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Article

A Study on the Long-Term Variations in Mass Extinction Efficiency Using Visibility Data in South Korea

1
Division of Earth Environmental System Science, Pukyong National University, Busan 48513, Korea
2
High Impact Weather Research Department, National Institute of Meteorological Sciences, Gangneung-si 25457, Korea
3
Department of Environmental Engineering, Pukyong National University, Busan 48513, Korea
*
Author to whom correspondence should be addressed.
Remote Sens. 2022, 14(7), 1592; https://doi.org/10.3390/rs14071592
Submission received: 2 March 2022 / Revised: 20 March 2022 / Accepted: 24 March 2022 / Published: 25 March 2022
(This article belongs to the Section Atmospheric Remote Sensing)

Abstract

:
Fine particulate matter (PM) release is regulated by environmental policies in most countries. This study investigated long–term trends in the mass extinction efficiency (Qe) of aerosols in Northeast Asia. For this purpose, the Qe was calculated using visibility, PM2.5 recorded between 2015 and 2020, and PM10 recorded between 2001 and 2020 at eight Korean sites. The Qe of PM10 (Qe,10) showed an increasing trend with 0.06~0.22 (m2/g)/yr in seven cities except for Jeju. The Qe of PM2.5 (Qe,2.5) also showed an increasing trend with 0.28–2.47 (m2/g)/yr in all cities. In this study, PM10 and PM2.5, were divided into low, moderate, and high concentrations, and the Qe value change by year was examined. Qe,10 showed a tendency to decrease at low concentrations (19–21 μg/m3). However, at moderate (69–71 μg/m3) and high concentrations (139–141 μg/m3), Qe,10 increased in most regions. Qe,2.5 showed an increasing trend at low concentration (9–11 μg/m3), moderate concentration (29–31 μg/m3), and high concentration (69–71 μg/m3), except for Suwon and Pohang, where data were insufficient for analysis. Both Qe,10 and Qe,2.5 showed an increasing trend. The increase in Qe indicated that the visibility-impairing effect of PM can increase even if the same concentration of PM is present. The visibility-impairing effects of PM vary based on the composition, size and other characteristics of the particles in the atmosphere at a given point in time and not simply the quantity of particles. This means that reducing the quantity of particles does not reliably produce a proportionate improvement in visibility. Air quality policies must take the variable nature of PM particles and their effect on visibility into account so that more consistent improvements in air quality can be achieved.

Graphical Abstract

1. Introduction

Atmospheric aerosols can play an essential role in moderating atmospheric radiation exposure and climate change by scattering and absorbing solar radiation. They are significantly implicated in environmental issues, such as visibility, air quality, and public health [1,2,3,4,5,6,7]. In particular, many previous studies have confirmed that particulate matter (PM), which consists of small aerosol particles, is closely related to human health [8,9,10,11,12]. In 2013, the International Agency for Research on Cancer (IARC) under the World Health Organization (WHO) designated fine particulate matter as a group 1 carcinogen [13].
Northeast Asia, where Korea, China, and Japan locate, is one of the world’s most important PM source regions [14]. Air pollutants that can travel long distances, such as PM, are not only a problem for a given country but also a common problem for neighboring countries. In particular, Korea, located downwind of Northeast Asia, is directly affected by PM generated in China [15,16,17,18]. Northeast Asia has made efforts to reduce PM at the national level by implementing government policies and because of this PM has shown a decreasing trend [19,20,21]. In Beijing, the capital of China, PM2.5 decreased to −1.5 (µg/m3)/yr from 2000 to 2015 [22], and Shanghai, the second-largest city in China, also recorded a decrease in PM2.5 from 1999 to 2012 [23]. In the case of Tokyo, the capital of Japan, the PM2.5 concentration decreased by 49.8% between 2001 and 2010 [24]. In Korea, the national PM10 concentration steadily decreased from 2001 to 2018, and the PM2.5 concentration in Seoul, the capital of Korea, also decreased from 2003 to 2017 [25].
However, visibility has not increased in proportion to the reduction in PM and anxiety about PM has increased. For example, from 2013 to 2018, PM2.5, in southern China, significantly decreased from 52 to 33 μg/m3, but the frequency of low visibility did not decrease significantly [26]. Moreover, even in eastern China during the same period, the frequency of low-visibility haze did not improve significantly, compared to a significant decrease in PM2.5 [27]. In Korea, according to a survey on the perception of PM conducted by the Ministry of Environment in 2019, 92.3% answered that “the concentration of PM has increased compared to 10 years ago,” confirming that the anxiety about PM has increased compared to the past [28].
Visibility is an indicator that can be easily used by citizens to determine air pollution. It refers to the maximum distance at which people can recognize objects in the air. Visibility is related to the extinction of light, and visibility deteriorates when light is extinguished by particles and gases in the atmosphere [29]. This extinction of light is more affected by particles than gases, and smaller particles have a greater effect than larger ones [1,30,31,32]. Many studies have already reported that visibility and PM are closely related [1,33,34,35]. When all other conditions are the same, visibility deteriorates when the concentration of PM increases, and when the concentration decreases, visibility improves. Citizens can make the assessment that PM mass concentration also decreases when visibility is improved.
Mass extinction efficiency (Qe) is an indicator that can determine the change in visibility by indicating the degree of light extinction according to the mass concentration of PM. It is essential to understand the Qe because light extinction depends on particle characteristics, such as particle size and chemical composition, and affects visibility [36,37,38]. A high Qe indicates that even if the same concentration of PM is distributed in the atmosphere, visibility may differ as different amounts of light may be dissipated depending on the particle characteristics or humidity. Many studies have been conducted to characterize the Qe of particles [27,39,40,41]. However, there are few studies on long-term changes in Qe.
Therefore, this study calculated Qe using long-term observed PM mass concentration and visibility data in Korea and confirmed the long-term trends in Qe from 2001 to 2020 (the most recent data available). Through this, we tried to analyze the long-term changes in the optical properties of PM and to determine the mechanism causing the effect that changes in PM concentration have on the deterioration of visibility.
First, in Section 2, the methods used in this study, such as the study regions, data, and Qe calculation method, are explained in detail. Section 3 examines the trends in visibility, PM mass concentration, and Qe in each region. Section 4 discusses our results in comparison to the results of previous research. Finally, a summary and conclusion of this study are presented in Section 5.

2. Materials and Methods

2.1. PM10, PM2.5 and Visibility Data

Visibility data for this study was taken from ground-based meteorological observations from the Korea Meteorological Administration (KMA). There were two types of visibility measurement methods available. The first method was the visual method in which an experienced observer measures the visibility distance based on whether the specified target points are visible. The other method used a visibility meter. In addition to PM, visibility is also affected by meteorological factors, such as relative humidity, fog, and precipitation [42,43]. Therefore, this study used the relative humidity and current weather using ground observation data from the KMA. Visibility deteriorates regardless of the concentration of PM when the relative humidity is over 90% or when precipitation and fog occur [44]. To minimize the influence of factors other than PM, data on days when relative humidity was over 90% or precipitation and fog occurred were excluded from the analysis.
We used the PM concentration data provided by the AirKorea Website (airkorea.or.kr). PM concentrations were measured using the β-ray absorption method; PM and visibility data were measured at hourly intervals. In these data, PM is divided into PM10 and PM2.5, according to the particle diameter. Particles with aerodynamic diameters <10 μm are defined as PM10, and particles with aerodynamic diameters <2.5 μm are defined as PM2.5. The PM10 observation network was established nationwide in Korea before 2000. Additionally, PM2.5 has been included in the atmospheric environment standard since 2015, and national observation data exist from that year. In addition, because we used visibility data and PM mass concentration simultaneously to calculate Qe, if at least one of the two data types did not exist on the same day and at the same time, Qe was not calculated. We divided the year into spring (March–May), summer (June–August), autumn (September–November), and winter (December–February). If one of the four seasons had a smaller amount of data compared to the other seasons, we judged that the Qe value could not represent the year, so the year was excluded from the analysis. For example, in the case of Daegu in 2017, the number of autumns (494) among 5,389 data were significantly smaller than that of spring (1802), summer (1200), and winter (1893), so the 2017 data in Daegu were excluded from the analysis. In addition, if there were no data for more than 15 days in a month, data for that month were also excluded from the analysis.

2.2. Analysis Sites

Along with Japan and China, Korea is located in East Asia, and its capital is Seoul. There are limited cases where the KMA’s ground observatory and the PM observatory are located at the same point. Therefore, in this study, if there was a PM observatory within 4 km of the ground meteorological observatory where visibility was observed, that point was selected as the analysis site. We compared ground meteorological observatories with the closest PM observatory. If the PM observatory’s data were insufficient to analyze the annual rate of change, the next closest PM observatory’s data were used. In this study, Seoul (37.571°N, 126.966°E), Suwon (37.258°N, 126.983°E), Chuncheon (37.903°N, 127.736°E), Wonju (37.338°N, 127.947°E), Pohang (36.032°N, 129.380°E), and Daegu (35.878°N, 128.653°E), Busan (35.105°N, 129.032°E), and Jeju (33.514°N, 126.530°E) were selected for a total of 8 cities. We divided administrative districts and living areas into four provinces: the Metropolitan area (Seoul, Suwon), Gangwon-do (Chuncheon, Wonju), Gyeongsang-do (Pohang, Daegu, Busan), and Jeju-island (Jeju). Detailed information on each city’s location is presented in Figure 1 and Table A1.

2.3. Calculation of Mass Extinction Efficiency (Qe)

Qe is a value that indicates the extinction intensity of light per unit particle mass. To calculate Qe, first, we calculate the extinction coefficient (bext) using visibility data. bext indicates how strongly light is scattered and absorbed by the substance. It can be calculated by putting visibility data into the Koschmieder equation [29]. This study, following Cheng et al. [39], used the following equation to calculate bext (Equations (1) and (2)):
b ext , 2.5 ( M m 1 ) = 3912 [ Visibility ] 0.6 ( [ P M 10 P M 2.5 ] ) 10 0.33 [ N O 2 ]
In Equation (1), the unit of visibility is km, the units of PM10 and PM2.5 are μg/m3, and the unit of NO2 is ppb. The process of subtracting 0.6((PM10–PM2.5)) and 10 (Mm–1) from this equation takes into account coarse particles (PM2.5–10) and Rayleigh scattering, respectively. 0.33[NO2] accounts for the absorption of surrounding NO2 molecules. NO2 data and PM concentration were obtained from the AirKorea website.
b ext , 10 ( M m 1 ) = 3912 [ Visibility ] 10 0.33 [ N O 2 ]
Therefore, when calculating the bext of PM10, the process of subtracting 0.6((PM10–PM2.5)) was omitted, unlike PM2.5. In equation (1) and (2), 3,912 is a value obtained using a brightness contrast threshold of 0.02. The World Health Organization (WHO) uses 0.02 and the International Civil Aviation Organization (ICAO) uses 0.05, and the recommended value is different for each organization. In this study, as in Cheng et al. (2017) [39], 0.02 was applied as the brightness contrast threshold, a value often used in studies related to visibility in large cities or industrial areas such as Seoul.
By calculating bext using Equations (1) and (2) and dividing it by the PM mass concentration, we calculated the Qe value. The equation for Qe can be expressed as follows (Equation (3)):
Q e , i ( m 2 / g ) = b ext , i ( M m 1 ) P M i ( μ g / m 3 )
where PM is the PM mass concentration, and i distinguishes between PM2.5 and PM10. After calculating Qe for each year and month, we analyzed the long-term trends.

2.4. Mann–Kendall Test and Sen’s Slope

The trend slopes of all graphs shown in this study were obtained through a simple linear regression analysis. In addition, annual visibility, PM mass concentration, and Qe values were applied to the non-parametric Mann–Kendall (MK) test and Sen’s slope [45,46,47]. The MK test is mainly used to confirm the trend of data that repeats an increasing or decreasing trend and is relatively insensitive to missing values and outliers. The MK test can determine the significant increase or decrease trend of time series data but cannot quantitatively express the rate of change of the trend. Therefore, the slope can be confirmed by assuming that the data have a linear tendency through Sen’s slope. The MK test is divided into a null hypothesis without a tendency and an alternative hypothesis with a clear trend. These hypotheses were confirmed and determined through Z–scores and p-values. When |Z| > 1.96, the null hypothesis is rejected, and an alternative hypothesis with a tendency is accepted with a 95% confidence level (CL). When |Z| > 2.57, the alternative hypothesis was confirmed with a 99% CL. The sign of the Z–score value indicates a tendency to increase or decrease. In addition, in the case of p-value, when it has a value less than 0.05, it is considered a statistically significant value.

3. Results

3.1. Visibility and PM Mass Concentration Trend

Before examining Qe, we examined trends in the annual average of visibility and PM mass concentration. Figure 2 shows the annual average visibility and PM10 mass concentrations from 2001 to 2020. Table 1 shows the trend slopes of visibility, PM10, and PM2.5, through simple linear regression analysis, and the statistical test for the trend is shown in Table 2 and Table 3.
Although there was a difference in the degree of increase or decrease between cities, PM10 showed a clear decreasing trend overall. This trend had a CL of 99% in all cities except Jeju. This decreasing trend was similar to the previous study that confirmed that PM10 in Korea decreased to −0.61 ± 0.08 (μg/m3)/yr from 1999 to 2018 [48]. Visibility in 2020 compared to 2001 was improved in most cities, but not significantly so in some cases. In the case of the visibility results in Table 2, only Wonju, Pohang, Daegu, and Jeju had a high CL of 99%. After running the MK test, the degree of improvement in visibility in the remaining cities had a low CL of less than 95%. In particular, in Wonju, where the PM10 and visibility data had a high CL of 99%, visibility worsened to −0.12 km/yr, even though the PM10 concentration was greatly reduced to −0.82 (μg/m3)/yr. In the case of Chuncheon, another city in Gangwon-do, visibility improved until 2015. However, visibility continued to deteriorate from 2016, and visibility in the years 2017 (16.0 ± 5.1 km), 2018 (15.5 ± 5.2 km), and 2019 (15.7 ± 5.3 km) was lower than that in 2002 (16.9 ± 4.1 km). Gangwon-do, which includes Wonju and Chuncheon, can be divided into Yeongdong and Yeongseo based on the location of the Taebaek Mountains. Wonju and Chuncheon correspond to the Yeongseo of Gangwon-do, located west of the Taebaek Mountains. The geographical location close to the Metropolitan area blocked by mountain ranges in the east shows the effect of increasing the concentration of PM in the area, as PM generated in the Metropolitan area moves along the air current when a westerly wind blows. Wonju is one of the cities where high concentrations of PM occur frequently.
The Metropolitan area has a high probability of generating higher PM concentrations than other sites because the population, vehicles, and businesses are concentrated. Therefore, the Korean government is making efforts to reduce PM in various ways, such as reducing old diesel vehicles, expanding the supply of low-emission vehicles, and encouraging the use of public transportation. As a result, Seoul showed the greatest reduction in PM10 among the eight cities, decreasing by –1.86 (μg/m3)/yr. In Suwon, another city in the Metropolitan area, PM10 has been continuously decreasing by –1.14 (μg/m3)/yr. Contrarily, the slope of the trend in improving visibility was 0.04 km/yr in Seoul and 0.09 km/yr in Suwon, lower values than Daegu (0.15 km/yr) and Jeju (0.12 km/yr), which had smaller PM10 decreasing trend slopes. In addition, the Seoul and Suwon results had a low CL, unlike the trend of visibility improvement in Daegu and Jeju, which had a high CL of 99%.
Busan, which is part of Gyeongsang-do, is a port city located in southeast Korea. In particular, Busan is an area with serious air pollution caused by PM, and it has been selected as one of the world’s ten most polluted ports (ultrafine particle pollution) along with China, Dubai, and Singapore [49]. However, in Busan, as in other cities, PM10 is steadily decreasing, but the trend of visibility improvement was 0.04 km/yr, which is not a significant improvement compared to other cities, and the improvement trend had a low CL lower than 95%.
Figure 3 shows the annual average values of PM2.5, and visibility from 2015 to 2020. In the cases of Suwon and Pohang, compared to other cities, it was not easy to identify accurate trends and produce statistical test results because there was little data. Table 1 shows the annual average trend, and Table 3, which shows the statistical test results, PM2.5, allows visibility trends in the six cities to be confirmed. PM2.5 decreased or did not show a significant change. Wonju, Busan, and Jeju showed a trend of decreasing PM2.5, with a high CL of 95%, but the Seoul, Chuncheon, and Daegu results had a low CL. However, a clear trend could not be found in the visibility data, as it had a CL of less than 95% in all cities. As shown in Figure 3, some cities have worse visibility than in the past. Except for Suwon and Pohang, Wonju showed the most significant decrease in PM2.5 after Pohang at –3.29 (μg/m3)/yr, but visibility did not noticeably change. Busan and Jeju PM2.5 significantly decreased to –2.34 (μg/m3)/yr and –1.98 (μg/m3)/yr, respectively with a 95% CL. However, there was no clear trend in visibility. In Figure 2 and Figure 3, we identified cities whose visibility did not improve significantly or worsen compared to the PM mass concentration, which has continuously decreased since the past. Accordingly, we examined the long-term trend by calculating the Qe value of the particles per unit mass, which is directly related to visibility.

3.2. Long-Term Trend in Mass Extinction Efficiency (Qe)

Table 4 shows the average Qe over the entire period, regardless of city. The mass extinction efficiency of PM10(Qe,10) and PM2.5 (Qe,2.5) both showed an increasing trend, although overall, the Qe,2.5 value was higher than Qe,10. Kim (2015) [30] reported that the mass extinction coefficients of PM10 and PM2.5 were 2.7 ± 0.2 m2/g and 4.7 ± 0.2 m2/g, respectively. Moreover, Cheng et al. (2013) [50] reported that the Qe of PM2.5 was 4.08 m2/g, and that of PM2.5-10 was 0.58 m2/g. Thus, our result that Qe,2.5 had a higher value than Qe,10 is consistent with these aforementioned studies. Husar and Falke (1996) [51] showed that the average mass scattering efficiency of PM2.5 value in various regions was 7.4 m2/g and varied from 4 to 12 m2/g. The Qe values of this study were higher than those of previous studies. Statistical test results for the Qe,10 trend were Z = 3.4715, P = 0.0005 and Sen’s slope = 0.0726 and for Qe,2.5, Z = 2.6301, P = 0.0085 and Sen’s slope = 0.8522, with a high CL of 99%.
Figure 4 shows the annual Qe,10 values from 2001 to 2020, and the detailed Qe,10 values for the city are listed in Table 5. The Qe,10 trend slope value through simple linear regression analysis is shown in Table 1, together with the PM and visibility trend slope. There was an increasing trend in Qe,10 in all cities except Jeju. In Table 2, which shows the statistical tests for Qe,10, all cities except Chuncheon and Jeju had a CL higher than 95%, and Seoul, Pohang, and Busan had a high CL of 99%.
Wonju Qe,10 had an increasing trend of 0.22 (m2/g)/yr, the steepest increase among the eight cities. Qe,10 in 2012 was 4.3 ± 2.3 m2/g, which was quite low, but it had a high value continuously since Qe,10 increased to 6.2 ± 6.4 m2/g in 2015. Seoul’s results, which had a high CL of 99%, have Qe,10 increasing at 0.15 (m2/g)/yr, which was the second steepest increase after Wonju. Seoul’s Qe,10 showed the highest value at 8.1 ± 4.1 m2/g in 2014, and then it showed a lower value again in 2015 (6.5 ± 3.0 m2/g) and 2016 (5.7 ± 2.5 m2/g). Seoul had a high Qe,10 again after 2017. Unlike the other seven cities, Jeju’s Qe,10 decreased to −0.08 (m2/g)/yr, but the CL for the trend was less than 95%.
The annual average mass extinction efficiency (Qe,2.5) of PM2.5, from 2015 to 2020, is shown in Figure 5, and the annual values are shown in Table 6. As shown in Table 1, the slope of Qe,2.5 in all cities showed an increasing trend. Table 3 presents the statistical test results for this trend. The increasing Qe,2.5 trend in Wonju, Busan, and Jeju had a high CL of more than 95%. As for Qe,10, Wonju had the steepest increasing trend with a Qe,2.5 slope of 2.47 (m2/g)/yr. In addition, except for Suwon and Pohang, where data are few, the city showing the steepest increase after Wonju was Chuncheon with a slope of 1.12 (m2/g)/yr. However, the slope of the increasing trend of Qe,2.5 in Chuncheon had a low CL of less than 95%. As can be seen in Figure 3, although PM2.5 decreased in Wonju and Chuncheon, visibility did not improve, or even though there was no significant change in PM2.5, visibility deteriorated.
In addition, Busan’s Qe,2.5 value continuously increased to 1.10 (m2/g)/yr (Figure 5). Busan’s Qe,2.5 values increased rapidly from 11.3 ± 6.7 m2/g in 2019 to 15.4 ± 9.1 m2/g in 2020 (Table 5). Jeju’s Qe,2.5 increased to 0.99 (m2/g)/yr in 2015~2020, whereas Qe,10 decreased over the period 2001–2020. However, when looking at the Qe,10 values for 2016–2020 in Figure 4, it can be seen that after showing the lowest Qe,10 at 5.0 ± 2.4 m2/g in 2016, Jeju’s Qe,10 value also increased to 6.8 ± 2.5 m2/g in 2020.
As mentioned above, since PM2.5 was observed from 2015, there were insufficient data to examine the trend as an annual average. The monthly average value and trend slope of Qe,2.5 from 2015 to 2020 are shown in Figure 6; Table 7 shows statistical test results. Except for Suwon, the increasing trend of Qe,2.5 in the remaining seven cities showed a high CL of more than 95%. The monthly Qe,2.5′s slope ranged from 0.04 to 0.23 (m2/g)/mth. Seoul showed the steepest trend slope after Wonju in the annual average Qe,10, but the monthly average Qe,2.5 showed a slope of 0.05 (m2/g)/mth, which was not evident compared to other cities. In the case of Wonju, the monthly average Qe,2.5 showed the highest slope at 0.23 (m2/g)/mth, which was similar to the annual average Qe,10 and Qe,2.5. Chuncheon, another city of Gangwon-do, also had the steepest slope after Wonju with a monthly average Qe,2.5 slope of 0.11 (m2/g)/mth. The data from Suwon and Pohang was insufficient to confirm the trend. On comparing the trends of the monthly average Qe,2.5 of the two cities, Pohang showed an increasing trend at 0.10 (m2/g)/mth, but Suwon showed no apparent increase at 0.06 (m2/g)/mth. In Daegu, the Qe,2.5 value increased sharply in 2018, but no apparent increase has been recorded since then. In Busan and Jeju, the Qe,2.5 slope showed an increasing trend of 0.10 (m2/g)/mth.

4. Discussion

4.1. Qe Trend by Fixed PM

This study aimed to understand the change in the extinction characteristics of PM from the change in Qe value. As a result of analyzing changes in Qe values by month and year from 2001 to 2020, Qe increased overall. To more clearly confirm this trend identified so far, we looked at the change in Qe by year at the same PM concentration. Among the PM10 and PM2.5 data, certain PM concentrations were randomly chosen and categories representing low, moderate, and high concentrations were designated. The respective Qe values at the PM concentrations were extracted to determine the annual average change. PM10 was divided into 19–21 μg/m3 (low), 69–71 μg/m3 (moderate), 139–141 μg/m3 (high), and PM2.5, which was divided into 9–11 μg/m3 (low), 29–31 μg/m3 (moderate), 69–71 μg/m3 (high). Then, only the data corresponding to each PM concentration were extracted, and the Qe change trend was examined. Figure 7 shows the Qe,10 of PM10 by year, divided into three categories from 2001 to 2020, and Table 8 shows the Qe trend slope according to the fixed PM concentration by year.
When PM10 was low, the Qe,10 value showed a decreasing trend in all the cities. However, in the case of moderate and high concentrations, Qe,10 increased in most cities, reflecting the overall Qe,10 value trend. In particular, the Qe,10 trends in Wonju were 0.27 (m2/g)/yr and 0.33 (m2/g)/yr for moderate and high concentrations, respectively, which was significantly higher than in other cities.
Annual changes in Qe,2.5 were confirmed by dividing low, moderate, and high concentrations into 9–11 μg/m3, 29–31 μg/m3, and 69–71 μg/m3, respectively. With the exception of Suwon and Pohang in Figure 7 and Table 8, Qe,2.5 showed an increasing trend in most cities, regardless of concentration classification. In particular, the trend of increasing Qe,2.5 was more evident in moderate and high concentrations than in low. In the case of high concentration, the Qe,2.5 of Seoul decreased to −0.14 (m2/g)/yr, unlike other cities. However, when compared with other cities, Qe,2.5 showed consistently high values even with the same PM2.5 concentration. Qe,2.5 and Qe,10 showed an increasing trend at both moderate and high PM concentrations, which indicates that the deterioration in visibility is not related to the PM concentration.

4.2. Qe,2.5 Data Comparison

Figure 8 shows the Qe,2.5 value reported in previous studies conducted in Northeast Asia compared with the Qe,2.5 value obtained in this study [27,30,39,40,50,52,53,54,55,56,57,58,59]. As some studies showed only the mass scattering efficiency value, the Qe,2.5 value was calculated again using the empirical SSA value of 0.8 as in Cheng et al. (2017) [39]. Other studies used a wavelength of 550 nm except for Liu et al. (2020) [27] and Jing et al. (2015) [54] that used wavelengths of 589 and 525 nm, respectively. Liu et al. (2020) [27] showed that the PM2.5 decreased from 2013 to 2018, but the Qe,2.5 value in 2018 increased compared to that in 2013 due to an increase in the proportion of aerosol nitrate and an increase in relative humidity. Similar to the observation of increase in Qe,2.5 by Liu et al. (2020) [27] in eastern China, our results also indicate increasing trend of Qe,2.5 in most of the regions in this study compared to the past data. The data from our study confirms the long-term increasing trend of Qe,10 and Qe,2.5. This trend of increasing Qe,2.5 is similar to the result of shin et al. (2022) [60].
Many previous studies related to Qe found that light extinction caused by particles is affected by particle properties such as size, composition, or meteorological factors such as relative humidity. Qe varies depending on the diameter of the particle, and Qe of PM2.5 is approximately three times higher than that of PM10 [36,37]. In addition, Qe varies according to the mass ratio of components of PM2.5, and Qe increases as the mass fraction of carbonaceous substances and secondary inorganic species with high hygroscopicity (sulfate, nitrate, and ammonia) increase [39].

5. Conclusions

This study examined the long-term trends in Qe, one of the optical characteristics of PM, using PM10 and visibility data from 2001 to 2020 and PM2.5 from 2015 to 2020 in Korea. Looking at annual Qe, Qe,10 increased from 0.06 to 0.22 (m2/g)/yr in all cities except Jeju. However, statistical test results for Chuncheon and Jeju showed a CL less than 95%. Qe,2.5 increased in all cities from 0.28 to 2.47 (m2/g)/yr, but only Wonju, Busan, and Jeju had a CL higher than 95%. The monthly Qe,2.5 increased from 0.04 to 0.23 (m2/g)/mth, and the statistical test result had a CL higher than 95% in all cities except Suwon. Finally, after dividing the PM10 and PM2.5 data into low, moderate, and high concentrations, Qe changes were observed. When PM10 was at a low concentration (19–21 μg/m3), Qe,10 showed a tendency to decrease. Contrarily, Qe,10 in most cities showed an increasing trend at moderate concentration (69–71 μg/m3) and high concentration (139–141 μg/m3). Qe,2.5 increased in most cities except for Suwon and Pohang at low (9–11 μg/m3), moderate (29–31 μg/m3), and high concentration (69–71 μg/m3). However, in the case of, Qe,2.5 of Seoul showed a decreasing trend for high concentrations but Qe,2.5 remained high throughout the study period, which differed from other cities.
The increasing trend of Qe shown in this study indicates that PM particle size and composition are changing in ways that are causing Qe to increase. The increase in the Qe value means that even if the amount of PM is reduced by various policies, citizens do not necessarily experience or report proportional improvement in visibility and may feel that such polices have not been effective. Therefore, to increase the effect of PM reduction and make effective PM–related policies, it is necessary to consider the particle size and composition of PM as well as its mass concentration. Additional research is needed to understand the change in particle size or composition so that the cause of the increase in Qe can be identified.

Author Contributions

Conceptualization and methodology: Y.N.; Software: S.J., M.E.P. and J.S. (Juseon Shin); Validation: J.S. (Juhyeon Sim) and J.S. (Juseon Shin); Formal analysis: S.J. and N.D.; Manuscript preparation (Draft): S.J.; Manuscript review and editing: Y.N., S.J. and N.D.; Supervision: Y.N. All authors have read and agreed to the published version of the manuscript.

Funding

This work was supported by the “Graduate school of Particulate matter specialization.” of Korea Environmental Industry & Technology Institute grant, funded by the Ministry of Environment, Republic of Korea.

Institutional Review Board Statement

Not applicable.

Informed Consent Statement

Not applicable.

Data Availability Statement

The PM data used in this study are freely available through the AirKorea homepage at https://www.airkorea.or.kr/web (accessed on 18 March 2022) and the visibility and weather data used in this study are freely available through the KMA data portal at https://data.kma.go.kr/cmmn/main.do (accessed on 20 March 2022).

Acknowledgments

This work was supported by the “Graduate school of Particulate matter specialization” of Korea Environmental Industry & Technology Institute grant funded by the Ministry of Environment, Republic of Korea.

Conflicts of Interest

The authors declare no conflict of interest.

Appendix A

Table A1. Location of ground meteorological observatory (top) and PM observatory (bottom).
Table A1. Location of ground meteorological observatory (top) and PM observatory (bottom).
ProvinceCityStation NumberAddressLongitudeLatitude
Metropolitan areaSeoul10852, Songwol-gil, Jongno-gu, Seoul126.966°N37.571°E
111,12115, Deoksugung-gil, Jung-gu, Seoul126.975°N37.564°E
Suwon119276, Gwonseon-ro, Gwonseon-gu, Suwon-si, Gyeonggi-do126.983°N37.258°E
131,11168, Sinpung-ro 23beon-gil, Paldal-gu, Suwon-si, Gyeonggi-do127.011°N37.284°E
Gangwon-doChuncheon10112, Chungyeol-ro 91beon-gil, Chuncheon-si, Gangwon-do127.736°N37.903°E
132,112135, Jungang-ro, Chuncheon-si, Gangwon-do127.721°N37.876°E
Wonju114159, Dangu-ro, Wonju-si, Gangwon-do127.947°N37.338°E
632,122171, Dangu-ro, Wonju-si, Gangwon-do127.948°N37.337°E
Gyeongsang-doPohang13870, Songdo-ro, Nam-gu, Pohang-si, Gyeongsangbuk-do129.380°N36.032°E
437,114138, Daehae-ro, Nam-gu, Pohang-si, Gyeongsangbuk-do129.366°N36.019°E
Daegu14310, Hyodong-ro 2-gil, Dong-gu, Daegu128.653°N35.878°E
422,1611000, Gukchaebosang-ro, Suseong-gu, Daegu128.640°N35.865°E
Busan1595-11, Bokbyeongsan-gil 32beon-gil, Jung-gu, Busan129.032°N35.105°E
221,11210, Gwangbok-ro 55beon-gil, Jung-gu, Busan129.031°N35.100°E
Jeju-islandJeju18432, Mandeok-ro 6-gil, Jeju-si, Jeju-do126.530°N33.514°E
339,11110, Gwangyang 9-gil, Jeju-si, Jeju-do126.532°N33.500°E

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Figure 1. Location of cities studied.
Figure 1. Location of cities studied.
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Figure 2. Eight cities’ annual average and trend in visibility and PM10 2001–2020.
Figure 2. Eight cities’ annual average and trend in visibility and PM10 2001–2020.
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Figure 3. Eight cities’ annual average and trend in visibility and PM2.5 in 2015–2020.
Figure 3. Eight cities’ annual average and trend in visibility and PM2.5 in 2015–2020.
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Figure 4. Qe,10 annual average and trend 2001–2020.
Figure 4. Qe,10 annual average and trend 2001–2020.
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Figure 5. Qe,2.5 annual average and trend 2015–2020.
Figure 5. Qe,2.5 annual average and trend 2015–2020.
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Figure 6. Qe,2.5 monthly average and trend from 2015 to 2020.
Figure 6. Qe,2.5 monthly average and trend from 2015 to 2020.
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Figure 7. Change in Qe for each concentration category of PM10 and PM2.5 in each city. PM10: (a) 19–21 μg/m3 (low), (b) 69–71 μg/m3 (moderate), (c) 139–141 μg/m3 (high); PM2.5: (d) 9–11 μg/m3 (low), (e) 29–31 μg/m3 (moderate), (f) 69–71 μg/m3 (high).
Figure 7. Change in Qe for each concentration category of PM10 and PM2.5 in each city. PM10: (a) 19–21 μg/m3 (low), (b) 69–71 μg/m3 (moderate), (c) 139–141 μg/m3 (high); PM2.5: (d) 9–11 μg/m3 (low), (e) 29–31 μg/m3 (moderate), (f) 69–71 μg/m3 (high).
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Figure 8. Comparison of Qe,2.5 values from this and previous studies at wavelength 550 nm. * Used wavelength 589 nm. ** Used wavelength 525 nm.
Figure 8. Comparison of Qe,2.5 values from this and previous studies at wavelength 550 nm. * Used wavelength 589 nm. ** Used wavelength 525 nm.
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Table 1. Regional visibility, PM (PM10, PM2.5) and Qe yearly trend slope (calculated with linear regression analysis).
Table 1. Regional visibility, PM (PM10, PM2.5) and Qe yearly trend slope (calculated with linear regression analysis).
2001–20202015–2020
ProvinceCityVisibility
(km/yr)
PM10
((μg/m3)/yr)
Qe,10
((m2/g)/yr)
Visibility
(km/yr)
PM2.5
((μg/m3)/yr)
Qe,2.5
((m2/g)/yr)
Metropolitan
Area
Seoul0.04–1.860.15−0.14−0.100.41
Suwon0.09–1.140.070.53–1.060.30
Gangwon-doChuncheon0.01–1.250.06−0.61−0.291.12
Wonju−0.12−0.820.22−0.03–3.292.47
Gyeongsang-doPohang0.84–1.590.11−0.02–4.402.20
Daegu0.15−0.990.06−0.190.160.28
Busan0.04–1.280.120.11–2.341.10
Jeju-island Jeju0.12−0.39−0.08−0.09–1.980.99
Table 2. MK test and Sen’s slope of Visibility, PM10 and Qe,10 annual trends 2001–2020 (Clear trend with 95% CL for |z| > 1.96 and 99% CL for |z| > 2.57).
Table 2. MK test and Sen’s slope of Visibility, PM10 and Qe,10 annual trends 2001–2020 (Clear trend with 95% CL for |z| > 1.96 and 99% CL for |z| > 2.57).
VisibilityPM10Qe,10
ProvinceCityzpSlopezpSlopezpSlope
Metropolitan
area
Seoul0.94090.34680.0269–4.83420.0000–1.53203.14710.00160.1326
Suwon0.94550.34440.0517–3.64680.0003–1.05942.20610.02740.0610
Gangwon-doChuncheon0.07580.93960.0168–3.18170.0015–1.16881.43940.15010.0546
Wonju–2.72890.0064−0.1216–2.37900.0174−0.84402.44900.01430.2113
Gyeongsang-doPohang2.65890.00780.0833–4.33820.0000–1.63993.07870.00210.1153
Daegu2.84670.00440.1673–3.06570.0022–1.03722.29930.02150.0571
Busan1.46940.14170.0445–3.98840.0000–1.34233.49860.00050.1161
Jeju-island Jeju3.79600.00010.1278–1.71960.0855−0.4943–1.65470.0980−0.0818
Table 3. MK Test and Sen’s slope for visibility, PM2.5 and Qe,2.5 annual trend 2015–2020 (clear trend with 95% confidence level for |z| > 1.96 and 99% confidence level for |z| > 2.57). There were few data available for analysis of annual trends for Suwon and Pohang.
Table 3. MK Test and Sen’s slope for visibility, PM2.5 and Qe,2.5 annual trend 2015–2020 (clear trend with 95% confidence level for |z| > 1.96 and 99% confidence level for |z| > 2.57). There were few data available for analysis of annual trends for Suwon and Pohang.
VisibilityPM2.5Qe,2.5
ProvinceCityzpSlopezpSlopezpSlope
Metropolitan
area
Seoul−0.75150.4524−0.157401−0.06981.12720.25970.3664
Suwon010.533201–1.0639010.3035
Gangwon-doChuncheon–1.71460.0864−0.6571–1.22470.2207−0.38291.71460.08641.0276
Wonju−0.24500.8065−0.0687–2.20450.0275–3.15752.20450.02752.4609
Gyeongsang-doPohang01−0.0167–1.04450.2963–4.40761.04450.29632.1945
Daegu–1.22470.2207−0.23300.24490.80650.37140.73480.46240.3024
Busan1.50290.13290.0824–2.63010.0085–2.06902.63010.00850.6510
Jeju-island Jeju−0.37570.7071−0.1005–2.25440.0242–1.96962.25440.02421.0405
Table 4. Total Qe,10 (2001–2020), Qe,2.5 (2015–2020) with MK test and Sen’s slope.
Table 4. Total Qe,10 (2001–2020), Qe,2.5 (2015–2020) with MK test and Sen’s slope.
Qe,10 Qe,2.5
CityzpSlopezpSlope
3.4715 0.00050.07262.63010.00850.8522
20016.0 ± 3.8Data unavailable
20025.7 ± 5.3
20036.0 ± 4.6
20045.2 ± 4.4
20055.4 ± 4.7
20066.0 ± 5.0
20076.2 ± 5.6
20086.3 ± 5.5
20096.6 ± 5.7
20106.2 ± 6.6
20116.2 ± 7.4
20126.5 ± 6.2
20136.2 ± 4.5
20146.1 ± 5.1
20156.2 ± 4.611.1 ± 12.2
20166.3 ± 5.811.3 ± 9.8
20176.6 ± 3.711.7 ± 7.4
20187.3 ± 10.213.3 ± 16.5
20197.1 ± 5.713.8 ± 12.9
20207.8 ± 9.515.4 ± 16.1
Table 5. Qe,10 by city from 2001 to 2020.
Table 5. Qe,10 by city from 2001 to 2020.
Qe,10 (m2/g)
ProvinceCity20012002200320042005200620072008200920102011201220132014201520162017201820192020
Metropolitan
area
Seoul6.9 ± 4.83.6 ± 1.84.3 ± 2.34.1 ± 2.45.1 ± 3.06.3 ± 4.57.1 ± 7.27.7 ± 5.67.3 ± 6.17.3 ± 5.17.0 ± 5.47.4 ± 3.77.8 ± 6.28.1 ± 4.16.5 ± 3.05.7 ± 2.57.3 ± 3.07.9 ± 3.38.0 ± 3.57.7 ± 3.8
Suwon5.1 ± 3.16.4 ± 5.66.5 ± 4.25.2 ± 2.3 5.5 ± 2.86.1 ± 2.66.4 ± 2.86.4 ± 2.75.5 ± 2.54.9 ± 2.16.7 ± 2.96.3 ± 2.57.1 ± 3.2 7.0 ± 3.36.8 ± 3.36.9 ± 5.1
Gangwon-doChuncheon 6.0 ± 8.55.2 ± 3.94.6 ± 3.36.0 ± 9.27.4 ± 10.15.3 ± 3.66.4 ± 5.97.4 ± 7.87.0 ± 8.56.3 ± 5.56.6 ± 3.76.2 ± 3.96.3 ± 3.15.9 ± 3.35.4 ± 2.56.4 ± 3.57.5 ± 5.17.3 ± 5.4
Wonju5.6 ± 3.16.1 ± 6.94.5 ± 3.33.7 ± 2.2 6.8 ± 6.17.9 ± 9.05.5 ± 4.45.3 ± 3.46.5 ± 12.46.8 ± 18.74.3 ± 2.35.0 ± 2.44.9 ± 2.76.2 ± 6.47.6 ± 12.77.5 ± 6.59.0 ± 17.39.5 ± 13.312.0 ± 26.7
Gyeongsang-doPohang6.0 ± 3.93.9 ± 3.53.8 ± 2.13.3 ± 2.34.0 ± 3.84.8 ± 3.95.3 ± 3.76.6 ± 4.15.5 ± 3.15.7 ± 2.95.7 ± 3.45.2 ± 3.15.1 ± 2.35.9 ± 4.46.0 ± 3.16.6 ± 3.0 5.9 ± 2.66.3 ± 2.56.3 ± 2.4
Daegu6.2 ± 3.36.0 ± 3.2 5.6 ± 2.8 6.4 ± 4.16.6 ± 3.46.2 ± 2.97.2 ± 4.66.2 ± 3.26.2 ± 3.45.9 ± 2.9 6.4 ± 2.7 7.2 ± 4.26.8 ± 2.97.5 ± 4.5
Busan4.8 ± 2.8 5.0 ± 2.84.2 ± 2.53.8 ± 1.64.1 ± 1.74.3 ± 1.84.8 ± 2.35.5 ± 2.55.8 ± 3.05.9 ± 3.75.8 ± 2.75.6 ± 2.54.9 ± 2.25.4 ± 8.45.8 ± 2.85.7 ± 2.55.8 ± 2.36.4 ± 2.97.6 ± 3.9
Jeju-island Jeju7.0 ± 4.88.3 ± 6.88.7 ± 5.86.4 ± 4.86.2 ± 3.75.9 ± 3.26.6 ± 9.76.3 ± 3.78.0 ± 6.56.1 ± 4.46.9 ± 7.17.8 ± 14.06.3 ± 5.15.6 ± 7.35.7 ± 3.65.0 ± 2.45.3 ± 2.46.7 ± 2.76.5 ± 2.96.8 ± 2.5
Table 6. Qe,2.5 by city from 2015 to 2020.
Table 6. Qe,2.5 by city from 2015 to 2020.
ProvinceCityQe,2.5 (m2/g)
201520162017201820192020
Metropolitan
area
Seoul12.5 ± 7.010.5 ± 6.212.8 ± 5.914.6 ± 8.413.9 ± 6.912.9 ± 8.7
Suwon 14.1 ± 8.013.2 ± 9.014.7 ± 12.4
Gangwon-doChuncheon10.7 ± 6.810.4 ± 6.012.9 ± 10.813.9 ± 9.814.6 ± 14.1
Wonju 9.4 ± 6.110.9 ± 8.314.4 ± 23.616.1 ± 27.719.2 ± 33.8
Gyeongsang-doPohang 11.2 ± 8.414.5 ± 10.415.6 ± 10.4
Daegu13.3 ± 11.211.9 ± 6.2 15.4 ± 19.513.3 ± 10.314.0 ± 9.8
Busan8.9 ± 19.49.5 ± 6.410.2 ± 6.410.5 ± 6.111.3 ± 6.715.4 ± 9.1
Jeju-island Jeju9.4 ± 5.210.6 ± 6.610.0 ± 5.512.0 ± 5.312.6 ± 6.214.8 ± 7.0
Table 7. MK Test and Sen’s slope for monthly trends of PM2.5, Qe,2.5 during 2015–2020 (clear trend with 95% CL for |z| > 1.96 and 99% CL for |z| > 2.57).
Table 7. MK Test and Sen’s slope for monthly trends of PM2.5, Qe,2.5 during 2015–2020 (clear trend with 95% CL for |z| > 1.96 and 99% CL for |z| > 2.57).
VisibilityPM2.5Qe,2.5
ProvinceCityzpSlopezpSlopezpSlope
Metropolitan
area
Seoul−0.76320.4453−0.0077–1.17160.2414−0.03832.61050.00900.0452
Suwon3.26510.00110.0452–2.84280.0045−0.15331.81940.06890.0463
Gangwon-doChuncheon–2.26030.0238−0.0245–2.11210.0347−0.10754.35650.00000.0991
Wonju0.42930.66770.0105–3.58210.0003−0.34925.40660.00000.1797
Gyeongsang-doPohang0.19180.84790.0011–2.86120.0042−0.15223.52090.00040.1100
Daegu–1.48310.1380−0.0097−0.54230.5876−0.02272.53460.01130.0399
Busan2.03510.04180.0129–5.28130.0000−0.22575.34090.00000.1056
Jeju-island Jeju–1.06900.2851−0.0061–5.18730.0000−0.19975.64890.00000.1063
Table 8. Annual Qe trend slope for each concentration category of PM10 and PM2.5 based on linear regression analysis.
Table 8. Annual Qe trend slope for each concentration category of PM10 and PM2.5 based on linear regression analysis.
PM10PM2.5
2001–20202015–2020
Qe,10 ((m2/g)/yr)Qe,2.5 ((m2/g)/yr)
ProvinceCityLowModerateHighLowModerateHigh
19–21 μg/m369–71 μg/m3139–141 μg/m39–11 μg/m329–31 μg/m369–71 μg/m3
Metropolitan
area
Seoul−0.050.180.210.170.25−0.14
Suwon−0.080.110.17−0.07−0.68–1.35
Gangwon-doChuncheon−0.090.100.130.180.871.43
Wonju−0.020.270.330.091.050.96
Gyeongsang-doPohang−0.070.040.09−0.060.654.34
Daegu−0.090.04−0.02−0.020.150.40
Busan−0.010.050.090.140.220.23
Jeju-island Jeju−0.100.020.100.020.481.60
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Joo, S.; Dehkhoda, N.; Shin, J.; Park, M.E.; Sim, J.; Noh, Y. A Study on the Long-Term Variations in Mass Extinction Efficiency Using Visibility Data in South Korea. Remote Sens. 2022, 14, 1592. https://doi.org/10.3390/rs14071592

AMA Style

Joo S, Dehkhoda N, Shin J, Park ME, Sim J, Noh Y. A Study on the Long-Term Variations in Mass Extinction Efficiency Using Visibility Data in South Korea. Remote Sensing. 2022; 14(7):1592. https://doi.org/10.3390/rs14071592

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Joo, Sohee, Naghmeh Dehkhoda, Juseon Shin, Mi Eun Park, Juhyeon Sim, and Youngmin Noh. 2022. "A Study on the Long-Term Variations in Mass Extinction Efficiency Using Visibility Data in South Korea" Remote Sensing 14, no. 7: 1592. https://doi.org/10.3390/rs14071592

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