Status: this preprint was under review for the journal ACP but the revision was not accepted.
Observations of total peroxy nitrates and total alkyl nitrates during the OP3 campaign: isoprene nitrate chemistry above a south-east Asian tropical rain forest
E. Aruffo,P. Di Carlo,C. Dari-Salisburgo,F. Biancofiore,F. Giammaria,J. Lee,S. Moller,M. J. Evans,J. R. Hopkins,C. Jones,A. R. MacKenzie,and C. N. Hewitt
Abstract. Measurements of total peroxy nitrates (ΣRO2NO2, ΣPNs), total alkyl nitrates (ΣRONO2, ΣANs) and nitrogen dioxide (NO2) were made above the surface of a Malaysian tropical rain forest in Borneo, using a laser-induced fluorescence instrument developed at the University of L'Aquila (Italy). This new instrument uses the direct excitation of NO2 at 532 nm in order to measure its concentrations detecting by the NO2 fluorescence at wavelengths longer than 610 nm. ΣPNs and ΣANs are indirectly measured after their thermal dissociation into NO2. Observations showed enhanced levels of NO2 during nighttime, an increase of ΣPNs during the afternoon and almost no evident diurnal cycle of ΣANs. The diurnal maximums of 200 pptv for ΣPNs and ΣANs are well below the peaks reported in other forest sites. A box model constrained with measured species, reproduces well the observed ΣPNs, but overestimates ΣANs concentrations. The reason of this model-observation discrepancy could be a wrong parameterization in the isoprene nitrates (INs) chemistry mechanism. Sensitivity tests show that: (1) reducing the yield of INs from the reaction of peroxy nitrates with NO to almost the lowest values reported in literature (5%), (2) reducing the INs recycling to 70% and (3) keeping the INs dry deposition at 4 cm s−1, improve the agreement between modelled and measured ΣANs of 20% on average. These results imply that in the tropical rain forest, even if ΣPNs and ΣANs concentrations are lower than those observed in other North American forests, the yield and dry deposition of INs are similar. Another comparable result is that in the INs oxidation its recycling dominates with only a 30% release of NO2, which has implications on tropospheric ozone production and aerosol budget.
Received: 29 Dec 2011 – Discussion started: 10 Feb 2012
Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
E. Aruffo,P. Di Carlo,C. Dari-Salisburgo,F. Biancofiore,F. Giammaria,J. Lee,S. Moller,M. J. Evans,J. R. Hopkins,C. Jones,A. R. MacKenzie,and C. N. Hewitt
E. Aruffo,P. Di Carlo,C. Dari-Salisburgo,F. Biancofiore,F. Giammaria,J. Lee,S. Moller,M. J. Evans,J. R. Hopkins,C. Jones,A. R. MacKenzie,and C. N. Hewitt
E. Aruffo,P. Di Carlo,C. Dari-Salisburgo,F. Biancofiore,F. Giammaria,J. Lee,S. Moller,M. J. Evans,J. R. Hopkins,C. Jones,A. R. MacKenzie,and C. N. Hewitt
Viewed
Total article views: 2,108 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,489
459
160
2,108
144
140
HTML: 1,489
PDF: 459
XML: 160
Total: 2,108
BibTeX: 144
EndNote: 140
Views and downloads (calculated since 01 Feb 2013)
Cumulative views and downloads
(calculated since 01 Feb 2013)
Saved
Latest update: 21 Nov 2024
E. Aruffo
Center of Excellence CETEMPS Universita' degli studi di L'Aquila, Via Vetoio, Coppito, L'Aquila, Italy
Dipartimento di Fisica, Universita' degli studi di L'Aquila, Via Vetoio, Coppito, L'Aquila, Italy
P. Di Carlo
Center of Excellence CETEMPS Universita' degli studi di L'Aquila, Via Vetoio, Coppito, L'Aquila, Italy
Dipartimento di Fisica, Universita' degli studi di L'Aquila, Via Vetoio, Coppito, L'Aquila, Italy
C. Dari-Salisburgo
Center of Excellence CETEMPS Universita' degli studi di L'Aquila, Via Vetoio, Coppito, L'Aquila, Italy
F. Biancofiore
Center of Excellence CETEMPS Universita' degli studi di L'Aquila, Via Vetoio, Coppito, L'Aquila, Italy
Dipartimento di Chimica, Ingegneria Chimica e Materiali, Universita' degli studi di L'Aquila, Via Vetoio, Coppito, L'Aquila, Italy
F. Giammaria
Dipartimento di Fisica, Universita' degli studi di L'Aquila, Via Vetoio, Coppito, L'Aquila, Italy
J. Lee
Departement of Chemistry, University of York, York, YO10 5DD, UK
National Centre for Atmospheric Science, Department of Chemistry, University of York, York, YO10 5DD, UK
S. Moller
Departement of Chemistry, University of York, York, YO10 5DD, UK
M. J. Evans
Institute for Climate and Atmospheric Science, School of Earth and the Environment, University of Leeds, LS28WE, UK
J. R. Hopkins
Departement of Chemistry, University of York, York, YO10 5DD, UK
National Centre for Atmospheric Science, Department of Chemistry, University of York, York, YO10 5DD, UK
C. Jones
Departement of Chemistry, University of York, York, YO10 5DD, UK
A. R. MacKenzie
Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, UK
C. N. Hewitt
Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, UK