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Search Results (3,071)

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19 pages, 7476 KiB  
Article
Cyclic and Multi-Year Characterization of Surface Ozone at the WMO/GAW Coastal Station of Lamezia Terme (Calabria, Southern Italy): Implications for Local Environment, Cultural Heritage, and Human Health
by Francesco D’Amico, Daniel Gullì, Teresa Lo Feudo, Ivano Ammoscato, Elenio Avolio, Mariafrancesca De Pino, Paolo Cristofanelli, Maurizio Busetto, Luana Malacaria, Domenico Parise, Salvatore Sinopoli, Giorgia De Benedetto and Claudia Roberta Calidonna
Environments 2024, 11(10), 227; https://doi.org/10.3390/environments11100227 (registering DOI) - 17 Oct 2024
Abstract
Unlike stratospheric ozone (O3), which is beneficial for Earth due to its capacity to screen the surface from solar ultraviolet radiation, tropospheric ozone poses a number of health and environmental issues. It has multiple effects that drive anthropogenic climate change, ranging [...] Read more.
Unlike stratospheric ozone (O3), which is beneficial for Earth due to its capacity to screen the surface from solar ultraviolet radiation, tropospheric ozone poses a number of health and environmental issues. It has multiple effects that drive anthropogenic climate change, ranging from pure radiative forcing to a reduction of carbon sequestration potential in plants. In the central Mediterranean, which itself represents a hotspot for climate studies, multi-year data on surface ozone were analyzed at the Lamezia Terme (LMT) WMO/GAW coastal observation site, located in Calabria, Southern Italy. The site is characterized by a local wind circulation pattern that results in a clear differentiation between Western-seaside winds, which are normally depleted in pollutants and GHGs, and Northeastern-continental winds, which are enriched in these compounds. This study is the first detailed attempt at evaluating ozone concentrations at LMT and their correlations with meteorological parameters, providing new insights into the source of locally observed tropospheric ozone mole fractions. This research shows that surface ozone daily and seasonal patterns at LMT are “reversed” compared to the patterns observed by comparable studies applied to other parameters and compounds, thus confirming the general complexity of anthropogenic emissions into the atmosphere and their numerous effects on atmospheric chemistry. These observations could contribute to the monitoring and verification of new regulations and policies on environmental protection, cultural heritage preservation, and the mitigation of human health hazards in Calabria. Full article
(This article belongs to the Special Issue Advances in Urban Air Pollution: 2nd Edition)
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<p>(<b>A</b>) Location of Lamezia Terme’s observation site (LMT) in the Mediterranean basin. (<b>B</b>) DEM (Digital Elevation Model) shows the location of LMT in central Calabria and the key orographic features of the Catanzaro isthmus that play a major role in local wind circulation. Additional maps and details showing the observation site itself and local emission sources are available in D’Amico et al. (2024a, 2024b, 2024c) [<a href="#B87-environments-11-00227" class="html-bibr">87</a>,<a href="#B88-environments-11-00227" class="html-bibr">88</a>,<a href="#B89-environments-11-00227" class="html-bibr">89</a>].</p>
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<p>(<b>A</b>) Location of Lamezia Terme’s observation site (LMT) in the Mediterranean basin. (<b>B</b>) DEM (Digital Elevation Model) shows the location of LMT in central Calabria and the key orographic features of the Catanzaro isthmus that play a major role in local wind circulation. Additional maps and details showing the observation site itself and local emission sources are available in D’Amico et al. (2024a, 2024b, 2024c) [<a href="#B87-environments-11-00227" class="html-bibr">87</a>,<a href="#B88-environments-11-00227" class="html-bibr">88</a>,<a href="#B89-environments-11-00227" class="html-bibr">89</a>].</p>
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<p>Wind rose of frequency counts and wind speed thresholds, based on hourly data gathered at LMT between 2015 and 2023. Each bar has an angle of 8 degrees. Calm refers to instances of 0 m/s, that have never occurred (0%) during the observation period.</p>
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<p>Main characteristics of daily patterns as observed at the LMT observation site between 2015 and 2023. All data refer to hourly aggregations. (<b>A</b>) Ozone mole fractions are grouped on a yearly basis (2022 and 2023 are excluded due to their lower coverage rate, as shown in <a href="#environments-11-00227-t001" class="html-table">Table 1</a>). (<b>B</b>) Average hourly concentrations of ozone, differentiated by season. (<b>C</b>) Seasonal changes in temperatures.</p>
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<p>Smoothed seasonal percentile rose plots showing hourly variations in ozone concentration thresholds by wind direction. Shaded areas refer to percentiles, while the radius refers to observed mole fractions in ppb.</p>
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<p>Correlation between wind speeds and ozone mole fractions, divided by sector. (<b>A</b>) Western-seaside (240–300° N); (<b>B</b>) Northeastern-continental (0–90° N); (<b>C</b>) total data.</p>
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<p>Evaluation of the OWE (Ozone Weekend Effect) based on hourly ozone data gathered at LMT, differentiated by weekdays. The dotted horizontal line represents average concentrations. (<b>A</b>) Western-seaside (240–300° N); (<b>B</b>) Northeastern-continental (0–90° N); (<b>C</b>) total data.</p>
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<p>(<b>A</b>) Multi-year variability of surface ozone mole fractions at LMT. The years 2022 and 2023 are not shown due to their lower coverage rate. (<b>B</b>) yearly cycle with monthly averages differentiated by wind corridor. (<b>C</b>) differentiated monthly averages referring to the entire observation period (2015–2023).</p>
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<p>(<b>A</b>) Multi-year variability of surface ozone mole fractions at LMT. The years 2022 and 2023 are not shown due to their lower coverage rate. (<b>B</b>) yearly cycle with monthly averages differentiated by wind corridor. (<b>C</b>) differentiated monthly averages referring to the entire observation period (2015–2023).</p>
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23 pages, 2584 KiB  
Article
Environmental Benefits of Hydrogen-Powered Buses: A Case Study of Coke Oven Gas
by Magdalena Gazda-Grzywacz, Przemysław Grzywacz and Piotr Burmistrz
Energies 2024, 17(20), 5155; https://doi.org/10.3390/en17205155 - 16 Oct 2024
Viewed by 249
Abstract
This study conducted a Life Cycle Assessment (LCA) of alternative (electric and hydrogen) and conventional diesel buses in a large metropolitan area. The primary focus was on hydrogen derived from coke oven gas, a byproduct of the coking process, which is a crucial [...] Read more.
This study conducted a Life Cycle Assessment (LCA) of alternative (electric and hydrogen) and conventional diesel buses in a large metropolitan area. The primary focus was on hydrogen derived from coke oven gas, a byproduct of the coking process, which is a crucial step in the steel production value chain. The functional unit was 1,000,000 km traveled over 15 years. LCA analysis using SimaPro v9.3 revealed significant environmental differences between the bus types. Hydrogen buses outperformed electric buses in all 11 environmental impact categories and in 5 of 11 categories compared to conventional diesel buses. The most substantial improvements for hydrogen buses were observed in ozone depletion (8.6% of diesel buses) and global warming (29.9% of diesel buses). As a bridge to a future dominated by green hydrogen, employing grey hydrogen from coke oven gas in buses provides a practical way to decrease environmental harm in regions abundant with this resource. This interim solution can significantly contribute to climate policy goals. Full article
(This article belongs to the Special Issue Pyrolysis and Gasification of Biomass and Waste II)
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<p>Limit of the LCA analysis system in the adopted well-to-wheel (WTW) framework for the public bus fleet. Prepared on the basis of [<a href="#B19-energies-17-05155" class="html-bibr">19</a>,<a href="#B23-energies-17-05155" class="html-bibr">23</a>].</p>
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<p>LCIA results of the WTT phase for diesel, hydrogen from coke oven gas, and electricity in 2020 for 1 MJ of energy contained in the energy carrier.</p>
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<p>TTW phase LCIA results for diesel, electric battery, and electric fuel cell buses.</p>
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<p>LCIA results of the vehicle bus cradle-to-gate stage, for FU 1 of the DB bus, EVB, and FCEVB.</p>
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<p>LCIA results for the Fuel Bus Life Cycle + Vehicle Bus Life Cycle phase, for DB. CML method for a 100 km FU over an assumed 15-year life cycle.</p>
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<p>LCIA results for the Fuel Bus Life Cycle + Vehicle Bus Life Cycle phase for EVB. Midpoints of the CML method for the 100 km distance of the FU over an assumed 15-year life cycle.</p>
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<p>LCIA results for the Fuel Bus Life Cycle + Vehicle Bus Life Cycle phase for the FCEVB. Midpoints of the CML method for the 100 km FU distance over an assumed 15-year life cycle.</p>
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<p>Life cycle comparison results of FBLC + VBLC for DB, EVB, and FCEVB.</p>
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<p>LCIA results from the WTT phase for electricity in the current and future modeled national mix for 1 MJ of energy contained in an energy carrier.</p>
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<p>FBLC + VBLC life cycle comparison results for DB, EVB (2020/2030/2040), and FCEVB.</p>
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<p>Share of hydrogen FCEVB vehicles in the SR fleet and change in accidental environmental loads of the CML method versus the base case.</p>
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18 pages, 14457 KiB  
Article
Variations of Planetary Wave Activity in the Lower Stratosphere in February as a Predictor of Ozone Depletion in the Arctic in March
by Pavel Vargin, Andrey Koval, Vladimir Guryanov, Eugene Volodin and Eugene Rozanov
Atmosphere 2024, 15(10), 1237; https://doi.org/10.3390/atmos15101237 - 16 Oct 2024
Viewed by 261
Abstract
This study is dedicated to the investigation of the relationship between the wave activity in February and temperature variations in the Arctic lower stratosphere in March. To study this relationship, the correlation coefficients (CCs) between the minimum temperature of the Arctic lower stratosphere [...] Read more.
This study is dedicated to the investigation of the relationship between the wave activity in February and temperature variations in the Arctic lower stratosphere in March. To study this relationship, the correlation coefficients (CCs) between the minimum temperature of the Arctic lower stratosphere in March (Tmin) and the amplitude of the planetary wave with zonal number 1 (PW1) in February were calculated. Tmin determines the conditions for the formation of polar stratospheric clouds (PSCs) following the chemical destruction of the ozone layer. The NCEP and ERA5 reanalysis data and the modern and future climate simulations of the Earth system models INM CM5 and SOCOLv4 were employed. It is shown that the maximum significant CC value between Tmin at 70 hPa in the polar region in March and the amplitude of the PW1 in February in the reanalysis data in the lower stratosphere is 0.67 at the pressure level of 200 hPa. The CCs calculated using the model data are characterized by maximum values of ~0.5, also near the same pressure level. Thus, it is demonstrated that the change in the planetary wave activity in the lower extratropical stratosphere in February can be one of the predictors of the Tmin. For further analysis of the dynamic structure in the lower stratosphere, composites of 10 seasons with the lowest and highest Tmin of the Arctic lower stratosphere in March were assembled. For these composites, differences in the vertical distribution and total ozone content, surface temperature, and residual meridional circulation (RMC) were considered, and features of the spatial distribution of wave activity fluxes were investigated. The obtained results may be useful for the development of forecasting of the Arctic winter stratosphere circulation, especially for the late winter season, when substantial ozone depletion occurs in some years. Full article
(This article belongs to the Special Issue Measurement and Variability of Atmospheric Ozone)
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<p>The zonal mean temperature averaged over 70–90° N and <span class="html-italic">Tmin</span> in March over 1948–2024 (NCEP-R) (black and green lines 1–2, respectively) (<b>a</b>); vertical profile of the correlation coefficient between the amplitude of PW1 averaged over 45–75° N in the range of pressure levels from 700 hPa to 10 hPa in February and <span class="html-italic">Tmin</span> at 70 hPa in the polar cap 70–90° N in March in the following data sets: NCEP reanalysis data over the periods of 1948–2024, 1948–1978, 1979–2024, and ERA5 reanalysis (1979–2023) (<b>b</b>); INMCM5 historical simulations (1965–2014, mean over experiments HIST1–HIST5) under the SSP2-4.5 and SSP5-8.5 scenarios (2015–2100), ERA5 reanalysis (1979–2023), NCEP (1979–2024) reanalysis data, and SOCOLv4 simulations under SSP2-4.5 and SSP5-8.5 scenarios (2015–2099, 3 ensembles mean) (<b>c</b>); INM CM5 historical experiments HIST1–HIST5 and the mean for the period of 1965–2014 (<b>d</b>).</p>
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<p>Scatter diagram of PW1 amplitude in geopotential meters (gpm) at 200 hPa averaged over 45–75° N in February and <span class="html-italic">Tmin</span> in the polar cap 70–90° N at 70 hPa in March from 1979 to 2024 (years are marked by black squares). Selected in the next section for cold and warm composites 10 years with the lowest and highest <span class="html-italic">Tmin</span> in March are marked by blue and red colors, respectively.</p>
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<p>Altitude–longitude cross-section of geopotential height difference (gpm) in the latitudinal belt 45–75° N (<b>а</b>); polar projections at the pressure levels 200 hPa (<b>b</b>) and 500 hPa (<b>c</b>) in February between “warm” and “cold” composites. The regions with significance at the 95% level for positive or negative changes are marked by gray dots.</p>
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<p>Altitude–latitudinal cross-section of PW1 amplitude (gpm) in February for “warm” and “cold” composites and the difference between them ((<b>a</b>–<b>c</b>) respectively). The same but for PW2 (<b>d</b>–<b>f</b>). The regions with significance at the 95% level for positive or negative changes are marked by gray dots.</p>
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<p>Altitude–latitudinal cross-sections of zonal mean heat flux (K m/s) in February for “warm” and “cold” composites (<b>a</b>,<b>b</b>) and the difference between them (<b>c</b>). The regions with significance at the 95% level for positive or negative changes are marked by gray dots.</p>
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<p>Altitude–latitudinal cross-sections of Plumb fluxes (<span class="html-italic">Fy</span>, <span class="html-italic">Fz</span> components, vectors) (m<sup>2</sup>/s<sup>2</sup>) and zonal mean wind (m/s, contours) in February of “warm” and “cold” composites and the difference between them (<b>a</b>–<b>c</b>). Altitude–longitudinal cross-sections of Plumb fluxes (<span class="html-italic">Fx</span>, <span class="html-italic">Fz</span> components, vectors) and geopotential height (contours) for “warm” and “cold” composites averaged over 45–75° N (<b>d</b>,<b>e</b>) and the difference between them for geopotential height and <span class="html-italic">Fz</span> (<b>f</b>). <span class="html-italic">Fz</span> is multiplied by 100. The area with the strongest upward propagation of wave activity fluxes from the troposphere to the stratosphere is highlighted by a purple oval (<b>f</b>).</p>
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<p>Vertical Plumb fluxes <span class="html-italic">Fz</span> component of “warm” and “cold” composites in February at the pressure level of 100 hPa (<b>a</b>,<b>b</b>). Difference of <span class="html-italic">Fz</span> (m<sup>2</sup>/s<sup>2</sup>) in February between “warm” and “cold” composites at 100 hPa (<b>c</b>) and 30 hPa (<b>d</b>).</p>
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<p>Temperature difference (K) (<b>a</b>) and ozone concentration at 70 hPa (%) (<b>a</b>,<b>b</b>) and total ozone content (%) in March between “warm” and “cold” composites (<b>b</b>,<b>c</b>).</p>
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<p>Temperature difference between ”warm” and “cold” composites at 1000 hPa in February (<b>a</b>), March (<b>b</b>), April (<b>c</b>), and May (<b>d</b>). The regions with significance at the 95% level for positive or negative changes are marked by gray dots.</p>
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<p>Temperature difference between ”warm” and “cold” composites at 1000 hPa in February (<b>a</b>), March (<b>b</b>), April (<b>c</b>), and May (<b>d</b>). The regions with significance at the 95% level for positive or negative changes are marked by gray dots.</p>
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<p>Altitude–latitude distribution of temperature (K, contours) and the RMC components (m/s, arrows) for “warm” and “cold” composites ((<b>a</b>,<b>b</b>), respectively); the eddy term of the RMC (m/s, arrows) and its vertical component (contours) for the “warm” and “cold” composites ((<b>d</b>,<b>e</b>), respectively); the differences in the corresponding values are shown in panels (<b>c</b>,<b>f</b>). The vertical components are multiplied by 200.</p>
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19 pages, 819 KiB  
Review
Research Progress on Physical Preservation Technology of Fresh-Cut Fruits and Vegetables
by Dixin Chen, Yang Zhang, Jianshe Zhao, Li Liu and Long Zhao
Horticulturae 2024, 10(10), 1098; https://doi.org/10.3390/horticulturae10101098 (registering DOI) - 16 Oct 2024
Viewed by 390
Abstract
Fresh-cut fruits and vegetables have become more popular among consumers because of their nutritional value and convenience. However, the lower shelf life of fresh-cut fruits and vegetables due to processing and mechanical damage is a critical factor affecting their market expansion, and advances [...] Read more.
Fresh-cut fruits and vegetables have become more popular among consumers because of their nutritional value and convenience. However, the lower shelf life of fresh-cut fruits and vegetables due to processing and mechanical damage is a critical factor affecting their market expansion, and advances in preservation technology are needed to prolong their shelf life. Some traditional chemical preservatives are disliked by health-seeking consumers because of worries about toxicity. Chemical preservation is inexpensive and highly efficient, but sometimes it carries risks for human health. Biological preservation methods are safer and more appealing, but they are not applicable to large-scale production. Physical fresh-keeping methods have been used for the storage and transportation of fresh-cut fruits and vegetables due to the ease of application. This review discusses current research in fresh-keeping technology for the preservation of fresh-cut fruits and vegetables. Preservation methods include low temperature, modified atmosphere packaging, cold plasma, pulsed light, ultrasonics, ultraviolet light, and ozonated water. As promising alternatives to chemical methods, these novel processes have been evaluated singly or combined with natural preservatives or other methods to extend the shelf life of fresh-cut fruits and vegetables and to provide references and assessments for further development and application of fresh-cut fruit and vegetable preservation technology. Full article
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<p>Effects of various physical treatments for the preservation of appearance, flavor, texture and other qualities of fresh-cut fruits and vegetables.</p>
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12 pages, 258 KiB  
Article
Effect of Treatment of Neuropathic and Ischemic Diabetic Foot Ulcers with the Use of Local Ozone Therapy Procedures—An Observational Single Center Study
by Jarosław Pasek, Sebastian Szajkowski and Grzegorz Cieślar
Clin. Pract. 2024, 14(5), 2139-2150; https://doi.org/10.3390/clinpract14050169 (registering DOI) - 16 Oct 2024
Viewed by 130
Abstract
Background: Diabetes ranks high among worldwide global health problems, and diabetic foot ulcer syndrome (DFU) is considered as one of its most serious complications. The purpose of this study was to evaluate the impact of local ozone therapy procedures on the wound healing [...] Read more.
Background: Diabetes ranks high among worldwide global health problems, and diabetic foot ulcer syndrome (DFU) is considered as one of its most serious complications. The purpose of this study was to evaluate the impact of local ozone therapy procedures on the wound healing process in patients with two DFU types: neuropathic and ischemic. Material and Methods: In the retrospective study reported here, the treatment outcomes of 90 patients were analyzed: 44 males (48.8%) and 46 females (51.2%), in the age range between 38 and 87 years of age, with neuropathic (group 1) and ischemic (group 2) diabetic foot ulcers treated by means of local ozone therapy. The assessment of therapeutic effects in both groups of patients included an analysis of the rate of ulcer healing using planimetry and an analysis of the intensity of pain associated with ulcers performed using the VAS scale. Results: After the application of ozone therapy procedures, a statistically significant decrease in the surface area of the ulcers was obtained in both groups of patients, respectively: in group 1 from 7 (6–7.5) cm2 to 3 (2–3.5) cm2 and in group 2 from 7.5 (6.5–8) cm2 to 5 (4.5–5.5) cm2 (p < 0.001), with a complete healing of ulcers not observed in any patients from groups 1 and 2. After treatment, the surface area of the assessed ulcers was smaller in the neuropathic group. The intensity of pain experienced after treatment also decreased with statistical significance in both groups (p < 0.001). Conclusions: Short-term local ozone therapy was effective in promoting wound healing and alleviating pain in patients with DFUs of both neuropathic and ischemic etiology. The effectiveness of therapy in the neuropathic type of DFUs was significantly higher than in the ischemic type, in which patients had a higher incidence of risk factors and more advanced lesions, characterized by a larger initial ulcer area and greater intensity of pain. Full article
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 (registering DOI) - 16 Oct 2024
Viewed by 222
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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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 (registering DOI) - 15 Oct 2024
Viewed by 348
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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29 pages, 4811 KiB  
Review
A Comprehensive Review on Various Phases of Wastewater Technologies: Trends and Future Perspectives
by José Fernandes, Paulo J. Ramísio and Hélder Puga
Eng 2024, 5(4), 2633-2661; https://doi.org/10.3390/eng5040138 (registering DOI) - 15 Oct 2024
Viewed by 408
Abstract
Wastewater Treatment Plants (WWTPs) encompass a range of processes from preliminary to advanced stages. Conventional treatments are increasingly inadequate for handling emergent pollutants, particularly organic compounds with carcinogenic potential that pose risks to aquifers. Recent advancements prioritize integrating Advanced Oxidation Processes (AOPs) and [...] Read more.
Wastewater Treatment Plants (WWTPs) encompass a range of processes from preliminary to advanced stages. Conventional treatments are increasingly inadequate for handling emergent pollutants, particularly organic compounds with carcinogenic potential that pose risks to aquifers. Recent advancements prioritize integrating Advanced Oxidation Processes (AOPs) and adsorbents with conventional methods to effectively retain organic pollutants and enhance mineralization. There is a growing preference for non-chemical or minimally chemical approaches. Innovations such as combining ozone and other biological processes with photo-sono-assisted methods, alongside integrating AOPs with adsorbents, are promising. These approaches leverage catalyst-assisted reactions to optimize oxidation efficiency. This review aims to provide a holistic perspective on WWTP processes, spanning wastewater intake to the production of potable water, highlighting key technologies, operational challenges, and future trends. The focus is on advancing sustainable practices and enhancing treatment efficacy to safeguard water quality and address evolving environmental concerns effectively. Full article
(This article belongs to the Special Issue Green Engineering for Sustainable Development 2024)
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<p>Wastewater treatment plant stages, from preliminary to advanced treatment processes.</p>
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<p>Scheme of representation of the primary processes: coagulation, flocculation and flotation, and respective sedimentation.</p>
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<p>Activated sludge process with biological and sedimentation tank with possibility of recycling the sludge.</p>
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<p>Sequencing batch reactor sequence with integration of 1—Feeding, 2—Reaction, 3—Sludge Withdrawal, 4—Settling, and 5—Effluent Withdrawal.</p>
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<p>Schematic of Moving Bed Biofilm Reactor (MBBR) functionality in aerobic and anaerobic conditions.</p>
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<p>Industrial method for ozone generation in wastewater treatment using the corona discharge technique.</p>
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<p>Ultrasonic-based wastewater treatment with horn configuration and mechanism of formation of bubbles cavitation and release of hydroxical radicals.</p>
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<p>Mechanism of adsorption between a liquid and the absorbent. The process is characterized by three main layers: absorbent, adsorbate and absorptive.</p>
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15 pages, 956 KiB  
Article
Healthiness and Safety of Smart Environments through Edge Intelligence and Internet of Things Technologies
by Rafiq Ul Islam, Pasquale Mazzei and Claudio Savaglio
Future Internet 2024, 16(10), 373; https://doi.org/10.3390/fi16100373 - 14 Oct 2024
Viewed by 409
Abstract
Smart environments exploit rising technologies like Internet of Things (IoT) and edge intelligence (EI) to achieve unseen effectiveness and efficiency in every tasks, including air sanitization. The latter represents a key preventative measure–made even more evident by the COVID-19 pandemic–to significantly reduce disease [...] Read more.
Smart environments exploit rising technologies like Internet of Things (IoT) and edge intelligence (EI) to achieve unseen effectiveness and efficiency in every tasks, including air sanitization. The latter represents a key preventative measure–made even more evident by the COVID-19 pandemic–to significantly reduce disease transmission and create healthier and safer indoor spaces, for the sake of its occupants. Therefore, in this paper, we present an IoT-based system aimed at the continuous monitoring of the air quality and, through EI techniques, at the proactively activation of ozone lamps, while ensuring safety in sanitization. Indeed, these devices ensure extreme effectiveness in killing viruses and bacteria but, due to ozone toxicity, they must be properly controlled with advanced technologies for preventing occupants from dangerous exposition as well as for ensuring system reliability, operational efficiency, and regulatory compliance. Full article
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<p>System architecture.</p>
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<p>UV-C lamp effectiveness vs. lifetime (hours) [<a href="#B27-futureinternet-16-00373" class="html-bibr">27</a>].</p>
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<p>The ozonizer machine CRJ O3-UV-500.</p>
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<p>The Node-Red flow.</p>
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<p>Snapshot of the PostgreSQL database for collecting the sensors’ data.</p>
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12 pages, 3102 KiB  
Article
Modeling Analysis of Nocturnal Nitrate Formation Pathways during Co-Occurrence of Ozone and PM2.5 Pollution in North China Plain
by Wei Dai, Keqiang Cheng, Xiangpeng Huang and Mingjie Xie
Atmosphere 2024, 15(10), 1220; https://doi.org/10.3390/atmos15101220 - 13 Oct 2024
Viewed by 428
Abstract
The rapid formation of secondary nitrate (NO3) contributes significantly to the nocturnal increase of PM2.5 and has been shown to be a critical factor for aerosol pollution in the North China Plain (NCP) region in summer. To explore the [...] Read more.
The rapid formation of secondary nitrate (NO3) contributes significantly to the nocturnal increase of PM2.5 and has been shown to be a critical factor for aerosol pollution in the North China Plain (NCP) region in summer. To explore the nocturnal NO3 formation pathways and the influence of ozone (O3) on NO3 production, the WRF-CMAQ model was utilized to simulate O3 and PM2.5 co-pollution events in the NCP region. The simulation results demonstrated that heterogeneous hydrolysis of dinitrogen pentoxide (N2O5) accounts for 60% to 67% of NO3 production at night (22:00 to 05:00) and is the main source of nocturnal NO3. O3 enhances the formation of NO3 radicals, thereby further promoting nocturnal N2O5 production. In the evening (20:00 to 21:00), O3 sustains the formation of hydroxyl (OH) radicals, resulting in the reaction between OH radicals and nitrogen dioxide (NO2), which accounts for 48% to 64% of NO3 formation. Our results suggest that effective control of O3 pollution in NCP can also reduce NO3 formation at night. Full article
(This article belongs to the Section Air Quality)
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<p>The WRF-CMAQ simulation domains, with red and blue dots, denote the locations of meteorological and environmental observation sites. The blue dashed rectangle marked North China Plain.</p>
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<p>Time series of 3 hourly observations (black dashed line) and hourly simulation (red solid line), 2 m temperature (T<sub>2</sub>), 2 m relative humidity (RH<sub>2</sub>), and 10 m wind speed (WS<sub>10</sub>) during the five air pollution episodes. The statistical metric correlation coefficient (<span class="html-italic">R</span>) and normalized mean bias (NMB) are shown.</p>
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<p>Time series of hourly observation (black dashed line) and simulation (red solid line) O<sub>3</sub> (ppb) and PM<sub>2.5</sub> (μg m<sup>−3</sup>) concentration during the five air pollution episodes. The statistical metric correlation coefficient (<span class="html-italic">R</span>) and normalized mean bias (NMB) are shown. The values of 100 μg m<sup>−3</sup> (51 ppb) and 35 μg m<sup>−3</sup> were marked with blue dashed lines, respectively.</p>
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<p>Average diurnal variations in concentrations of major PM<sub>2.5</sub> composition, O<sub>3</sub>, and PM<sub>2.5</sub> during pollution episodes. The black carbon (BC), dust, and primary organic aerosol (POA) are represented as primary aerosol components (PRI).</p>
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<p>Average diurnal variations of (<b>a</b>) HNO<sub>3</sub> and (<b>b</b>) N<sub>2</sub>O<sub>5</sub> production rates by different pathways, and associated with total HNO<sub>3</sub> production rates (HNO3prod), total N<sub>2</sub>O<sub>5</sub> production rates (N2O5prod), HNO<sub>3</sub>, N<sub>2</sub>O<sub>5</sub>, and NO<sub>3</sub> radical concentrations during pollution episodes. “OH + NO<sub>2</sub>”, “HET N<sub>2</sub>O<sub>5</sub>”, “NO<sub>3</sub> + VOC”, “Others” and “NO<sub>2</sub> + NO<sub>3</sub>” represented different chemical reaction pathways described in <a href="#atmosphere-15-01220-t001" class="html-table">Table 1</a> and <a href="#sec2dot1-atmosphere-15-01220" class="html-sec">Section 2.1</a>.</p>
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<p>Average diurnal variations of NO<sub>3</sub> radical production rates from the “O<sub>3</sub> + NO<sub>2</sub>” pathway, the concentration of NO<sub>3</sub> radicals (blue solid line), HO<span class="html-italic"><sub>x</sub></span> radicals (blue dashed line), O<sub>3</sub> (red solid line) and NO<sub>2</sub> (red dashed line). “O<sub>3</sub> + NO<sub>2</sub>” represented chemical reaction pathway is described in <a href="#atmosphere-15-01220-t001" class="html-table">Table 1</a> and <a href="#sec2dot1-atmosphere-15-01220" class="html-sec">Section 2.1</a>.</p>
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28 pages, 11475 KiB  
Article
A Study of the Influence of Ion-Ozonized Water on the Properties of Pasta Dough Made from Wheat Flour and Pumpkin Powder
by Bauyrzhan Iztayev, Auyelbek Iztayev, Talgat Kulazhanov, Galiya Iskakova, Madina Yakiyayeva, Bayan Muldabekova, Meruyet Baiysbayeva and Sholpan Tursunbayeva
Foods 2024, 13(20), 3253; https://doi.org/10.3390/foods13203253 - 13 Oct 2024
Viewed by 406
Abstract
Water treated with ion ozone improves the technological qualities of food products. Therefore, ion-ozonated water was used in the work, and whole-grain flour from soft wheat of the Almaly variety and pumpkin powder were used as raw materials to improve the quality and [...] Read more.
Water treated with ion ozone improves the technological qualities of food products. Therefore, ion-ozonated water was used in the work, and whole-grain flour from soft wheat of the Almaly variety and pumpkin powder were used as raw materials to improve the quality and nutritional value of the pasta. This study investigated the effects of ion-ozone concentration in ion-ozonated water Cio, water temperature tw, pumpkin powder content Cpp and drying temperature td on various characteristics affecting the quality of pasta, including its organoleptic physical, chemical, and rheological properties. These characteristics were assessed by conducting multiple experiments, a total of 25 indicators were determined, such as humidity, acidity, cooking properties, deformation, and other basic quality indicators. To reduce the number of experiments and obtain a reliable assessment of the influence of individual factors on the quality indicators of pasta, methods involving the multifactorial design of experiments were applied. Data processing and all necessary calculations were carried out using the PLAN sequential regression analysis program. Consequently, our findings indicate that minimizing dry water (DM) loss in cooking water requires a dual approach: increasing ion-ozone concentration and optimizing pasta composition and drying conditions, specifically by reducing pumpkin powder content and drying temperature. As a result, it was established that to obtain high-quality pasta from whole-grain flour with high quality and rheological properties, it is necessary to use the following optimal production modes: ion-ozone concentration in ion-ozonated water Cio = 2.5 × 10−6 mg/cm3, water temperature tw = 50 °C, pumpkin powder content Cpp = 3.0%, and pasta drying temperature td = 50 °C. The resulting pasta is an environmentally friendly product with a high content of biologically active substances. Full article
(This article belongs to the Section Food Engineering and Technology)
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<p>Control sample and test samples of pasta made from whole-grain flour from Almaly soft wheat and pumpkin powder using ion-ozonated water.</p>
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<p>Control sample and test samples of pasta made from whole-grain flour from Almaly soft wheat and pumpkin powder using ion-ozonated water.</p>
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<p>The response surface of the joint influence of factors C<sub>pp</sub> and t<sub>d</sub> on the protein content in pasta.</p>
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<p>The response surface of the joint influence of factors C<sub>io</sub>, C<sub>pp</sub>, t<sub>d</sub> on the content of dry substances in pasta.</p>
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19 pages, 3947 KiB  
Article
Modeling of Biologically Effective Daily Radiant Exposures over Europe from Space Using SEVIRI Measurements and MERRA-2 Reanalysis
by Agnieszka Czerwińska and Janusz Krzyścin
Remote Sens. 2024, 16(20), 3797; https://doi.org/10.3390/rs16203797 - 12 Oct 2024
Viewed by 274
Abstract
Ultraviolet solar radiation at the Earth’s surface significantly impacts both human health and ecosystems. A biologically effective daily radiant exposure (BEDRE) model is proposed for various biological processes with an analytical formula for its action spectrum. The following processes are considered: erythema formation, [...] Read more.
Ultraviolet solar radiation at the Earth’s surface significantly impacts both human health and ecosystems. A biologically effective daily radiant exposure (BEDRE) model is proposed for various biological processes with an analytical formula for its action spectrum. The following processes are considered: erythema formation, previtamin D3 synthesis, psoriasis clearance, and inactivation of SARS-CoV-2 virions. The BEDRE model is constructed by multiplying the synthetic BEDRE value under cloudless conditions by a cloud modification factor (CMF) parameterizing the attenuation of radiation via clouds. The CMF is an empirical function of the solar zenith angle (SZA) at midday and the daily clearness index from the Spinning Enhanced Visible and Infrared Imager (SEVIRI) measurements on board the second-generation Meteosat satellites. Total column ozone, from MERRA-2 reanalysis, is used in calculations of clear-sky BEDRE values. The proposed model was trained and validated using data from several European ground-based spectrophotometers and biometers for the periods 2014–2023 and 2004–2013, respectively. The model provides reliable estimates of BEDRE for all biological processes considered. Under snow-free conditions and SZA < 45° at midday, bias and standard deviation of observation-model differences are approximately ±5% and 15%, respectively. The BEDRE model can be used as an initial validation tool for ground-based UV data. Full article
(This article belongs to the Section Environmental Remote Sensing)
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<p>The location of the UV measuring stations shown in <a href="#remotesensing-16-03797-t001" class="html-table">Table 1</a> (created with Google My Maps: Map data 2024).</p>
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<p>Normalized action spectra for the specific biological effects: erythema appearance (black), photosynthesis of previtamin D<sub>3</sub> in human skin (blue), psoriasis clearance (green), and inactivation of SARS-CoV-2 virions (red).</p>
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<p>Scatter plot of UBE model against measured daily erythemal radiant exposure at Belsk for all-sky conditions for different ranges of noon SZA: (<b>a</b>) SZA &lt; 45°; (<b>b</b>) SZA ≥ 45° and SZA &lt; 60°; (<b>c</b>) SZA ≥ 60°. The dotted line is the 1–1 agreement line. The solid curve represents smoothed values from the LOWESS filter [<a href="#B43-remotesensing-16-03797" class="html-bibr">43</a>].</p>
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<p>Scatter plot RE<sub>BIOL</sub>(D) from the UBE model with <math display="inline"><semantics> <mrow> <msub> <mrow> <mover accent="true"> <mrow> <mi mathvariant="sans-serif">α</mi> </mrow> <mo stretchy="false">^</mo> </mover> </mrow> <mrow> <mi mathvariant="normal">E</mi> <mi mathvariant="normal">R</mi> <mi mathvariant="normal">Y</mi> <mi mathvariant="normal">T</mi> </mrow> </msub> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <msub> <mrow> <mover accent="true"> <mrow> <mi mathvariant="sans-serif">β</mi> </mrow> <mo stretchy="false">^</mo> </mover> </mrow> <mrow> <mi mathvariant="normal">E</mi> <mi mathvariant="normal">R</mi> <mi mathvariant="normal">Y</mi> <mi mathvariant="normal">T</mi> </mrow> </msub> </mrow> </semantics></math> when SZA<sub>N</sub> &lt; 45° versus corresponding values from spectral measurements at Belsk for the period 2011–2023: (<b>a</b>) for VITD, (<b>b</b>) for PSOR, and (<b>c</b>) for SARS.</p>
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<p>Scatter plot of the modeled (UBE model with <math display="inline"><semantics> <mrow> <msub> <mrow> <mover accent="true"> <mrow> <mi mathvariant="sans-serif">α</mi> </mrow> <mo stretchy="false">^</mo> </mover> </mrow> <mrow> <mi mathvariant="normal">E</mi> <mi mathvariant="normal">R</mi> <mi mathvariant="normal">Y</mi> <mi mathvariant="normal">T</mi> </mrow> </msub> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <msub> <mrow> <mover accent="true"> <mrow> <mi mathvariant="sans-serif">β</mi> </mrow> <mo stretchy="false">^</mo> </mover> </mrow> <mrow> <mi mathvariant="normal">E</mi> <mi mathvariant="normal">R</mi> <mi mathvariant="normal">Y</mi> <mi mathvariant="normal">T</mi> </mrow> </msub> </mrow> </semantics></math>) versus the measured daily radiant exposure for all-sky conditions and different ranges of SZA at noon: (<b>a</b>) Reading for SZA<sub>N</sub> &lt; 45°; (<b>b</b>) Reading for SZA<sub>N</sub> ≥ 45° and SZA<sub>N</sub> &lt; 60°; (<b>c</b>) Reading for SZA ≥ 60°; (<b>d</b>) Vienna for SZA<sub>N</sub> &lt;45°; (<b>e</b>) Vienna for SZA<sub>N</sub> ≥ 45° and SZA<sub>N</sub> &lt; 60°; (<b>f</b>) Vienna for SZA ≥ 60°. The dotted line is the 1–1 agreement line. The solid curve represents smoothed values from the Lowess filter [<a href="#B43-remotesensing-16-03797" class="html-bibr">43</a>].</p>
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<p>Scatter plot of the modeled (UBE model with <math display="inline"><semantics> <mrow> <msub> <mrow> <mover accent="true"> <mrow> <mi mathvariant="sans-serif">α</mi> </mrow> <mo stretchy="false">^</mo> </mover> </mrow> <mrow> <mi mathvariant="normal">E</mi> <mi mathvariant="normal">R</mi> <mi mathvariant="normal">Y</mi> <mi mathvariant="normal">T</mi> </mrow> </msub> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <msub> <mrow> <mover accent="true"> <mrow> <mi mathvariant="sans-serif">β</mi> </mrow> <mo stretchy="false">^</mo> </mover> </mrow> <mrow> <mi mathvariant="normal">E</mi> <mi mathvariant="normal">R</mi> <mi mathvariant="normal">Y</mi> <mi mathvariant="normal">T</mi> </mrow> </msub> </mrow> </semantics></math>) versus measured daily erythemal radiant exposure for different ranges of noon SZA: (SZA &lt; 45°; SZA ≥ 45° and SZA &lt; 60°; and SZA ≥ 60°: (<b>a</b>–<b>c</b>) Diekirch (Luxembourg); (<b>d</b>–<b>f</b>) Uccle (Belgium); (<b>g</b>–<b>i</b>) Davos (Switzerland); (<b>j</b>–<b>l</b>) Chisinau (Moldavia). As these stations were not used in UBE training, all available daily data in the period 2004–2023 have been used. The dotted line is the 1–1 perfect agreement line. The solid curve represents smoothed values from the Lowess filter [<a href="#B43-remotesensing-16-03797" class="html-bibr">43</a>].</p>
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<p>Scatter plot of the modeled (UBE model with <math display="inline"><semantics> <mrow> <msub> <mrow> <mover accent="true"> <mrow> <mi mathvariant="sans-serif">α</mi> </mrow> <mo stretchy="false">^</mo> </mover> </mrow> <mrow> <mi mathvariant="normal">E</mi> <mi mathvariant="normal">R</mi> <mi mathvariant="normal">Y</mi> <mi mathvariant="normal">T</mi> </mrow> </msub> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <msub> <mrow> <mover accent="true"> <mrow> <mi mathvariant="sans-serif">β</mi> </mrow> <mo stretchy="false">^</mo> </mover> </mrow> <mrow> <mi mathvariant="normal">E</mi> <mi mathvariant="normal">R</mi> <mi mathvariant="normal">Y</mi> <mi mathvariant="normal">T</mi> </mrow> </msub> </mrow> </semantics></math>) versus measured daily erythemal radiant exposure for different ranges of noon SZA: (SZA &lt; 45°; SZA ≥ 45° and SZA &lt; 60°; and SZA ≥ 60°: (<b>a</b>–<b>c</b>) Diekirch (Luxembourg); (<b>d</b>–<b>f</b>) Uccle (Belgium); (<b>g</b>–<b>i</b>) Davos (Switzerland); (<b>j</b>–<b>l</b>) Chisinau (Moldavia). As these stations were not used in UBE training, all available daily data in the period 2004–2023 have been used. The dotted line is the 1–1 perfect agreement line. The solid curve represents smoothed values from the Lowess filter [<a href="#B43-remotesensing-16-03797" class="html-bibr">43</a>].</p>
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<p>Scatter plot of the modeled (UBE model with <math display="inline"><semantics> <mrow> <msub> <mrow> <mover accent="true"> <mrow> <mi mathvariant="sans-serif">α</mi> </mrow> <mo stretchy="false">^</mo> </mover> </mrow> <mrow> <mi mathvariant="normal">E</mi> <mi mathvariant="normal">R</mi> <mi mathvariant="normal">Y</mi> <mi mathvariant="normal">T</mi> </mrow> </msub> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <msub> <mrow> <mover accent="true"> <mrow> <mi mathvariant="sans-serif">β</mi> </mrow> <mo stretchy="false">^</mo> </mover> </mrow> <mrow> <mi mathvariant="normal">E</mi> <mi mathvariant="normal">R</mi> <mi mathvariant="normal">Y</mi> <mi mathvariant="normal">T</mi> </mrow> </msub> </mrow> </semantics></math>) versus the measured daily radiant exposure for all-sky conditions and SZA at noon less than 45°: (<b>a</b>) VITD for Reading; (<b>b</b>) PSOR for Reading; (<b>c</b>) SARS for Reading; (<b>d</b>) VITD for Uccle; (<b>e</b>) PSOR for Uccle; (<b>f</b>) SARS for Uccle. The dotted line is the 1–1 agreement line. The solid curve represents smoothed values from the Lowess filter [<a href="#B43-remotesensing-16-03797" class="html-bibr">43</a>].</p>
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<p>Scatter plot of the modeled (UBE model with <math display="inline"><semantics> <mrow> <msub> <mrow> <mover accent="true"> <mrow> <mi mathvariant="sans-serif">α</mi> </mrow> <mo stretchy="false">^</mo> </mover> </mrow> <mrow> <mi mathvariant="normal">E</mi> <mi mathvariant="normal">R</mi> <mi mathvariant="normal">Y</mi> <mi mathvariant="normal">T</mi> </mrow> </msub> </mrow> </semantics></math> and <math display="inline"><semantics> <mrow> <msub> <mrow> <mover accent="true"> <mrow> <mi mathvariant="sans-serif">β</mi> </mrow> <mo stretchy="false">^</mo> </mover> </mrow> <mrow> <mi mathvariant="normal">E</mi> <mi mathvariant="normal">R</mi> <mi mathvariant="normal">Y</mi> <mi mathvariant="normal">T</mi> </mrow> </msub> </mrow> </semantics></math>) versus the measured daily radiant exposure for all-sky conditions and SZA at noon less than 45°: (<b>a</b>) VITD for Reading; (<b>b</b>) PSOR for Reading; (<b>c</b>) SARS for Reading; (<b>d</b>) VITD for Uccle; (<b>e</b>) PSOR for Uccle; (<b>f</b>) SARS for Uccle. The dotted line is the 1–1 agreement line. The solid curve represents smoothed values from the Lowess filter [<a href="#B43-remotesensing-16-03797" class="html-bibr">43</a>].</p>
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19 pages, 10490 KiB  
Article
Source Attribution Analysis of an Ozone Concentration Increase Event in the Main Urban Area of Xi’an Using the WRF-CMAQ Model
by Ju Wang, Yuxuan Cai, Sainan Zou, Xiaowei Zhou and Chunsheng Fang
Atmosphere 2024, 15(10), 1208; https://doi.org/10.3390/atmos15101208 - 10 Oct 2024
Viewed by 365
Abstract
The significant increase in ambient ozone (O3) levels across China highlights the urgent need to investigate the sources and mechanisms driving regional O3 events, particularly in densely populated urban areas. This study focuses on Xi’an, located in northwestern China on [...] Read more.
The significant increase in ambient ozone (O3) levels across China highlights the urgent need to investigate the sources and mechanisms driving regional O3 events, particularly in densely populated urban areas. This study focuses on Xi’an, located in northwestern China on the Guanzhong Plain near the Qinling Mountains, where the unique topography contributes to pollutant accumulation. Urbanization and industrial activities have significantly increased pollutant emissions. Utilizing the Weather Research and Forecasting–Community Multiscale Air Quality Model (WRF-CMAQ), we analyzed the contributions of specific regional and industrial sources to rising O3 levels, particularly during an atypical winter event characterized by unusually high concentrations. Our findings indicated that boundary conditions were the primary contributor to elevated O3 levels during this event. Notably, Xianyang and Baoji accounted for 30% and 22% of the increased O3 levels in Xi’an, respectively. Additionally, residential sources and transportation accounted for 31% and 28% of the O3 increase. Within the Xi’an metropolitan area, Baqiao District (18–27%) and Weiyang District (23–30%) emerged as leading contributors. The primary industries contributing to this rise included residential sources (28–37%) and transportation (35–43%). These insights underscore the need for targeted regulatory measures to mitigate O3 pollution in urban settings. Full article
(This article belongs to the Section Air Quality)
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<p>Map showing the triple-nested simulation domains, urban areas, and topography for each nest.</p>
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<p>Daily mean O<sub>3</sub> concentrations in February 2020 (red line) vs. February 2019 (black line), February 2021 (blue line), February 2022 (green line), and average O<sub>3</sub> concentrations for each month (dashed line).</p>
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<p>Comparison of temperature time series of meteorological stations in Xi’an.</p>
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<p>Comparison of wind-speed time series of meteorological stations in Xi’an.</p>
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<p>Comparison of O<sub>3</sub>-concentration time series in Xi’an.</p>
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<p>Contribution rates of O<sub>3</sub> to the 12 tagged regions under the regional source apportionment scenario. (<b>a</b>,<b>b</b>) are the contribution of each tagged region in d02 to O<sub>3</sub> in 2020 vs. in 2019, (<b>c</b>,<b>d</b>) are the contribution of each tagged region in d03 to O<sub>3</sub> in 2020 vs. in 2019.</p>
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<p>Contribution rates of O<sub>3</sub> to the 12 tagged regions under the source apportionment scenario for different emission types. (<b>a</b>,<b>b</b>) are the contribution of each tagged region in d02 to O<sub>3</sub> in 2020 vs. in 2019, (<b>c</b>,<b>d</b>) are the contribution of each tagged region in d03 to O<sub>3</sub> in 2020 vs. in 2019.</p>
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<p>Contribution rates of O<sub>3</sub> to the tagged regions of d02 under the regional source apportionment scenario in 2019 (<b>a</b>) and 2020 (<b>b</b>).</p>
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<p>Contribution rates of O<sub>3</sub> to the tagged regions of d02 under the source apportionment scenario for different emission types in February 2020: (<b>a</b>) IH; (<b>b</b>) PH; (<b>c</b>) TH; (<b>d</b>) RH.</p>
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<p>Contribution rates of O<sub>3</sub> to the tagged regions of d02 under the source apportionment scenario for different emission types in February 2019: (<b>a</b>) IH; (<b>b</b>) PH; (<b>c</b>) TH; (<b>d</b>) RH.</p>
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<p>Contribution rates of O<sub>3</sub> to the tagged regions of d02 under the source apportionment scenario for different emission types in February 2019: (<b>a</b>) IH; (<b>b</b>) PH; (<b>c</b>) TH; (<b>d</b>) RH.</p>
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<p>Contribution rates of O<sub>3</sub> to the tagged regions of d03 under the regional source apportionment scenario in 2019 (<b>a</b>) and 2020 (<b>b</b>).</p>
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<p>Contribution rates of O<sub>3</sub> to the tagged regions of d03 under the source apportionment scenario for different emission types in February 2020: (<b>a</b>) IH; (<b>b</b>) PH; (<b>c</b>) TH; (<b>d</b>) RH.</p>
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<p>Contribution rates of O<sub>3</sub> to the tagged regions of d03 under the source apportionment scenario for different emission types in February 2019: (<b>a</b>) IH; (<b>b</b>) PH; (<b>c</b>) TH; (<b>d</b>) RH.</p>
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16 pages, 7469 KiB  
Article
Estimation of Surface Ozone Effects on Winter Wheat Yield across the North China Plain
by Feng Wang, Tuanhui Wang, Haoming Xia, Hongquan Song, Shenghui Zhou and Tianning Zhang
Agronomy 2024, 14(10), 2326; https://doi.org/10.3390/agronomy14102326 - 10 Oct 2024
Viewed by 336
Abstract
Surface ozone (O3) pollution has adverse impacts on the yield of winter wheat. The North China Plain (NCP), one of the globally significant primary regions for winter wheat production, has been frequently plagued by severe O3 pollution in recent years. [...] Read more.
Surface ozone (O3) pollution has adverse impacts on the yield of winter wheat. The North China Plain (NCP), one of the globally significant primary regions for winter wheat production, has been frequently plagued by severe O3 pollution in recent years. In this study, the effects of O3 pollution on winter wheat yield and economic impact were evaluated in the NCP during the 2015–2018 seasons using the regional atmospheric chemical transport model (WRF-Chem), O3 metrics including the phytotoxic surface O3 dose above 12 nmol m−2 s−1 (POD12), and the accumulated daytime O3 above 40 ppb (AOT40). Results showed that the modeled O3, exposure-based AOT40, and flux-based POD12 increased during the winter wheat growing season from 2015 to 2018. The annual average daytime O3, exposure-based AOT40, and flux-based POD12 were 44 ppb, 5.32 ppm h, and 1.78 mmol m−2, respectively. During 2015–2018, winter wheat relative production loss averaged 10.9% with AOT40 and 14.6% with POD12. This resulted in an average annual production loss of 12.4 million metric tons, valued at approximately USD 4.5 billion. This study enhances our understanding of the spatial sensitivity of winter wheat to O3 impacts, and suggests that controlling O3 pollution during the key growth stages of winter wheat or improving its O3 tolerance will enhance food security. Full article
(This article belongs to the Section Agroecology Innovation: Achieving System Resilience)
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<p>Maps of the domains used in WRF-Chem. (<b>a</b>) D01, Domain 1, representing all of China. (<b>b</b>) D02, Domain 2, showing locations of monitoring stations. In both maps, the shaded area represents the North China Plain (NCP).</p>
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<p>Spatial distributions of mean daytime (08:00–18:00) surface O<sub>3</sub> during winter wheat growing season ((<b>a</b>) 2015; (<b>b</b>) 2016; (<b>c</b>) 2017; (<b>d</b>) 2018).</p>
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<p>County-level AOT40 in the winter wheat growing season over the NCP ((<b>a</b>) 2015; (<b>b</b>) 2016; (<b>c</b>) 2017; (<b>d</b>) 2018).</p>
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<p>County-scale g<sub>sto</sub> during the winter wheat growing seasons over the NCP ((<b>a</b>) 2015; (<b>b</b>) 2016; (<b>c</b>) 2017; (<b>d</b>) 2018).</p>
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<p>County-scale POD<sub>12</sub> in the winter wheat growing seasons over the NCP ((<b>a</b>) 2015; (<b>b</b>) 2016; (<b>c</b>) 2017; (<b>d</b>) 2018).</p>
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<p>County-scale winter wheat relative yield reduction based on AOT40 ((<b>a</b>) 2015; (<b>b</b>) 2016; (<b>c</b>) 2017; (<b>d</b>) 2018).</p>
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<p>County-level winter wheat relative yield reduction based on POD<sub>12</sub> ((<b>a</b>) 2015; (<b>b</b>) 2016; (<b>c</b>) 2017; (<b>d</b>) 2018).</p>
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<p>Annual production loss of winter wheat (WPL), production of winter wheat (WP), and winter wheat economic loss (WEL) of the NCP during 2015–2018.</p>
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15 pages, 2939 KiB  
Article
Development of Air Pollution Forecasting Models Applying Artificial Neural Networks in the Greater Area of Beijing City, China
by Panagiotis Fazakis, Konstantinos Moustris and Georgios Spyropoulos
Sustainability 2024, 16(19), 8721; https://doi.org/10.3390/su16198721 - 9 Oct 2024
Viewed by 620
Abstract
The ever-increasing industrialization of certain areas of the planet combined with the simultaneous degradation of the natural environment are alarming phenomena, especially in the field of human health. The concentration of particulate matter with an aerodynamic diameter of 2.5 μm (PM2.5) [...] Read more.
The ever-increasing industrialization of certain areas of the planet combined with the simultaneous degradation of the natural environment are alarming phenomena, especially in the field of human health. The concentration of particulate matter with an aerodynamic diameter of 2.5 μm (PM2.5) and 10 μm (PM10), nitrogen oxides (NOx), carbon monoxide (CO), sulfur dioxide (SO2), and ozone (O3) needs constant monitoring, as they consist of the main cause for many diseases. Based on the existence of statutory limits from the World Health Organization (WHO) for the concentration of each of the aforementioned air pollutants, it is considered necessary to develop forecasting systems that have the ability to correlate the current meteorological data with the concentrations of the above pollutants. In this work, the attempt to predict air pollutant concentrations in the wider area of Beijing, China, is successfully carried out using artificial neural network (ANN) models. In the frame of a specific work, a significant number of ANNs are developed. For this purpose, an open-access meteorological and air pollution database was used. Finally, a statistical evaluation of the developed prognostic models was carried out. The results showed that ANNs present a remarkable prognostic ability in order to forecast air pollution levels in an urban environment. Full article
(This article belongs to the Section Pollution Prevention, Mitigation and Sustainability)
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<p>Schematic representation of an ANN neuron.</p>
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<p>MLP architecture topology [<a href="#B24-sustainability-16-08721" class="html-bibr">24</a>].</p>
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<p>Map with the positions of the nine (9) examined locations, Beijing, China.</p>
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<p>Indicative illustration of the linear correlation of PM<sub>2.5</sub> concentrations between sites 3 and 1 (<b>a</b>), sites 3 and 4 (<b>b</b>), sites 3 and 6 (<b>c</b>), and sites 3 and 8 (<b>d</b>).</p>
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<p>Box and Whisker plot of index of agreement (IA) for all the training scenarios and each examined pollutant.</p>
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<p>Box and Whisker plot of Success Index (SI) for all training scenarios and for each examined pollutant.</p>
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