Abstract
Abstract. The CANOPEE project aims to better understand the biosphere–atmosphere exchanges of biogenic volatile organic compounds (BVOCs) in the case of Mediterranean ecosystems and the impact of in-canopy processes on the atmospheric chemical composition above the canopy. Based on an intensive field campaign, the objective of our work was to determine the chemical composition of the air inside a canopy as well as the net fluxes of reactive species between the canopy and the boundary layer. Measurements were carried out during spring 2012 at the field site of the Oak Observatory of the Observatoire de Haute Provence (O3HP) located in the southeast of France. The site is a forest ecosystem dominated by downy oak, Quercus pubescens Willd., a typical Mediterranean species which features large isoprene emission rates. Mixing ratios of isoprene, its degradation products methylvinylketone (MVK) and methacrolein (MACR) and several other oxygenated VOC (OxVOC) were measured above the canopy using an online proton transfer reaction mass spectrometer (PTR-MS), and fluxes were calculated by the disjunct eddy covariance approach. The O3HP site was found to be a very significant source of isoprene emissions, with daily maximum ambient concentrations ranging between 2–16 ppbv inside and 2–5 ppbv just above the top of the forest canopy. Significant isoprene fluxes were observed only during daytime, following diurnal cycles with midday net emission fluxes from the canopy ranging between 2.0 and 9.7 mg m−2 h1. Net isoprene normalized flux (at 30 °C, 1000 μmol quanta m−2 s−1) was estimated at 7.4 mg m−2 h−1. Evidence of direct emission of methanol was also found exhibiting maximum daytime fluxes ranging between 0.2 and 0.6 mg m−2 h−1, whereas flux values for monoterpenes and others OxVOC such as acetone and acetaldehyde were below the detection limit. The MVK+MACR-to-isoprene ratio provided useful information on the oxidation of isoprene, and is in agreement with recent findings proposing weak production yields of MVK and MACR, in remote forest regions where the NOx concentrations are low. In-canopy chemical oxidation of isoprene was found to be weak and did not seem to have a significant impact on isoprene concentrations and fluxes above the canopy.
Highlights
Volatile organic compounds (VOCs) are emitted into the atmosphere from natural sources as well as from anthropogenic sources
On 14 and 31 July followed by a new increase in the end of August (9.8 ppbv); concentrations decreased during the autumn when the leaves of the downy oak were still persistent and no significant isoprene concentration above detection limit was detected after November
We have presented atmospheric measurements at high resolution for concentrations and direct above-canopy fluxes of Biogenic VOCs (BVOCs) for a Mediterranean downy oak forest
Summary
Volatile organic compounds (VOCs) are emitted into the atmosphere from natural sources (biogenic emissions) as well as from anthropogenic sources. Monoterpenes, sesquiterpenes and oxygenated compounds, such as methanol, acetone and acetaldehyde may be important regarding atmospheric chemical processes (Guenther et al, 1995; Kesselmeier et al, 1998; Kesselmeier and Staudt, 1998; Fuentes et al, 2000; Park et al, 2013). Despite their relatively low atmospheric concentrations BVOCs are key components of tropospheric chemistry. BVOCs influence gas phase atmospheric chemistry; several studies have demonstrated that the oxidation of monoterpenes, sesquiterpenes, and, to a lesser extent, of isoprene, contributes to the formation of secondary organic aerosols (SOAs) in the troposphere (Griffin et al, 1999; Claeys et al, 2004). The contribution estimate of BVOCs to SOA formation is still rather uncertain: (Andreae and Crutzen, 1997) calculated this contribution to be in the range of 30–270 Tg year−1 whereas more recently Tsigaridis and Kanakidou (2003) estimated a smaller range of 2.5–44.5 Tg yr−1
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