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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 564
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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16 pages, 4515 KiB  
Article
Modeling and Simulation of Reel Motion in a Foxtail Millet Combine Harvester
by Zhenwei Liang, Jia Liu, Deyong Yang and Kangcheng Ouyang
Agriculture 2025, 15(1), 19; https://doi.org/10.3390/agriculture15010019 - 25 Dec 2024
Viewed by 240
Abstract
Due to the high plant height, heavy ear, and easy forward tilt of millet during harvesting, the reel of a traditional combine harvester is often difficult to adapt to the special growth characteristics of millet, resulting in serious grain loss. Therefore, optimizing the [...] Read more.
Due to the high plant height, heavy ear, and easy forward tilt of millet during harvesting, the reel of a traditional combine harvester is often difficult to adapt to the special growth characteristics of millet, resulting in serious grain loss. Therefore, optimizing the design of the reel is important to improve the harvesting efficiency of millet and reduce the grain header loss. In order to determine the optimal reel speed ratio(λ), kinematics simulation experiments and analysis were carried out under different combinations of forward speed and reel revolution speed. The results showed that the supporting effect of the reel is insufficient when λ ≤ 1, and the trochoidal trajectory of the reel can provide a backward driving force when λ > 1, the optimum speed ratio of the reel should be controlled between 1.5 and 1.6. Field experiments results showed that the grain header loss rate was the lowest (0.9%) when λ = 1.6. This study provides key guidance for the adjustment of the combine harvester, effectively reducing the grain header loss rate in harvesting millet, and improving the harvesting efficiency. Full article
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<p>Structural diagram of eccentric reel. 1. Spring-tooth shaft. 2. Spring-finger. 3. Reel wheel shaft. 4. Eccentric strap. 5. Eccentric main spoke disc. 6. Main spoke disk.</p>
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<p>Schematic diagram of reel installation position in combine harvester. 1. Reel. 2. Cutter.</p>
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<p>Schematic diagram of reel installation position of millet combine harvester. 1. Reel. 2. Cutter.</p>
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<p>Reel 3D model with constraints added in RecurDyn software.</p>
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<p>Reel movement status with <math display="inline"><semantics> <mrow> <mi>λ</mi> <mtext> </mtext> </mrow> </semantics></math>&lt; 1. (<b>a</b>) Motion trajectory of the reel arm; (<b>b</b>) Horizontal displacement curve of the finger bar ends; (<b>c</b>) Horizontal velocity curve of the finger bar ends.</p>
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<p>Reel movement status with <math display="inline"><semantics> <mrow> <mi>λ</mi> </mrow> </semantics></math> = 1. (<b>a</b>) Motion trajectory of the reel arm; (<b>b</b>) Horizontal displacement curve of the finger bar ends; (<b>c</b>) Horizontal velocity curve of the finger bar ends.</p>
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<p>Reel movement status with <math display="inline"><semantics> <mrow> <mi>λ</mi> </mrow> </semantics></math> &gt; 1. (<b>a</b>) Motion trajectory of the reel arm; (<b>b</b>) Horizontal displacement curve of the finger bar ends; (<b>c</b>) Horizontal velocity curve of the finger bar ends.</p>
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<p>Reel revolution speed change curve with <math display="inline"><semantics> <mrow> <mi>λ</mi> </mrow> </semantics></math> = 1.2.</p>
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<p>Reel speed change curve with <math display="inline"><semantics> <mrow> <mi>λ</mi> </mrow> </semantics></math> = 1.8.</p>
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<p>Schematic diagram of reel when harvesting.</p>
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<p>Function curve of reel action degree with reel speed ratio.</p>
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<p>4LZ-6B Millet combine harvester. 1. Reel. 2. Hydraulic motor.</p>
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<p>Sample trough after harvesting. 1. Stems. 2. Sampling trough. 3. Grains header loss.</p>
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<p>Variation in millet loss rate under different reel speed ratios (<math display="inline"><semantics> <mrow> <mi>λ</mi> </mrow> </semantics></math>).</p>
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23 pages, 11421 KiB  
Article
Simulation and Assessment of Episodic Dust Storms in Eastern Saudi Arabia Using HYSPLIT Trajectory Model and Satellite Observations
by Abdulrahman Suhail Alzaid, Ismail Anil and Omer Aga
Atmosphere 2024, 15(12), 1515; https://doi.org/10.3390/atmos15121515 - 18 Dec 2024
Viewed by 460
Abstract
The “dust belt” region extending from the western Sahara to the Gobi Desert frequently generates severe dust storms that cause hazardous air quality and disrupt daily activities. Dust storm management systems with proactive mitigation strategies can minimize the detrimental impacts of dust storms. [...] Read more.
The “dust belt” region extending from the western Sahara to the Gobi Desert frequently generates severe dust storms that cause hazardous air quality and disrupt daily activities. Dust storm management systems with proactive mitigation strategies can minimize the detrimental impacts of dust storms. This study applies the HYSPLIT model to simulate dust storms in Saudi Arabia, specifically targeting the eastern region. The study’s main objective is to calibrate and validate the model’s dust storm prediction module for the eastern region of Saudi Arabia. The validated HYSPLIT model, with optimized parameters such as threshold friction velocity, particle release rate, and dry deposition velocity from model calibration studies, showed a strong linear correlation between measured and predicted values. It achieved an R2 of 0.9965, indicating excellent model accuracy. The main findings of the source apportionment approach, employing air particle backward trajectories and frequency analyses, indicated that the northern regions, specifically Iraq and Syria, were the primary sources of the severe dust storms observed in the receptor area. The outcomes of this study will be a reference for future research aimed at improving dust storm management systems and selecting sites for tree-planting campaigns under the “Saudi & Middle East Green Initiatives”. Full article
(This article belongs to the Section Atmospheric Techniques, Instruments, and Modeling)
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Figure 1
<p>The geographic location of the PM<sub>10</sub> monitoring station (the dashed line shows the zoom out of the study area).</p>
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<p>Daily average PM<sub>10</sub> mass concentrations measured in 2022.</p>
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<p>The 3-day wind rose plots of the first dust storm (<b>a</b>) and the second dust storm (<b>b</b>).</p>
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<p>Dust emission locations in the HYSPLIT model for the selected domain (Dots represent dust emission locations).</p>
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<p>(<b>a</b>) Three-day backward air particle trajectories (Star symbol represents receptor location), (<b>b</b>) frequency analysis of backward trajectories, surface dust concentration maps on 26 January (<b>c</b>), 27 January (<b>d</b>), and 28 January (<b>e</b>), and (<b>f</b>) satellite imagery on 28 January 2022.</p>
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<p>(<b>a</b>) Three-day backward air particle trajectories (Star symbol represents receptor location), (<b>b</b>) frequency analysis of backward trajectories, surface dust concentration maps on 26 January (<b>c</b>), 27 January (<b>d</b>), and 28 January (<b>e</b>), and (<b>f</b>) satellite imagery on 28 January 2022.</p>
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<p>(<b>a</b>) Three-day backward air particle trajectories (Star symbol represents receptor location), (<b>b</b>) frequency analysis of backward trajectories, surface dust concentration maps on 9 March (<b>c</b>), 10 March (<b>d</b>), and 11 March (<b>e</b>), and (<b>f</b>) satellite imagery on 11 March 2022.</p>
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<p>(<b>a</b>) Three-day backward air particle trajectories (Star symbol represents receptor location), (<b>b</b>) frequency analysis of backward trajectories, surface dust concentration maps on 9 March (<b>c</b>), 10 March (<b>d</b>), and 11 March (<b>e</b>), and (<b>f</b>) satellite imagery on 11 March 2022.</p>
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<p>Observed and predicted PM<sub>10</sub> concentrations between 27–31 January 2022.</p>
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<p>PM<sub>10</sub> concentration predictions from 25 January 2022 to 30 January 2022, averaged between 0 and 100 m AGL; release started at 00:00 25 January 2022.</p>
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<p>PM<sub>10</sub> concentration predictions from 25 January 2022 to 30 January 2022, averaged between 0 and 100 m AGL; release started at 00:00 25 January 2022.</p>
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<p>Observed and predicted PM<sub>10</sub> concentrations between 8–14 March 2022.</p>
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<p>PM<sub>10</sub> concentration predictions from 8 March 2022 to 13 March 2022 averaged between 0 and 100 m AGL; release started at 00:00 on 8 March 2022.</p>
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<p>PM<sub>10</sub> concentration predictions from 8 March 2022 to 13 March 2022 averaged between 0 and 100 m AGL; release started at 00:00 on 8 March 2022.</p>
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26 pages, 8006 KiB  
Article
Research on Downhole MTATBOT Positioning and Autonomous Driving Strategies Based on Odometer-Assisted Inertial Measurement
by Mingrui Hao, Xiaoming Yuan, Jie Ren, Yueqi Bi, Xiaodong Ji, Sihai Zhao, Miao Wu and Yang Shen
Sensors 2024, 24(24), 7935; https://doi.org/10.3390/s24247935 - 12 Dec 2024
Viewed by 437
Abstract
In response to the current situation of backward automation levels, heavy labor intensities, and high accident rates in the underground coal mine auxiliary transportation system, the mining trackless auxiliary transportation robot (MTATBOT) is presented in this paper. The MTATBOT is specially designed for [...] Read more.
In response to the current situation of backward automation levels, heavy labor intensities, and high accident rates in the underground coal mine auxiliary transportation system, the mining trackless auxiliary transportation robot (MTATBOT) is presented in this paper. The MTATBOT is specially designed for long-range, space-constrained, and explosion-proof underground coal mine environments. With an onboard perception and autopilot system, the MTATBOT can perform automated and unmanned subterranean material transportation. This paper proposes an integrated odometry-based method to improve position estimation and mitigate location ambiguities for simultaneous localization and mapping (SLAM) in large-scale, GNSS-denied, and perceptually degraded subterranean transport roadway scenarios. Additionally, this paper analyzes the robot dynamic model and presents a nonlinear control strategy for the robot to autonomously track a planned trajectory based on the path-following error dynamic model. Finally, the proposed algorithm and control strategy are tested and validated both in a virtual transport roadway environment and in an active underground coal mine. The test results indicate that the proposed algorithm can obtain more accurate and robust robot odometry and better large-scale underground roadway mapping results compared with other SLAM solutions. Full article
(This article belongs to the Section Sensors and Robotics)
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<p>Explosion-proof rubber-wheeled vehicles manufactured by China Coal Technology &amp; Engineering Group, Taiyuan Research Institute. (<b>a</b>) A traditional explosion-proof rubber-wheeled vehicle for material transport; (<b>b</b>) an autonomous driving prototype of an underground coal mine transport vehicle.</p>
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<p>The trackless auxiliary transportation robot system used for material distribution in underground coal mines.</p>
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<p>Structural configuration of the explosion-proof wheeled transport robot.</p>
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<p>Powertrain arrangement of the explosion-proof wheeled transport robot. ① Explosion-proof electric steering gear; ② Steering swing arm; ③ Steering tie rod; ④ Wheel-side enclosed wet brake; ⑤ Drive axle shaft; ⑥ Reducer and differential gear; ⑦ Explosion-proof permanent magnet motor.</p>
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<p>Multi-type material containers of the trackless auxiliary transportation robot system.</p>
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<p>Autopilot system configuration of the trackless auxiliary transportation robot system.</p>
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<p>Perceptually degraded environment of an auxiliary transport roadway in the China Energy Group Bulianta Coal Mine.</p>
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<p>The sensors’ arrangement in the environment perception system in explosion-proof electric boxes. (<b>a</b>) The main explosion-proof electric box; (<b>b</b>) the corner explosion-proof electric box.</p>
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<p>Detection range of the EWTBOT’s environment perception system. Top: Bird’s-eye view of the Lidar and millimeter-wave radar horizon on the EWTBOT. Bottom: Bird’s-eye view of RGB-D cameras and laser distance sensors’ horizon on the EWTBOT.</p>
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<p>Architectural overview of the EWTBOT’s localization strategy.</p>
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<p>Factor graph and range measurements of the EWTBOT.</p>
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<p>Multi-type motion forms of the explosion-proof wheeled transport robot. <span class="html-italic">G</span> is the robot CoG, positioned at <span class="html-italic">X<sub>h</sub></span> and <span class="html-italic">Y<sub>h</sub></span> in the global Cartesian coordinate system <span class="html-italic">XOY</span>. <span class="html-italic">xGy</span> is the robot body coordinate system with the robot’ longitudinal axis as the <span class="html-italic">x</span>-axis and its lateral direction as the <span class="html-italic">y</span>-axis. <span class="html-italic">L</span> is the robot’s axis distance. <span class="html-italic">D</span> is the robot’s wheel distance. <span class="html-italic">P</span> is the instantaneous center of steering of the robot. <math display="inline"><semantics> <mrow> <mi>ϕ</mi> </mrow> </semantics></math> is the yaw angle of the robot. <span class="html-italic">R<sub>min</sub></span> is the robot’s minimum turning radius. <span class="html-italic">R<sub>max</sub></span> is the robot’s maximum turning radius. (<b>a</b>) Front/Rear-wheel steering. (<b>b</b>) Four-wheel steering. (<b>c</b>) Crab-walking.</p>
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<p>Two-degrees-of-freedom model of the explosion-proof wheeled transport robot. <span class="html-italic">G</span> is the robot’s CoG; <span class="html-italic">P</span> is the instantaneous center of steering of the robot; <span class="html-italic">F<sub>yf</sub></span> and <span class="html-italic">F<sub>yr</sub></span> are the lateral tire forces of the front and rear axles; <span class="html-italic">F<sub>xf</sub></span> and <span class="html-italic">F<sub>xr</sub></span> are the components of force provided by the front and rear tires, respectively, in their direction of rolling; <span class="html-italic">V</span> is the robot’s velocity vector in the center of gravity, which has a longitudinal component <span class="html-italic">v<sub>x</sub></span> and a lateral component <span class="html-italic">v<sub>y</sub></span>, which identify the sideslip angle <span class="html-italic">β</span>; <span class="html-italic">V<sub>f</sub></span> is the front tire’s velocity vector; and <span class="html-italic">V<sub>r</sub></span> is the rear tire’s velocity vector. (<b>a</b>) Dynamic analysis of the 2-DOF model. (<b>b</b>) Velocity vectors’ geometrical relationship in the model.</p>
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<p>Two-degrees-of-freedom model of the explosion-proof wheeled transport robot. <span class="html-italic">G</span> is the robot’s CoG; <span class="html-italic">P</span> is the instantaneous center of steering of the robot; <span class="html-italic">F<sub>yf</sub></span> and <span class="html-italic">F<sub>yr</sub></span> are the lateral tire forces of the front and rear axles; <span class="html-italic">F<sub>xf</sub></span> and <span class="html-italic">F<sub>xr</sub></span> are the components of force provided by the front and rear tires, respectively, in their direction of rolling; <span class="html-italic">V</span> is the robot’s velocity vector in the center of gravity, which has a longitudinal component <span class="html-italic">v<sub>x</sub></span> and a lateral component <span class="html-italic">v<sub>y</sub></span>, which identify the sideslip angle <span class="html-italic">β</span>; <span class="html-italic">V<sub>f</sub></span> is the front tire’s velocity vector; and <span class="html-italic">V<sub>r</sub></span> is the rear tire’s velocity vector. (<b>a</b>) Dynamic analysis of the 2-DOF model. (<b>b</b>) Velocity vectors’ geometrical relationship in the model.</p>
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<p>Path-following error dynamics model of the explosion-proof wheeled transport robot. <math display="inline"><semantics> <mrow> <mover accent="true"> <mrow> <mi>v</mi> </mrow> <mo stretchy="false">→</mo> </mover> </mrow> </semantics></math> is the robot’s actual velocity vector; <span class="html-italic">G</span> is the robot’s CoG; <span class="html-italic">Q</span> is the orthogonal projection of <span class="html-italic">G</span> on the desired path; and <span class="html-italic">d</span> is the distance from <span class="html-italic">G</span> to <span class="html-italic">Q</span>.</p>
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<p>Motion control scheme framework of the MTATBOT.</p>
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<p>Simulation testing model of the MTATBOT. (<b>a</b>) Simulated underground roadway environment. A solid white line represents the traverse through the roadway, while arrows depict the direction of the traverse; yellow circles denote the action area of UWB beacons. (<b>b</b>) Simulated model of the MTATBOT.</p>
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<p>Simulation tests of the MTATBOT’s simultaneous localization and mapping solutions. (<b>a</b>) The results of Visual-based SLAM; (<b>b</b>) the results of Lidar-based SLAM; (<b>c</b>) the results of Lidar-inertial-based SLAM; and (<b>d</b>) the results of integrated-odometry-based SLAM.</p>
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<p>Comparison of MTATBOT trajectories based on different odometry information with the Ground Truth. (<b>a</b>) The comparative results on a three-dimensional scale; (<b>b</b>) the comparative results on a planar scale.</p>
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<p>Physical prototype of the MTATBOT.</p>
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<p>Mapping result of test underground roadways based on the MTATBOT. A total of 10 spherical targets were pre-arranged along the roadways, and UWB beacons were also deployed with each target to provide location information. The MTATBOT embarked on its journey from the starting point, traversed the length of the tunnel, and returned to its origin, successfully conducting environmental detection and mapping.</p>
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<p>The robot’s traversed trajectories obtained by the used methods during the field experiment. The spherical targets’ positions relative to the start point, which were measured by an electronic total station, are also labeled in the graph. Compared to the other algorithms with large start-to-end drifts, the proposed method can obtain a closed traversed path when the robot returned to the start point.</p>
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25 pages, 5900 KiB  
Article
Investigation of the Spatio-Temporal Distribution and Seasonal Origin of Atmospheric PM2.5 in Chenzhou City
by Xiaolong Chen, Hongfeng Zhang, Cora Un In Wong and Fanbo Li
Appl. Sci. 2024, 14(23), 11221; https://doi.org/10.3390/app142311221 - 2 Dec 2024
Viewed by 530
Abstract
The objective of this study was to elucidate the transmission pathways and spatial distribution of potential source areas for PM2.5 pollution in Chenzhou City across diverse seasons in southern Hunan. Utilizing Sampling Kriging interpolation analysis, we modeled the temporal and spatial oscillations [...] Read more.
The objective of this study was to elucidate the transmission pathways and spatial distribution of potential source areas for PM2.5 pollution in Chenzhou City across diverse seasons in southern Hunan. Utilizing Sampling Kriging interpolation analysis, we modeled the temporal and spatial oscillations of PM2.5 concentrations in Chenzhou City, complemented by HYSPLIT air mass backward trajectories. Furthermore, the model conducted cluster analysis to identify discernible patterns. Our findings unveiled marked seasonal variations in PM2.5 concentrations within Chenzhou City. The pinnacle is discerned during winter (75.13 μg·m−3), whereas the nadir is pronounced in summer (27.64 μg·m−3). Notably, the PM2.5/PM10 ratio surpasses 0.55 during both autumn and winter. Spatially, Chenzhou exhibits an annual average distribution of PM2.5 pollution characterized by a gradient “from north to south in the western and central sectors, tapering towards the east”. Pollution source analysis suggests that PM2.5 pollution in Chenzhou City is predominantly ascribed to local emissions. Transmission pathway analysis reveals that the primary transmission corridors, spanning northwest Guangdong, southwestern Henan, Hubei, southern Anhui, and specific zones of southwestern Jiangxi, consistently align with external PM2.5 pollution sources affecting Chenzhou City throughout the year. Noteworthy seasonal disparities emerge in the spatial distribution and contribution of potential source regions. During spring, autumn, and winter, the predominant contributing regions are primarily located in adjacent provinces. In contrast, during summer, regions with relatively elevated values predominantly streak across the central and western sectors of Jiangxi and the southeastern Hunan region. A comprehensive examination of the seasonal distribution patterns, potential transmission routes, and likely contributing sources of PM2.5 in Chenzhou City can offer invaluable insights for regional atmospheric environmental governance. Furthermore, it underscores the paramount importance of collaborative regional strategies directed towards the prevention and control of PM2.5 pollution. Full article
(This article belongs to the Special Issue Air Pollution and Its Impact on the Atmospheric Environment)
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<p>Distribution of ambient air quality monitoring stations (national control points) in the five sub-districts and national control cities of Chenzhou City (the illustration was crafted utilizing ArcGIS software, version 10.2. For further reference, the following URL link is provided: <a href="https://www.arcgis.com/index.html" target="_blank">https://www.arcgis.com/index.html</a> (accessed on 16 October 2023).</p>
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<p>The diurnal variations in concentrations of PM<sub>2.5</sub>, PM<sub>10</sub>, and the ratio of PM<sub>2.5</sub> to PM<sub>10</sub> in Chenzhou City spanning from March 2022 to February 2023. (Note: The dashed lines in (<b>a</b>,<b>b</b>) delineate the standard daily average secondary concentration thresholds, while the dashed lines in (<b>c</b>) serve as dividing markers at 0.45 and 0.55, respectively).</p>
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<p>Seasonal fluctuations in PM<sub>2.5</sub> and PM<sub>10</sub> concentrations in Chenzhou City (Note: In a box plot, (1) the colored balls represent outliers in the data set, (2) the triangles are used to represent the mean, because the mean is an important reference point in the box plot, indicating the average trend of the data set. (3) The black line is used to represent the distribution range of the data, especially to connect the upper and lower bounds of the box, i.e., the third quartile (Q3).).</p>
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<p>Spatial distribution patterns of annual mean PM<sub>2.5</sub> in Chenzhou City (note: the illustration was crafted utilizing ArcGIS software, specifically version 10.2. For further reference, the software can be accessed at the following URL: <a href="https://www.arcgis.com/index.html" target="_blank">https://www.arcgis.com/index.html</a> (accessed on 16 October 2023)).</p>
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<p>Spatial patterns of annual average concentrations of SO<sub>2</sub>, CO, NO<sub>2</sub>, and PM<sub>2.5</sub>/PM<sub>10</sub> in Chenzhou City ((<b>a</b>) Annual average concentration spatial distribution of SO<sub>2</sub> (<b>b</b>) Annual average concentration spatial distribution of CO (<b>c</b>) Annual average concentration spatial distribution of NO<sub>2</sub> (<b>d</b>) Annual average concentration spatial distribution of PM<sub>2.5</sub>/PM<sub>10</sub>) (note: the illustration was crafted utilizing ArcGIS software, specifically version 10.2. For further reference, the software can be accessed at the following URL: <a href="https://www.arcgis.com/index.html" target="_blank">https://www.arcgis.com/index.html</a> (accessed on 16 October 2023)).</p>
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<p>Seasonal variations in the spatial distribution of PM<sub>2.5</sub> in Chenzhou City ((<b>a</b>) PM<sub>2.5</sub> spatial distribution (spring) (<b>b</b>) PM<sub>2.5</sub> spatial distribution (Summer) (<b>c</b>) PM<sub>2.5</sub> spatial distribution (Autumn) (<b>d</b>) PM<sub>2.5</sub> spatial distribution (Winter)) (note: the illustration was crafted utilizing ArcGIS software, specifically version 10.2. For further reference, please visit the following URL: <a href="https://www.arcgis.com/index.html" target="_blank">https://www.arcgis.com/index.html</a> (accessed on 16 October 2023)).</p>
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<p>Seasonal variations in backward trajectory cluster analysis for Chenzhou City ((<b>a</b>) Backward Trajectory Cluster Analysis (Spring) (<b>b</b>) Backward Trajectory Cluster Analysis (Summer) (<b>c</b>) Backward Trajectory Cluster Analysis (Autumn) (<b>d</b>) Backward Trajectory Cluster Analysis (Winter)) (note: the illustration was crafted utilizing ArcGIS software, specifically version 10.2. For further reference, please visit the following URL: <a href="https://www.arcgis.com/index.html" target="_blank">https://www.arcgis.com/index.html</a> (accessed on 16 October 2023)).</p>
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<p>Seasonal distribution of potential PM<sub>2.5</sub> source areas in Chenzhou City ((<b>a</b>) Spring distribution (<b>b</b>) Summer distribution (<b>c</b>) Autumn distribution (<b>d</b>) Winter distribution) (note: the illustration was crafted utilizing ArcGIS software, specifically version 10.2. For further reference, please visit the following URL: <a href="https://www.arcgis.com/index.html" target="_blank">https://www.arcgis.com/index.html</a> (accessed on 16 October 2023)).</p>
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<p>Seasonal variations in PM<sub>2.5</sub> Concentration-Weighted Trajectories across Chenzhou City((<b>a</b>) Spring trajectory (<b>b</b>) Summer trajectory (<b>c</b>) Autumn trajectory (<b>d</b>) Winter trajectory) (note: the illustration was crafted utilizing ArcGIS software, specifically version 10.2. For further reference, please visit the following URL: <a href="https://www.arcgis.com/index.html" target="_blank">https://www.arcgis.com/index.html</a> (accessed on 16 October 2023)).</p>
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20 pages, 1529 KiB  
Article
Data-Driven Bus Trajectory Tracking Based on Feedforward–Feedback Model-Free Adaptive Iterative Learning Control
by Weijie Xiu, Yongqiang Xie, Ye Ren and Li Wang
Electronics 2024, 13(23), 4673; https://doi.org/10.3390/electronics13234673 - 26 Nov 2024
Viewed by 529
Abstract
This paper presents a scheme for the feedforward–feedback longitudinal trajectory tracking control of buses. The scheme is specifically designed to address the periodic and repetitive nature of bus operations. First, the vehicle’s longitudinal dynamics are linearized along the iterative axis via full-form dynamic [...] Read more.
This paper presents a scheme for the feedforward–feedback longitudinal trajectory tracking control of buses. The scheme is specifically designed to address the periodic and repetitive nature of bus operations. First, the vehicle’s longitudinal dynamics are linearized along the iterative axis via full-form dynamic linearization (FFDL), and parameters such as the pseudo-gradient are estimated with data and a projection algorithm to grasp the dynamic characteristics of the system. To better handle complex real-world traffic conditions, we then propose the forward and backward structure. At the same time, the iterative axis design performance index is verified, and the forward partial control law, namely, model-free adaptive iterative learning control (MFAILC), is derived. In order to further enhance the robustness to disturbance and other factors, the control law of the feedback part is designed with active disturbance rejection control (ADRC). A key advantage of this control approach is its sole reliance on the data generated during vehicle operation, without the need for specific information about the controlled vehicle. This feature enables the method to be adaptable to different vehicle types and resilient to various disturbances. Finally, MATLAB simulations are used to verify the practicality of the proposed method. Full article
(This article belongs to the Special Issue Development and Advances in Autonomous Driving Technology)
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<p>Longitudinal bus dynamics.</p>
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<p>Route map of Bus No. 961.</p>
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<p>The maximum tracking error without disturbances: (<b>a</b>) the maximum speed error; (<b>b</b>) the maximum displacement error.</p>
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<p>The maximum tracking error under different weight ratios.</p>
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<p>Input of the system without disturbances.</p>
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<p>Tracking results for FFDL-MFAFILC without disturbances: (<b>a</b>) the speed tracing; (<b>b</b>) the path tracing.</p>
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<p>Comparison of tacking results without disturbances: (<b>a</b>) the speed tracing; (<b>b</b>) the path tracing.</p>
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<p>Disturbances.</p>
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<p>The max tracking error with disturbances: (<b>a</b>) the maximum speed error; (<b>b</b>) the maximum displacement error.</p>
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<p>Input of the system with disturbances.</p>
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<p>Tracking results for FFDL-MFAFILC with disturbances: (<b>a</b>) the speed tracing; (<b>b</b>) the path tracing.</p>
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<p>Comparison of tacking results with disturbances: (<b>a</b>) the speed tracing; (<b>b</b>) the path tracing.</p>
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25 pages, 3646 KiB  
Article
Application of Compensation Algorithms to Control the Speed and Course of a Four-Wheeled Mobile Robot
by Gennady Shadrin, Alexander Krasavin, Gaukhar Nazenova, Assel Kussaiyn-Murat, Albina Kadyroldina, Tamás Haidegger and Darya Alontseva
Sensors 2024, 24(22), 7233; https://doi.org/10.3390/s24227233 - 12 Nov 2024
Viewed by 816
Abstract
This article presents a tuned control algorithm for the speed and course of a four-wheeled automobile-type robot as a single nonlinear object, developed by the analytical approach of compensation for the object’s dynamics and additive effects. The method is based on assessment of [...] Read more.
This article presents a tuned control algorithm for the speed and course of a four-wheeled automobile-type robot as a single nonlinear object, developed by the analytical approach of compensation for the object’s dynamics and additive effects. The method is based on assessment of external effects and as a result new, advanced feedback features may appear in the control system. This approach ensures automatic movement of the object with accuracy up to a given reference filter, which is important for stable and accurate control under various conditions. In the process of the synthesis control algorithm, an inverse mathematical model of the robot was built, and reference filters were developed for a closed-loop control system through external effect channels, providing the possibility of physical implementation of the control algorithm and compensation of external effects through feedback. This combined approach allows us to take into account various effects on the robot and ensure its stable control. The developed algorithm provides control of the robot both when moving forward and backward, which expands the capabilities of maneuvering and planning motion trajectories and is especially important for robots working in confined spaces or requiring precise movement into various directions. The efficiency of the algorithm is demonstrated using a computer simulation of a closed-loop control system under various external effects. It is planned to further develop a digital algorithm for implementation on an onboard microcontroller, in order to use the new algorithm in the overall motion control system of a four-wheeled mobile robot. Full article
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<p>Inverse system model based on feedforward control system.</p>
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<p>Inverse system model based on feedback control system.</p>
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<p>Inverse model of the control object as a signal converter.</p>
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<p>Series connection of the signal converter (“reference filter”) and the inverse model of the control object.</p>
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<p>The diagram of the robot’s location on a plane in fixed coordinates <math display="inline"><semantics> <mrow> <msub> <mrow> <mi mathvariant="normal">x</mi> </mrow> <mrow> <mi mathvariant="normal">N</mi> </mrow> </msub> </mrow> </semantics></math>, <math display="inline"><semantics> <mrow> <msub> <mrow> <mi mathvariant="normal">y</mi> </mrow> <mrow> <mi mathvariant="normal">N</mi> </mrow> </msub> </mrow> </semantics></math>. <math display="inline"><semantics> <mrow> <msub> <mrow> <mi mathvariant="normal">x</mi> </mrow> <mrow> <mn>01</mn> </mrow> </msub> </mrow> </semantics></math>—robot speed; <math display="inline"><semantics> <mrow> <msub> <mrow> <mi mathvariant="normal">x</mi> </mrow> <mrow> <mn>02</mn> </mrow> </msub> </mrow> </semantics></math>—front wheel steering angle; <math display="inline"><semantics> <mrow> <msub> <mrow> <mi mathvariant="normal">x</mi> </mrow> <mrow> <mn>03</mn> </mrow> </msub> </mrow> </semantics></math>—robot course.</p>
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<p>The connection of the curvature and the trajectory and the angular velocity of the mobile robot.</p>
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<p>A schematic diagram of the steering wheel angle and the radius of the circle tangent to the trajectory.</p>
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<p>A block diagram of the robot’s speed and course control system.</p>
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<p>Transient processes in the robot control system during single-step changes in speed and heading tasks and forward movement. The designations of the variables correspond to their designations in Equations (25) and (52).</p>
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<p>Transient processes in the robot control system during single-step changes in speed and heading tasks and backward movement.</p>
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<p>Transient processes in the robot control system during single-step changes in speed and heading tasks. The speed command changes 3 s after the heading command was changed.</p>
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<p>Transient processes in the robot control system with a single-step change in the speed task and 3 radians per course.</p>
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<p>The robot control signals presented (<b>top figure</b>) in the case when the movement of the robot was in fixed coordinates (<b>bottom figure</b>) and when the course assignment changed by ±180 degrees every 10 s.</p>
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<p>The robot maneuvers when moving back and forth.</p>
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<p>Transient processes in the robot control system when sequentially changing the coefficients <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>k</mi> </mrow> <mrow> <mn>1</mn> </mrow> </msub> </mrow> </semantics></math> … <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>k</mi> </mrow> <mrow> <mn>4</mn> </mrow> </msub> </mrow> </semantics></math> of the robot’s mathematical model by ±50% relative to their calculated values while tuning the regulator to the calculated values.</p>
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<p>Transient processes in the robot control system at a nominal speed of 1 m/s and a course of 1 radian after 5 s and under the influence of disturbances.</p>
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20 pages, 9296 KiB  
Article
Spatiotemporal Distribution, Meteorological Influence, and Potential Sources of Air Pollution over Hainan Island, China
by Yuying Yu, Huayuan Zhou, Zhizhong Zhao, Yunhua Chang, Dan Wu, Zhongqin Li, Feiteng Wang, Mengyang Fang and Xi Zhou
Atmosphere 2024, 15(11), 1336; https://doi.org/10.3390/atmos15111336 - 7 Nov 2024
Viewed by 564
Abstract
Data on particulate matter, gaseous pollutants, and AQI values from three cities (Haikou, Sanya, and Danzhou) between January 2018 and December 2022 were obtained in order to analyze the spatiotemporal distribution characteristics of air pollution, the correlation between pollutants with meteorological conditions, and [...] Read more.
Data on particulate matter, gaseous pollutants, and AQI values from three cities (Haikou, Sanya, and Danzhou) between January 2018 and December 2022 were obtained in order to analyze the spatiotemporal distribution characteristics of air pollution, the correlation between pollutants with meteorological conditions, and the potential sources in Hainan Island. The spatiotemporal distribution’s characteristics demonstrated that the annual mean concentrations of SO2, NO2, CO, O3, PM10 and PM2.5 were 4.34 ± 1.11 μg m−3, 9.87 ± 1.87 μg m−3, 0.51 ± 0.06 mg m−3, 73.04 ± 6.36 μg m−3, 27.31 ± 3.63 μg m−3, and 14.01 ± 2.02 μg m−3, respectively. The yearly mean concentrations were trending downward in the past few years and were below the National Ambient Air Quality Standard (NAAQS) Grade II. Summer was the season with the lowest concentrations of all pollutants (3.84 μg m−3, 7.34 μg m−3, 0.42 mg m−3, 52.80 μg m−3, 18.67 μg m−3 and 8.67 μg m−3 for SO2, NO2, CO, O3, PM10 and PM2.5, respectively), and afternoons were the time with the lowest concentrations of pollutants (except for 78.04 μg m−3 for O3). The influence of meteorological conditions on pollutants was examined: there was a prominent positive correlation between temperature and O3 in summer, and relative humidity largely influenced the concentrations of PM. The pollution in Hainan was affected more by regional transport; according to the backward trajectory results, Hainan is susceptible to air masses from Guangdong and Fujian to the northeast, the Indochina Peninsula to the southwest, and the South China Sea to the southeast. The results of PSCF and CWT analyses indicated that Guangdong, Jiangxi, Hunan, and Fujian were the primary potential sources of PM2.5 and O3. Full article
(This article belongs to the Section Air Quality)
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<p>This study’s geographical location. ArcGIS 10.2 was used to process the DEM data that were obtained from the Geospatial Data Cloud (<a href="http://www.gscloud.cn/" target="_blank">http://www.gscloud.cn/</a>, accessed on 19 September 2023).</p>
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<p>Annual variation in air pollution concentration from 2018 to 2022 in Hainan.</p>
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<p>Seasonal variation in air pollution concentration from 2018 to 2022 in Hainan.</p>
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<p>Diurnal variation in concentrations of air pollutants from 2018 to 2022.</p>
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<p>Relationship between air pollutants, wind direction, and wind speed.</p>
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<p>Impact of meteorological conditions (temperature, relative humidity) on air pollutants.</p>
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<p>Air quality index (AQI) and primary pollutants in Hainan.</p>
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<p>The air trajectory clusterings for Haikou (<b>a</b>), Sanya (<b>b</b>), and Danzhou (<b>c</b>) produced using the(Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT4) model.</p>
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<p>The air trajectory clusterings for Haikou (<b>a</b>), Sanya (<b>b</b>), and Danzhou (<b>c</b>) produced using the(Hybrid Single-Particle Lagrangian Integrated Trajectory (HYSPLIT4) model.</p>
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<p>Distribution of WPSCF for PM<sub>2.5</sub> (<b>a</b>–<b>c</b>) and O<sub>3</sub> (<b>d</b>–<b>f</b>) in Haikou, Sanya, and Danzhou.</p>
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<p>Distribution of WCWT for PM<sub>2.5</sub> (<b>a</b>–<b>c</b>) and O<sub>3</sub> (<b>d</b>–<b>f</b>) in Haikou, Sanya, and Danzhou.</p>
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<p>Distribution of WCWT for PM<sub>2.5</sub> (<b>a</b>–<b>c</b>) and O<sub>3</sub> (<b>d</b>–<b>f</b>) in Haikou, Sanya, and Danzhou.</p>
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18 pages, 5155 KiB  
Article
Ground-Based MAX-DOAS Observations for Spatiotemporal Distribution and Transport of Atmospheric Water Vapor in Beijing
by Hongmei Ren, Ang Li, Zhaokun Hu, Hairong Zhang, Jiangman Xu and Shuai Wang
Atmosphere 2024, 15(10), 1253; https://doi.org/10.3390/atmos15101253 - 20 Oct 2024
Viewed by 1111
Abstract
Understanding the spatiotemporal distribution and transport of atmospheric water vapor in urban areas is crucial for improving mesoscale models and weather and climate predictions. This study employs Multi-Axis Differential Optical Absorption Spectroscopy to monitor the dynamic distribution and transport flux of water vapor [...] Read more.
Understanding the spatiotemporal distribution and transport of atmospheric water vapor in urban areas is crucial for improving mesoscale models and weather and climate predictions. This study employs Multi-Axis Differential Optical Absorption Spectroscopy to monitor the dynamic distribution and transport flux of water vapor in Beijing within the tropospheric layer (0–4 km) from June 2021 to May 2022. The seasonal peaks in precipitable water occur in August, reaching 39.13 mm, with noticeable declines in winter. Water vapor was primarily distributed below 2.0 km and generally decreases with increasing altitude. The largest water vapor transport flux occurs in the southeast–northwest direction, whereas the smallest occurs in the southwest–northeast direction. The maximum flux, observed at about 1.2 km in the southeast–northwest direction during summer, reaches 31.77 g/m2/s (transported towards the southeast). Before continuous rainfall events, water vapor transport, originating primarily from the southeast, concentrates below 1 km. Backward trajectory analysis indicates that during the rainy months, there was a higher proportion of southeasterly winds, especially at lower altitudes, with air masses from the southeast at 500 m accounting for 69.11%. This study shows the capabilities of MAX-DOAS for remote sensing water vapor and offers data support for enhancing weather forecasting and understanding urban climatic dynamics. Full article
(This article belongs to the Section Atmospheric Techniques, Instruments, and Modeling)
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<p>The schematic diagram (<b>left</b>) and location (<b>right</b>) of the multi-axis differential optical absorption spectroscopy (MAX-DOAS) instrument.</p>
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<p>Examples of typical DOAS fits of O<sub>4</sub> and H<sub>2</sub>O at 10:55:15 a.m. local time (LT) on 14 May 2022.</p>
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<p>The illustration of the directions of the wind speeds calculated in this paper (<span class="html-italic">u</span> represents the zonal wind, <span class="html-italic">v</span> represents the meridional wind, <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>W</mi> </mrow> <mrow> <mi>S</mi> <mi>W</mi> <mo>−</mo> <mi>N</mi> <mi>E</mi> </mrow> </msub> </mrow> </semantics></math> represents the southwest–northeast wind, and <math display="inline"><semantics> <mrow> <msub> <mrow> <mi>W</mi> </mrow> <mrow> <mi>S</mi> <mi>E</mi> <mo>−</mo> <mi>N</mi> <mi>W</mi> </mrow> </msub> </mrow> </semantics></math> represents the southeast–northwest wind).</p>
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<p>Comparison of hourly average precipitable water measurements between MAX-DOAS and AERONET: (<b>a</b>) time series analysis; (<b>b</b>) correlation analysis.</p>
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<p>Comparison of Water Vapor Mixing Ratio Concentrations between MAX-DOAS and ERA5: (<b>a</b>) 200 m; (<b>b</b>) 400 m; (<b>c</b>) 600 m; (<b>d</b>) 800 m.</p>
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<p>Monthly average distribution of precipitable water.</p>
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<p>Seasonal distribution box plot of precipitable water. The central black line on each box indicates the median, the central black circle on each box indicates the mean, and the bottom (top) edge of each box indicates the 25th (75th) percentile. The vertical bars represent the range from the 5th to the 95th percentiles of the data.</p>
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<p>Diurnal variation of precipitable water.</p>
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<p>Vertical distribution of water vapor mixing ratio concentrations by month.</p>
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<p>Seasonal vertical distribution of water vapor transport flux in different directions: (<b>a</b>–<b>d</b>) east–west direction; (<b>e</b>–<b>h</b>) north–south direction; (<b>i</b>–<b>l</b>) southwest–northeast direction; (<b>m</b>–<b>p</b>) southeast–northwest direction.</p>
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<p>Seasonal and annual average distributions of vertically integrated water vapor transport flux in various directions: (<b>a</b>) seasonal average distribution; (<b>b</b>) annual average distribution.</p>
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<p>Wind speed and direction, along with H<sub>2</sub>O MR at different altitudes: (<b>a</b>) at 200 m; (<b>b</b>) at 600 m; (<b>c</b>) at 1000 m; (<b>d</b>) at 1400 m; (<b>e</b>) at 1800 m; (<b>f</b>) at 2200 m.</p>
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<p>Distribution of precipitable water in the Beijing area before rainfall.</p>
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<p>Vertical distribution of water vapor transport flux before rainfall: (<b>a</b>–<b>c</b>) East-West direction; (<b>d</b>–<b>f</b>) North-South direction; (<b>g</b>–<b>i</b>) Southwest-Northeast direction; (<b>j</b>–<b>l</b>) Southeast-Northwest direction.</p>
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<p>72 h backward trajectories of air masses at an altitude of 500 m from June 2021 to May 2022, across different months.</p>
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<p>72 h backward trajectories of air masses at an altitude of 1000 m from June 2021 to May 2022, across different months.</p>
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<p>72 h backward trajectories of air masses at an altitude of 1500 m from June 2021 to May 2022, across different months.</p>
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<p>Statistical results of the 72 h backward trajectories of air masses from the day before precipitation during the observation period at (<b>a</b>) 500 m, (<b>b</b>) 1000 m, and (<b>c</b>) 1500 m.</p>
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24 pages, 4047 KiB  
Article
Bidirectional Planning for Autonomous Driving Framework with Large Language Model
by Zhikun Ma, Qicong Sun and Takafumi Matsumaru
Sensors 2024, 24(20), 6723; https://doi.org/10.3390/s24206723 - 19 Oct 2024
Viewed by 1319
Abstract
Autonomous navigation systems often struggle in dynamic, complex environments due to challenges in safety, intent prediction, and strategic planning. Traditional methods are limited by rigid architectures and inadequate safety mechanisms, reducing adaptability to unpredictable scenarios. We propose SafeMod, a novel framework enhancing safety [...] Read more.
Autonomous navigation systems often struggle in dynamic, complex environments due to challenges in safety, intent prediction, and strategic planning. Traditional methods are limited by rigid architectures and inadequate safety mechanisms, reducing adaptability to unpredictable scenarios. We propose SafeMod, a novel framework enhancing safety in autonomous driving by improving decision-making and scenario management. SafeMod features a bidirectional planning structure with two components: forward planning and backward planning. Forward planning predicts surrounding agents’ behavior using text-based environment descriptions and reasoning via large language models, generating action predictions. These are embedded into a transformer-based planner that integrates text and image data to produce feasible driving trajectories. Backward planning refines these trajectories using policy and value functions learned through Actor–Critic-based reinforcement learning, selecting optimal actions based on probability distributions. Experiments on CARLA and nuScenes benchmarks demonstrate that SafeMod outperforms recent planning systems in both real-world and simulation testing, significantly improving safety and decision-making. This underscores SafeMod’s potential to effectively integrate safety considerations and decision-making in autonomous driving. Full article
(This article belongs to the Section Vehicular Sensing)
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<p>Overall framework of SafeMod. SafeMod takes multi-view image sequences as input, transforms them into BEV embedding and sense description, outputs them and samples one action to control the vehicle.</p>
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<p>Framework detail of BEV-planning module. The BEV-planning module processes bird’s-eye-view (BEV) features through multiple transformers to generate strategic vehicle control actions, incorporating BEV feature extraction, motion and map predictions, inter-query interactions, and final trajectory planning based on high-level driving commands.</p>
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<p>Overall framework of video sense module. The video sense module processes video inputs to extract structured sensory information and generate multi-turn dialogues for enhanced scene understanding, utilizing a pre-trained video encoder to obtain video embeddings, a cross-modality projector for alignment with language embeddings, and a perception module to continuously update the agent’s hidden states based on the extracted data, ultimately predicting context-specific actions for navigation.</p>
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<p>Intersection traffic negotiation. The module identifies the vehicles at the intersection, anticipates their behavior, and selects a safe right-turn maneuver while avoiding collisions. It analyzes the scooter and cars’ positions, predicting their paths and adjusting speed or direction to maintain safe distances. After passing the intersection, the framework continues monitoring for lane changes or sudden movements, ensuring smooth traffic flow and preventing conflicts.</p>
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<p>Lane changing. The module identifies the vehicle ahead while driving on a multi-lane road, anticipates its stationary behavior, and selects a safe lane change maneuver to the left. It analyzes the traffic light at the intersection and the presence of vehicles, predicting possible stops and adjusting speed accordingly to maintain safe movement.</p>
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<p>Example of action output.</p>
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<p>Policy generation in backward planning using Q-function optimization.</p>
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<p>The aerial views of Town5 within the CARLA simulator. To evaluate the vehicle’s performance comprehensively, we used Town5 by focusing on several critical areas. First, it assesses the vehicle’s ability to manage right-of-way and prevent accidents at complex intersections involving multiple vehicles (traffic negotiation). Second, it evaluates the vehicle’s capacity to detect and circumvent suddenly appearing obstacles, such as road obstructions (obstacle avoidance). Third, it tests the vehicle’s responses to emergency stopping situations and its ability to execute swift lane changes to evade potential hazards (braking and lane changing).</p>
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<p>Backward performance test. The evaluation results indicate that the backward planning module consistently outperforms the baseline method across all metrics, especially in the 1 s interval of each metric. These improvements demonstrate the module’s capability to handle complex driving scenarios more safely and deliver more accurate autonomous driving.</p>
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21 pages, 7736 KiB  
Article
Carbonyl Compounds Observed at a Suburban Site during an Unusual Wintertime Ozone Pollution Event in Guangzhou
by Aoqi Ge, Zhenfeng Wu, Shaoxuan Xiao, Xiaoqing Huang, Wei Song, Zhou Zhang, Yanli Zhang and Xinming Wang
Atmosphere 2024, 15(10), 1235; https://doi.org/10.3390/atmos15101235 - 16 Oct 2024
Viewed by 736
Abstract
Carbonyl compounds are important oxygenated volatile organic compounds (VOCs) that play significant roles in the formation of ozone (O3) and atmospheric chemistry. This study presents comprehensive field observations of carbonyl compounds during an unusual wintertime ozone pollution event at a suburban [...] Read more.
Carbonyl compounds are important oxygenated volatile organic compounds (VOCs) that play significant roles in the formation of ozone (O3) and atmospheric chemistry. This study presents comprehensive field observations of carbonyl compounds during an unusual wintertime ozone pollution event at a suburban site in Guangzhou, South China, from 19 to 28 December 2020. The aim was to investigate the characteristics and sources of carbonyls, as well as their contributions to O3 formation. Formaldehyde, acetone, and acetaldehyde were the most abundant carbonyls detected, with average concentrations of 7.11 ± 1.80, 5.21 ± 1.13, and 3.00 ± 0.94 ppbv, respectively, on pollution days, significantly higher than those of 2.57 ± 1.12, 2.73 ± 0.88, and 1.10 ± 0.48 ppbv, respectively, on nonpollution days. The Frame for 0-D Atmospheric Modeling (F0AM) box model simulations revealed that local production accounted for 62–88% of observed O3 concentrations during the pollution days. The calculated ozone formation potentials (OFPs) for various precursors (carbonyls and VOCs) indicated that carbonyl compounds contributed 32.87% of the total OFPs on nonpollution days and 36.71% on pollution days, respectively. Formaldehyde, acetaldehyde, and methylglyoxal were identified as the most reactive carbonyls, and formaldehyde ranked top in OFPs, and it alone contributed 15.92% of total OFPs on nonpollution days and 18.10% of total OFPs on pollution days, respectively. The calculation of relative incremental reactivity (RIR) indicates that ozone sensitivity was a VOC-limited regime, and carbonyls showed greater RIRs than other groups of VOCs. The model simulation showed that secondary formation has a significant impact on formaldehyde production, which is primarily controlled by alkenes and biogenic VOCs. The characteristic ratios and backward trajectory analysis also indicated the indispensable impacts of local primary sources (like industrial emissions and vehicle emissions) and regional sources (like biomass burning) through transportation. This study highlights the important roles of carbonyls, particularly formaldehyde, in forming ozone pollution in megacities like the Pearl River Delta region. Full article
(This article belongs to the Section Air Quality)
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<p>Location of the observation site (green star).</p>
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<p>Time series of meteorological parameters and major pollutants during the sampling period, with shaded areas indicating the pollution days.</p>
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<p>Diurnal variations of major carbonyls during pollution days and nonpollution days.</p>
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<p>The contributions of different VOC groups to ozone formation potential (OFP) during the nonpollution and pollution days.</p>
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<p>Carbonyls and NMHC compounds with the top 10 OFP values during nonpollution and pollution days.</p>
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<p>Model simulation of O<sub>3</sub> formation.</p>
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<p>Calculated RIRs for ozone formation from precursors (carbonyls, NMHCs, and NOx).</p>
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<p>Observed and simulated concentrations of formaldehyde during the sampling period.</p>
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<p>Model-simulated production rate (P (HCHO)) and loss rate (L (HCHO)) of formaldehyde through different reaction pathways during nonpollution days (<b>a</b>) and pollution days (<b>b</b>).</p>
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<p>The calculated RIRs of the five major HC groups for the formation of formaldehyde.</p>
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<p>Model-calculated RIRs of the individual top 10 NMHC species for the formation of formaldehyde during pollution days.</p>
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<p>Correlation analysis of formaldehyde to acetaldehyde (<b>a</b>), acetaldehyde to propanal (<b>b</b>), toluene to benzene (<b>c</b>), and m,p-xylene to ethylbenzene (<b>d</b>) during nonpollution days and pollution days.</p>
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<p>Mean 48 h back trajectories of clusters at the Huadu site (black star) during nonpollution days (<b>a</b>) and pollution days (<b>b</b>).</p>
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<p>Backward trajectory and fire hotspot map within 48 h during the sampling period from 19 to 28 December 2020 (24 trajectories per day) at the Huadu site (black star).</p>
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20 pages, 12135 KiB  
Article
Southern South American Long-Distance Pollen Dispersal and Its Relationship with Atmospheric Circulation
by Claudio F. Pérez, Ana G. Ulke and María I. Gassmann
Aerobiology 2024, 2(4), 85-104; https://doi.org/10.3390/aerobiology2040007 - 12 Oct 2024
Viewed by 845
Abstract
This paper addresses the study of synoptic-scale meteorological conditions that favor long-range pollen transport in southern South America combining airborne pollen counts, modeled three-dimensional backward trajectories, and synoptic and surface meteorological data. Alnus pollen transport trajectories indicate origins predominantly in montane forests of [...] Read more.
This paper addresses the study of synoptic-scale meteorological conditions that favor long-range pollen transport in southern South America combining airborne pollen counts, modeled three-dimensional backward trajectories, and synoptic and surface meteorological data. Alnus pollen transport trajectories indicate origins predominantly in montane forests of the Yungas between 1500 and 2800 m altitude. The South American Low-Level Jet is the main meteorological feature that explains 64% of the detected pollen arrival at the target site. Podocarpus and Nothofagus pollen instead are linked primarily to the widespread Subantartic forests in southern Patagonia. Their transport patterns are consistent with previous studies, which show an association with synoptic patterns related to cold front passages carrying pollen in the free atmosphere (27% for Nothofagus and 25% for Podocarpus). These results show the significance of understanding long-distance pollen transport for disciplines such as climate change reconstruction and agriculture, emphasizing the need for further research to refine atmospheric circulation models and refine interpretations of past vegetation and climate dynamics. Full article
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Graphical abstract

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<p>(<b>a</b>) Even-hour <span class="html-italic">Alnus</span> trajectories arriving at 1500 m a.s.l. from 14 UTC of 31 August–12 UTC of 1 September 2013 and (<b>b</b>) 14 UTC of 1 September–12 UTC of 2nd September 2013. The Yungas Forest is shaded in green.</p>
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<p>Mean geopotential height at 1000 hPa (black solid lines) and 500/1000 hPa thickness fields (gray dashed lines) for the <span class="html-italic">Alnus</span> case study (31 August–1 September 2013). The shaded area shows the highest heights of the Andes (above 1500 m a.s.l.).</p>
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<p>Images of 850 hPa winds (vectors, m s<sup>−1</sup>) and areas satisfying the modified Bonner’s criteria for (<b>a</b>) 06 UTC 31 August and (<b>b</b>) 06 UTC 1 September showing the position of the cold front. Shading indicates wind speeds at 850 hPa greater than 12, 16, and 20 m s<sup>−1</sup>. White contours indicate a 700/850 hPa wind difference greater than 6, 8, and 10 m s<sup>−1</sup>. Dashed line masks altitudes above 1500 m.</p>
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<p>Images of the 800–750 hPa layer mean flow for 06 UTC 31 August (<b>a</b>) and 06 UTC 1 September showing the position of the cold front (<b>b</b>). The dashed line marks the 1500 m altitude, while the shaded area masks altitudes higher than 3250 m. The color scale shows the horizontal wind intensity (m s<sup>−1</sup>).</p>
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<p>Vertical cross sections (30.97° S) showing the horizontal wind (vectors, m s<sup>−1</sup>) and omega (lines, Pa s<sup>−1</sup>) by the end of the SALLJ event. The star shows the position of Sunchales. Panels show the situation every 6 h from 30 August to 1 September 2013. The shaded area shows the Andes and Córdoba ranges. The star indicates the position of Sunchales.</p>
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<p>Vertical cross sections (19° S) showing the horizontal wind (vectors, m s<sup>−1</sup>) and omega (lines, Pa s<sup>−1</sup>) at the latitude where the SALLJ passes over the Yungas. Panels show the situation every 6 h from 29 August to 31 August 2013 when the event started. The shaded area shows the Andes and Brazilian ranges.</p>
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<p>Even-hour <span class="html-italic">Nothofagus</span> (<b>a</b>) and <span class="html-italic">Podocarpus</span> (<b>b</b>) trajectories arriving at 750 m a.s.l. on 14 UTC of 24 November–12 UTC of 25 November 2012, and 14 UTC 24 October–12 UTC 25 October 2013, respectively. Light-colored lines show trajectories not passing over the pollen source area (see text). Straight lines represent the construction cuts of the Hovmöller diagrams in <a href="#aerobiology-02-00007-f008" class="html-fig">Figure 8</a> and <a href="#aerobiology-02-00007-f009" class="html-fig">Figure 9</a>. The shaded area shows the geographic distribution of the Subantarctic forests.</p>
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<p>Hovmöller diagram for <span class="html-italic">Nothofagus</span> case study from 15 November to 1 December 2012. The space cut corresponds to the straight line in <a href="#aerobiology-02-00007-f007" class="html-fig">Figure 7</a>a. Lines show the 700 hPa geopotential height (gpm) and the shaded areas show 700 hPa omega (Pa s<sup>−1</sup>). The lower panel shows the associated topography and the vertical line represents the geographical location of Sunchales.</p>
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<p>Hovmöller diagram for <span class="html-italic">Podocarpus</span> case study from 15 October to 1 November 2013. The space cut corresponds to the straight line in <a href="#aerobiology-02-00007-f007" class="html-fig">Figure 7</a>b. Lines show the 700 hPa geopotential height (gpm), and shaded areas show 700 hPa omega (Pa s<sup>−1</sup>). The lower panel shows the associated topography and the vertical line represents the geographical location of Sunchales.</p>
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<p>Cartoons describing the transient synoptic patterns (see <a href="#aerobiology-02-00007-t001" class="html-table">Table 1</a>, <a href="#aerobiology-02-00007-t002" class="html-table">Table 2</a> and <a href="#aerobiology-02-00007-t003" class="html-table">Table 3</a>) recognized for <span class="html-italic">Alnus</span>, <span class="html-italic">Nothofagus</span>, and <span class="html-italic">Podocarpus</span> pollen arrival at Sunchales. The red star shows the city’s location. (<b>a</b>) leading-edge trough, (<b>b</b>) trough–eastern high, (<b>c</b>) low–eastern high, (<b>d</b>) weak high, (<b>e</b>) eastern high, (<b>f</b>) weak low, (<b>g</b>) ridge, (<b>h</b>) trough, (<b>i</b>) post-frontal, (<b>j</b>) low, (<b>k</b>) high.</p>
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19 pages, 11711 KiB  
Article
Long-Term Halocarbon Observations in an Urban Area of the YRD Region, China: Characteristic, Sources Apportionment and Health Risk Assessment
by Yuchun Jiang, Anqi Zhang, Qiaoli Zou, Lu Zhang, Hanfei Zuo, Jinmei Ding, Zhanshan Wang, Zhigang Li, Lingling Jin, Da Xu, Xin Sun, Wenlong Zhao, Bingye Xu and Xiaoqian Li
Toxics 2024, 12(10), 738; https://doi.org/10.3390/toxics12100738 - 12 Oct 2024
Viewed by 718
Abstract
To observe the long-term variations in halocarbons in the Yangtze River Delta (YRD) region, this study analyzes halocarbon concentrations and composition characteristics in Shanxi from 2018 to 2020, exploring their origins and the health effects. The total concentration of halocarbons has shown an [...] Read more.
To observe the long-term variations in halocarbons in the Yangtze River Delta (YRD) region, this study analyzes halocarbon concentrations and composition characteristics in Shanxi from 2018 to 2020, exploring their origins and the health effects. The total concentration of halocarbons has shown an overall increasing trend, which is driven by both regulated substances (CFC-11 and CFC-113) and unregulated substances, such as dichloromethane, chloromethane and chloroform. The results of the study also reveal that dichloromethane (1.194 ± 1.003 to 1.424 ± 1.004 ppbv) and chloromethane (0.205 ± 0.185 to 0.666 ± 0.323 ppbv) are the predominant halocarbons in Shanxi, influenced by local and northwestern emissions. Next, this study identifies that neighboring cities in Zhejiang Province and other YRD areas are potentially affected by backward trajectory models. Notably, chloroform and 1,2-dichloroethane have consistently surpassed acceptable thresholds, indicating a significant carcinogenic risk associated with solvent usage. This research sheds light on the evolution of halocarbons in the YRD region, offering valuable data for the control and reduction in halocarbon emissions. Full article
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<p>Geographic location of the Shanxi site.</p>
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<p>Wind rose diagrams illustrating the distribution of wind direction and frequency for the period 2018-2022 at the Shanxi site.</p>
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<p>Time series of halocarbons at the Shanxi monitoring site from 2018 to 2022, showing (<b>a</b>) concentration levels and (<b>b</b>) chemical species composition.</p>
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<p>Seasonal variation in halocarbons at the Shanxi site.</p>
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<p>Diurnal variation of major halocarbon species and total halocarbons.</p>
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<p>Main potential source regions of halocarbons. (<b>a</b>) represents the total halocarbons, and (<b>b</b>) focuses on a specific substance, as indicated in the lower right corner.</p>
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<p>Possible sources of tracer halocarbons for air pollution transport during 2018–2019 at the Shanxi site.</p>
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<p>Interannual variation in non-carcinogenic risk of atmospheric halocarbons in Shanxi. The dashed line indicates the threshold value.</p>
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<p>Interannual variation in carcinogenic risk of atmospheric halocarbons in Shanxi. The dashed lines indicate the acceptable risk level (1 × 10<sup>−6</sup>) and the tolerable risk level (1 × 10<sup>−4</sup>).</p>
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19 pages, 7895 KiB  
Article
A Novel Trajectory Prediction Method Based on CNN, BiLSTM, and Multi-Head Attention Mechanism
by Yue Xu, Quan Pan, Zengfu Wang and Baoquan Hu
Aerospace 2024, 11(10), 822; https://doi.org/10.3390/aerospace11100822 - 8 Oct 2024
Viewed by 2173
Abstract
A four-dimensional (4D) trajectory is a multi-dimensional time series that embodies rich spatiotemporal features. However, its high complexity and inherent uncertainty pose significant challenges for accurate prediction. In this paper, we present a novel 4D trajectory prediction model that integrates convolutional neural networks [...] Read more.
A four-dimensional (4D) trajectory is a multi-dimensional time series that embodies rich spatiotemporal features. However, its high complexity and inherent uncertainty pose significant challenges for accurate prediction. In this paper, we present a novel 4D trajectory prediction model that integrates convolutional neural networks (CNNs), bidirectional long short-term memory networks (BiLSTMs), and multi-head attention mechanisms. This model effectively addresses the characteristics of aircraft flight trajectories and the difficulties associated with simultaneously extracting spatiotemporal features using existing prediction methods. Specifically, we leverage the local feature extraction capabilities of CNNs to extract key spatial and temporal features from the original trajectory data, such as geometric shape information and dynamic change patterns. The BiLSTM network is employed to consider both forward and backward temporal orders in the trajectory data, allowing for a more comprehensive capture of long-term dependencies. Furthermore, we introduce a multi-head attention mechanism that enhances the model’s ability to accurately identify key information in the trajectory data while minimizing the interference of redundant information. We validated our approach through experiments conducted on a real ADS-B trajectory dataset. The experimental results demonstrate that the proposed method significantly outperforms comparative approaches in terms of trajectory estimation accuracy. Full article
(This article belongs to the Section Aeronautics)
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<p>CNN structure.</p>
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<p>LSTM structure.</p>
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<p>BiLSTM structure.</p>
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<p>Structure of the proposed model.</p>
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<p>Self-attention mechanism.</p>
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<p>Multi-head attention mechanism.</p>
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<p>Batch size and test set percentage settings.</p>
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<p>Flowchart of network training.</p>
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<p>Five signals over time. (<b>a</b>) Height. (<b>b</b>) Speed. (<b>c</b>) Angle. (<b>d</b>) Longitude. (<b>e</b>) Latitude.</p>
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<p>Comparison of predicted and true trajectories of different methods. (<b>a</b>) Height. (<b>b</b>) Speed. (<b>c</b>) Angle. (<b>d</b>) Longitude. (<b>e</b>) Latitude.</p>
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<p>Performance of different methods under four metrics. (<b>a</b>) MSE. (<b>b</b>) RMSE. (<b>c</b>) MAE. (<b>d</b>) R<sup>2</sup>.</p>
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<p>Results of ablation experiments. (<b>a</b>) MSE. (<b>b</b>) RMSE. (<b>c</b>) MAE. (<b>d</b>) R<sup>2</sup>.</p>
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12 pages, 10071 KiB  
Article
A Self-Propelled Linear Piezoelectric Micro-Actuator Inspired by the Movement Patterns of Aquatic Beetles
by Xinjie Wang and Gen Wang
Micromachines 2024, 15(10), 1197; https://doi.org/10.3390/mi15101197 - 27 Sep 2024
Viewed by 798
Abstract
The locomotion mechanisms and structural characteristics of insects in nature offer new perspectives and solutions for designing miniature actuators. Inspired by the underwater movement of aquatic beetles, this paper presents a bidirectional self-propelled linear piezoelectric micro-actuator (SLPMA), whose maximum size in three dimensions [...] Read more.
The locomotion mechanisms and structural characteristics of insects in nature offer new perspectives and solutions for designing miniature actuators. Inspired by the underwater movement of aquatic beetles, this paper presents a bidirectional self-propelled linear piezoelectric micro-actuator (SLPMA), whose maximum size in three dimensions is currently recognized as the smallest known of the self-propelled piezoelectric linear micro-actuators. Through the superposition of two bending vibration modes, the proposed actuator generates an elliptical motion trajectory at its driving feet. The size was determined as 15 mm × 12.8 mm × 5 mm after finite element analysis (FEA) through modal and transient simulations. A mathematical model was established to analyze and validate the feasibility of the proposed design. Finally, a prototype was fabricated, and an experimental platform was constructed to test the driving characteristics of the SLPMA. The experimental results showed that the maximum no-load velocity and maximum carrying load of the prototype in the forward motion were 17.3 mm/s and 14.8 mN, respectively, while those in the backward motion were 20.5 mm/s and 15.9 mN, respectively. Full article
(This article belongs to the Collection Piezoelectric Transducers: Materials, Devices and Applications)
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<p>Biomimetic principles and motion mechanism. (<b>a</b>) Motion mechanism of aquatic beetle underwater; (<b>b</b>) fundamental principle of vibrator motion.</p>
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<p>Self-propelled piezoelectric linear micro-actuator. (<b>a</b>) Voltage actuation for the PZT elements; (<b>b</b>) detailed dimensions of the micro-actuator; (<b>c</b>) micro-actuator prototype.</p>
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<p>The motion process of the micro-actuator within one cycle.</p>
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<p>Mode deformation and frequency.</p>
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<p>Simulation data results: (<b>a</b>) X-Y displacement trajectory simulation curves. (<b>b</b>) Displacement-time curve of point-B.</p>
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<p>Impedance-phase curve.</p>
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<p>Modal amplitude testing experimental setup.</p>
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<p>The displacements of driving feet versus frequency.</p>
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<p>Driving characteristic testing setup. (<b>a</b>) Velocity testing; (<b>b</b>) output force testing.</p>
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<p>The velocities of the piezoelectric actuator with the different preloads.</p>
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<p>Forward motion characteristics at different voltages. (<b>a</b>) Relationship between frequency and speed; (<b>b</b>) relationship between frequency and output force.</p>
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<p>Backward motion characteristics at different voltages. (<b>a</b>) Relationship between frequency and speed; (<b>b</b>) relationship between frequency and output force.</p>
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