Abstract

A single particle Lagrangian Stochastic model has been developed and applied with the purpose of simulating the concentration fluctuations dispersion. This model treats concentration variance as a quantity whose motion is driven by an advection-diffusion process so that it can be studied by a single particle model. A parameterization for both velocity standard deviations and Lagrangian time-scales is required as input to the model. The paper is focused on the estimation of the best parameterization needed to simulate both mean and standard deviation concentrations in a case study. We consider the FFT-07 field experiment. The trials took place at Dugway Proving Ground, UTAH (USA) and consist of a dispersion analysis of a gas emitted from a point-like source in different atmospheric conditions with a continuous emission technique. The very small spatial scales (a few hundred meters) and short duration (about 10 minutes) that characterize the trials make the comparison with model results very challenging, since traditional boundary layer parameterizations fail in correctly reproducing the turbulent field and, as a consequence, the dispersion simulation yields unsatisfactorily results. We vary the coefficients of the turbulence parameterization to match the small-scale turbulence. Furthermore, we show that the parameterization for the variance dissipation time-scale, already tested in neutral conditions, can be used also in stable and unstable conditions and in low-wind speed conditions. The model gives good results as far as mean concentration is concerned and rather satisfactory results for the concentration standard deviations. Comparison between model results and observation is shown through both statistical and graphical analyses.

Highlights

  • When we talk about dispersion in the atmosphere we mean to study the distribution of the average concentration

  • A Lagrangian stochastic model is tested against data measured in a field experiment

  • Both mean concentrations and concentration standard deviations dispersion were simulated and the results compared against the observations

Read more

Summary

Introduction

When we talk about dispersion in the atmosphere we mean to study the distribution of the average concentration. In the experiments considered here the wind speed varies between 1.2 and 2.7 m/s, i.e., almost always in low wind conditions It is well-known that in these conditions the dispersion parameters (standard deviations of the wind speed components and Lagrangian timescales) take on values that are significantly different from those in high wind conditions, and traditional parameterizations of the turbulence in the planetary boundary layer fail. This is the reason why the values of these parameterizations have been modified and, as demonstrated in this work, the traditional parameterizations are not able to provide satisfactory results.

Langevin Stochastic Model
The FFT-07 Experiment
Statistical Analysis
Mean Concentration
Concentration Variance
Graphical Analysis
Conclusions
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call