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Measurements of level-crossing statistics of concentration fluctuations in plumes dispersing in the atmospheric surface layer
Authors:Eugene Yee  R. Chan  P. R. Kosteniuk  G. M. Chandler  C. A. Biltoft  J. F. Bowers
Affiliation:(1) Defence Research Establishment Suffield, Box 4000, T1A 8K6 Medicine Hat, Alberta, Canada;(2) Kosteniuk Consulting Ltd, #21-719 10th Street East, S7K 0H2 Saskatoon, Saskatchewan, Canada;(3) S & J Engineering, Inc., 3447 Kennedy Rd, Suite 6, M1V 3S1 Scarborough, Ontario, Canada;(4) Meteorology Division, Materiel test Directorate, U.S. Army Dugway Proving Ground, 84022-5000 Dugway, Utah, USA
Abstract:The statistics of level crossings and local extremes in concentration fluctuations in plumes dispersing in the atmosphere have been investigated. A set of concentration fluctuation tracer experiments has been utilized to measure the statistical propertics of the upcrossing interval (inter-arrival time between consecutive concentration bursts), excursion duration (persistence or width of concentration bursts), and concentration amplitude (difference between the maximum and minimum concentrations between successive upcrossings) with respect to a range of concentration crossing levels. In particular, the effect of downwind distance and atmospheric stratification on the level-crossing statistics has been studied in detail. It is shown that the effect of increasing atmospheric stability on level-crossing statistics is similar to the effect of increasing distance from the source in the sense that level-crossing statistics of concentration fluctuations in stable stratification resemble those in neutral stratification, but at a greater downwind distance. It is also found that the distribution of the interval between consecutive upcrossings of a concentration level, as well as the duration of an excursion across a concentration level, can be approximated by a lognormal distribution, whereas the distribution of the concentration amplitude is best characterized by a gamma distribution. Some implications of these results for the modeling of level-crossing statistics of concentration fluctuations are discussed.
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