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4. Atmospheric chemical transport models 4.1 Introduction 4.2 Box model 4.3 Three dimensional atmospheric chemical transport model
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4.1 Introduction Questions What is the contribution of source A to the concentration of pollutants at site B? What is the most cost-effective strategy for reducing pollutant concentrations below an air quality standard? What will be the effect on air quality of the addition of the reduction of a specific air pollutant emission flux? What should one place a future source to minimize its environmental impacts? What will be the air quality tomorrow or the day after?
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The atmosphere is an extremely reactive system in which numerous physical and chemical processes occur simultaneously. Mathematical models provide the necessary framework for integration of our understanding of individual atmospheric processes and study of their interaction. Three basic components of an atmospheric model are species emission, transport and physiochemical transformations
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① Eulerian model: describes the concentrations in an array of fixed computational cells ② Lagrangian model: simulates concentration change of air parcel as it is advected in the atmosphere. 출처 : http://www.romair.eu/model-description.php?lhttp://www.romair.eu/model-description.php?l ang=en 출처 : http://www.shodor.org/os411/courses/411f/module03/unit05/http://www.shodor.org/os411/courses/411f/module03/unit05/ page01.html
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Classification based on dimension ① box model( 상자 모델 ): zero-dimensional Concentrations are functions of time only. C(t) ② column model: one-dimensional Horizontally homogeneous layers Concentrations are functions of height and time. C(z, t) ③ two dimensional model: often used in description of global atmospheric chemistry ④ three dimensional model: c(x,y,z,t)
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4.2 Box model ( 상자모델 ) 4.1.1 Eulerian box model Assume that the height (H) of the box equal the mixing layer height. : background concentration : mass emission ratekg/h -1 : chemical production rate (kg m -3 h -1 ) : removal rate(dry deposition, wet deposition)
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1) For constant mixing height residence time
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Problem 1 Ex1) An inert species has as initial concentration and is emitted at a rate. Assuming that its background concentration is, calculate its steady-state concentration over a city characterized by an average wind speed of 3m/s. Assume that the city has dimensions and a constant mixing height of 1000m.
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2) For changing mixing height with time ① For decreasing mixing height No direct change of the concentration inside the mixed layer Because the box will be smaller, surface sources and sinks will have a more significant effect. ② For increasing mixing height Entrainment and subsequent dilution will change the concentration. : the concentration above the box.
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Mass balance Neglecting
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4.1.2 Lagrangian Box model No advection term
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Problem 2 Ex 2) SO 2 is emitted in an urban area with a flux of 2000 g m -3. The mixing height over the area is 1000m, the atmospheric residence time 20h, and SO 2 reacts with an average rate of 3 % h -1. Rural areas around the city are characterized by a SO 2 concentration equal to 2 g m -3. What is the average SO 2 concentration in the urban airshed for the above conditions? Assume an SO 2 dry deposition velocity of 1cms -1 and a cloud/ fog-free atmosphere
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4.3 Three dimensional atmospheric chemical model Input data: three dimensional meteorological field, emission data, initial and boundary condition of pollutants Example of three dimensional model RADM(Regional Acid Deposition Model) UAM(Urban Airshed Model), CMAQ (Community Multiscale air quality) Chemical transport model : eddy diffusivity
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4.2.1 Coordinate system
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4.2.2 Initial conditions
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Unlike initial condition, boundary conditions, especially at the upwind boundaries, continue to affect predictions throughout the simulations. Therefore, one should try to place the limits of the modeling domain in relatively clean areas where boundary conditions are relatively well know and have a relatively small effect on model predictions. Uncertainty of side boundary conditions in urban air pollution model prediction may be reduced by use of larger scale models to provide the boundary condition to the urban scale model. : nesting technique
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4.2.4 Numerical solution of chemical transport models
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Operator splitting
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Diffusion Crank-Nicholson algorithm
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Advection
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