SCALING THE TURBULENT TRANSPORT OF CHEMICAL-COMPOUNDS IN THE SURFACE-LAYER UNDER NEUTRAL AND STRATIFIED CONDITIONS

Citation
S. Galmarini et al., SCALING THE TURBULENT TRANSPORT OF CHEMICAL-COMPOUNDS IN THE SURFACE-LAYER UNDER NEUTRAL AND STRATIFIED CONDITIONS, Quarterly Journal of the Royal Meteorological Society, 123(537), 1997, pp. 223-242
Citations number
26
Categorie Soggetti
Metereology & Atmospheric Sciences
ISSN journal
00359009
Volume
123
Issue
537
Year of publication
1997
Part
A
Pages
223 - 242
Database
ISI
SICI code
0035-9009(1997)123:537<223:STTTOC>2.0.ZU;2-8
Abstract
A model of the vertical transport of chemically reactive species is pr esented which is applicable to all possible stability conditions in th e atmospheric surface-layer. The non-dimensional formulation adopted a llows any chemical scheme to be included. An equation hierarchy is pre sented for a fully second-order closure description of the process. Th e model describes comprehensively the turbulence/chemistry process by calculating the mean concentrations, the turbulent fluxes and concentr ation covariances of the chemical species. It explicitly takes into ac count the chemical transformation in first- and second-order variable equations. The model is applied to the NO-NO2-O-3 cycle and to the so- called 'night-time' chemical scheme of nitrogen oxides. An analysis of the flux budget indicates that the relative importance of the chemist ry term in the flux equation varies with distance from the surface. Fo r atmospheric neutral conditions, it is suggested that the chemistry t erm in the flux equation can be used to make an a priori evaluation of the possible effect of chemistry upon the nux of a chemical species. The model also shows that under stable conditions, despite the greatly reduced activity of turbulence, differences can occur between the tur bulent transport of an inert tracer and that of a chemically reactive species. Under any stratification and for typical surface-layer fluxes of nitrogen oxides, the intensity of segregation is very low and can in general be neglected in model calculations.