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Observed versus simulated OH reactivity during Korus-AQ campaign

Implications for emission inventory and chemical environment in East Asia

Bibliographic Data

ID19568650
AuthorsHyeonmin Kim (0000-0003-4715-0893, Seoul National University), Rokjin J Park (0000-0001-8922-0234, Seoul National University), Saewung Kim (0000-0003-4847-3272, University of California, Irvine), W H Brune (0000-0002-1609-4051, Pennsylvania State University), Glenn S Diskin (0000-0002-3617-0269, Langley Research Center), Amy Fried (0000-0002-5230-3527, Institute of Arctic and Alpine Research), Alan Fried, Samuel R Hall (0000-0002-2060-7112, NSF National Center for Atmospheric Research), A J Weinheimer (0000-0001-6175-8286, NSF National Center for Atmospheric Research), Paul Wennberg, P O Wennberg (0000-0002-6126-3854, California Institute of Technology), Armin Wisthaler (0000-0001-5050-3018, University of Oslo), D R Blake (0000-0002-8283-5014, University of California, Irvine), Kirk Ullmann (0000-0002-4724-9634, NSF National Center for Atmospheric Research)
Year2022
Volume10
Issue1
Publication date2022-09-08
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueElementa Science of the Anthropocene (JOURNAL)
Journal identifiersISSN: 2325-1026 • E-ISSN: 2325-1026
PublisherUniversity of California Press (PUBLISHER • US)
DOI10.1525/elementa.2022.00030
OpenAlexW4295886248
LanguageEN
Citations received2
References cited93

We present a holistic examination of tropospheric OH reactivity (OHR) in South Korea using comprehensive NASA DC-8 airborne measurements collected during the Korea–United States Air Quality field study and chemical transport models. The observed total OHR (tOHR) averaged in the planetary boundary layer (PBL, <2.0 km) and free troposphere was 5.2 s−1 and 2.0 s−1 during the campaign, respectively. These values were higher than the calculated OHR (cOHR, 3.4 s−1, 1.0 s−1) derived from trace-gas observations, indicating missing OHR fractions in the PBL and free troposphere of 35% and 50%, respectively. Incorporating nonobserved secondary species from the observationally constrained box model increased cOHR to 4.0 s−1 in the PBL and 1.3 s−1 in the free troposphere. Simulated OHR (sOHR, 2.7 s−1, 0.8 s−1) was substantially lower than both tOHR and cOHR by as much as 60%. This underestimate was substantial in the free troposphere and marine boundary layer of the marginal sea (Yellow Sea). We then discuss the potential causes of unaccounted OHR. First, we suggest improving the accuracy of tropospheric reaction kinetics, which vary significantly in the available literature. Second, underestimated emissions of anthropogenic CO and oxygenated volatile organic compounds in East Asia contributed to the discrepancy between tOHR and sOHR. In addition, oxygenated and biogenic volatile organic compounds emitted from the marginal sea may contribute substantially to the regional OHR. Typical chemical transport models underestimate these sources, leading to a large missing OHR fraction. Despite this discrepancy, we found that simulated OH concentrations were comparable with those observed during the campaign because of slow OH recycling rates in the models; therefore, the models predicted less formation of photochemical oxidation products such as ozone

Air quality index · Atmospheric sciences · Boundary layer · Box model · Chemical transport model · Climatology · East Asia · Geography · Meteorology · Photochemistry · Physics · Planetary boundary layer · Thermodynamics · Trace gas · Troposphere · Air Quality and Health Impacts · Atmospheric chemistry and aerosols · Atmospheric Ozone and Climate · Chemistry · Environmental Science · Environmental Chemistry · Geology

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Unique citing works2
Citations per year2
Citation span2025 - 2026 (2)
Citation velocitycurrent
Highly citedNo
Citation typesNeutral: 2

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