Extreme Values of Contaminant Concentration in the Atmospheric Boundary-Layer. Nils Mole ( University of Sheffield ) Thom Schopflocher Paul Sullivan ( University of Western Ontario ). Background. Typical diffusing plume.
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Nils Mole (University of Sheffield)
Paul Sullivan (University of Western Ontario)
Typical diffusing plume
The texture of the contaminant field consists of concentration in very thin sparsely distributed sheets.
Fixed point measurements showing large peaks of concentration
As the sum of two functions,
Moments of p(θ),
For sufficiently large n,
θ2 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 & θmax= a/k.
ncan be found from
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.
The measured pdf of θ/Co (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 θc/Co.
Variation with downwind distance X of the percentage range and area accounted for by the GPD, i.e. by θ ≥θc. (a) Range 1 − θc/θmax, (b) area A. The squares represent centreline measurements, and the crosses measurements at about 1L from the centreline.
Variation on the centreline of GPD parameters (estimated from the data of Sawford & Tivendale 1992) with downstream distance X. (a) θmax/Co (squares), a/Co (triangles) and 10k (crosses), (b) θmax/Co (squares), and the approximation to θmax/Co in the no diffusion case based (curve).
Variation across the plume of GPD parameters normalized by their centreline
values. (a) θmax, (b) k, (c) a, (d) η. The line in (d) is that on which the normalized value of η equals C/Co.
are currently under investigation.
Variation of centreline η with downstream distance X.