Investigation of a potential HCHO measurement artifact from ISOPOOH

dc.contributor.authorSt. Clair, Jason
dc.contributor.authorRivera-Rios, Jean C.
dc.contributor.authorCrounse, John D.
dc.contributor.authorPraske, Eric
dc.contributor.authorKim, Michelle J.
dc.contributor.authorWolfe, Glenn
dc.contributor.authorKeutsch, Frank N.
dc.contributor.authorWennberg, Paul O.
dc.contributor.authorHanisco, Thomas F.
dc.date.accessioned2020-06-17T15:59:25Z
dc.date.available2020-06-17T15:59:25Z
dc.date.issued2016-09-16
dc.description.abstractRecent laboratory experiments have shown that a first generation isoprene oxidation product, ISOPOOH, can decompose to methyl vinyl ketone (MVK) and methacrolein (MACR) on instrument surfaces, leading to overestimates of MVK and MACR concentrations. Formaldehyde (HCHO) was suggested as a decomposition co-product, raising concern that in situ HCHO measurements may also be affected by an ISOPOOH interference. The HCHO measurement artifact from ISOPOOH for the NASA In Situ Airborne Formaldehyde instrument (ISAF) was investigated for the two major ISOPOOH isomers, (1,2)-ISOPOOH and (4,3)-ISOPOOH, under dry and humid conditions. The dry conversion of ISOPOOH to HCHO was 3 ± 2 % and 6 ± 4 % for (1,2)-ISOPOOH and (4,3)-ISOPOOH, respectively. Under humid (relative humidity of 40–60 %) conditions, conversion to HCHO was 6 ± 4 % for (1,2)-ISOPOOH and 10 ± 5 % for (4,3)-ISOPOOH. The measurement artifact caused by conversion of ISOPOOH to HCHO in the ISAF instrument was estimated for data obtained on the 6 September 2013 flight of the Studies of Emissions and Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys (SEAC⁴RS) campaign. Prompt ISOPOOH conversion to HCHO was the source of < 4 % of the observed HCHO, including in the high-isoprene boundary layer. Time-delayed conversion, where previous exposure to ISOPOOH affects measured HCHO later in the flight, was conservatively estimated to be < 10 % of observed HCHO, and is significant only when high ISOPOOH sampling periods immediately precede periods of low HCHO.en_US
dc.description.sponsorshipF. N. Keutsch and J. C. RiveraRios were supported by the National Science Foundation (AGS 1628491, 1628530, 1247421, 1321987). J. M. St. Clair, G. M. Wolfe, and T. F. Hanisco were supported by NASA (NNH12ZDA001N-UACO). M. J. Kim was supported by the National Science Foundation (AGS PRF 1524860).en_US
dc.description.urihttps://www.atmos-meas-tech.net/9/4561/2016/en_US
dc.format.extent8 pagesen_US
dc.genrejournal articlesen_US
dc.identifierdoi:10.13016/m2hp1r-qpwa
dc.identifier.citation: St. Clair, J. M., Rivera-Rios, J. C., Crounse, J. D., Praske, E., Kim, M. J., Wolfe, G. M., Keutsch, F. N., Wennberg, P. O., and Hanisco, T. F.: Investigation of a potential HCHO measurement artifact from ISOPOOH, Atmos. Meas. Tech., 9, 4561–4568, https://doi.org/10.5194/amt-9-4561-2016, 2016.en_US
dc.identifier.urihttps://doi.org/10.5194/amt-9-4561-2016
dc.identifier.urihttp://hdl.handle.net/11603/18910
dc.language.isoen_USen_US
dc.publisherCopernicus Publicationsen_US
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Joint Center for Earth Systems Technology
dc.relation.ispartofUMBC Faculty Collection
dc.relation.ispartofUMBC Physics Department
dc.rightsThis item is likely protected under Title 17 of the U.S. Copyright Law. Unless on a Creative Commons license, for uses protected by Copyright Law, contact the copyright holder or the author.
dc.rightsAttribution 3.0 Unported*
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/*
dc.titleInvestigation of a potential HCHO measurement artifact from ISOPOOHen_US
dc.typeTexten_US

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