Fluxes of CO2 and isoprenoids were measured for the first time in Stipa tenacissima L (alfa grass), a perennial tussock grass dominant in the driest areas of Europe. In addition, we studied how those fluxes were influenced by environmental conditions, leaf ontogeny and UV radiation and compared emission rates in two contrasting seasons: summer when plants are mostly inactive and autumn, the growing season in this region. Leaf ontogeny significantly affected both photosynthesis and isoprenoids emission. Isoprene emission was positively correlated with photosynthesis, although a low isoprene emission was detected in brown leaves with a net carbon loss. Moreover, leaves with a significant lower photosynthesis emitted only monoterpenes, while at higher photosynthetic rates also isoprene was produced. Ambient UV radiation uncoupled photosynthesis and isoprene emission.It is speculated that alfa grass represent an exception from the general rules governing plant isoprenoid emitters.

Thirteen secondary organic aerosol (SOA) tracers of isoprene, monoterpenes and sesquiterpenes were measured for PM₂.₅ aerosols collected at the summit of Mt. Wuyi (1139 m, a.s.l.), to investigate their seasonality and formation mechanism. Concentrations of the isoprene and monoterpene SOA tracers were much higher in summer than those in other seasons. In contrast, β-caryophyllinic acid was found to be the lowest in summer. Concentrations of those BSOA tracers showed a positive correlation with temperature (R² = 0.52–0.70), and a negative correlation with relative humidity (R² = 0.43–0.78). Moreover, thermodynamic model (i.e., ISORROPIA-II) calculation results showed that acidity conditions are favorable for BSOA formation. Robust linear correlations between the BSOA tracers and anthropogenic pollutants such as SO₂ (R² = 0.53–0.7) and NO₂ (R² = 0.37–0.54) were observed for all the samples, suggesting that SO₂ and NOx can enhance BSOA production in the remote mountain area of southeast China, which is related to an acid-catalyzed heterogeneous chemistry. Moreover, we also found a significant correlation between the concentrations of the BSOA tracers and levoglucosan especially for β-caryophyllinic acid, indicating that biomass burning plumes from the distant lowland regions could influence the production of BSOA in the mountain free troposphere. Our results clearly demonstrated that anthropogenic emissions in China could enhance BSOA formation in the distant mountain regions.

Contributed Measurements of BVOC emissions, meteorological parameters, and solar radiation were carried out in a temperate forest, China during the summer seasons in 2010 and 2011. Terpenoid emissions were measured using the Relaxed Eddy Accumulation (REA) technique on an above-canopy tower. Isoprene contributed 79.1% and 82.0% of terpenoid emissions in 2010 and 2011 summer. The monoterpene emissions were dominated by α–pinene, contributing 6.3% and 12.2% of the total terpenoid emissions in 2010 and 2011 summer. Terpenoid emissions exhibited strong diurnal variations. Isoprene and monoterpene emissions maxima typically occurred a few hours after the noon PAR peak and coincided with the daily temperature maximum. During 2011 summer, the mean isoprene emission flux (mg m–2 h–1) was 0.889, mean total monoterpene emission flux was 0.143. Emission factors, representing the emission expected at a temperature of 30 °C, for this site were 0.32mg m–2 h–1 for total monoterpenes and 4.3mg m–2 h–1 for isoprene. The observations were used to evaluate the isoprene and monoterpene emission magnitude and variability predicted by the MEGANv2.1 model. Canopy scale isoprene and monoterpene emission factors based on these observations fall within the range of emission factors assigned to locations within 50km of the site by the MEGANv2.1 emission model. When using the site specific landcover data for the site, the measured emission factors are 12% for isoprene and 20% for monoterpenes lower than the MEGANv2.1 emission factors. MEGANv2.1 predicts that variations in light intensity should result in significant changes in isoprene emissions during the study but this was not evident in the observations. Observed diurnal, seasonal and interannual variations in isoprene and monoterpene emissions were strongly correlated with air temperature which was the dominant driving variable for MEGANv2.1 during the study period. The observed temperature response for isoprene and monoterpenes is similar to the temperature sensitivity of the MEGANv2.1 response functions.

Une estimation des emissions biogeniques annuelles de composes organiques volatils (COV) non methaniques dues a la couverture forestiere en France a ete realisee. Trente-deux especes d'arbres representant 98 % de la foret francaise ont ete retenues pour l'estimation. Celle-ci a porte sur un reseau constitue de 93 mailles (departements) de 75 km x 75 km de dimensions moyennes. On a affecte des taux d'emission et des densites de biomasse foliaire specifiques a chacune des 32 especes. Les variables micrometeorologiques (temperatures, intensites lumineuses) ont ete collectees pour l'ensemble des departements francais. Un effort a ete fait pour utiliser, dans les algorithmes de calcul de "Guenther" des facteurs emissifs specifiques aux especes poussant en France ou bien dans les pays limitrophes de celle-ci. Sur les cinq annees (1994-1998) de l'etude, on a calcule la moyenne annuelle des emissions d'isoprene, de monoterpenes et autres composes organiques volatils (ACOV) a l'echelle des departements et de la France. Sur le plan national, l'isoprene dont l'emission estimee est de 457 kt/an represente environ 49 % de l'emission totale, alors que les monoterpenes avec 350 kt/an, et les ACOV avec 129 kt/an representent respectivement 37 % et 14 % du total. L'emission biogenique annuelle de COV en France represente sensiblement la moitie de la source anthropique. Cependant, dans certaines regions (mediterraneennes), les emissions naturelles peuvent largement depasser durant certaines periodes les emissions anthropiques. Notons que l'ensemble de ces resultats demeure empreint d'une grande incertitude, puisque les estimations effectuees sont proposees avec des facteurs correctifs qui peuvent atteindre des valeurs comprises entre 4 et 7