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14 pages, 4382 KiB  
Article
Investigations on Stubble-Burning Aerosols over a Rural Location Using Ground-Based, Model, and Spaceborne Data
by Katta Vijayakumar, Panuganti China Sattilingam Devara and Saurabh Yadav
Atmosphere 2024, 15(11), 1383; https://doi.org/10.3390/atmos15111383 (registering DOI) - 17 Nov 2024
Abstract
Agriculture crop residue burning has become a major environmental problem facing the Indo-Gangetic plain, as well as contributing to global warming. This paper reports the results of a comprehensive study, examining the variations in aerosol optical, microphysical, and radiative properties that occur during [...] Read more.
Agriculture crop residue burning has become a major environmental problem facing the Indo-Gangetic plain, as well as contributing to global warming. This paper reports the results of a comprehensive study, examining the variations in aerosol optical, microphysical, and radiative properties that occur during biomass-burning events at Amity University Haryana (AUH), at a rural station in Gurugram (Latitude: 28.31° N, Longitude: 76.90° E, 285 m AMSL), employing ground-based observations of AERONET and Aethalometer, as well as satellite and model simulations during 7–16 November 2021. The smoke emissions during the burning events enhanced the aerosol optical depth (AOD) and increased the Angstrom exponent (AE), suggesting the dominance of fine-mode aerosols. A smoke event that affected the study region on 11 November 2021 is simulated using the regional NAAPS model to assess the role of smoke in regional aerosol loading that caused an atmospheric forcing of 230.4 W/m2. The higher values of BC (black carbon) and BB (biomass burning), and lower values of AAE (absorption Angstrom exponent) are also observed during the peak intensity of the smoke-event period. A notable layer of smoke has been observed, extending from the surface up to an altitude of approximately 3 km. In addition, the observations gathered from CALIPSO regarding the vertical profiles of aerosols show a qualitative agreement with the values obtained from AERONET observations. Further, the smoke plumes that arose due to transport of a wide-spread agricultural crop residue burning are observed nationwide, as shown by MODIS imagery, and HYSPLIT back trajectories. Thus, the present study highlights that the smoke aerosol emissions during crop residue burning occasions play a critical role in the local/regional aerosol microphysical and radiation properties, and hence in the climate variability. Full article
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<p>The MODIS-Aqua satellite true color image of fires over Punjab state on 11 November 2021. Here, the red color indicates fire detection using VIIRS satellite and the blue-colored star mark indicates the observational site Gurgaon (Amity University).</p>
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<p>Day-to-day variation in AOD at different wavelengths (nm).</p>
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<p>Day-to-day variation in the AERONET (<b>a</b>) fine-mode and coarse-mode AOD at 500 nm; (<b>b</b>) Ångström exponent a in the spectral band 440–870 nm; and (<b>c</b>) fine-mode fraction at 500 nm over the experimental site. The vertical bars show one standard deviation from the mean area-averaged value.</p>
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<p>Time evolution of aerosol volume size distribution for different aerosol radius (in um) over observation site from 7 to 16 November 2021.</p>
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<p>Day-to-day variation in SSA at all wavelengths. The vertical bars show one standard deviation from the mean area-averaged value.</p>
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<p>Day-to-day variation in Aerosol Radiative Forcing (ARF).</p>
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<p>Daily mean variation in (<b>a</b>) BC mass concentration and absorption Ångström exponent (AAE); and (<b>b</b>) biomass burning (BB%) during smoke event period.</p>
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<p>The concentration of smoke at the surface on 11 November 2021 during 00:00, 06:00, 12:00, and 18:00 h UTC.</p>
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<p>(<b>a</b>) CALIPSO retrieved the aerosol classification (sub-type profile), and (<b>b</b>) vertical feature mask on 11 November 2021 over the studied region.</p>
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<p>(<b>a</b>) Active true color image on 11 November 2021. (<b>b</b>) NOAA HYSPLIT hourly backward trajectories ending at Amity University Haryana (AUH), India on 11 November 2021.</p>
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11 pages, 1981 KiB  
Article
Image Dehazing Technique Based on DenseNet and the Denoising Self-Encoder
by Kunxiang Liu, Yue Yang, Yan Tian and Haixia Mao
Processes 2024, 12(11), 2568; https://doi.org/10.3390/pr12112568 (registering DOI) - 16 Nov 2024
Viewed by 382
Abstract
The application value of low-quality photos taken in foggy conditions is significantly lower than that of clear images. As a result, restoring the original image information and enhancing the quality of damaged images on cloudy days are crucial. Commonly used deep learning techniques [...] Read more.
The application value of low-quality photos taken in foggy conditions is significantly lower than that of clear images. As a result, restoring the original image information and enhancing the quality of damaged images on cloudy days are crucial. Commonly used deep learning techniques like DehazeNet, AOD-Net, and Li have shown encouraging progress in the study of image dehazing applications. However, these methods suffer from a shallow network structure leading to limited network estimation capability, reliance on atmospheric scattering models to generate the final results that are prone to error accumulation, as well as unstable training and slow convergence. Aiming at these problems, this paper proposes an improved end-to-end convolutional neural network method based on the denoising self-encoder-DenseNet (DAE-DenseNet), where the denoising self-encoder is used as the main body of the network structure, the encoder extracts the features of haze images, the decoder performs the feature reconstruction to recover the image, and the boosting module further performs the feature fusion locally and globally, and finally outputs the dehazed image. Testing the defogging effect in the public dataset, the PSNR index of DAE-DenseNet is 22.60, which is much higher than other methods. Experiments have proved that the dehazing method designed in this paper is better than other algorithms to a certain extent, and there is no color oversaturation or an excessive dehazing phenomenon in the image after dehazing. The dehazing results are the closest to the real image and the viewing experience feels natural and comfortable, with the image dehazing effect being very competitive. Full article
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<p>Self-encoder network structure.</p>
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<p>(<b>a</b>) Structure of ResNet, (<b>b</b>) structure of Dense Block, (<b>c</b>) multiple Dense Blocks connected to form DenseNet.</p>
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<p>(<b>a</b>) DAE-DenseNet based image dehazing network, (<b>b</b>) encoder structure unit, (<b>c</b>) decoder structure unit.</p>
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<p>RESIDE training set images. (<b>a</b>) Clear image, (<b>b</b>) <span class="html-italic">A</span> = 0.85, β = 0.2, (<b>c</b>) <span class="html-italic">A</span> = 1.0, β = 0.2, (<b>d</b>) <span class="html-italic">A</span> = 0.8, β = 0.16.</p>
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<p>Example of experimental results of different dehazing methods. (<b>a</b>–<b>c</b>) shows images of three different scenarios.</p>
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16 pages, 7250 KiB  
Article
Spatial-Temporal Assessment of Dust Events and Trend Analysis of Sand Drift Potential in Northeastern Iran, Gonabad
by Mohammad Reza Rahdari, Rasoul Kharazmi, Jesús Rodrigo-Comino and Andrés Rodríguez-Seijo
Land 2024, 13(11), 1906; https://doi.org/10.3390/land13111906 - 14 Nov 2024
Viewed by 373
Abstract
In recent years, northeastern Iran, particularly Khorasan Razavi province, has experienced wind erosion and dust storms, although large-scale studies are limited. To assess wind patterns, sand drift, and dust events, hourly wind data were analyzed using Fryberger’s method, along with trend analysis through [...] Read more.
In recent years, northeastern Iran, particularly Khorasan Razavi province, has experienced wind erosion and dust storms, although large-scale studies are limited. To assess wind patterns, sand drift, and dust events, hourly wind data were analyzed using Fryberger’s method, along with trend analysis through the Mann–Kendall and Sen’s slope tests. Additionally, MODIS satellite data and Google Earth Engine helped identify event frequency and spatial patterns. The results show that east (12%) and southeast winds (9.6%) are the most frequent, with an average annual wind speed of 4.39 knots. Sand drift potential (DP = 96, RDP = 21.6) indicates sand movement from southeast to northwest, with a multi-directional wind system (unidirectional index of 0.22). The results of the AOD index show that the amount of dust in the north and northwest part is more than other locations, and more than 500 events with dust has been registered over the last two decades. These findings suggest that policymakers should monitor these trends to mitigate the environmental and infrastructural damage caused by blowing sand. Full article
(This article belongs to the Special Issue The Impact of Extreme Weather on Land Degradation and Conservation)
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<p>Location of study area (<b>a</b>), territories affected by wind erosion processes (<b>b</b>−<b>d</b>, [<a href="#B47-land-13-01906" class="html-bibr">47</a>]) and 3D map (<b>e</b>).</p>
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<p>Annual and seasonal frequency of wind rose data (<b>a</b>) and wind storms (<b>b</b>).</p>
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<p>Annual sand drift potential. Red arrow represents RDP and RDD.</p>
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<p>Monitoring of sand drift potential (<b>a</b>), resultant drift potential (<b>b</b>), and unit directional index (<b>c</b>).</p>
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<p>Assessment of dust events on the annual scale during the last two decades.</p>
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<p>Spatial-temporal assessment of dusty days on monthly scale during the last two decades.</p>
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<p>Changes in the trend of sand drift potential (horizontal axis) on the monthly scale.</p>
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14 pages, 7249 KiB  
Article
Characterization of the Elemental Composition of Aerosols Emitted in the Dry Season of the Pantanal Wetland, Brazil
by Lucas Cardoso Ramos, Thais Costa Brunelli, Flávio César Vicentin, Leone Francisco Amorim Curado, André Matheus de Souza Lima, Fernando Gonçalves Morais, Rafael da Silva Palácios, Nicolas Neves de Oliveira and João Basso Marques
Atmosphere 2024, 15(11), 1361; https://doi.org/10.3390/atmos15111361 - 13 Nov 2024
Viewed by 341
Abstract
The Brazilian Pantanal region experiences intense biomass burning during the dry season, releasing large quantities of gasses and particles into the atmosphere, which have serious implications on both the climate system and public health. Understanding the dynamics of these emissions is crucial for [...] Read more.
The Brazilian Pantanal region experiences intense biomass burning during the dry season, releasing large quantities of gasses and particles into the atmosphere, which have serious implications on both the climate system and public health. Understanding the dynamics of these emissions is crucial for mitigating the impact on the ecosystem, its functioning, and potential anthropogenic disturbances. This study focused on analyzing emissions in the northern Pantanal during the 2022 drought. Concentrations of fine particulate matter (PM2.5), black carbon (BC), and 25 chemical elements were measured using gravimetry, reflectance analysis, and X-Ray fluorescence, respectively, from samples collected between August and October 2022. The average concentrations of PM2.5 and BC increased approximately 4-fold and 2.5-fold, respectively, compared to averages from a decade ago. Significant increases were also observed in elements such as sulfur (S), potassium (K), iron (Fe), and silicon (Si). The maximum concentrations were comparable to values typical of the southern Amazon, a region known for high deforestation rates and land use changes. Elemental analysis revealed substantial shifts in concentrations, primarily associated with biomass burning (BB) and soil suspension. Additionally, enrichment factor (Ef) analysis showed that lead (Pb) levels, correlated with human activities, were 200 times higher than those found under clean atmospheric conditions. Full article
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<p>(<b>a</b>) Sampling site BAPP, Private Natural Heritage Reserve of SESC Pantanal–Baía das Pedras, state of Mato Grosso, north of Brazilian Pantanal, (<b>b</b>) Representation of the sampling system of atmospheric aerosol.</p>
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<p>Concentration variation of PM<sub>2.5</sub>, BC, and Dust concentration (μg m<sup>‒3</sup>) measured in the BAPP, between August and October 2022.</p>
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<p>(<b>A</b>) Variation of Aerosol Optical Depth (AOD) 500 nm, Accumulated Rain (AR), and (<b>B</b>) meteorological conditions for the analysis period, where FRP, RH, Rn, and Ta stand for Fire Radiative Power, Relative Humidity, Net Radiation, and Air Temperature, respectively.</p>
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<p>Geographical distribution of fires by period in the municipalities of Mato Grosso in the Pantanal biome between August and October 2022.</p>
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<p>Roses of wind indicating the mean velocity and direction of the wind throughout the period between August and October 2022 measured at the micrometeorological tower in the BAPP.</p>
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<p>Variation in the mean concentration of major chemical elements during the study period.</p>
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<p>Enrichment factors (Ef) for the PM<sub>2.5</sub> fraction. Enrichment factors close to 1 indicate a natural source while enrichment factors &gt; 1 indicate an anthropogenic source.</p>
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20 pages, 9093 KiB  
Article
The Role of Subsurface Changes and Environmental Factors in Shaping Urban Heat Islands in Southern Xinjiang
by Cong Wen, Hajigul Sayit, Ali Mamtimin, Yu Wang, Jian Peng, Ailiyaer Aihaiti, Meiqi Song, Jiacheng Gao, Junjian Liu, Yisilamu Wulayin, Fan Yang, Wen Huo and Chenglong Zhou
Remote Sens. 2024, 16(21), 4089; https://doi.org/10.3390/rs16214089 - 1 Nov 2024
Viewed by 371
Abstract
The urban heat island (UHI) effect is one of the most prominent surface climate changes driven by human activities. This study examines the UHI characteristics and influencing factors in the Southern Xinjiang urban agglomeration using MODIS satellite data combined with observational datasets. Our [...] Read more.
The urban heat island (UHI) effect is one of the most prominent surface climate changes driven by human activities. This study examines the UHI characteristics and influencing factors in the Southern Xinjiang urban agglomeration using MODIS satellite data combined with observational datasets. Our results reveal a significant increase in impervious surfaces in the region between 1995 and 2015, with the most rapid expansion occurring from 2010 to 2015. This urban expansion is the primary driver of changes in UHI intensity. The analysis from 2000 to 2015 shows substantial spatial variation in UHI effects across cities. Hotan recorded the highest annual average daytime UHI intensity of 3.7 °C, while Aksu exhibited the lowest at approximately 1.6 °C. Daytime UHI intensity generally increased during the study period, with the highest intensities observed in the summer. However, nighttime UHI trends varied across cities, with most showing an increase in intensity. Temperature, precipitation, and aerosol optical depth (AOD) were identified as the main factors influencing annual average daytime UHI intensity, while PM10 concentration showed a weak and inconsistent correlation with UHI intensity, varying by city and season. Full article
(This article belongs to the Section Atmospheric Remote Sensing)
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<p>Map of urban agglomeration distribution in South Xinjiang (the number under the city name represents the population in that city in 2015).</p>
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<p>Trends in impervious surface changes in the South Xinjiang urban agglomeration, 1995–2015.</p>
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<p>Spatial changes in impervious surface in the Southern Xinjiang urban agglomeration, 1995–2015.</p>
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<p>Characteristics of daytime land surface temperature changes in urban agglomerations in South Xinjiang.</p>
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<p>Characteristics of nighttime land surface temperature changes in urban agglomerations in South Xinjiang.</p>
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<p>Spatial distribution of urban heat island intensity in urban agglomerations in South Xinjiang during daytime.</p>
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<p>Spatial distribution of urban heat island intensity in urban agglomerations in South Xinjiang during nighttime.</p>
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<p>Annual variation in urban heat island intensity in the South Xinjiang urban agglomeration, 2000–2015 ((<b>a</b>). Aksu, (<b>b</b>). Atushi, (<b>c</b>). Hotan, (<b>d</b>). Kashgar, (<b>e</b>). Korla).</p>
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<p>Seasonal variation in urban heat island intensity in the South Xinjiang urban agglomeration, 2000–2015 ((<b>a</b>). Spring, (<b>b</b>). Summer, (<b>c</b>). Autumn, (<b>d</b>). Winter).</p>
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16 pages, 12424 KiB  
Article
Studying the Constitutive Model of Damage for a Stainless Steel Argon–Oxygen Decarburization Slag Mixture
by Liuyun Huang, Zhuxin Lan, Guogao Wei, Yuliang Chen and Tun Li
Appl. Sci. 2024, 14(21), 10006; https://doi.org/10.3390/app142110006 - 1 Nov 2024
Viewed by 520
Abstract
The purpose of this study was to fully explore the mechanical properties of five different doses of an Argon–Oxygen Decarburization slag mixture in an unconfined compressive strength test. The peak stress, elastic modulus, and stress–strain curve of the mixture were studied for 90 [...] Read more.
The purpose of this study was to fully explore the mechanical properties of five different doses of an Argon–Oxygen Decarburization slag mixture in an unconfined compressive strength test. The peak stress, elastic modulus, and stress–strain curve of the mixture were studied for 90 days. Based on the experimental data and according to the theory of damage mechanics, the concept of damage threshold (t) was introduced to construct a damage constitutive model. Referring to the damage threshold of concrete, that of the mixture was determined to be 0.7 times higher than the peak strain, and the correlation coefficient between the established model and the test curve was above 0.85. These results indicate that the addition of AOD slag and fly ash can cause hydration reactions, increase the quantity of hydration products, and enhance the peak stress and elastic modulus of the mixture. The maximum increases were 94.9% and 43.1%, respectively. Parameters a and b reflect the peak stress and brittleness of the mixture, respectively. The incorporation of Argon–Oxygen Decarburization slag can make the mixture less brittle and improve its properties. The incorporation of Argon–Oxygen Decarburization slag can protect the mixture from damage. The maximum decrease is 40.2%. Full article
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<p>XRD pattern of AOD.</p>
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<p>Grain size frequency and cumulative grain size distribution curves. (<b>a</b>) AOD. (<b>b</b>) Fly ash.</p>
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<p>The shapes of the specimens during the compression process. (<b>a</b>) Initial loading stage. (<b>b</b>) Crack germination stage. (<b>c</b>) Crack propagation stage. (<b>d</b>) After destruction.</p>
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<p>Stress–strain curve of AOD slag.</p>
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<p>Relationship between peak stress and dosage.</p>
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<p>Relationship between elastic modulus and dosage.</p>
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<p>XRD patterns of hydration products in mixtures at 90 days.</p>
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<p>SEM micro-morphology of AOD slag with different dosages. (<b>a</b>,<b>b</b>) A-0; (<b>c</b>,<b>d</b>) A-3; and (<b>e</b>,<b>f</b>) A-12.</p>
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<p>SEM micro-morphology of AOD slag with different dosages. (<b>a</b>,<b>b</b>) A-0; (<b>c</b>,<b>d</b>) A-3; and (<b>e</b>,<b>f</b>) A-12.</p>
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<p>Comparison of test and model curves under different damage thresholds. (<b>a</b>) A-0; (<b>b</b>) A-3; (<b>c</b>) A-6; (<b>d</b>) A-9; and (<b>e</b>) A-12.</p>
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<p>Effect of parameters on damage constitutive model curves. (<b>a</b>) <span class="html-italic">a</span>; (<b>b</b>) <span class="html-italic">b</span>.</p>
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<p>Relationship between parameters and substitution rate. (<b>a</b>) <span class="html-italic">a</span>; (<b>b</b>) <span class="html-italic">b</span>.</p>
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<p>Test and model curves. (<b>a</b>) A-0; (<b>b</b>) A-3; (<b>c</b>) A-6; (<b>d</b>) A-9; and (<b>e</b>) A-12.</p>
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<p>Mixture damage variables. (<b>a</b>) Mixture damage variable curve; (<b>b</b>) damage growth rate.</p>
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26 pages, 20396 KiB  
Article
Spatiotemporal Variations and Driving Factor Analysis of Aerosol Optical Depth in Terrestrial Ecosystems in Northern Xinjiang from 2001 to 2023
by Zequn Xiang, Hongqi Wu, Yanmin Fan, Yu Dang, Yanan Bi, Jiahao Zhao, Wenyue Song, Tianyuan Feng and Xu Zhang
Atmosphere 2024, 15(11), 1302; https://doi.org/10.3390/atmos15111302 - 29 Oct 2024
Viewed by 434
Abstract
Investigating the spatiotemporal variations in Aerosol Optical Depth (AOD) in terrestrial ecosystems and their driving factors is significant for deepening our understanding of the relationship between ecosystem types and aerosols. This study utilized 1 km resolution AOD data from the Moderate Resolution Imaging [...] Read more.
Investigating the spatiotemporal variations in Aerosol Optical Depth (AOD) in terrestrial ecosystems and their driving factors is significant for deepening our understanding of the relationship between ecosystem types and aerosols. This study utilized 1 km resolution AOD data from the Moderate Resolution Imaging Spectroradiometer (MODIS) and Mann–Kendall (M-K) trend test to analyze the spatiotemporal variations in AOD in seven ecosystems in Northern Xinjiang from 2001 to 2023. The geographic detector model was employed to investigate the effects of driving factors, including gross domestic product, population density, specific humidity, precipitation, temperature, wind speed, soil moisture, and elevation, on the distribution of AOD in the ecosystems. The results indicate that over the past 23 years, wetlands had the highest annual average AOD values, followed by settlements, farmlands, deserts, grasslands, others, and forests, respectively. Furthermore, the AOD values decrease with increasing ecosystem elevation. The annual mean of AOD in Northern Xinjiang generally shows a fluctuating upward trend. The M-K test shows that the proportion of area with an increasing trend in AOD in the settlement ecosystems is the highest (92.17%), while the proportion of area with a decreasing trend in the forest ecosystem is the highest (21.78%). On a seasonal scale, grassland, settlement, farmland, forest, and wetland ecosystems exhibit peak values in spring and winter, whereas desert and other ecosystems only show peaks in spring. Different types of ecosystems show different sensitivities to driving factors. Grassland and forest ecosystems are primarily influenced by temperature and altitude, while desert and settlement ecosystems are most affected by wind speed and humidity. Farmlands are mainly influenced by wind speed and altitude, wetlands are significantly impacted by population density and humidity, and other ecosystems are predominantly affected by humidity and altitude. This paper serves as a reference for targeted air pollution prevention and regional ecological environmental protection. Full article
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<p>A schematic map of the location of the study area.</p>
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<p>Ecosystem distribution and typical landscape images.</p>
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<p>Scatter plot of AERONET AOD and MODIS MAIAC AOD from 2001 to 2023.</p>
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<p>(<b>a</b>) Spatial distribution of annual mean AOD averaged from 2001 to 2023 over Northern Xinjiang. (<b>b</b>) Elevation of Northern Xinjiang.</p>
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<p>The distribution of the annual mean AOD averaged from 2001 to 2023 in ecosystems at different elevations. (<b>a</b>) Entire study area; (<b>b</b>) grasslands; (<b>c</b>) deserts; (<b>d</b>) settlements; (<b>e</b>) farmlands; (<b>f</b>) forests; (<b>g</b>) wetlands; (<b>h</b>) others.</p>
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<p>A box plot of the interannual mean AOD values for different ecosystem types across elevation intervals from 2001 to 2023.</p>
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<p>A box plot of the interannual seasonal mean AOD values for different ecosystem types across elevation intervals from 2001 to 2023: (<b>a</b>) spring, March to May; (<b>b</b>) summer, June to August; (<b>c</b>) autumn, September to October; (<b>d</b>) winter, November to February.</p>
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<p>Spatial distribution of AOD change trend.</p>
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<p>Proportion of pixel area of change trend by ecosystem types.</p>
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<p>Annual average AOD changes of ecosystem types from 2001 to 2023.</p>
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<p>Interannual monthly mean changes in AOD in different ecosystems from 2001 to 2023.</p>
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<p>Spatial distribution of interannual monthly mean of AOD in Northern Xinjiang.</p>
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<p>Results of interaction detector. (<b>a</b>–<b>g</b>)The numbers represent the explanatory power of the interaction of driving factors.* represents two-factor enhancement, and ** represents nonlinear enhancement.</p>
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<p>The results of the risk detector. The horizontal axis represents the mean of the AOD, and the vertical axis represents the driving factors in different classifications. Red and green represent the highest and lowest AOD values, respectively.</p>
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14 pages, 219 KiB  
Article
Words and Images Matter: Perspectives on Suicide, Mental Health Concerns and Alcohol and Other Drug Use Depiction
by Dara L. Sampson, Hannah Cootes, Elizabeth Paton, Jennifer Peprah, Danielle Simmonette, Milena Heinsch, Frances Kay-Lambkin and Jaelea Skehan
Healthcare 2024, 12(21), 2120; https://doi.org/10.3390/healthcare12212120 - 24 Oct 2024
Viewed by 557
Abstract
Background/objectives: The way in which topics like suicide, mental health concerns and alcohol and other drug use are communicated matters. It has the potential to have either a positive or negative impact on people and communities, particularly those with a lived experience of [...] Read more.
Background/objectives: The way in which topics like suicide, mental health concerns and alcohol and other drug use are communicated matters. It has the potential to have either a positive or negative impact on people and communities, particularly those with a lived experience of these concerns. This article draws on the findings of a qualitative study designed to explore the experiences and perceptions of stakeholders on the imagery and language used to depict suicide, mental health concerns or alcohol and other drug use. Methods: The focus group method was used as a form of participatory action research to gain an in-depth understanding of the experiences and views of those who use or are impacted by language and imagery about suicide, mental ill-health and AOD use, including those with lived experiences of these topics. Results: A series of 10 focus groups were created in February and March 2022 with media and other professional communicators; people identifying as having a lived experience of suicide, mental ill-health or alcohol and other drug use; mental health and suicide prevention sector professionals; and people from priority populations (n = 49). From these focus groups, principles were developed as well as exemplars of helpful and less helpful depictions. Rather than prescriptive or static rules, the participants indicated that safe representations require an ongoing engagement with the principle of “do no harm”. Conclusions: A positive conclusion arose—that words and images have the potential to promote help-seeking, challenge stigma or stereotypes and create change. Full article
18 pages, 6507 KiB  
Article
Estimation of PM2.5 Using Multi-Angle Polarized TOA Reflectance Data from the GF-5B Satellite
by Ruijie Zhang, Hui Chen, Ruizhi Chen, Chunyan Zhou, Qing Li, Huizhen Xie and Zhongting Wang
Remote Sens. 2024, 16(21), 3944; https://doi.org/10.3390/rs16213944 - 23 Oct 2024
Viewed by 566
Abstract
The use of satellite data to estimate PM2.5 is an appropriate approach for long-term, substantial monitoring and assessment. To estimate PM2.5, the majority of the algorithms now in use utilize the top-of-atmosphere (TOA) reflectance or aerosol optical depth (AOD) derived [...] Read more.
The use of satellite data to estimate PM2.5 is an appropriate approach for long-term, substantial monitoring and assessment. To estimate PM2.5, the majority of the algorithms now in use utilize the top-of-atmosphere (TOA) reflectance or aerosol optical depth (AOD) derived from scalar satellite data. However, there is relatively little research on the retrieval of PM2.5 using multi-angle polarized data. With its directional polarimetric camera (DPC), the Chinese new-generation satellite Gaofen 5B (henceforth referred to as GF-5B) offers a unique opportunity to close this gap in multi-angle polarized observation data. In this research, we utilized TOA data from the DPC payload and applied the gradient boosting machine method to simulate the impact of the observation angle, wavelength, and polarization information on the accuracy of PM2.5 retrieval. We identified the optimal conditions for the effective estimation of PM2.5. The quantitative results indicated that, under these optimal conditions, the PM2.5 concentrations retrieved by GF-5B showed a strong correlation with the ground-based data, achieving an R2 of 0.9272 and an RMSE of 7.38 µg·m−3. By contrast, Himawari-8’s retrieval accuracy under similar data conditions consisted of an R2 of 0.9099 and RMSE of 7.42 µg·m−3, indicating that GF-5B offers higher accuracy. Furthermore, the retrieval results in this study demonstrated an R2 of 0.81 when compared to the CHAP dataset, confirming the feasibility and effectiveness of the use of GF-5B for PM2.5 retrieval and providing support for PM2.5 estimation through multi-angle polarized data. Full article
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<p>Geographical location and administrative division of the study area.</p>
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<p>Process flow diagram for estimation of PM<sub>2.5</sub> concentrations proposed in this study.</p>
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<p>Impact of model parameters on inversion ((<b>Left</b>): n_estimators, (<b>Right</b>): n_depth).</p>
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<p>Relative importance ranking of the variables in the model.</p>
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<p>Impact of different angles and bands on inversion accuracy (only TOA remote sensing data).</p>
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<p>Inversion accuracy of PM<sub>2.5</sub> under auxiliary data.</p>
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<p>Impact of different angles and bands on inversion accuracy (TOA data combined with meteorological and auxiliary data).</p>
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<p>Comparison of inversion accuracy between Scheme 1 (<b>Left</b>) and Scheme 2 (<b>Right</b>).</p>
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<p>Monthly results of PM<sub>2.5</sub> estimation by GF-5B ((<b>a</b>–<b>l</b>) representing January to December).</p>
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<p>Comparison of annual average values between GF-5B (<b>a</b>) results and the CHAP dataset (<b>b</b>).</p>
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<p>Comparison of estimation results between GF-5B (<b>left</b>) and Himawari-8 (<b>right</b>).</p>
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<p>The maps of the R<sup>2</sup>, RMSE, and MAE for various stations in the Beijing–Tianjin–Hebei region derived from GF-5B (<b>a</b>–<b>c</b>) and Himawari-8 (<b>d</b>–<b>f</b>).</p>
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<p>Scatter plot comparing GF-5B results with CHAP data..</p>
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22 pages, 3270 KiB  
Article
The Effects of Air Quality and the Impact of Climate Conditions on the First COVID-19 Wave in Wuhan and Four European Metropolitan Regions
by Marina Tautan, Maria Zoran, Roxana Radvan, Dan Savastru, Daniel Tenciu and Alexandru Stanciu
Atmosphere 2024, 15(10), 1230; https://doi.org/10.3390/atmos15101230 - 15 Oct 2024
Viewed by 580
Abstract
This paper investigates the impact of air quality and climate variability during the first wave of COVID-19 associated with accelerated transmission and lethality in Wuhan in China and four European metropolises (Milan, Madrid, London, and Bucharest). For the period 1 January–15 June 2020, [...] Read more.
This paper investigates the impact of air quality and climate variability during the first wave of COVID-19 associated with accelerated transmission and lethality in Wuhan in China and four European metropolises (Milan, Madrid, London, and Bucharest). For the period 1 January–15 June 2020, including the COVID-19 pre-lockdown, lockdown, and beyond periods, this study used a synergy of in situ and derived satellite time-series data analyses, investigating the daily average inhalable gaseous pollutants ozone (O3), nitrogen dioxide (NO2), and particulate matter in two size fractions (PM2.5 and PM10) together with the Air Quality Index (AQI), total Aerosol Optical Depth (AOD) at 550 nm, and climate variables (air temperature at 2 m height, relative humidity, wind speed, and Planetary Boundary Layer height). Applied statistical methods and cross-correlation tests involving multiple datasets of the main air pollutants (inhalable PM2.5 and PM10 and NO2), AQI, and aerosol loading AOD revealed a direct positive correlation with the spread and severity of COVID-19. Like in other cities worldwide, during the first-wave COVID-19 lockdown, due to the implemented restrictions on human-related emissions, there was a significant decrease in most air pollutant concentrations (PM2.5, PM10, and NO2), AQI, and AOD but a high increase in ground-level O3 in all selected metropolises. Also, this study found negative correlations of daily new COVID-19 cases (DNCs) with surface ozone level, air temperature at 2 m height, Planetary Boundary PBL heights, and wind speed intensity and positive correlations with relative humidity. The findings highlight the differential impacts of pandemic lockdowns on air quality in the investigated metropolises. Full article
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<p>Location of the investigated metropolitan areas Wuhan (China), Milan (Italy), Madrid (Spain), London (UK), and Bucharest (Romania).</p>
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<p>Temporal distribution of the daily mean ground level of ozone concentrations in the investigated metropolises during 1 January 2020–15 June 2020.</p>
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<p>Temporal patterns of the daily mean ground level of nitrogen dioxide concentrations in the investigated metropolises from 1 January 2020 to 15 June 2020.</p>
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<p>Temporal patterns of the daily mean Air Quality Index in the investigated metropolises during 1 January 2020–15 June 2020.</p>
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<p>Temporal patterns of the daily mean AOD in the investigated metropolises from 1 January 2019 to 15 June 2020.</p>
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<p>Temporal patterns of the daily new COVID-19 cases (DNCs) in the investigated metropolises from 1 January 2019 to 15 June 2020.</p>
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<p>Temporal patterns of the total COVID-19 cases recorded during January 2020–15 June 2020 in the investigated metropolises.</p>
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<p>Temporal patterns of the total COVID-19 deaths recorded during January 2020–15 June 2020 in the investigated metropolises.</p>
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15 pages, 3423 KiB  
Article
Comparative Study of Deflector Configurations under Variable Vertical Angle of Incidence and Wind Speed through Transient 3D CFD Modeling of Savonius Turbine
by Hady Aboujaoude, Guillaume Polidori, Fabien Beaumont, Sébastien Murer, Yessine Toumi and Fabien Bogard
Computation 2024, 12(10), 204; https://doi.org/10.3390/computation12100204 - 14 Oct 2024
Viewed by 734
Abstract
The demand for clean and sustainable energy has led to the exploration of innovative technologies for renewable energy generation. The Savonius turbine has emerged as a promising solution for harnessing wind energy in urban environments due to its unique design, simplicity, structural stability, [...] Read more.
The demand for clean and sustainable energy has led to the exploration of innovative technologies for renewable energy generation. The Savonius turbine has emerged as a promising solution for harnessing wind energy in urban environments due to its unique design, simplicity, structural stability, and ability to capture wind energy from any direction. However, the efficiency of Savonius turbines poses a challenge that affects their overall performance. Extensive research efforts have been dedicated to enhancing their efficiency and optimizing their performance in urban settings. For instance, an axisymmetric omnidirectional deflector (AOD) was introduced to improve performance in all wind directions. Despite these advancements, the effect of wind incident angles on Savonius turbine performance has not been thoroughly investigated. This study aims to fill this knowledge gap by examining the performance of standard Savonius configurations (STD) compared to the basic configuration of the deflector (AOD1) and to the optimized one (AOD2) under different wind incident angles and wind speeds. One key finding was the consistent superior performance of this AOD2 configuration across all incident angles and wind speeds. It consistently outperformed the other configurations, demonstrating its potential as an optimized configuration for wind turbine applications. For instance, at an incident angle of 0°, the power coefficient of the configuration of AOD2 was 61% more than the STD configuration. This ratio rose to 88% at an incident angle of 20° and 125% at an incident angle of 40°. Full article
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<p>Geometric parameters of the Savonius rotor and the different wind incident angle θ.</p>
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<p>(<b>a</b>) AOD2 (optimized cone), (<b>b</b>) AOD1 (truncated cone), (<b>c</b>) STD (without deflector).</p>
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<p>Computational domain and mesh cross sections used.</p>
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<p>Solver’s algorithm. (<b>a</b>) Coupled solver algorithm. (<b>b</b>) Segregated solver algorithm. (<b>c</b>) Hybrid solver scheme [<a href="#B23-computation-12-00204" class="html-bibr">23</a>].</p>
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<p>Power coefficient for different meshes.</p>
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<p>Power coefficient of different turbine configurations (STD, AOD1, and AOD2) under varying incidence angle and tip speed ranges. (<b>a</b>) Wind speed of 3.5 m·s<sup>−1</sup>, (<b>b</b>) wind speed of 7 m·s<sup>−1</sup>, (<b>c</b>) wind speed of 14 m·s<sup>−1</sup>.</p>
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<p>Performance increase ratio <math display="inline"><semantics> <mrow> <msubsup> <mrow> <mi>P</mi> <mi>I</mi> <mi>R</mi> </mrow> <mrow> <mi mathvariant="sans-serif">θ</mi> </mrow> <mrow> <mi>A</mi> <mi>O</mi> <mi>D</mi> <mn>2</mn> <mo>|</mo> <mi>S</mi> <mi>T</mi> <mi>D</mi> </mrow> </msubsup> </mrow> </semantics></math> curve versus θ.</p>
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<p>Pressure contour and velocity streamlines for STD and AOD2 at 7 m·s<sup>−1</sup> wind speed for λ = 1.0. (<b>a</b>) STD horizontal plane pressure contour at z = 0 at θ = 0°, (<b>b</b>) STD vertical plane pressure contour at y = 0 at θ = 0°, (<b>c</b>) STD vertical plane velocity streamlines at y = 0 at θ = 0°, (<b>d</b>) AOD2 horizontal plane pressure contour at z = 0 at θ = 0°, (<b>e</b>) AOD2 vertical plane pressure contour at y = 0 at θ = 0°, (<b>f</b>) AOD2 vertical plane velocity streamlines at y = 0 at θ = 0°, (<b>g</b>) STD horizontal plane pressure contour at z = 0 at θ = 40°, (<b>h</b>) STD vertical plane pressure contour at y = 0 at θ = 40°, (<b>i</b>) STD vertical plane velocity streamlines at y = 0 at θ = 40°, (<b>j</b>) AOD2 horizontal plane pressure contour at z = 0 at θ = 40°, (<b>k</b>) AOD2 vertical plane pressure contour at y = 0 at θ = 40°, (<b>l</b>) AOD2 vertical plane velocity streamlines at y = 0 at θ = 40°.</p>
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18 pages, 12939 KiB  
Article
Dust Monitoring and Three-Dimensional Transport Characteristics of Dust Aerosol in Beijing, Tianjin, and Hebei
by Siqin Zhang, Jianjun Wu, Jiaqi Yao, Xuefeng Quan, Haoran Zhai, Qingkai Lu, Haobin Xia, Mengran Wang and Jinquan Guo
Atmosphere 2024, 15(10), 1212; https://doi.org/10.3390/atmos15101212 - 10 Oct 2024
Viewed by 514
Abstract
Global dust events have become more frequent due to climate change and increased human activity, significantly impacting air quality and human health. Previous studies have mainly focused on determining atmospheric dust pollution levels through atmospheric parameter simulations or AOD values obtained from satellite [...] Read more.
Global dust events have become more frequent due to climate change and increased human activity, significantly impacting air quality and human health. Previous studies have mainly focused on determining atmospheric dust pollution levels through atmospheric parameter simulations or AOD values obtained from satellite remote sensing. However, research on the quantitative description of dust intensity and its cross-regional transport characteristics still faces numerous challenges. Therefore, this study utilized Fengyun-4A (FY-4A) satellite Advanced Geostationary Radiation Imager (AGRI) imagery, Cloud-Aerosol Lidar, and Infrared Pathfinder Satellite Observation (CALIPSO) lidar, and other auxiliary data, to conduct three-dimensional spatiotemporal monitoring and a cross-regional transport analysis of two typical dust events in the Beijing–Tianjin–Hebei (BTH) region of China using four dust intensity indices Infrared Channel Shortwave Dust (Icsd), Dust Detection Index (DDI), dust value (DV), and Dust Strength Index (DSI)) and the HYSPLIT model. We found that among the four indices, DDI was the most suitable for studying dust in the BTH region, with a detection accuracy (POCD) of >88% at all times and reaching a maximum of 96.14%. Both the 2021 and 2023 dust events originated from large-scale deforestation in southern Mongolia and the border area of Inner Mongolia, with dust plumes distributed between 2 and 12 km being transported across regions to the BTH area. Further, when dust aerosols are primarily concentrated below 4 km and PM10 concentrations consistently exceed 600 µg/m3, large dust storms are more likely to occur in the BTH region. The findings of this study provide valuable insights into the sources, transport pathways, and environmental impacts of dust aerosols. Full article
(This article belongs to the Section Aerosols)
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<p>Administrative map. (<b>a</b>) National 1 km DEM elevation map. (<b>b</b>) PM<sub>10</sub> monitoring station distribution in Beijing-Tianjin-Hebei Region. (<b>c</b>) Bar chart of dust source management project construction in Beijing-Tianjin-Hebei Region (2015–2019).</p>
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<p>Technical flowchart.</p>
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<p>Histogram of frequency distribution for thin clouds, thick clouds, and dust under four dust intensity indices.</p>
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<p>Dust identification results in the Beijing–Tianjin–Hebei Region. AGRI true-color images for 15 March 2021, UTC 03:00–06:00 (<b>a<sub>1</sub></b>–<b>a<sub>4</sub></b>), and DDI distribution maps (<b>b<sub>1</sub></b>–<b>b<sub>4</sub></b>); AGRI true-color images for 22 March 2023, UTC 03:00–06:00 (<b>c<sub>1</sub></b>–<b>c<sub>4</sub></b>), and DDI distribution maps (<b>d<sub>1</sub></b>–<b>d<sub>4</sub></b>); DDI violin and boxplot statistics for 15 March 2021, and 22 March 2023, UTC 03:00–06:00 (<b>e</b>).</p>
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<p>HYSPLIT backward trajectory simulations and FY-4A true-color images for the two dust events: (<b>a</b>,<b>b</b>) Beijing backward trajectory simulation for 15 March 2021; (<b>d</b>,<b>e</b>) Beijing backward trajectory simulation for 22 March 2023; (<b>c</b>) an FY-4A true-color image for 15 March 2021, at UTC 04:00; (<b>f</b>) an FY-4A true-color image for 22 March 2023, at UTC 04:00.</p>
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<p>Vertical distribution characteristics of aerosols and hourly changes in PM<sub>10</sub> concentration in the BTH and Inner Mongolia regions: 15 March 2021, BTH and Inner Mongolia regions (<b>a<sub>1</sub></b>–<b>a<sub>3</sub></b>, <b>b<sub>1</sub></b>–<b>b<sub>3</sub></b>); 21 March 2023, BTH and Inner Mongolia regions (<b>c<sub>1</sub></b>–<b>c<sub>3</sub></b>, <b>d<sub>1</sub></b>–<b>d<sub>3</sub></b>).</p>
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15 pages, 3533 KiB  
Article
The Marine Antimicrobial Peptide AOD with Intact Disulfide Bonds Has Remarkable Antibacterial and Anti-Biofilm Activity
by Ruoyu Mao, Qingyi Zhao, Haiqiang Lu, Na Yang, Yuanyuan Li, Da Teng, Ya Hao, Xinxi Gu and Jianhua Wang
Mar. Drugs 2024, 22(10), 463; https://doi.org/10.3390/md22100463 - 8 Oct 2024
Viewed by 916
Abstract
American Oyster Defensin (AOD) is a marine peptide that is derived from North American mussels. It has been demonstrated to exhibit potent antimicrobial activity and high safety in both in vitro and in vivo models. In this study, to facilitate synthesis, mutants of [...] Read more.
American Oyster Defensin (AOD) is a marine peptide that is derived from North American mussels. It has been demonstrated to exhibit potent antimicrobial activity and high safety in both in vitro and in vivo models. In this study, to facilitate synthesis, mutants of AOD with fewer disulfide bonds were designed and subjected to structural, antimicrobial, and anti-biofilm analysis. The antimicrobial activity of AOD-derived peptides decreased after reduction in the disulfide bond, and among its three derivatives, only AOD-1 inhibited very few bacteria with a MIC value of 64 μg/mL, whereas the others had no inhibitory effect on pathogenic bacteria. The findings demonstrated that full disulfide bonds are indispensable for bactericidal activity, with the α-helix playing a pivotal role in inhibiting bacterial membranes. Furthermore, the results of the ATP, ROS, membrane potential, and membrane fluidity assays demonstrated that intracellular ATP, reactive oxygen species, and membrane fluidity were all increased, while membrane potential was reduced. This indicated that AOD resulted in the impairment of membrane fluidity and induced metabolic disorders, ultimately leading to bacterial death. The inhibitory effect of AOD on the biofilm of S. epidermidis G-81 was determined through the crystal violet and confocal microscopy. The results demonstrated that AOD exhibited a notable inhibitory impact on the biofilm of S. epidermidis G-81. The minimum biofilm inhibitory concentration of AOD on S. epidermidis G-81 was 16 μg/mL, and the minimum biofilm scavenging concentration was 32 μg/mL, which exhibited superior efficacy compared to that of lincomycin. The inhibitory effect on the primary biofilm was 90.3%, and that on the mature biofilm was 82.85%, with a dose-dependent inhibition effect. Concurrently, AOD cleared intra-biofilm organisms and reduced the number of biofilm-holding bacteria by six orders of magnitude. These data indicate that disulfide bonds are essential to the structure and activity of AOD, and AOD may potentially become an effective dual-action antimicrobial and anti-biofilm agent. Full article
(This article belongs to the Special Issue Marine Natural Products with Antifouling Activity, 3rd Edition)
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<p>CD spectra of AOD and its derivatives.</p>
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<p>The safety of AOD in vivo. (<b>A</b>) Changes in body weight of mice within seven days. (<b>B</b>) Staining of liver and kidney tissue sections of mice.</p>
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<p>PI and SYTO9 staining of <span class="html-italic">S. epidermidis</span> G-81 treated by AOD.</p>
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<p>Effects of AOD on cell membrane fluidity (<b>A</b>), intracellular ATP (<b>B</b>), and reactive oxygen species (<b>C</b>). Results were given as mean ± SD (<span class="html-italic">n</span> = 3). ns: not significant, * <span class="html-italic">p</span> &lt; 0.05, ** <span class="html-italic">p</span> &lt; 0.01, *** <span class="html-italic">p</span> &lt; 0.001, and **** <span class="html-italic">p</span> &lt; 0.0001.</p>
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<p>Effect of AOD on <span class="html-italic">S. epidermidis</span> G-81 primary (<b>A</b>) and mature (<b>B</b>) biofilms.</p>
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<p>Effect of AOD on primary (<b>A</b>) and mature (<b>B</b>) biofilms observed by LCSM.</p>
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<p>Effect of AOD on biofilm-retaining bacteria.</p>
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27 pages, 11457 KiB  
Article
From Polar Day to Polar Night: A Comprehensive Sun and Star Photometer Study of Trends in Arctic Aerosol Properties in Ny-Ålesund, Svalbard
by Sandra Graßl, Christoph Ritter, Jonas Wilsch, Richard Herrmann, Lionel Doppler and Roberto Román
Remote Sens. 2024, 16(19), 3725; https://doi.org/10.3390/rs16193725 - 7 Oct 2024
Viewed by 1074
Abstract
The climate impact of Arctic aerosols, like the Arctic Haze, and their origin are not fully understood. Therefore, long-term aerosol observations in the Arctic are performed. In this study, we present a homogenised data set from a sun and star photometer operated in [...] Read more.
The climate impact of Arctic aerosols, like the Arctic Haze, and their origin are not fully understood. Therefore, long-term aerosol observations in the Arctic are performed. In this study, we present a homogenised data set from a sun and star photometer operated in the European Arctic, in Ny-Ålesund, Svalbard, of the 20 years from 2004–2023. Due to polar day and polar night, it is crucial to use observations of both instruments. Their data is evaluated in the same way and follows the cloud-screening procedure of AERONET. Additionally, an improved method for the calibration of the star photometer is presented. We found out, that autumn and winter are generally more polluted and have larger particles than summer. While the monthly median Aerosol Optical Depth (AOD) decreases in spring, the AOD increases significantly in autumn. A clear signal of large particles during the Arctic Haze can not be distinguished from large aerosols in winter. With autocorrelation analysis, we found that AOD events usually occur with a duration of several hours. We also compared AOD events with large-scale processes, like large-scale oscillation patterns, sea ice, weather conditions, or wildfires in the Northern Hemisphere but did not find one single cause that clearly determines the Arctic AOD. Therefore the observed optical depth is a superposition of different aerosol sources. Full article
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<p>Different relevant processes during polar day (<b>a</b>) and polar night (<b>b</b>). The numbers indicate (1) sea spray formation; (2a–b and 8) (non-)marine secondary aerosol formation; (3) particle processing in fog; (4) Arctic Ice Nucleation Particles (INP) concentrations; (5 and 7) Long-range transport; (6, 10 and 11) cloud formation; (9) blowing snow. Figure is adapted from Schmale et al. [<a href="#B14-remotesensing-16-03725" class="html-bibr">14</a>].</p>
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<p>Map of Ny-Ålesund on Svalbard in the European Arctic (source: Svalbardkartet (<a href="https://geokart.npolar.no/Html5Viewer/index.html?viewer=Svalbardkartet" target="_blank">https://geokart.npolar.no/Html5Viewer/index.html?viewer=Svalbardkartet</a>, accessed on 2 October 2024)); courtesy of Norwegian Polar Institute.</p>
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<p>Relative availability of cloud-screened measurements <math display="inline"><semantics> <mrow> <mo>[</mo> <mo>%</mo> <mo>]</mo> </mrow> </semantics></math> over the course of a year separated between sun and star photometer.</p>
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<p>Overview of combined photometer data. Every point is a daily median AOD.</p>
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<p>The monthly median values for the AOD is shown for each year of 2004–2023 in grey. The blue lines indicate the median (solid) and mean (dashed) of these values.</p>
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<p>Box-and-whisker plots for AOD for every month measured by sun and star photometer. All individual data points after cloud-screening are taken into account. As a reference for the amount of data per month and year, see <a href="#remotesensing-16-03725-t001" class="html-table">Table 1</a>. 25th and 75th percentile are shown by the blue boxes, whiskers indicated 9th and 91th percentile, median is shown by <span style="color: #FF0000">−</span> and mean by <span style="color: #FF0000">+</span>.</p>
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<p>Deviation from monthly mean AOD values in dependency of the year.</p>
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<p>One exemplary day with PSC (9 February 2020), measured by the Raman Lidar KARL in Ny-Ålesund. The PSC is clearly visible in about 20 km altitude throughout the entire day.</p>
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<p>Daily median of Ångström Exponent for sun and star photometer.</p>
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<p>Density plot of AOD and Ångström Exponent (<math display="inline"><semantics> <mrow> <mi>A</mi> <mi>E</mi> </mrow> </semantics></math>) for Sun (<b>left</b>) and star photometer (<b>right</b>) for all individual measurements from 2004 to 2023.</p>
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<p>Monthly median values of the Ångström Exponent is shown in grey for all of the years 2004 to 2023. The median (solid) and mean (dashed) of these annual cycle is given in orange.</p>
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<p>Box-and-whisker plots for Ångström Exponent for every month measured by sun and star photometer. All individual data points after cloud screening are taken into account. As a reference for the amount of data per month and year, see <a href="#remotesensing-16-03725-t001" class="html-table">Table 1</a>. The 25th and 75th percentile are shown by the blue boxes, whiskers indicate the 9th and 91st percentile, and the median is shown by <span style="color: #FF0000">−</span> and mean by <span style="color: #FF0000">+</span>.</p>
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<p>Deviation from monthly <math display="inline"><semantics> <mrow> <mi>A</mi> <mi>E</mi> </mrow> </semantics></math> mean values to long-term median <math display="inline"><semantics> <mrow> <mi>A</mi> <mi>E</mi> </mrow> </semantics></math> values.</p>
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<p>Autocorrelations for each month across the 20-year period (shown in grey) are displayed. The green line represents the median autocorrelation function derived from all individual monthly autocorrelations. Vertical lines indicate key time intervals at 1 h and 1 day. Additionally, black diamonds highlight the vertexes within the data.</p>
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<p>Monthly median AOD values are given in blue. With a multiple linear regression this AOD is reconstructed by using the above-mentioned parameter coefficients.</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
Viewed by 768
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>
Full article ">Figure 12
<p>PM<sub>2.5</sub> distribution from 2010 to 2021.</p>
Full article ">Figure 12 Cont.
<p>PM<sub>2.5</sub> distribution from 2010 to 2021.</p>
Full article ">Figure 12 Cont.
<p>PM<sub>2.5</sub> distribution from 2010 to 2021.</p>
Full article ">Figure 13
<p>PM<sub>2.5</sub>Con trends by province.</p>
Full article ">Figure 14
<p>Average PM<sub>2.5</sub>Con.</p>
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