Biosphere–atmosphere interactions play a critical role in governing atmospheric composition, mediating the concentrations of key species such as ozone and aerosol, thereby influencing air quality and climate. The exchange of reactive trace gases and their oxidation products (both gas and particle phase) is of particular importance in this process. The FORCAsT (FORest Canopy Atmosphere Transfer) 1-D model is developed to study the emission, deposition, chemistry and transport of volatile organic compounds (VOCs) and their oxidation products in the atmosphere within and above the forest canopy. We include an equilibrium partitioning scheme, making FORCAsT one of the few canopy models currently capable of simulating the formation of secondary ...
Understanding the fate of ozone within and above forested environments is vital to assessing the ant...
A multilayer gas dry deposition model has been developed and implemented into a one-dimensional chem...
We report fluxes and dry deposition velocities for 16 atmospheric compounds above a southeastern Uni...
Biosphere-atmosphere interactions play a critical role in governing atmospheric composition, mediati...
Biosphere–atmosphere interactions play a critical role in governing atmospheric composition, mediati...
Gas-phase biogenic volatile organic compounds (BVOCs) are oxidized in the troposphere to produce sec...
Vegetation emits large quantities of biogenic volatile organic compounds (BVOC). At remote sites, th...
The concentrations and fluxes of reactive nitrogen species in the land-atmosphere system are control...
Measurements and modelling of surface / atmosphere exchange of trace gases and aerosols are used to ...
Biogenic volatile organic compounds (BVOCs) can react in the atmosphere to form organic nitrates, wh...
A one-dimensional canopy model was used to quantify the impact of photochemistry in modifying biosph...
Understanding of the atmosphere/forest canopy exchange of volatile organic compounds (VOCs) requires...
The exchange of trace gases between the biosphere and the atmosphere is an important process that co...
Abstract. Forest canopies are primary emission sources of biogenic volatile organic compounds (BVOCs...
[1] The exchange of oxidized nitrogen species (NOx) between the biosphere and atmosphere is controll...
Understanding the fate of ozone within and above forested environments is vital to assessing the ant...
A multilayer gas dry deposition model has been developed and implemented into a one-dimensional chem...
We report fluxes and dry deposition velocities for 16 atmospheric compounds above a southeastern Uni...
Biosphere-atmosphere interactions play a critical role in governing atmospheric composition, mediati...
Biosphere–atmosphere interactions play a critical role in governing atmospheric composition, mediati...
Gas-phase biogenic volatile organic compounds (BVOCs) are oxidized in the troposphere to produce sec...
Vegetation emits large quantities of biogenic volatile organic compounds (BVOC). At remote sites, th...
The concentrations and fluxes of reactive nitrogen species in the land-atmosphere system are control...
Measurements and modelling of surface / atmosphere exchange of trace gases and aerosols are used to ...
Biogenic volatile organic compounds (BVOCs) can react in the atmosphere to form organic nitrates, wh...
A one-dimensional canopy model was used to quantify the impact of photochemistry in modifying biosph...
Understanding of the atmosphere/forest canopy exchange of volatile organic compounds (VOCs) requires...
The exchange of trace gases between the biosphere and the atmosphere is an important process that co...
Abstract. Forest canopies are primary emission sources of biogenic volatile organic compounds (BVOCs...
[1] The exchange of oxidized nitrogen species (NOx) between the biosphere and atmosphere is controll...
Understanding the fate of ozone within and above forested environments is vital to assessing the ant...
A multilayer gas dry deposition model has been developed and implemented into a one-dimensional chem...
We report fluxes and dry deposition velocities for 16 atmospheric compounds above a southeastern Uni...