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Extreme Values of Contaminant Concentration in the Atmospheric Boundary-Layer Nils Mole (University of Sheffield) Thom Schopflocher Paul Sullivan (University.

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Presentation on theme: "Extreme Values of Contaminant Concentration in the Atmospheric Boundary-Layer Nils Mole (University of Sheffield) Thom Schopflocher Paul Sullivan (University."— Presentation transcript:

1 Extreme Values of Contaminant Concentration in the Atmospheric Boundary-Layer Nils Mole (University of Sheffield) Thom Schopflocher Paul Sullivan (University of Western Ontario)

2 2 Background Typical diffusing plume The texture of the contaminant field consists of concentration in very thin sparsely distributed sheets.

3 3 Background…

4 4 Fixed point measurements showing large peaks of concentration

5 5 High Concentration Tails pdf As the sum of two functions, Such that Moments of p(θ), For sufficiently large n,

6 6 Generalized Pareto Density function θ 2 is the largest source concentration and a, k > 0. for sufficiently large n, Moment ratios are linear in 1/n, which should yield the values of a, k & θ max = a/k. n can be found from

7 7 Experimental data Linear fits to the moment ratios for data from Sawford & Tivendale (1992). X is the downstream distance from the source, Z is the cross-stream distance from the centreline, and L is the mean plume width.

8 8 Experimental data The measured pdf of θ/C o (points), and GPD for fitted k and a values (curves). The right-hand panels show blow-ups of the tails. The dashed lines mark the estimated values of θ c /C o.

9 9 Experimental data Variation with downwind distance X of the percentage range and area accounted for by the GPD, i.e. by θ ≥ θ c. (a) Range 1 − θ c /θ max, (b) area A. The squares represent centreline measurements, and the crosses measurements at about 1L from the centreline.

10 10 Experimental data Variation on the centreline of GPD parameters (estimated from the data of Sawford & Tivendale 1992) with downstream distance X. (a) θ max /C o (squares), a/C o (triangles) and 10k (crosses), (b) θ max /C o (squares), and the approximation to θ max /C o in the no diffusion case based (curve).

11 11 Experimental data Variation across the plume of GPD parameters normalized by their centreline values. (a) θ max, (b) k, (c) a, (d) η. The line in (d) is that on which the normalized value of η equals C/C o.

12 12 Conclusions Have shown the evolution of the high concentration tails, including θmax, in terms of lower order moments of pdf. Further work (not shown here) using existing models of the moments provides a five parameter representation. Some promising schemes for the solution of the moments equation, are currently under investigation.

13 13 Examples of the possible GPD shapes.

14 14 Variation of centreline η with downstream distance X.


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