2017
DOI: 10.5194/acp-17-14309-2017
|View full text |Cite
|
Sign up to set email alerts
|

Boreal forest BVOC exchange: emissions versus in-canopy sinks

Abstract: Abstract. A multilayer gas dry deposition model has been developed and implemented into a one-dimensional chemical transport model SOSAA (model to Simulate the concentrations of Organic vapours, Sulphuric Acid and Aerosols) to calculate the dry deposition velocities for all the gas species included in the chemistry scheme. The new model was used to analyse in-canopy sources and sinks, including gas emissions, chemical production and loss, dry deposition, and turbulent transport of 12 featured biogenic volatile… Show more

Help me understand this report
View preprint versions

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

6
30
1

Year Published

2018
2018
2024
2024

Publication Types

Select...
6
2

Relationship

1
7

Authors

Journals

citations
Cited by 28 publications
(41 citation statements)
references
References 74 publications
6
30
1
Order By: Relevance
“…The latter also involves a potentially important role in the deposition to wet leaf surfaces (the inferred wet surface uptake resistances for the monoterpenes are ∼ 300 s m −1 , similar to values reported by Zhou et al (2017)); the MLC-CHEM uses relative humidity as a proxy for the fraction of the leaf surface being wet (Lammel, 1999;Sun et al, 2016). This results in substantially smaller estimates of canopy wetness on 17 October compared to the following days, which partly explains the simulated high α-pinene mixing ratios.…”
Section: Modelling Analysissupporting
confidence: 69%
“…The latter also involves a potentially important role in the deposition to wet leaf surfaces (the inferred wet surface uptake resistances for the monoterpenes are ∼ 300 s m −1 , similar to values reported by Zhou et al (2017)); the MLC-CHEM uses relative humidity as a proxy for the fraction of the leaf surface being wet (Lammel, 1999;Sun et al, 2016). This results in substantially smaller estimates of canopy wetness on 17 October compared to the following days, which partly explains the simulated high α-pinene mixing ratios.…”
Section: Modelling Analysissupporting
confidence: 69%
“…During intensive field campaigns, isoprene and terpene concentrations are usually investigated using proton transfer reaction mass spectrometry, a very efficient and fast technique (with a time resolution better than one second) but only providing 20 information about the sum of monoterpenes (Bouvier-Brown et al, 2009;de Gouw and Warneke, 2007;Park et al, 2014;Zhou et al, 2017, Kammer et al, 2018 and sesquiterpenes (Bouvier-Brown et al, 2009, 2007Kim et al, 2009;Park et al, 2014;Zhou et al, 2017), as it cannot distinguish individual structural isomers. If this type of instrument has recently been coupled to a fast gas-chromatography (GC) to separate monoterpenes (Materić et al, 2015), the feasibility for ambient…”
mentioning
confidence: 99%
“…Forest structure can be divided into three different layers: the forest floor, the understory and the canopy, and all of these act as sources of BVOCs. In forest stands, the canopy layer of living trees has a substantial volume and leaf area and it acts as the most important emission source for BVOCs (Zhou et al 2017), but can also act as a sink when atmospheric BVOCs such as MTs are taken up through stomata or when reaction products of rapidly reactive BVOCs such as SQTs are deposited on foliage (Zhou et al 2017). In addition to green foliage, wood, phloem and bark of trunk and branches of living trees act as important pools of stored BVOCs such as oleoresin MTs in conifer forests (Taipale et al 2011;Ghimire et al 2016).…”
Section: Bvocs Of Rhizosphere Litter and Understorymentioning
confidence: 99%