A controlled ammonia (NH
3) release experiment was performed at a grassland site. The aim was to quantify the effect of dry deposition between the source and the receptors (NH
3 measurement locations) on emission rate estimates by means of inverse dispersion modelling. NH
3 was released for three hours at a constant rate of
= 6.29 mg s
−1 from a grid of 36 orifices spread over an area of 250 m
2. The increase in line-integrated NH
3 concentration was measured with open-path optical miniDOAS devices at different locations downwind of the artificial source. Using a backward Lagrangian stochastic (bLS) dispersion model (
bLSmodelR), the fraction of the modelled release rate to the emitted NH
3 (
) was calculated from the measurements of the individual instruments.
was found to be systematically lower than 1, on average between 0.69 and 0.91, depending on the location of the receptor. We hypothesized that NH
3 dry deposition to grass and soil surfaces was the main factor responsible for the observed depletion of NH
3 between source and receptor. A dry deposition algorithm based on a deposition velocity approach was included in the bLS modelling. Model deposition velocities were evaluated from a ‘big-leaf’ canopy resistance analogy. Canopy resistances (generally termed
) that provided
= 1 ranged from 75 to 290 s m
−1, showing that surface removal of NH
3 by dry deposition can plausibly explain the original underestimation of
. The inclusion of a dry deposition process in dispersion modelling is crucial for emission estimates, which are based on concentration measurements of depositing tracers downwind of homogeneous area sources or heterogeneously-distributed hot spots, such as, e.g., urine patches on pastures in the case of NH
3.
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