The role of a suburban forest in controlling vertical trace gas and OH reactivity distributions - a case study for the Seoul metropolitan area
Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
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The role of a suburban forest in controlling vertical trace gas and OH reactivity distributions - a case study for the Seoul metropolitan area. / Kim, Saewung; Seco, Roger; Gu, Dasa; Sanchez, Dianne; Jeong, Daun; Guenther, Alex B.; Lee, Youngro; Mak, John E.; Su, Luping; Kim, Dan Bi; Lee, Youngjae; Ahn, Joon-Young; Mcgee, Tom; Sullivan, John; Long, Russell; Brune, William H.; Thames, Alexander; Wisthaler, Armin; Müller, Markus; Mikoviny, Thomas; Weinheimer, Andy; Yang, Melissa; Woo, Jung-Hun; Kim, Soyoung; Park, Hyunjoo.
I: Faraday Discussions, Bind 226, 2021, s. 537-550.Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
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T1 - The role of a suburban forest in controlling vertical trace gas and OH reactivity distributions - a case study for the Seoul metropolitan area
AU - Kim, Saewung
AU - Seco, Roger
AU - Gu, Dasa
AU - Sanchez, Dianne
AU - Jeong, Daun
AU - Guenther, Alex B.
AU - Lee, Youngro
AU - Mak, John E.
AU - Su, Luping
AU - Kim, Dan Bi
AU - Lee, Youngjae
AU - Ahn, Joon-Young
AU - Mcgee, Tom
AU - Sullivan, John
AU - Long, Russell
AU - Brune, William H.
AU - Thames, Alexander
AU - Wisthaler, Armin
AU - Müller, Markus
AU - Mikoviny, Thomas
AU - Weinheimer, Andy
AU - Yang, Melissa
AU - Woo, Jung-Hun
AU - Kim, Soyoung
AU - Park, Hyunjoo
PY - 2021
Y1 - 2021
N2 - We present trace gas vertical profiles observed by instruments on the NASA DC-8 and at a ground site during the Korea-US air quality study (KORUS) field campaign in May to June 2016. We focus on the region near the Seoul metropolitan area and its surroundings where both anthropogenic and natural emission sources play an important role in local photochemistry. Integrating ground and airborne observations is the major research goal of many atmospheric chemistry field campaigns. Although airborne platforms typically aim to sample from near surface to the free troposphere, it is difficult to fly very close to the surface especially in environments with complex terrain or a populated area. A detailed analysis integrating ground and airborne observations associated with specific concentration footprints indicates that reactive trace gases are quickly oxidized below an altitude of 700 m. The total OH reactivity profile has a rapid decay in the lower part of troposphere from surface to the lowest altitude (700 m) sampled by the NASA DC-8. The decay rate is close to that of very reactive biogenic volatile organic compounds such as monoterpenes. Therefore, we argue that photochemical processes in the bottom of the boundary layer, below the typical altitude of aircraft sampling, should be thoroughly investigated to properly assess ozone and secondary aerosol formation. This journal is
AB - We present trace gas vertical profiles observed by instruments on the NASA DC-8 and at a ground site during the Korea-US air quality study (KORUS) field campaign in May to June 2016. We focus on the region near the Seoul metropolitan area and its surroundings where both anthropogenic and natural emission sources play an important role in local photochemistry. Integrating ground and airborne observations is the major research goal of many atmospheric chemistry field campaigns. Although airborne platforms typically aim to sample from near surface to the free troposphere, it is difficult to fly very close to the surface especially in environments with complex terrain or a populated area. A detailed analysis integrating ground and airborne observations associated with specific concentration footprints indicates that reactive trace gases are quickly oxidized below an altitude of 700 m. The total OH reactivity profile has a rapid decay in the lower part of troposphere from surface to the lowest altitude (700 m) sampled by the NASA DC-8. The decay rate is close to that of very reactive biogenic volatile organic compounds such as monoterpenes. Therefore, we argue that photochemical processes in the bottom of the boundary layer, below the typical altitude of aircraft sampling, should be thoroughly investigated to properly assess ozone and secondary aerosol formation. This journal is
U2 - 10.1039/d0fd00081g
DO - 10.1039/d0fd00081g
M3 - Journal article
C2 - 33346290
AN - SCOPUS:85103249449
VL - 226
SP - 537
EP - 550
JO - Faraday Discussions
JF - Faraday Discussions
SN - 1359-6640
ER -
ID: 259494561