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dc.contributor.authorSchulze, Benjamin C.
Wallace, Henry W.
Flynn, James H.
Lefer, Barry L.
Erickson, Matt H.
Jobson, B. Tom
Dusanter, Sebastien
Griffith, Stephen M.
Hansen, Robert F.
Stevens, Philip S.
VanReken, Timothy
Griffin, Robert J.
dc.date.accessioned 2017-03-07T17:07:15Z
dc.date.available 2017-03-07T17:07:15Z
dc.date.issued 2017
dc.identifier.citation Schulze, Benjamin C., Wallace, Henry W., Flynn, James H., et al.. "Differences in BVOC oxidation and SOA formation above and below the forest canopy." Atmospheric Chemistry and Physics, 17, (2017) Copernicus Publications on behalf of the European Geosciences Union: 1828. http://dx.doi.org/10.5194/acp-17-1805-2017.
dc.identifier.urihttps://hdl.handle.net/1911/94020
dc.description.abstract Gas-phase biogenic volatile organic compounds (BVOCs) are oxidized in the troposphere to produce secondary pollutants such as ozone (O3), organic nitrates (RONO2), and secondary organic aerosol (SOA). Two coupled zero-dimensional models have been used to investigate differences in oxidation and SOA production from isoprene and α-pinene, especially with respect to the nitrate radical (NO3), above and below a forest canopy in rural Michigan. In both modeled environments (above and below the canopy), NO3 mixing ratios are relatively small (< 0.5 pptv); however, daytime (08:00–20:00 LT) mixing ratios below the canopy are 2 to 3 times larger than those above. As a result of this difference, NO3 contributes 12 % of total daytime α-pinene oxidation below the canopy while only contributing 4 % above. Increasing background pollutant levels to simulate a more polluted suburban or peri-urban forest environment increases the average contribution of NO3 to daytime below-canopy α-pinene oxidation to 32 %. Gas-phase RONO2 produced through NO3 oxidation undergoes net transport upward from the below-canopy environment during the day, and this transport contributes up to 30 % of total NO3-derived RONO2 production above the canopy in the morning (∼ 07:00). Modeled SOA mass loadings above and below the canopy ultimately differ by less than 0.5 µg m−3, and extremely low-volatility organic compounds dominate SOA composition. Lower temperatures below the canopy cause increased partitioning of semi-volatile gas-phase products to the particle phase and up to 35 % larger SOA mass loadings of these products relative to above the canopy in the model. Including transport between above- and below-canopy environments increases above-canopy NO3-derived α-pinene RONO2 SOA mass by as much as 45 %, suggesting that below-canopy chemical processes substantially influence above-canopy SOA mass loadings, especially with regard to monoterpene-derived RONO2.
dc.language.iso eng
dc.publisher Copernicus Publications on behalf of the European Geosciences Union
dc.rights This work is distributed under the Creative Commons Attribution 3.0 License.
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/us/
dc.title Differences in BVOC oxidation and SOA formation above and below the forest canopy
dc.type Journal article
dc.citation.journalTitle Atmospheric Chemistry and Physics
dc.citation.volumeNumber 17
dc.type.dcmi Text
dc.identifier.doihttp://dx.doi.org/10.5194/acp-17-1805-2017
dc.type.publication publisher version
dc.citation.firstpage 1828
dc.citation.articleNumber 1805


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