Formulation of stability-dependent empirical relations for turbulent intensities from surface layer turbulence measurements for dispersion parameterization in a lagrangian particle dispersion model

• Published in: Meteorology and atmospheric physics 2015-08, Vol.127 (4), p.435-450
• Main Authors: Hari Prasad, K. B. R. R., Srinivas, C. V., Satyanarayana, A. N. V., Naidu, C. V., Baskaran, R., Venkatraman, B.
• Format: Article
• Language: English
• Subjects: Aquatic Pollution; Atmospheric Sciences; Atmospheric turbulence; Computational fluid dynamics; Dispersions; Earth and Environmental Science; Earth Sciences; Fluid flow; Fourier transforms; Marine; Math. Appl. in Environmental Science; Mathematical models; Meteorology; Original Paper; Parametrization; Plumes; Pollution dispersion; Simulation; Terrestrial Pollution; Turbulence; Turbulent flow; Waste Water Technology; Water Management; Water Pollution Control; Wind
• ISSN: 0177-7971; 1436-5065
• DOI: 10.1007/s00703-015-0373-5

Season- and stability-dependent turbulence intensity ( σ u / u * , σ v / u * , σ w / u * ) relationships are derived from experimental turbulence measurements following surface layer scaling and local stability at the tropical coastal site Kalpakkam, India for atmospheric dispersion parameterization. Turbulence wind components ( u ′, v ′, w ′) measured with fast response UltraSonic Anemometers during an intense observation campaign for wind field modeling called Round Robin Exercise are used to formulate the flux–profile relationships using surface layer similarity theory and Fast Fourier Transform technique. The new relationships (modified Hanna scheme) are incorporated in a Lagrangian Particle Dispersion model FLEXPART-WRF and tested by conducting simulations for a field tracer dispersion experiment at Kalpakkam. Plume dispersion analysis of a ground level hypothetical release indicated that the new turbulent intensity formulations provide slightly higher diffusivity across the plume relative to the original Hanna scheme. The new formulations for σ u , σ v , σ w are found to give better agreement with observed turbulent intensities during both stable and unstable conditions under various seasonal meteorological conditions. The simulated concentrations using the two methods are compared with those obtained from a classical Gaussian model and the observed SF 6 concentration. It has been found that the new relationships provide comparatively higher diffusion across the plume relative to the model default Hanna scheme and provide downwind concentration results in better agreement with observations.