Application of similarity theory associate with eddy covariance technique for atmospheric stability classification in Thailand
Keywords:
Atmospheric Stability Classification, Monin Obukhov Similarity Theory (MOST), Eddy Covariance TechniqueAbstract
Atmospheric stability classification is essential for determining pollution accumulation tendencies in geographical areas. While the KU Tower monitoring station at Kasetsart University, Bangkok, can classify atmospheric stability via multiple methods, these classifications are impractical for general meteorological stations due to specialized equipment requirements. This study proposes before use of Monin-Obukhov Similarity Theory (MOST) as a solution, which requires only basic meteorological parameters. To validate this approach, we first compared three conventional methods at KU Tower from 2016-2023 (44,814 hourly measurements): The temperature Gradient (Delta-T), Richardson Number (Ri), and Monin-Obukhov (MO) using IRGASON equipment, against Solar Radiation Delta-T (SRDT) as reference. The MO Method showed the best agreement with SRDT (NMSE = 0.301). Building on this finding, we implemented MOST using basic meteorological data (wind speed, temperature and cloud cover) and geographical surface parameters (roughness length, albedo and Bowen ratio) from Google Earth Engine. A comparison between MOST and the validated MO Method reveals moderately similar (NMSE = 0.238), confirming the effectiveness of MOST for classifying atmospheric stability via widely available meteorological data. This method can support air quality management in Thailand through applications in land use planning, industrial zone designation, and area-specific emission regulations.
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Manisalidis, I., Stavropoulou, E., Stavropoulos, A., and Bezirtzoglou, E. (2020). Environmental and health impacts of air pollution: A review. Frontiers In Public Health, 8, 14.
Amaral, S. S., de Carvalho, J. A., Costa, M. A. M., and Pinheiro, C. (2015). An overview of particulate matter measurement instruments. Atmosphere, 6(9), 1327-1345.
Pelliccioni, A., Monti, P., Gariazzo, C., and Leuzzi, G. (2012). Some characteristics of the urban boundary layer above Rome, Italy, and applicability of Monin–Obukhov similarity. Environmental Fluid Mechanics, 12, 405-428.
Gifford, F. (1961). Use of routine meteorological observations for estimating atmospheric dispersion. Nuclear Safety, 2(4), 44-57.
Edokpa, D., and Nwagbara, M. (2017). Atmospheric stability pattern over port harcourt, Nigeria. Journal of Atmospheric Pollution, 5(1), 9-17.
Hunt, G. R., and Van Den Bremer, T. S. (2010). Classical plume theory: 1937–2010 and beyond. IMA Journal of Applied Mathematics, 76(3), 424-448.
Pasquill, F. (1961). The estimation of the dispersion of windborne material. Meteorological Magazine, 90(1063), 33-49.
DeMarrais, G. A. (1978). Atmospheric stability class determinations on a 481-meter tower in Oklahoma. Atmospheric Environment, 12(10), 1957-1962.
Pérez, I. A., García, M., Sánchez, M. L., and de Torre, B. (2004). Autocorrelation analysis of meteorological data from a RASS sodar. Journal of Applied Meteorology, 43(8), 1213-1223.
Bowen, B. M., Dewart, J. M., and Chen, A. I. (1983). Stability-class determination: A comparison for one site. Los Alamos National Laboratory.
Golder, D. H. (1972). Relations among stability parameters in the surface layer. Boundary-Layer Meteorology, 3, 47-58.
Oard, M. J. (1974). Application of a diagnostic Richardson number tendency to a case study of clear air turbulence. Journal of Applied Meteorology, 13(7), 771-777.
Aubinet, M. Vesala, T., and Papale, D. (2012). Eddy covariance: A practical guide to measurement and data analysis. Springer Science and Business Media.
Stull, R. B. (2012). An introduction to boundary layer meteorology (Vol. 13). Springer Science & Business Media.
Bailey, D. T. (2000). Meteorological monitoring guidance for regulatory modeling applications. EPA-454/R-99-005. U.S. Environmental Protection Agency, Office of Air Quality Planning and Standards.
Miles, J. W. (1961). On the stability of heterogeneous shear flows. Journal of Fluid Mechanics, 10(4), 496-508.
Businger, J. A., Wyngaard, J. C., Izumi, Y., and Bradley, E. F. (1971). Flux-profile relationships in the atmospheric surface layer. Journal of The Atmospheric Sciences, 28(2), 181-189.
Businger, J. A. (1973). Turbulence transfer in the atmospheric surface layer. In Workshop on Micrometeorology (pp. 67-100). American Meteorological Society, Boston, MA.
Sedefian, L., and Bennett, E. (1980). A comparison of turbulence classification schemes. Atmospheric Environment, 14(7), 741-750.
Kaimal, J. C., and Finnigan, J. J. (1994). Atmospheric boundary layer flows: Their structure and measurement. Oxford University Press.
Seinfeld, J. H., and Pandis, S. N. (2016). Atmospheric chemistry and physics: From air pollution to climate change (3rd ed.). John Wiley & Sons.
Arya, S. P. (1999). Air pollution meteorology and dispersion (Vol. 310). Oxford University Press New York.
Holtslag, A., and Van Ulden, A. (1983). A simple scheme for daytime estimates of the surface fluxes from routine weather data. Journal of Applied Meteorology and Climatology, 22(4), 517-529.
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