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Book ChapterDOI

Dispersion Modelling and Observations from Elevated Sources in Coastal Terrain

TLDR
In this article, Lagrangian Atmospheric Dispersion Model (LADM) is used to simulate the transport and diffusion of emissions from discrete sources, for impact distances ranging from hundreds of metres to a few hundred kilometres.
Abstract
This study is focussed on the Central Coast region of New South Wales, on the east coast of Australia, where Pacific Power Inc. operates three power stations, situated on small lakes within a few kilometres of the coast. One of the objectives of the study was to assess the suitability and value of our modelling system to the air quality assessment needs of Pacific Power in the region, including the evaluation of green-fields sites for future power stations. The dispersion of plumes from all power stations throughout the year is not only influenced by the terrain blocking and channeling of the synoptic winds, but also by mesoscale wind systems such as sea breezes and drainage flows. Our Lagrangian Atmospheric Dispersion Model (LADM) predicts winds and turbulence and uses these to simulate the transport and diffusion of emissions from discrete sources, for impact distances ranging from hundreds of metres to a few hundred kilometres. In this paper we compare LADM results to available observations in the far field.

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References
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Journal ArticleDOI

A parametric model of vertical eddy fluxes in the atmosphere

TL;DR: In this paper, a model for the representation of vertical eddy fluxes of heat, momentum and water vapour in a forecast model is presented, and two tests are presented, using the scheme in a one-dimensional model: the simulation of the diurnal cycle and the transformation of a polar air mass moving over the warm sea.
Journal ArticleDOI

Some aspects of turbulence structure through the depth of the convective boundary layer

TL;DR: In this article, a series of boundary layer measurements carried out at Ashchurch, Worcestershire during July 1976 are combined with those from the 1973 Minnesota experiment to provide a more complete description of the behaviour of some turbulence statistics through the depth of the convective boundary layer and into the stable air of the free atmosphere.
Journal ArticleDOI

Influence of diurnal and inertial boundary-layer oscillations on long-range dispersion

TL;DR: In this paper, coupled meteorological and Lagrangian particle models are used to examine horizontal dispersion over one to two diurnal cycles, and the results of the experiments indicate that vertical shear in the horizontal wind produced by diurnal and/or inertial oscillations in conjunction with or followed by vertical PBL mixing are capable of maintaining plume growth rates which are nearly linear with diffusion times up to 48 h.
Journal ArticleDOI

A skewed homogeneous lagrangian particle model for convective conditions

TL;DR: In this paper, the authors investigate the effect of homogeneous turbulence on ground-level concentration (glc) by comparing results with (a) the Willis and Deardorff laboratory experiments on dispersion in fully convective conditions and (b) the predictions of a model employing a more realistic inhomogeneous parameterization for the turbulence.
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