Small pollutant concentration gradients between levels above a plant canopy result in large uncertainties in estimated air–surface exchange fluxes when using existing micrometeorological gradient methods, including the aerodynamic gradient method (AGM) and the modified Bowen ratio method (MBR). A modified micrometeorological gradient method (MGM) is proposed in this study for estimating O<sub>3</sub> dry deposition fluxes over a forest canopy using concentration gradients between a level above and a level below the canopy top, taking advantage of relatively large gradients between these levels due to significant pollutant uptake in the top layers of the canopy. The new method is compared with the AGM and MBR methods and is also evaluated us...
Understanding if and how the spatial and temporal variability of the surrounding environment affects...
Ammonia fluxes were measured semi-continuously over oilseed rape (Brassica napus) as part of the EXA...
New micrometeorological measurements of small (0.1–0.2 μm diameter) aerosol particle fluxes using th...
Dry deposition fluxes of sulphate and nitrate have been determined over a coniferous canopy using th...
The dry deposition flux of NH3 to coniferous forest was determined by the micrometeorological gradie...
ised f y req Agricultural and Forest Meteorologymade above the treetops, as well as often within the...
Between June and September 2002, the fluxes of carbon dioxide (CO2) and ozone (O3), and nitrogen oxi...
The objective of the study was to measure the size dependence of cloudwater deposition and associate...
Ozone flux measurements over vegetation are important to estimate surface losses and ozone uptake by...
The failure of the Monin–Obukhov Similarity Theory (MOST) in the roughness sublayer is a major probl...
The Multilayer Model (MLM) has been used for many years to infer dry deposition fluxes from measured...
Accurate CO2 concentration gradient measurements are needed for the computation of advective flux te...
Since November 1992 continuous vertical concentration gradients of SO2, NO2 and NH3 as well as relev...
Quantification of the surface-atmosphere exchange of trace gases is recognized as an essential prere...
Accurate CO2 concentration gradient measurements are needed for the computation of advective flux te...
Understanding if and how the spatial and temporal variability of the surrounding environment affects...
Ammonia fluxes were measured semi-continuously over oilseed rape (Brassica napus) as part of the EXA...
New micrometeorological measurements of small (0.1–0.2 μm diameter) aerosol particle fluxes using th...
Dry deposition fluxes of sulphate and nitrate have been determined over a coniferous canopy using th...
The dry deposition flux of NH3 to coniferous forest was determined by the micrometeorological gradie...
ised f y req Agricultural and Forest Meteorologymade above the treetops, as well as often within the...
Between June and September 2002, the fluxes of carbon dioxide (CO2) and ozone (O3), and nitrogen oxi...
The objective of the study was to measure the size dependence of cloudwater deposition and associate...
Ozone flux measurements over vegetation are important to estimate surface losses and ozone uptake by...
The failure of the Monin–Obukhov Similarity Theory (MOST) in the roughness sublayer is a major probl...
The Multilayer Model (MLM) has been used for many years to infer dry deposition fluxes from measured...
Accurate CO2 concentration gradient measurements are needed for the computation of advective flux te...
Since November 1992 continuous vertical concentration gradients of SO2, NO2 and NH3 as well as relev...
Quantification of the surface-atmosphere exchange of trace gases is recognized as an essential prere...
Accurate CO2 concentration gradient measurements are needed for the computation of advective flux te...
Understanding if and how the spatial and temporal variability of the surrounding environment affects...
Ammonia fluxes were measured semi-continuously over oilseed rape (Brassica napus) as part of the EXA...
New micrometeorological measurements of small (0.1–0.2 μm diameter) aerosol particle fluxes using th...