Slow decreasing tendency of fine particles compared to coarse particles associated with recent hot summers in Seoul, Korea

Greem Lee, Hye Ryun Oh, Chang Hoi Ho, Doo Sun R. Park, Jinwon Kim, Lim Seok Chang, Jae Bum Lee, Jinsoo Choi, Minyoung Sung

Research output: Contribution to journalArticlepeer-review

10 Scopus citations

Abstract

In Seoul, South Korea, particulate matters (PMs) significantly decreased for the period 2005–2015 in concert with the implementation of air pollution reduction policies. This study reveals that PM with a diameter smaller than 2.5 μm (PM2.5) has a slower decreasing tendency than PM in the 2.5–10-μm range (PM2.5-10) during summer and that this discrepancy is attributable to the large increase in the summer surface air temperature for the analysis period (0.13°C year–1). During the daytime, especially in the afternoon when the hourly surface air temperature and its increasing rate are high, the difference between the decreasing rates of PM2.5 and PM2.5-10 is pronounced. The slower decrease in PM2.5 compared to PM2.5-10 likely results from the secondary PM2.5 formation being accelerated by the increase in the surface air temperature. Other atmospheric variables that can affect concentrations of PMs, such as insolation, relative humidity, precipitation, wind speed, and sea-level pressure, do not show a meaningful relationship with the discrepancy in the decreasing tendency between the two PMs. Our finding emphasizes the necessity of continuous monitoring and analysis of long-term variability in concentrations of PMs and related meteorological conditions, and the independent establishment of reduction policies for PM2.5 and PM2.5-10 to prepare for anthropogenic climate change and the subsequent air quality change.

Original languageEnglish
Pages (from-to)2185-2194
Number of pages10
JournalAerosol and Air Quality Research
Volume18
Issue number9
DOIs
StatePublished - Sep 2018

Bibliographical note

Publisher Copyright:
© Taiwan Association for Aerosol Research.

Keywords

  • PM
  • PM
  • Secondary formation
  • Surface air temperature
  • Urban area

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