In situ measurements of isoprene and monoterpenes within a south-east Asian tropical rainforest

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Abstract

Biogenic volatile organic compounds (BVOCs) emitted from tropical rainforests comprise a substantial fraction of global atmospheric VOC emissions, however there are only relatively limited measurements of these species in tropical rainforest regions. We present observations of isoprene, α-pinene, camphene, Δ-3-carene, γ-terpinene and limonene, as well as oxygenated VOCs (OVOCs) of biogenic origin such as methacrolein, in ambient air above a tropical rainforest in Malaysian Borneo during the Oxidant and Particle Photochemical Processes above a south-east Asian tropical rainforest (OP3) project in 2008. Daytime composition was dominated by isoprene, with an average mixing ratio of the order of ∼1 ppb. γ-terpinene, limonene and camphene were the most abundant monoterpenes, with average daytime mixing ratios of 102, 71 and 66 ppt respectively, and with an average monoterpene toisoprene ratio of 0.3 during sunlit hours, compared to 2.0 at night. Limonene and camphene abundances were seen to be related to both temperature and light conditions. In contrast, Î3-terpinene emission continued into the late afternoon/evening, under relatively low temperature and light conditions. The contributions of isoprene, monoterpenes and other classes of VOC to the volatile carbon budget and OH reactivity have been summarised for this rainforest location. We observe good agreement between surface and aircraft measurements of boundary layer isoprene and methacrolein above the natural rainforest, suggesting that the ground-level observations are broadly representative of isoprene emissions from this region. © 2011 Author(s).

Figures

  • Table 1. Mean average daytime VOC mixing ratios observed within the natural rainforest at Bukit Atur, and in air samples collected above the natural rainforest and oil palm plantations. In each case the range of observed daytime mixing ratios in ppt are given in brackets (5th and 95th percentiles) and the median mixing ratio is shown in curly brackets. Note that some VOCs routinely measured by the ground-based instrument, including acetaldehyde and benzene, are not reported as a result of instrumentation difficulties experienced during the OP3 field campaign.
  • Fig. 1. Correlation between isoprene mixing ratios in ambient air quantified by the independent Agilent (AG) and Perkin Elmer (PE) GCFID instruments at the Bukit Atur GAW station in April 2008. Note only mixing ratios derived from simultaneous measurements (sampling periods within ±5 min) were used for this comparison.
  • Fig. 2. Time-resolved measurements of isoprene and its oxidation product methacrolein, the monoterpenes α-pinene, camphene, 1-3- carene, limonene and γ -terpinene, methanol, and selected other VOCs thought to be of primarily anthropogenic origin (ethane, acetylene and propane) at the ground-bas d site at Bukit Atur d ring April 2008 (OP3-I) and June–July 2008 (OP3-III). Only limited monoterpene and OVOC data is shown from the first measurement period, due to instrument failures.
  • Fig. 3. Diurnal average PAR and temperature profiles and mixing ratios of isoprene, the three most abundant monoterpenes (limonene, γ -terpinene and camphene) and methacrolein. Note PAR, temperature and wind speed measurements correspond to a height of 75 m.
  • Fig. 4. Plots to show the correlations between isoprene, limonene, camphene and γ -terpinene vs. ambient air temperature and vs. PAR.
  • Table 2. Spearman’s rank correlation coefficients to demonstrate the degree of correlation between VOC mixing ratios with air temperature (◦C) and PAR (µmol m−2 s−1). Correlations with PAR are based upon 425 data pairs; temperature correlations are based on 534 data pairs (isoprene, acetylene and ethane) and 478 (monoterpenes and methacrolein).
  • Fig. 6. Average diurnal variation in the relative fractions of the individual monoterpenes α-pinene (red), camphene (grey), 1-3-carene (pink), γ -terpinene (blue) and limonene (orange), based upon measurements between 23 June–20 July.
  • Fig. 5. Correlations between the ambient isoprene mixing ratio with, (a) PAR and (b) temperature, in the morning (between midnight and midday – green circles) and in the afternoon (between midday and midnight – orange circles).

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Jones, C. E., Hopkins, J. R., & Lewis, A. C. (2011). In situ measurements of isoprene and monoterpenes within a south-east Asian tropical rainforest. Atmospheric Chemistry and Physics, 11(14), 6971–6984. https://doi.org/10.5194/acp-11-6971-2011

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