Reply to comments on ”Simulating ozone dry deposition at a boreal forest with a multi-layer canopy deposition model”
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“In SOSAA, the horizontal wind velocity (u and v), temperature (T ), specific humidity (qv), turbulent kinetic energy (TKE) and the specific dissipation of TKE (ω) are computed every time step (10 s) by prognostic equations. In order to represent the local to synoptic scale effects, u, v, T and qv near and within the canopy are nudged to local measurement data at SMEAR II station with a nudging factor of 0.01. A TKE-ω parameterization scheme is used to calculate the turbulent diffusion coefficients (Kt) (Sogachev, 2009),
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Reply to comments on “Simulating ozone dry deposition at a boreal forest with a multi-layer canopy deposition model”
1. Comments: (1) Authors state that they have implemented a multi-layer dry deposition model into SOSAA, which is a 1D chemical transport model. SOSAA is described in Section 2.3.1, which lists different modules and references but does not explain the model types or physical principles. The key elements of SOSAA relevant to the present study, especially turbulent mixing and the derivation of ed...
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