Top-down estimates of anthropogenic VOC emissions in South Korea using formaldehyde vertical column densities from aircraft during the KORUS-AQ campaign

Author:

Kwon Hyeong-Ahn12,Park Rokjin J.1,Oak Yujin J.1,Nowlan Caroline R.3,Janz Scott J.4,Kowalewski Matthew G.4,Fried Alan5,Walega James5,Bates Kelvin H.6,Choi Jinkyul5,Blake Donald R.7,Wisthaler Armin89,Woo Jung-Hun10

Affiliation:

1. School of Earth and Environmental Sciences, Seoul National University, Seoul, Republic of Korea

2. Now at: Atomic and Molecular Physics Division, Harvard-Smithsonian Center for Astrophysics, Cambridge, MA, USA

3. Atomic and Molecular Physics Division, Harvard-Smithsonian Center for Astrophysics, Cambridge, MA, USA

4. Atmospheric Chemistry and Dynamics Laboratory, National Aeronautics and Space Administration (NASA) Goddard Space Flight Center, Greenbelt, MD, USA

5. Institute of Arctic and Alpine Research, University of Colorado Boulder, Boulder, CO, USA

6. Harvard John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA

7. Department of Chemistry, University of California at Irvine, Irvine, CA, USA

8. Department of Chemistry, University of Oslo, Oslo, Norway

9. Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck, Austria

10. Department of Advanced Technology Fusion, Konkuk University, Seoul, Republic of Korea

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.

Publisher

University of California Press

Subject

Atmospheric Science,Geology,Geotechnical Engineering and Engineering Geology,Ecology,Environmental Engineering,Oceanography

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