−1, suggesting that karst ecosystems in China functioned as an AGC sink throughout the research period. The largest increase in AGC density, 1.29 Mg C ha−1 yr−1, was observed in Central China, indicating an AGC sink capacity stronger than that of other regions. Among the different land-use types, forests played a dominant role, exhibiting the largest net change in AGC density at 1.03 Mg C ha−1 yr−1. Furthermore, using the random forest model, temperature, soil clay content, and altitude were identified as the primary factors driving AGC changes. Our results enhance the understanding of the role of China’s karst terrestrial ecosystem in the global carbon cycle, emphasizing its contribution to the global carbon sink. Full article
(This article belongs to the Section Forest Inventory, Modeling and Remote Sensing)
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<p>The spread of karst landforms within China.</p>
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<p>AGC density spatial distribution. (<b>a</b>) Mean AGC density over the 2015–2021 timeframe. (<b>b</b>) Latitude-dependent fluctuations in AGC density. (<b>c</b>) Longitude-dependent fluctuations in AGC density.</p>
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<p>Variations in AGC density across different geographic regions (<b>a</b>) and land-use types (<b>b</b>), as well as AGC stock distribution (<b>c</b>,<b>d</b>). Letters a–g indicate that identical letters represent no significant difference, while different letters indicate a significant difference (<math display="inline"><semantics> <mrow> <mi>p</mi> <mo>&lt;</mo> <mn>0.05</mn> </mrow> </semantics></math>). Error bars represent the standard deviation (std).</p>
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<p>Dynamic changes in AGC from 2015 to 2021. (<b>a</b>) Yearly AGC changes across the study region. (<b>b</b>) Yearly AGC changes across different land-use types. (<b>c</b>) Yearly AGC changes across seven geographical regions. Error bars represent the standard deviation (std).</p>
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<p>Regional and land-use-based changes in AGC density in the karst regions of China from 2015 to 2021. (<b>a</b>) Changes across different regions. (<b>b</b>) Changes across different land-use types.</p>
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<p>Spatial changes in AGC density in the karst regions of China from 2015 to 2021. (<b>a</b>) Net AGC density change during 2015–2021. (<b>b</b>) Latitudinal variation in net AGC density change from 2015 to 2021.</p>
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<p>AGC trends in China’s karst regions from 2015 to 2021. Categories were defined based on the criteria outlined in <a href="#forests-15-02143-t0A3" class="html-table">Table A3</a>, where 1 indicates a non-significant trend, 2 represents a slightly significant increase, and 3 denotes a significant increase.</p>
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<p>Impact of environmental factors on AGC: SHAP values and partial dependence. (<b>a</b>) Bar chart displaying these average magnitudes of SHAP values for each environmental factor. (<b>b</b>–<b>e</b>) The marginal effect on AGC of Temp (<b>b</b>), SClay (<b>c</b>), Altitude (<b>d</b>), and Pre (<b>e</b>). The lines illustrate the average response in the random forest model for a specific variable, keeping the other variables at different values.</p>
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<p>A collection of bee swarm plots. Each dot’s position along the <span class="html-italic">x</span>-axis indicates the influence of a variable on the RF model’s prediction for a specific sample. When dots overlap at the same x-coordinate, they accumulate to reflect the density of the impact.</p>
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<p>Relationships between annual L-VOD in 2015 and the Saathci AGC benchmark map. The fitted curve (blue line) was obtained using Equation (6) in the main text. Each dot represents an individual data point, and asterisks indicate statistical significance with <math display="inline"><semantics> <mrow> <mi>p</mi> <mo>&lt;</mo> <mn>0.01</mn> </mrow> </semantics></math>.</p>
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<p>A comparison between the AGC derived from L-VOD and the AGC from GEDI during the period from 2019 to 2021. The 1:1 line indicates the perfect correlation where both variables have equal values, and each dot represents an individual data point.</p>
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23 pages, 10605 KiB  
Article
Estimation of Winter Wheat Stem Biomass by a Novel Two-Component and Two-Parameter Stratified Model Using Proximal Remote Sensing and Phenological Variables
by Weinan Chen, Guijun Yang, Yang Meng, Haikuan Feng, Heli Li, Aohua Tang, Jing Zhang, Xingang Xu, Hao Yang, Changchun Li and Zhenhong Li
Remote Sens. 2024, 16(22), 4300; https://doi.org/10.3390/rs16224300 - 18 Nov 2024
Viewed by 562
Abstract
The timely and precise estimation of stem biomass is critical for monitoring the crop growing status. Optical remote sensing is limited by the penetration of sunlight into the canopy depth, and thus directly estimating winter wheat stem biomass via canopy spectra remains a [...] Read more.
The timely and precise estimation of stem biomass is critical for monitoring the crop growing status. Optical remote sensing is limited by the penetration of sunlight into the canopy depth, and thus directly estimating winter wheat stem biomass via canopy spectra remains a difficult task. There is a stable linear relationship between the stem dry biomass (SDB) and leaf dry biomass (LDB) of winter wheat during the entire growth stage. Therefore, this study comprehensively considered remote sensing and crop phenology, as well as biomass allocation laws, to establish a novel two-component (LDB, SDB) and two-parameter (phenological variables, spectral vegetation indices) stratified model (Tc/Tp-SDB) to estimate SDB across the growth stages of winter wheat. The core of the Tc/Tp-SDB model employed phenological variables (e.g., effective accumulative temperature, EAT) to correct the SDB estimations determined from the LDB. In particular, LDB was estimated using spectral vegetation indices (e.g., red-edge chlorophyll index, CIred edge). The results revealed that the coefficient values (β0 and β1) of ordinary least squares regression (OLSR) of SDB with LDB had a strong relationship with phenological variables. These coefficient (β0 and β1) relationships were used to correct the OLSR model parameters based on the calculated phenological variables. The EAT and CIred edge were determined as the optimal parameters for predicting SDB with the novel Tc/Tp-SDB model, with r, RMSE, MAE, and distance between indices of simulation and observation (DISO) values of 0.85, 1.28 t/ha, 0.95 t/ha, and 0.31, respectively. The estimation error of SDB showed an increasing trend from the jointing to flowering stages. Moreover, the proposed model showed good potential for estimating SDB from UAV hyperspectral imagery. This study demonstrates the ability of the Tc/Tp-SDB model to accurately estimate SDB across different growing seasons and growth stages of winter wheat. Full article
(This article belongs to the Section Remote Sensing in Agriculture and Vegetation)
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<p>Geographical location of the study area and winter wheat field experiment. (<b>a</b>) Location of all experiments; (<b>b</b>) the layout of the experimental plots during 2019–2020; (<b>c</b>) experimental designs conducted during 2013–2015 (Exp. 1 and Exp. 2); (<b>d</b>) experimental designs conducted during 2019–2020 and 2021–2022 (Exp. 3 and Exp. 4).</p>
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<p>Daily average temperature during the four growing seasons of the study: (<b>a</b>) Exp. 1 (2013–2014); (<b>b</b>) Exp. 2 (2014–2015); (<b>c</b>) Exp. 3 (2019–2020); (<b>d</b>) Exp. 4 (2021–2022). Note: The sowing days (DAS = 0) of the four experiments were 1 October 2013, 7 October 2014, 27 September 2019, and 30 September 2021.</p>
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<p>Distribution of the measured LDB (<b>a</b>) and SDB (<b>b</b>) for the calibration and validation datasets. The μ and σ represent average and standard deviation, respectively.</p>
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<p>Flowchart of the approach used to develop and validate the Tc/Tp-SDB model.</p>
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<p>Winter wheat data collected in this study at different growth stages during the four-year experiment: (<b>a</b>) SDB, (<b>b</b>) LDB.</p>
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<p>Relationship between VIs and dry biomass variables at different stages of the 2019–2020 growing season. (<b>a</b>) SDB vs. CI<sub>red edge</sub>, (<b>b</b>) LDB vs. CI<sub>red edge</sub>, (<b>c</b>) SDB vs. ND<sub>LMA</sub>, (<b>d</b>) LDB vs. ND<sub>LMA</sub>.</p>
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<p>Relationship between LDB and SDB at different stages during four growing seasons: (<b>a</b>) 2013–2014, (<b>b</b>) 2014–2015, (<b>c</b>) 2019–2020, (<b>d</b>) 2021–2022.</p>
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<p>Average and standard deviation of the correlation coefficient r (<b>a</b>), RMSE (<b>b</b>), MAE (<b>c</b>), and DISO (<b>d</b>) using the test datasets from the 5-fold cross-validation.</p>
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<p>Relationship (<b>a</b>,<b>b</b>) between measured and estimated LDB using the CIred edge-LDB method, and the residual distributions between different LDB levels (<b>c</b>,<b>d</b>).</p>
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<p>Relationship between the measured and estimated SDB of winter wheat using the calibration datasets. (<b>a</b>) GDD; (<b>b</b>) EAT; (<b>c</b>) DOY; (<b>d</b>) DAS.</p>
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<p>Relationship between the measured and estimated SDB of winter wheat using the calibration datasets. (<b>a</b>) GDD; (<b>b</b>) EAT; (<b>c</b>) DOY; (<b>d</b>) DAS.</p>
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<p>Relationship (<b>a</b>,<b>b</b>) between the measured and estimated SDB of winter wheat using the validation datasets, and the residual distribution for the Tc/Tp-SDB-EAT and Tc/Tp-SDB-DOY models under different SDB levels (<b>c</b>,<b>d</b>).</p>
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<p>Relationship (<b>a</b>,<b>b</b>) between the measured and estimated SDB of winter wheat using the validation datasets, and the residual distribution for the Tc/Tp-SDB-EAT and Tc/Tp-SDB-DOY models under different SDB levels (<b>c</b>,<b>d</b>).</p>
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<p>SDB maps determined from the Tc/Tp-SDB model with UAV hyperspectral images. (<b>a</b>) SDB during the flagging stage (26<sup>th</sup> April); (<b>b</b>) SDB during the flowering stage (13<sup>th</sup> May).</p>
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<p>The distribution of the residuals of LDB and SDB in different growth stages (<b>a</b>), and the change of SLR with growth stage (<b>b</b>). Note: both (<b>a</b>,<b>b</b>) use all datasets.</p>
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<p>Relationship between the measured and estimated SDB of winter wheat using the validation datasets with models using only (<b>a</b>) CI<sub>red edge</sub>, (<b>b</b>) EAT.</p>
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14 pages, 2842 KiB  
Article
Integrating Multi-Source Remote Sensing Data for Forest Fire Risk Assessment
by Xinzhu Liu, Change Zheng, Guangyu Wang, Fengjun Zhao, Ye Tian and Hongchen Li
Forests 2024, 15(11), 2028; https://doi.org/10.3390/f15112028 - 18 Nov 2024
Viewed by 866
Abstract
Forest fires are a frequent and destructive phenomenon in Southwestern China, posing significant threats to ecological systems and human lives and property. In response to the growing need for effective forest fire prevention, this study introduces an innovative method for predicting and assessing [...] Read more.
Forest fires are a frequent and destructive phenomenon in Southwestern China, posing significant threats to ecological systems and human lives and property. In response to the growing need for effective forest fire prevention, this study introduces an innovative method for predicting and assessing forest fire risk. By integrating multi-source data, including optical and microwave remote sensing, meteorological, topographic, and human activity data, the approach enhances the sensitivity of risk models to vegetation water content and other critical factors. The vegetation water content is derived from both Vegetation Optical Depth and optical remote sensing data, allowing for a more accurate assessment of changes in vegetation moisture that influence fire risk. A time series prediction model, incorporating attention mechanisms, is used to assess the probability of fire occurrence. Additionally, the method includes fire spread simulations based on Cellular Automaton and Monte Carlo approaches to evaluate potential burn areas. This combined approach can provide a comprehensive fire risk assessment using the probability of both fire occurrence and potential fire spread. Experimental results show that the integration of microwave data and attention mechanisms improves prediction accuracy by 2.8%. This method offers valuable insights for forest fire management, aiding in targeted prevention strategies and resource allocation. Full article
(This article belongs to the Topic Application of Remote Sensing in Forest Fire)
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<p>(<b>a</b>) Study area showing the historical (2015–2018) fire point extracted from the NASA website and the DEM (Digital Elevation Model) as the background image. (<b>b</b>) Land classification in the study area extracted from MCD12Q1.</p>
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<p>(<b>a</b>) Monthly and (<b>b</b>) yearly fire frequency from 2015 to 2018, calculated from NASA website data in the study area, with trends highlighting high fire frequency from January to May.</p>
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<p>Driving factors in predicting forest fire occurrence: (<b>a</b>) temperature, (<b>b</b>) precipitational, (<b>c</b>) humidity, (<b>d</b>) wind speed, (<b>e</b>) VOD, (<b>f</b>) NDVI, (<b>g</b>) DEM, (<b>h</b>) slope, (<b>i</b>) aspect, (<b>j</b>) railway, and (<b>k</b>) highway.</p>
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<p>Deep learning model framework for predicting forest fire occurrence probability.</p>
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<p>The resulting ROC curve of the proposed mode.</p>
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<p>(<b>a</b>) The forest fire occurrence probability map using the proposed mode. (<b>b</b>) The forest fire potential burn probability using simulation. (<b>c</b>) The forest fire risk in the study area.</p>
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22 pages, 6049 KiB  
Article
Spatiotemporal Evolution Analysis of PM2.5 Concentrations in Central China Using the Random Forest Algorithm
by Gang Fang, Yin Zhu and Junnan Zhang
Sustainability 2024, 16(19), 8613; https://doi.org/10.3390/su16198613 - 4 Oct 2024
Cited by 1 | Viewed by 979
Abstract
This study focuses on Central China (CC), including Shanxi, Henan, Anhui, Hubei, Jiangxi, and Hunan provinces. The 2019 average annual precipitation (PRE), average annual temperature (TEM), average annual wind speed (WS), population density (POP), normalized difference vegetation index (NDVI), aerosol optical depth (AOD), [...] Read more.
This study focuses on Central China (CC), including Shanxi, Henan, Anhui, Hubei, Jiangxi, and Hunan provinces. The 2019 average annual precipitation (PRE), average annual temperature (TEM), average annual wind speed (WS), population density (POP), normalized difference vegetation index (NDVI), aerosol optical depth (AOD), gross domestic product (GDP), and elevation (DEM) data were used as explanatory variables to predict the average annual PM2.5 concentrations (PM2.5Cons) in CC. The average annual PM2.5Cons were predicted using different models, including multiple linear regression (MLR), back propagation neural network (BPNN), and random forest (RF) models. The results showed higher prediction accuracy and stability of the RF algorithm (RFA) than those of the other models. Therefore, it was used to analyze the contributions of the explanatory factors to the PM2.5 concentration (PM2.5Con) prediction in CC. Subsequently, the spatiotemporal evolution of the PM2.5Cons from 2010 to 2021 was systematically analyzed. The results indicated that (1) PRE and AOD had the most significant impacts on the PM2.5Cons. Specifically, the PRE and AOD values exhibited negative and positive correlations with the PM2.5Cons, respectively. The NDVI and WS were negatively correlated with the PM2.5Cons; (2) the southern and northern parts of Shanxi and Henan provinces, respectively, experienced the highest PM2.5Cons in the 2010–2013 period, indicating severe air pollution. However, the PM2.5Cons in the 2014–2021 period showed spatial decreasing trends, demonstrating the effectiveness of the implemented air pollution control measures in reducing pollution and improving air quality in CC. The findings of this study provide scientific evidence for air pollution control and policy making in CC. To further advance atmospheric sustainability in CC, the study suggested that the government enhance air quality monitoring, manage pollution sources, raise public awareness about environmental protection, and promote green lifestyles. Full article
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<p>Geographical location of Central China.</p>
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<p>Flowchart.</p>
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<p>Relationship between tree and error.</p>
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<p>Training set accuracy.</p>
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<p>Test set accuracy.</p>
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<p>Residual plot.</p>
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<p>Q–Q plot of residuals.</p>
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<p>Spatial distribution of explanatory variables.</p>
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<p>Spatial distribution of explanatory variables.</p>
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<p>Model accuracy.</p>
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<p>Ranking of important factors.</p>
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<p>Impact of influencing factors on PM<sub>2.5</sub>Con (Unit: <math display="inline"><semantics> <mrow> <mi mathvariant="normal">g</mi> <mo>/</mo> <msup> <mrow> <mi mathvariant="normal">m</mi> </mrow> <mrow> <mn>3</mn> </mrow> </msup> </mrow> </semantics></math>).</p>
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<p>PM<sub>2.5</sub> distribution from 2010 to 2021.</p>
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<p>PM<sub>2.5</sub> distribution from 2010 to 2021.</p>
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<p>PM<sub>2.5</sub> distribution from 2010 to 2021.</p>
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<p>PM<sub>2.5</sub>Con trends by province.</p>
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<p>Average PM<sub>2.5</sub>Con.</p>
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13 pages, 17472 KiB  
Article
High-Resolution Daily PM2.5 Exposure Concentrations in South Korea Using CMAQ Data Assimilation with Surface Measurements and MAIAC AOD (2015–2021)
by Jin-Goo Kang, Ju-Yong Lee, Jeong-Beom Lee, Jun-Hyun Lim, Hui-Young Yun and Dae-Ryun Choi
Atmosphere 2024, 15(10), 1152; https://doi.org/10.3390/atmos15101152 - 26 Sep 2024
Viewed by 1079
Abstract
Particulate matter (PM) in the atmosphere poses significant risks to both human health and the environment. Specifically, PM2.5, particulate matter with a diameter less than 2.5 micrometers, has been linked to increased rates of cardiovascular and respiratory diseases. In South Korea, concerns about [...] Read more.
Particulate matter (PM) in the atmosphere poses significant risks to both human health and the environment. Specifically, PM2.5, particulate matter with a diameter less than 2.5 micrometers, has been linked to increased rates of cardiovascular and respiratory diseases. In South Korea, concerns about PM2.5 exposure have grown due to its potential for causing premature death. This study aims to estimate high-resolution exposure concentrations of PM2.5 across South Korea from 2015 to 2021. We integrated data from the Community Multiscale Air Quality (CMAQ) model with surface air quality measurements, the Weather Research Forecast (WRF) model, the Normalized Difference Vegetation Index (NDVI), and the Multi-Angle Implementation of Atmospheric Correction (MAIAC) Aerosol Optical Depth (AOD) satellite data. These data, combined with multiple regression analyses, allowed for the correction of PM2.5 estimates, particularly in suburban areas where ground measurements are sparse. The simulated PM2.5 concentration showed strong correlations with observed values R (ranging from 0.88 to 0.94). Spatial distributions of annual PM2.5 showed a significant decrease in PM2.5 concentrations from 2015 to 2021, with some fluctuation due to the COVID-19 pandemic, such as in 2020. The study produced highly accurate daily average high-resolution PM2.5 exposure concentrations. Full article
(This article belongs to the Special Issue Novel Insights into Air Pollution over East Asia)
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<p>Locations of ambient air quality monitoring stations in the region of China and Korea (blue dots: china monitoring stations, green dots: south korea monitoring stations).</p>
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<p>Modeling domain (Domain 1: East Asia, Domain 2: South Korea).</p>
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<p>Scatter plots of MLRs with observations for 2015–2021.</p>
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<p>Reanalyzed average seasonal PM2.5 distribution in 2015–2021.</p>
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<p>Reanalyzed average seasonal PM2.5 distribution in 2015–2021.</p>
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<p>Reanalyzed annual PM2.5 distribution in 2015–2021.</p>
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29 pages, 3577 KiB  
Review
Recent Advances in Light Penetration Depth for Postharvest Quality Evaluation of Fruits and Vegetables
by Yuping Huang, Jie Xiong, Ziang Li, Dong Hu, Ye Sun, Haojun Jin, Huichun Zhang and Huimin Fang
Foods 2024, 13(17), 2688; https://doi.org/10.3390/foods13172688 - 26 Aug 2024
Cited by 1 | Viewed by 1877
Abstract
Light penetration depth, as a characteristic parameter reflecting light attenuation and transmission in biological tissues, has been applied in nondestructive detection of fruits and vegetables. Recently, with emergence of new optical detection technologies, researchers have begun to explore methods evaluating optical properties of [...] Read more.
Light penetration depth, as a characteristic parameter reflecting light attenuation and transmission in biological tissues, has been applied in nondestructive detection of fruits and vegetables. Recently, with emergence of new optical detection technologies, researchers have begun to explore methods evaluating optical properties of double-layer or even multilayer fruit and vegetable tissues due to the differences between peel and pulp in the chemical composition and physical properties, which has gradually promoted studies on light penetration depth. A series of demonstrated research on light penetration depth could ensure the accuracy of the optical information obtained from each layer of tissue, which is beneficial to enhance detection accuracy for quality assessment of fruits and vegetables. Therefore, the aim of this review is to give detailed outlines about the theory and principle of light penetration depth based on several emerging optical detection technologies and to focus primarily on its applications in the field of quality evaluation of fruits and vegetables, its future applicability in fruits and vegetables and the challenges it may face in the future. Full article
(This article belongs to the Section Food Packaging and Preservation)
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<p>Schematic of the interaction between light and an object.</p>
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<p>Energy variations of Rayleigh scattering and Raman scattering (energy level: Em &lt; En).</p>
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<p>Relationship between light attenuation and light penetration depth in tissues.</p>
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<p>(<b>a</b>) Schematic representation of extrapolated boundary; (<b>b</b>) MC simulation for diffuse reflectance and absorption of tissues; (<b>c</b>) transmission process of photons in the AD method.</p>
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<p>(<b>a</b>) Flowchart of the MC simulation of a single photon; (<b>b</b>) flowchart of the IAD method.</p>
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<p>(<b>a</b>) Short-pulsed illumination at the surface of a semi-infinite turbid medium; (<b>b</b>) schematic of time-resolved system for measuring optical properties, in which PMT is a photomultiplier tube and SYNC is the synchronization signal.</p>
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<p>(<b>a</b>) Schematic illustrations of configuration of single-fiber and “banana-shape” path of light transfer; (<b>b</b>) multifiber array based on a multiplexer; (<b>c</b>) multifiber array based on a multiplexer; (<b>d</b>) multichannel curved array based on spatially resolved system.</p>
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<p>(<b>a</b>) Schematic illustrations of noncontact SRS systems; (<b>b</b>) schematic of an SFDI system for spectral image acquisition.</p>
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17 pages, 6355 KiB  
Technical Note
Estimation of Soil Organic Carbon Density on the Qinghai–Tibet Plateau Using a Machine Learning Model Driven by Multisource Remote Sensing
by Qi Chen, Wei Zhou and Wenjiao Shi
Remote Sens. 2024, 16(16), 3006; https://doi.org/10.3390/rs16163006 - 16 Aug 2024
Cited by 1 | Viewed by 1032
Abstract
Soil organic carbon (SOC) plays a vital role in the global carbon cycle and soil quality assessment. The Qinghai–Tibet Plateau is one of the largest plateaus in the world. Therefore, in this region, SOC density and the spatial distribution of SOC are highly [...] Read more.
Soil organic carbon (SOC) plays a vital role in the global carbon cycle and soil quality assessment. The Qinghai–Tibet Plateau is one of the largest plateaus in the world. Therefore, in this region, SOC density and the spatial distribution of SOC are highly sensitive to climate change and human intervention. Given the insufficient understanding of the spatial distribution of SOC density in the Qinghai–Tibet Plateau, this study utilized machine learning (ML) algorithms to estimate the density and distribution pattern of SOC density in the region. In this study, we first collected multisource data, such as optical remote sensing data, synthetic aperture radar) (SAR) data, and other environmental variables, including socioeconomic factors, topographic factors, climate factors, and soil properties. Then, we used ML algorithms, namely random forest (RF), extreme gradient boosting (XGBoost), and light gradient boosting machine (LightGBM), to estimate the topsoil SOC density and spatial distribution patterns of SOC density. We also aimed to investigate any driving factors. The results are as follows: (1) The average SOC density is 5.30 kg/m2. (2) Among the three ML algorithms used, LightGBM showed the highest validation accuracy (R2 = 0.7537, RMSE = 2.4928 kgC/m2, MAE = 1.7195). (3) The normalized difference vegetation index (NDVI), valley depth (VD), and temperature are crucial in predicting the spatial distribution of topsoil SOC density. Feature importance analyses conducted using the three ML models all showed these factors to be among the top three in importance, with contribution rates of 14.08%, 12.29%, and 14.06%; 17.32%, 20.73%, and 24.62%; and 16.72%, 11.96%, and 20.03%. (4) Spatially, the southeastern part of the Qinghai–Tibet Plateau has the highest topsoil SOC density, with recorded values ranging from 8.41 kg/m2 to 13.2 kg/m2, while the northwestern part has the lowest density, with recorded values ranging from 0.85 kg/m2 to 2.88 kg/m2. Different land cover types showed varying SOC density values, with forests and grasslands having higher SOC densities compared to urban and bare land areas. The findings of this study provide a scientific basis for future soil resource management and improved carbon sequestration accounting in the Qinghai–Tibet Plateau. Full article
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<p>The spatial location of the study area and the soil sampling points.</p>
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<p>Ranking of key influencing factors of SOC density based on Boruta feature selection method.</p>
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<p>SOC density mapping of Qinghai–Tibet Plateau based on (<b>a</b>) LightGBM model, (<b>b</b>) land cover types, (<b>c</b>) correlation matrix of LUCC and input variables, and (<b>d</b>) analysis of the relationship between SOC density and LUCC.</p>
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<p>Analysis of Relative Importance of Variables using (<b>a</b>) RF Model (<b>b</b>) XGBoost Model and (<b>c</b>) LightGBM Model.</p>
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<p>Validation of measured SOC using (<b>a</b>) this study’s LightGBM 500 m, (<b>b</b>) SoilGrids250m prediction, and (<b>c</b>) SoilGrids1km prediction.</p>
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<p>Spatial distribution of topsoil SOC density using (<b>a</b>) this study’s LightGBM 500 m, (<b>b</b>) SoilGrids250m prediction, and (<b>c</b>) SoilGrids1km prediction.</p>
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30 pages, 18624 KiB  
Article
Harnessing Machine Learning Algorithms to Model the Association between Land Use/Land Cover Change and Heatwave Dynamics for Enhanced Environmental Management
by Kumar Ashwini, Briti Sundar Sil, Abdulla Al Kafy, Hamad Ahmed Altuwaijri, Hrithik Nath and Zullyadini A. Rahaman
Land 2024, 13(8), 1273; https://doi.org/10.3390/land13081273 - 12 Aug 2024
Cited by 2 | Viewed by 2267
Abstract
As we navigate the fast-paced era of urban expansion, the integration of machine learning (ML) and remote sensing (RS) has become a cornerstone in environmental management. This research, focusing on Silchar City, a non-attainment city under the National Clean Air Program (NCAP), leverages [...] Read more.
As we navigate the fast-paced era of urban expansion, the integration of machine learning (ML) and remote sensing (RS) has become a cornerstone in environmental management. This research, focusing on Silchar City, a non-attainment city under the National Clean Air Program (NCAP), leverages these advanced technologies to understand the urban microclimate and its implications on the health, resilience, and sustainability of the built environment. The rise in land surface temperature (LST) and changes in land use and land cover (LULC) have been identified as key contributors to thermal dynamics, particularly focusing on the development of urban heat islands (UHIs). The Urban Thermal Field Variance Index (UTFVI) can assess the influence of UHIs, which is considered a parameter for ecological quality assessment. This research examines the interlinkages among urban expansion, LST, and thermal dynamics in Silchar City due to a substantial rise in air temperature, poor air quality, and particulate matter PM2.5. Using Landsat satellite imagery, LULC maps were derived for 2000, 2010, and 2020 by applying a supervised classification approach. LST was calculated by converting thermal band spectral radiance into brightness temperature. We utilized Cellular Automata (CA) and Artificial Neural Networks (ANNs) to project potential scenarios up to the year 2040. Over the two-decade period from 2000 to 2020, we observed a 21% expansion in built-up areas, primarily at the expense of vegetation and agricultural lands. This land transformation contributed to increased LST, with over 10% of the area exceeding 25 °C in 2020 compared with just 1% in 2000. The CA model predicts built-up areas will grow by an additional 26% by 2040, causing LST to rise by 4 °C. The UTFVI analysis reveals declining thermal comfort, with the worst affected zone projected to expand by 7 km2. The increase in PM2.5 and aerosol optical depth over the past two decades further indicates deteriorating air quality. This study underscores the potential of ML and RS in environmental management, providing valuable insights into urban expansion, thermal dynamics, and air quality that can guide policy formulation for sustainable urban planning. Full article
(This article belongs to the Special Issue Geospatial Data in Land Suitability Assessment: 2nd Edition)
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<p>Location map of the study area (<b>A</b>) India and Assam, (<b>B</b>) Assam and Silchar, and (<b>C</b>) Silchar City.</p>
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<p>Population density in (<b>A</b>) 2000, (<b>B</b>) 2010, and (<b>C</b>) 2020.</p>
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<p>Methodological Flowchart (<b>A</b>) LST and UTFVI estimation (<b>B</b>) LULC prediction approach.</p>
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<p>ANN model architecture for predicting (<b>A</b>) LST and (<b>B</b>) UTFVI.</p>
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<p>Predicted and measured (<b>A</b>) LST and (<b>B</b>) UTFVI for 2020.</p>
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<p>LULC for the years (<b>A</b>) 2000, (<b>B</b>) 2010, and (<b>C</b>) 2020.</p>
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<p>Decadal % change in area from 2000 to 2020.</p>
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<p>Annual average trend in (<b>a</b>) MODIS AOD and (<b>b</b>) PM<sub>2.5</sub> for the last two decades in the study area.</p>
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<p>LULC for the years (<b>A</b>) 2030 and (<b>B</b>) 2040.</p>
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<p>LST for the years (<b>A</b>) 2000, (<b>B</b>) 2010, and (<b>C</b>) 2020.</p>
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<p>Predicted LST for (<b>A</b>) 2030 and (<b>B</b>) 2040.</p>
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<p>UTFVI for the years (<b>A</b>) 2000, (<b>B</b>) 2010, and (<b>C</b>) 2020.</p>
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<p>Predicted UTFVI for (<b>A</b>) 2030 and (<b>B</b>) 2040.</p>
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<p>Urban and rural population of the world, 1950–2050 [<a href="#B104-land-13-01273" class="html-bibr">104</a>].</p>
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<p>Overall percentage change In LULC from 2000 to 2040.</p>
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<p>Directional change map of urban areas from 2000 to 2040.</p>
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<p>The overall change in the area statistics of LST from 2000 to 2040.</p>
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<p>Trend in (<b>A</b>) T<sub>max</sub> and (<b>B</b>) T<sub>min</sub> for Silchar City using RCP4.5 data.</p>
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17 pages, 2212 KiB  
Article
Improvements to a Crucial Budyko-Fu Parameter and Evapotranspiration Estimates via Vegetation Optical Depth over the Yellow River Basin
by Xingyi Wang and Jiaxin Jin
Remote Sens. 2024, 16(15), 2777; https://doi.org/10.3390/rs16152777 - 29 Jul 2024
Viewed by 920
Abstract
Against the backdrop of global warming and vegetation restoration, research on the evapotranspiration mechanism of the Yellow River basin has become a hot topic. The Budyko-Fu model is widely used to estimate basin-scale evapotranspiration, and its crucial parameter ω is used to characterize [...] Read more.
Against the backdrop of global warming and vegetation restoration, research on the evapotranspiration mechanism of the Yellow River basin has become a hot topic. The Budyko-Fu model is widely used to estimate basin-scale evapotranspiration, and its crucial parameter ω is used to characterize the underlying surface and climate characteristics of different basins. However, most studies only use factors such as the normalized difference vegetation index (NDVI), which represents the greenness of vegetation, to quantify the relationship between ω and the underlying surface, thereby neglecting richer vegetation information. In this study, we used long time-series multi-source remote sensing data from 1988 to 2015 and stepwise regression to establish dynamic estimation models of parameter ω for three subwatersheds of the upper Yellow River and quantify the contribution of underlying surface factors and climate factors to this parameter. In particular, vegetation optical depth (VOD) was introduced to represent plant biomass to improve the applicability of the model. The results showed that the dynamic estimation models of parameter ω established for the three subwatersheds were reasonable (R2 = 0.60, 0.80, and 0.40), and parameter ω was significantly correlated with the VOD and standardized precipitation evapotranspiration index (SPEI) in all watersheds. The dominant factors affecting the parameter in the different subwatersheds also differed, with underlying surface factors mainly affecting the parameter in the watershed before Longyang Gorge (BLG) (contributing 64% to 76%) and the watershed from Lanzhou to Hekou Town (LHT) (contributing 63% to 83%) and climate factors mainly affecting the parameter in the watershed from Longyang Gorge to Lanzhou (LGL) (contributing 75% to 93%). The results of this study reveal the changing mechanism of evapotranspiration in the Yellow River watershed and provide an important scientific basis for regional water balance assessment, global change response, and sustainable development. Full article
(This article belongs to the Special Issue Remote Sensing for Terrestrial Hydrologic Variables)
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<p>Three subwatersheds of the upper Yellow River basin.</p>
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<p>Technology roadmap for the study.</p>
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<p>Trend charts of evapotranspiration (<b>a</b>), potential evapotranspiration (<b>b</b>), and precipitation (<b>c</b>) in the three subwatersheds of the upper Yellow River from 1988 to 2015 as well as the trend chart of parameter <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">ω</mi> </mrow> </semantics></math> (<b>d</b>) after the moving average treatment.</p>
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<p>Distribution of parameter <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">ω</mi> </mrow> </semantics></math> of the three subwatersheds on the Budyko curve.</p>
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<p>The variation trends of underlying surface factors VOD (<b>a</b>) and NDVI (<b>b</b>), as well as climate factors SPEI (<b>c</b>) and TMP (<b>d</b>) in the three subwatersheds from 1988 to 2015.</p>
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<p>Spearman correlation analysis heatmap between parameter <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">ω</mi> </mrow> </semantics></math> and the respective variable factors in the BLG (<b>a</b>), LGL (<b>b</b>), and LHT (<b>c</b>), * represents significant correlation between variables.</p>
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<p>Residual plot of true and predicted values for parameter <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">ω</mi> </mrow> </semantics></math> (<b>a</b>–<b>c</b>) and watershed evapotranspiration (<b>d</b>–<b>f</b>).</p>
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<p>Quantification of the contribution of factors to parameter <math display="inline"><semantics> <mrow> <mi mathvariant="sans-serif">ω</mi> </mrow> </semantics></math> using the standardized coefficient method (<b>a</b>) and R<sup>2</sup> decomposition method (<b>b</b>).</p>
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15 pages, 20542 KiB  
Article
Long-Term Ecological and Environmental Quality Assessment Using an Improved Remote-Sensing Ecological Index (IRSEI): A Case Study of Hangzhou City, China
by Cheng Cai, Jingye Li and Zhanqi Wang
Land 2024, 13(8), 1152; https://doi.org/10.3390/land13081152 - 27 Jul 2024
Cited by 1 | Viewed by 939
Abstract
The integrity and resilience of our environment are confronted with unprecedented challenges, stemming from the escalating pressures of urban expansion and the need for ecological preservation. This study proposes an Improved Remote Sensing Ecological Index (IRSEI), which employs humidity (WET), the Normalized Difference [...] Read more.
The integrity and resilience of our environment are confronted with unprecedented challenges, stemming from the escalating pressures of urban expansion and the need for ecological preservation. This study proposes an Improved Remote Sensing Ecological Index (IRSEI), which employs humidity (WET), the Normalized Difference Vegetation Index (NDVI), Land Surface Temperature (LST), a standardized Building–Bare Soil Index (NDBSI), aerosol optical depth (AOD), and the comprehensive salinity index (CSI). The IRSEI model was utilized to assess the ecological quality of Hangzhou over the period from 2003 to 2023. Additionally, the random forest model was employed to analyze the factors driving ecological quality. Furthermore, the gradient effect in the horizontal direction away from the urban center was examined using the buffer zone method. Our analysis reveals the following: (1) approximately 95% of the alterations in ecological quality observed from 2003 to 2023 exhibited marginal improvements, declines, or were negligible; (2) the transformations in IRSEI during this period, including variations in surface temperature and transportation networks, exhibited strong correlations (0.85) with human activities. Moreover, the influence of AOD and the comprehensive salinity index on IRSEI demonstrated distinct spatial disparities; (3) the IRSEI remained generally stable up to 30 km outside the city center, indicating a trend of agglomeration in the center and significant areas in the surroundings. The IRSEI serves as a robust framework for bolstering the assessment of regional ecological health, facilitating ecological preservation and rejuvenation efforts, and fostering coordinated sustainable regional development. Full article
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<p>Study area location map.</p>
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<p>Spatial distribution map of ecological factors.</p>
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<p>Spatial distribution map of ecological quality in Hangzhou.</p>
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<p>Spatial distribution map of ecological quality in Hangzhou.</p>
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<p>Regional-level distribution map of ecological quality decreased significantly in Hangzhou.</p>
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<p>Spatial distribution map of ecological quality in Hangzhou, 2003–2023.</p>
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19 pages, 12973 KiB  
Article
A Novel Flexible Geographically Weighted Neural Network for High-Precision PM2.5 Mapping across the Contiguous United States
by Dongchao Wang, Jianfei Cao, Baolei Zhang, Ye Zhang and Lei Xie
ISPRS Int. J. Geo-Inf. 2024, 13(7), 217; https://doi.org/10.3390/ijgi13070217 - 22 Jun 2024
Cited by 2 | Viewed by 1294
Abstract
Air quality degradation has triggered a large-scale public health crisis globally. Existing machine learning techniques have been used to attempt the remote sensing estimates of PM2.5. However, many machine learning models ignore the spatial non-stationarity of predictive variables. To address this issue, this [...] Read more.
Air quality degradation has triggered a large-scale public health crisis globally. Existing machine learning techniques have been used to attempt the remote sensing estimates of PM2.5. However, many machine learning models ignore the spatial non-stationarity of predictive variables. To address this issue, this study introduces a Flexible Geographically Weighted Neural Network (FGWNN) to estimate PM2.5 based on multi-source remote sensing data. FGWNN incorporates the Flexible Geographical Neuron (FGN) and Geographical Activation Function (GWAF) within the framework of Artificial Neural Network (ANN) to capture the intricate spatial non-stationary relationships among predictive variables. A robust air quality remote sensing estimation model was constructed using remote sensing data of Aerosol Optical Depth (AOD), Normalized Difference Vegetation Index (NDVI), Temperature (TMP), Specific Humidity (SPFH), Wind Speed (WIND), and Terrain Elevation (HGT) as inputs, and Ground-Based PM2.5 as the observation. The results indicated that FGWNN successfully generates PM2.5 remote sensing data with a 2.5 km spatial resolution for the contiguous United States (CONUS) in 2022. It exhibits higher regression accuracy compared to traditional ANN and Geographically Weighted Regression (GWR) models. FGWNN holds the potential for applications in high-precision and high-resolution remote sensing scenarios. Full article
(This article belongs to the Special Issue HealthScape: Intersections of Health, Environment, and GIS&T)
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<p>The spatial distribution of PM2.5 concentration monitored by ground-based stations over the CONUS in 2022.</p>
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<p>Mean distribution of PM2.5 driving factors across the CONUS in 2022. (<b>a</b>) AOD: Aerosol Optical Depth; (<b>b</b>) NDVI: Normalized Difference Vegetation Index; (<b>c</b>) TMP: temperature; (<b>d</b>) SPFH: specific humidity; (<b>e</b>) WIND: wind speed; (<b>f</b>) HGT: terrain elevation.</p>
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<p>The FGWNN network architecture for PM2.5 inversion.</p>
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<p>Comparison of the effects before and after implementing the uniformization strategy. (<b>a</b>) Non-uniformization GN; (<b>b</b>) Uniformization GN; (<b>c</b>) Learning curve under non-uniformization mode; (<b>d</b>) Learning curve under uniformization mode; (<b>e</b>) Estimated local R<sup>2</sup> for non-uniformization mode; (<b>f</b>) Estimated local R<sup>2</sup> for uniformization mode.</p>
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<p>FGN number optimization (marked by red dotted circle) and comparison of computational cost changes.</p>
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<p>Scatter plots of estimated versus observed PM2.5 for the (<b>a</b>) MLR, (<b>b</b>) ANN, (<b>c</b>) GWR, and (<b>d</b>) FGWNN models.</p>
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<p>Trends in global regression metrics across the four seasons of 2022.</p>
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<p>Boxplots of local regression metrics across the four seasons of 2022. (<b>a</b>) Local RMSE in Spring; (<b>b</b>) Local RMSE in Summer; (<b>c</b>) Local R<sup>2</sup> in Spring; (<b>d</b>) Local R<sup>2</sup> in Summer; (<b>e</b>) Local RMSE in Autumn; (<b>f</b>) Local RMSE in Winter; (<b>g</b>) Local R<sup>2</sup> in Autumn; (<b>h</b>) Local R<sup>2</sup> in Winter.</p>
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<p>Local RMSE results for year and seasons in 2022 via FGWNN model.</p>
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<p>Satellite-derived mapping of ground-level PM2.5 concentration over CONUS in 2022.</p>
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<p>Three states of SDF. (<b>a</b>) Sparse state; (<b>b</b>) Biased state; (<b>c</b>) Ideal state: uniform and dense placement of FGNs.</p>
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<p>Spatial resolutions corresponding to the different study region levels. (<b>a</b>) CONUS; (<b>b</b>) Pacific Division; (<b>c</b>) California State; (<b>d</b>) Los Angeles County.</p>
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22 pages, 21135 KiB  
Article
Assessing the Nonlinear Relationship between Land Cover Change and PM10 Concentration Change in China
by Xiankang Xu, Jian Hao, Yuxin Liang and Jingwei Shen
Land 2024, 13(6), 766; https://doi.org/10.3390/land13060766 - 29 May 2024
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Abstract
Inhalable particulate matter (PM10) is a major air pollutant that has significant impacts on environmental climate and human health. Land-cover change is also a key factor influencing changes in atmospheric pollution. Changes in land-cover types can lead to changes in the [...] Read more.
Inhalable particulate matter (PM10) is a major air pollutant that has significant impacts on environmental climate and human health. Land-cover change is also a key factor influencing changes in atmospheric pollution. Changes in land-cover types can lead to changes in the sources and sinks of air pollutants, thus affecting the spatial distribution of PM10, which poses a threat to human health. Therefore, exploring the relationship between PM10 concentration change and land-cover change is of great significance. In this study, we constructed an extreme randomized trees model (ET) based on ground PM10 monitoring data, satellite-based aerosol optical depth (AOD) data, and auxiliary data including meteorological, vegetation, and population data to retrieve ground-level PM10 concentrations across China. The coefficient of determination (R2), the mean absolute error (MAE), and the root mean square error (RMSE) of the model were 0.878, 5.742 μg/m3, and 8.826 μg/m3, respectively. Based on this, we analyzed the spatio-temporal distribution of PM10 concentrations in China from 2015 to 2021. High PM10 values were mainly observed in the desert areas of northwestern China and the Beijing–Tianjin–Hebei urban agglomeration. The majority of China showed a significant decrease in PM10 concentrations. Additionally, we also analyzed the nonlinear response mechanism of the PM10 concentration change to land-cover change. The PM10 concentration is sensitive to forest and barren land change. Therefore, strengthening the protection of forests and desertification control can significantly reduce air pollution. Attention should also be paid to emission management in agricultural activities and urbanization processes. Full article
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<p>Overview of the study area.</p>
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<p>The framework of the study.</p>
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<p>Model accuracy at each monitoring station from 2015 to 2021: (<b>a</b>) R<sup>2</sup>, (<b>b</b>) MAE, (<b>c</b>) RMSE.</p>
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<p>Annual and multiple-year mean PM<sub>10</sub> maps (1 km × 1 km) in China.</p>
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<p><span class="html-italic">p</span>-value of PM<sub>10</sub> trend over China.</p>
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<p>Spatial distribution of the annual PM<sub>10</sub> concentration trend in China (μg/m<sup>3</sup>/year).</p>
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<p>Spatial distribution of land cover in China in 2015 and 2021.</p>
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<p>Land-cover change spatial distribution in China.</p>
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<p>The proportion of PM<sub>10</sub> concentrations at different levels across land-cover types.</p>
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<p>Nonlinear relationship between PM<sub>10</sub> concentrations and land-cover types in 2015. (<b>a</b>) Forest; (<b>b</b>) Glassland; (<b>c</b>) Wetland and Water; (<b>d</b>) Cropland; (<b>e</b>) Urban; (<b>f</b>) Barren land.</p>
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<p>Nonlinear relationship between PM<sub>10</sub> concentrations and land-cover types in 2021. (<b>a</b>) Forest; (<b>b</b>) Glassland; (<b>c</b>) Wetland and Water; (<b>d</b>) Cropland; (<b>e</b>) Urban; (<b>f</b>) Barren land.</p>
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