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24 pages, 16942 KiB  
Article
Optimal Drought Index Selection for Soil Moisture Monitoring at Multiple Depths in China’s Agricultural Regions
by Peiwen Yao, Hong Fan and Qilong Wu
Agriculture 2025, 15(4), 423; https://doi.org/10.3390/agriculture15040423 - 17 Feb 2025
Viewed by 159
Abstract
Droughts are a major driver of global environmental degradation, threatening lives and causing significant economic losses, with approximately 80% of these losses linked to agricultural drought, characterized by soil moisture deficits. Remote sensing technology offers high spatiotemporal resolution data for continuous monitoring of [...] Read more.
Droughts are a major driver of global environmental degradation, threatening lives and causing significant economic losses, with approximately 80% of these losses linked to agricultural drought, characterized by soil moisture deficits. Remote sensing technology offers high spatiotemporal resolution data for continuous monitoring of soil moisture and drought severity. However, the effectiveness of remote sensing drought indices across different soil depths remains unclear. This study assessed the performance of eight widely used drought indices—Perpendicular Drought Index (PDI), Modified Perpendicular Drought Index (MPDI), Temperature Condition Index (TCI), Vegetation Condition Index (VCI), Vegetation Health Index (VHI), Normalized Vegetation Supply Water Index (NVSWI), Temperature–Vegetation Dryness Index (TVDI), and Standardized Precipitation–Evapotranspiration Index (SPEI) at multiple timescales—in monitoring soil moisture at five depths (0–50 cm, at 10 cm intervals) across nine agricultural regions of China from 2001 to 2020. Results reveal that the monitoring performance of drought indices varies significantly across regions and soil depths, with a general decline in performance as soil depth increases. For soil depths between 10–40 cm, VCI and NVSWI exhibited the highest accuracy, while PDI, MPDI, and VHI performed optimally in the Northeast China Plain. At 50 cm depth, however, optical remote sensing indices struggled to accurately capture soil moisture conditions. Additionally, TCI and TVDI showed notable lag effects, with 4-month and 5-month delays, respectively, while SPEI exhibited cumulative effects over 3–6 months. These findings provide critical insights to guide the selection of appropriate drought indices for soil moisture monitoring, aiding agricultural drought management and decision-making. Full article
(This article belongs to the Section Agricultural Soils)
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<p>China’s croplands in 2001–2020 and division of nine agricultural regions.</p>
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<p>(<b>a</b>–<b>t</b>) Spatial performance of different drought indices on capturing soil moisture at a soil depth of 10 cm.</p>
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<p>(<b>a</b>–<b>t</b>) Spatial performance of different drought indices on capturing soil moisture at a soil depth of 20 cm.</p>
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<p>(<b>a</b>–<b>t</b>) Spatial performance of different drought indices on capturing soil moisture at a soil depth of 30 cm.</p>
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<p>(<b>a</b>–<b>t</b>) Spatial performance of different drought indices on capturing soil moisture at a soil depth of 40 cm.</p>
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<p>(<b>a</b>–<b>t</b>) Spatial performance of different drought indices on capturing soil moisture at a soil depth of 50 cm.</p>
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<p>Boxplots for overall performance of different drought indices on capturing soil moisture at soil depths of 10–50 cm.</p>
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<p>Boxplots of overall performance of different drought indices in capturing 10 cm soil moisture at different lag phases.</p>
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<p>Boxplots of overall performance of SPEI-1, -3, -6, -9, and -12 in capturing soil moisture at soil depths of 10–50 cm.</p>
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16 pages, 6008 KiB  
Article
Spatial and Temporal Variations of Vegetation Water Content Using VOD and VPD in China During 2000–2016
by Yibing Sun, Zhaodan Cao, Chengqiu Wu and Xiaoer Zhao
Water 2025, 17(4), 568; https://doi.org/10.3390/w17040568 - 15 Feb 2025
Viewed by 446
Abstract
Vegetation water content, characterized by vapor pressure deficit (VPD) and vegetation optical depth (VOD), can represent vegetation health in terrestrial ecosystems. In this study, using remote sensing Ku-band VOD and VPD, the spatiotemporal distribution assessment, Mann-Kendall trend analysis, seasonal trend decomposition, and correlation [...] Read more.
Vegetation water content, characterized by vapor pressure deficit (VPD) and vegetation optical depth (VOD), can represent vegetation health in terrestrial ecosystems. In this study, using remote sensing Ku-band VOD and VPD, the spatiotemporal distribution assessment, Mann-Kendall trend analysis, seasonal trend decomposition, and correlation analysis and significance testing were conducted to investigate the spatiotemporal distribution patterns, seasonal variations and correlations of VPD and VOD across China from 2000 to 2016. And the correlation between climate factors (temperature and precipitation) with VOD and VPD was discussed. The results show the following: (1) The annual mean VPD in China predominantly ranged from 0 to 4 KPa, while the annual mean VOD were centered around 0 to 2 during 2000–2016. Spatially, the VOD peaked at 1–2 in southwest China. VPD have significant seasonal variations across China, with high VPD in the summer. (2) The VPD and VOD in most regions of China fluctuated and showed an upward trend from 2000 to 2016, with significantly increased VPD in northwest and southwest China. (3) On a monthly scale, regions where VOD positively correlated with VPD accounted for 89.69% of the total area of China. The proportion of areas with a significant positive correlation was 82.96%. The proportion of areas with a negative correlation was 10.31%, and the proportion of areas with a significant negative correlation was 5.41%. Annual VOD and VPD exhibited a positive correlation of 61.28% of China’s total territory. Among these, the area exhibiting a significant positive correlation made up 6.15%. The area demonstrating a negative correlation amounted to 38.72%, and the area with a significant negative correlation constituted 2.22%. This study can contribute to understanding vegetation water content dynamics across China, which is crucial for ecosystem sustainability in China. Full article
(This article belongs to the Section Ecohydrology)
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<p>Spatial distribution of annual VOD across China from 2000 to 2016.</p>
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<p>Spatial distribution of annual VPD across China from 2000 to 2016.</p>
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<p>M–K trend of VOD and VPD slope during 2000–2016 across China.</p>
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<p>Spatial distribution of seasonal VOD variations across China from 2000 to 2016.</p>
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<p>Time-series decomposition of VOD in China from 2000 to 2016.</p>
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<p>Spatial distribution of seasonal VPD variations across China from 2000 to 2016.</p>
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<p>Time–series decomposition of VPD data in China from 2000 to 2016.</p>
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<p>Correlation and significance test of monthly VPD and VOD data.</p>
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<p>Correlation and significance test of yearly VPD and VOD data.</p>
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<p>Correlation and significance tests with VPD and VOD lag time of 1 month.</p>
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<p>Annual precipitation and temperature across China from 2000 to 2016.</p>
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<p>Change trends of (<b>A</b>) precipitation and (<b>B</b>) temperature across China in 2000–2016.</p>
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<p>Correlation between the (<b>a</b>) temperature with the VOD; (<b>b</b>) precipitation with the VOD; (<b>c</b>) temperature with the VPD; (<b>d</b>) temperature with the VPD.</p>
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29 pages, 12829 KiB  
Article
Evaluating the Relationship Between Vegetation Status and Soil Moisture in Semi-Arid Woodlands, Central Australia, Using Daily Thermal, Vegetation Index, and Reflectance Data
by Mauro Holzman, Ankur Srivastava, Raúl Rivas and Alfredo Huete
Remote Sens. 2025, 17(4), 635; https://doi.org/10.3390/rs17040635 - 13 Feb 2025
Viewed by 423
Abstract
Wet rainfall pulses control vegetation growth through evapotranspiration in most dryland areas. This topic has not been extensively analyzed with respect to the vast semi-arid ecosystems of Central Australia. In this study, we investigated vegetation water responses to in situ root zone soil [...] Read more.
Wet rainfall pulses control vegetation growth through evapotranspiration in most dryland areas. This topic has not been extensively analyzed with respect to the vast semi-arid ecosystems of Central Australia. In this study, we investigated vegetation water responses to in situ root zone soil moisture (SM) variations in savanna woodlands (Mulga) in Central Australia using satellite-based optical and thermal data. Specifically, we used the Land Surface Water Index (LSWI) derived from the Advanced Himawari Imager on board the Himawari 8 (AHI) satellite, alongside Land Surface Temperature (LST) from MODIS Terra and Aqua (MOD/MYD11A1), as indicators of vegetation water status and surface energy balance, respectively. The analysis covered the period from 2016 to 2021. The LSWI increased with the magnitude of wet pulses and showed significant lags in the temporal response to SM, with behavior similar to that of the Enhanced Vegetation Index (EVI). By contrast, LST temporal responses were quicker and correlated with daily in situ SM at different depths. These results were consistent with in situ relationships between LST and SM, with the decreases in LST being coherent with wet pulse magnitude. Daily LSWI and EVI scores were best related to subsurface SM through quadratic relationships that accounted for the lag in vegetation response. Tower flux measures of gross primary production (GPP) were also related to the magnitude of wet pulses, being more correlated with the LSWI and EVI than LST. The results indicated that the vegetation response varied with SM depths. We propose a conceptual model for the relationship between LST and SM in the soil profile, which is useful for the monitoring/forecasting of wet pulse impacts on vegetation. Understanding the temporal changes in rainfall-driven vegetation in the thermal/optical spectra associated with increases in SM can allow us to predict the spatial impact of wet pulses on vegetation dynamics in extensive drylands. Full article
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Figure 1
<p>Map of major vegetation groups showing the location of Alice Springs Mulga (ASM) and Ti Tree Ozflux sites (data source: Dynamic Land Cover Dataset Version 2.1).</p>
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<p>Workflow diagram of satellite data (AHI and MODIS) and field data. Both data sources were considered to obtain LST and spectral indices and analyze vegetation response to SM during rainfall wet pulses.</p>
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<p>Study periods, data from the ASM OzFlux station. (<b>a</b>) Daily SM at different depths and GPP; (<b>b</b>) rainfall; (<b>c</b>) in situ SM, EVI, and LSWI values from the AHI; (<b>d</b>) maximum GPP and LSWI values in function of magnitude of wet pulses expressed as m<sup>3</sup>/m<sup>3</sup>. Vertical lines show the 5 analyzed wet pulses during late spring and summer: 2016–2017 and 2020–2021, the wettest seasons, and 2018–2019, the driest season.</p>
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<p>Study periods, data from the ASM OzFlux station. (<b>a</b>) Daily SM at different depths and GPP; (<b>b</b>) rainfall; (<b>c</b>) in situ SM, EVI, and LSWI values from the AHI; (<b>d</b>) maximum GPP and LSWI values in function of magnitude of wet pulses expressed as m<sup>3</sup>/m<sup>3</sup>. Vertical lines show the 5 analyzed wet pulses during late spring and summer: 2016–2017 and 2020–2021, the wettest seasons, and 2018–2019, the driest season.</p>
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<p>Detailed temporal series of the EVI and LSW from the AHI and SM in ASM for each analyzed season: (<b>a</b>) 2017–2018 (normal), (<b>b</b>) 2018–2019 (moderately dry), (<b>c</b>) 2019–2020 (normal), (<b>d</b>) 2020–2021 (extremely wet). Lags between peaks in SM and spectral indices are included.</p>
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<p>MYD/MOD11A1, in situ daily LST and actual evapotranspiration during the study period in ASM. In situ LST was calculated from upwelling longwave radiances measured by the pyrgeometer CNR1.</p>
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<p>Detailed temporal series of MODIS LST, daily in situ LST and SM in ASM during the 5 analyzed seasons: (<b>a</b>) 2016–2017 (extremely wet), (<b>b</b>) 2017–2018 (normal), (<b>c</b>) 2018–2019 (moderately dry), (<b>d</b>) 2019–2020 (normal), and (<b>e</b>) 2020–2021 (extremely wet).</p>
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<p>Relationship between daily in situ SM at different depths, LSWI (<b>left</b>) and EVI (<b>right</b>) from AHI in ASM (<span class="html-italic">n</span> = 356).</p>
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<p>Relationship between average in situ LST and SM at different depths (the best correlation up to 4 days is included) in ASM (<span class="html-italic">n</span> = 475). Although correlation at 100 cm depth is included, most of the time LST fluctuates according to shallower SM.</p>
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<p>Relationship between daily in situ SM at different depths, MOD11A1 (<span class="html-italic">n</span> = 287) and MYD11A1 (n = 274).</p>
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<p>Relationship between daily in situ GPP (gC/m<sup>2</sup>), LSWI (<b>left</b>), and EVI (<b>right</b>) values from the AHI in ASM (n = 145). Note that 2018–2019 was not included, as there was no evident growing season.</p>
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<p>Relationship between daily in situ GPP (gC/m<sup>2</sup>), MOD LST (<b>left</b>), and MYD LST (<b>right</b>) in ASM (n = 232).</p>
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<p>Conceptual model of satellite-derived LST from MODIS (<b>left</b>) and daily in situ GPP (<b>right</b>) as a function of daily SM for the Mulga woodland area. For the GPP plot, the maximum GPP values and average of the maximum values of SM in the soil profile for each analyzed pulse were considered. GPP versus maximum LSWI from the AHI is included. Note that on the left plot, SM values correspond to ASM data (a similar pattern was observed in Ti Tree).</p>
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<p>Study periods: data from the Ti Tree OzFlux station. (<b>a</b>) Daily SM at different depths and GPP; (<b>b</b>) rainfall; (<b>c</b>) in situ SM, EVI, and LSWI values from the AHI; (<b>d</b>) maximum GPP and LSWI values in function of magnitude of wet pulses expressed as m<sup>3</sup>/m<sup>3</sup>. Vertical lines show the analyzed wet pulses during late spring and summer. SM at a 60 cm depth was considered under spinifex, given the lack of data under Mulga.</p>
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<p>MYD/MOD11A1, in situ daily LST and actual evapotranspiration during the study period in the Ti Tree station. In situ LST was calculated from upwelling longwave radiances measured by the pyrgeometer CNR1.</p>
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<p>Relationship between daily in situ SM at different depths: the LSWI (<b>left</b>) and EVI (<b>right</b>) from the AHI in the Ti Tree station (n = 236).</p>
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<p>Relationship between average in situ LST and SM at different depths (the best correlation up to 4 days is included) in the Ti Tree station (n = 377).</p>
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<p>Relationship between daily in situ SM at different depths: MOD11A1 (<b>left</b>, n = 251) and MYD11A1 (<b>right</b>, n = 239) in the Ti Tree station.</p>
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<p>Relationship between daily in situ GPP (gC/m<sup>2</sup>), LSWI (<b>left</b>), and EVI (<b>right</b>) values from the AHI in the Ti Tree station (n = 51). Note that 2018–2019 was not included, as there was no evident growing season.</p>
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<p>Relationship between daily in situ GPP (gC/m<sup>2</sup>), MOD LST (<b>left</b>, n = 177), and MYD LST (<b>right</b>, n = 169) in the Ti Tree station.</p>
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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 953
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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<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 911
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 794
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 658
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 727
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 1166
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 1108
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 1256
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 2116
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 1134
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 3 | Viewed by 2506
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
Cited by 1 | Viewed by 1015
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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