Abstract

Nonmethane volatile organic compounds (NMVOCs) result in ozone and aerosol production that adversely affects the environment and human health. For modeling purposes, anthropogenic NMVOC emissions have been typically compiled using the “bottom-up” approach. To minimize uncertainties of the bottom-up emission inventory, “top-down” NMVOC emissions can be estimated using formaldehyde (HCHO) observations. In this study, HCHO vertical column densities (VCDs) obtained from the Geostationary Trace gas and Aerosol Sensor Optimization spectrometer during the Korea–United States Air Quality campaign were used to constrain anthropogenic volatile organic compound (AVOC) emissions in South Korea. Estimated top-down AVOC emissions differed from those of the up-to-date bottom-up inventory over major anthropogenic source regions by factors of 1.0 ± 0.4 to 6.9 ± 3.9. Our evaluation using a 3D chemical transport model indicates that simulated HCHO mixing ratios using the top-down estimates were in better agreement with observations onboard the DC-8 aircraft during the campaign relative to those with the bottom-up emission, showing a decrease in model bias from –25% to –13%. The top-down analysis used in this study, however, has some limitations related to the use of HCHO yields, background HCHO columns, and AVOC speciation in the bottom-up inventory, resulting in uncertainties in the AVOC emission estimates. Our attempt to constrain diurnal variations of the AVOC emissions using the aircraft HCHO VCDs was compromised by infrequent aircraft observations over the same source regions. These limitations can be overcome with geostationary satellite observations by providing hourly HCHO VCDs.

Highlights

  • Nonmethane volatile organic compounds (NMVOCs) are emitted by biogenic and anthropogenic activities and contribute to ozone production and the formation of secondary organic aerosols (Sillman, 1999; Kanakidou et al, 2005)

  • We explore the future application of HCHO observations from geostationary satellites by examining the diurnal variation in anthropogenic volatile organic compound (AVOC) emissions

  • We found that our top-down estimate in Daesan is higher than the result of Fried et al (2020) who conducted a top-down estimate of VOC emissions focusing on the Daesan petrochemical complexes using their HCHO observations aboard the DC-8 aircraft

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Summary

Introduction

Nonmethane volatile organic compounds (NMVOCs) are emitted by biogenic and anthropogenic activities and contribute to ozone production and the formation of secondary organic aerosols (Sillman, 1999; Kanakidou et al, 2005). We used 10 m winds from the GEOS-FP meteorological data to calculate the air residence time over source regions (Figure 2) where AVOC emissions were estimated.

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