1972
DOI: 10.3402/tellusa.v24i5.10659
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Evaluation of atmospheric dilution factors for effluents diffused from an elevated continuous point source

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Cited by 42 publications
(10 citation statements)
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“…The plume height is here set externally as a forcing term h t ¼ h u t , based on the theoretical formulae for buoyant plume rise by Briggs (13) . Similarly, in both models s y and s z are set externally using a site-specific parameterisation of the dispersion parameters (14) , for example, s y;t ¼ s u y;t , that depends on the distance from the source and the atmospheric stability according to the Pasquill-Gifford scheme (15) . A simple random walk process is used to govern the temporal variations of the remaining (free) state variables, cf.…”
Section: Numerical Resultsmentioning
confidence: 99%
“…The plume height is here set externally as a forcing term h t ¼ h u t , based on the theoretical formulae for buoyant plume rise by Briggs (13) . Similarly, in both models s y and s z are set externally using a site-specific parameterisation of the dispersion parameters (14) , for example, s y;t ¼ s u y;t , that depends on the distance from the source and the atmospheric stability according to the Pasquill-Gifford scheme (15) . A simple random walk process is used to govern the temporal variations of the remaining (free) state variables, cf.…”
Section: Numerical Resultsmentioning
confidence: 99%
“…The second tower of the Belgian Nuclear Research Centre (SCK•CEN) is 120 m high and located in Mol (Geographical coordinates: 51 • 13'04"N and 5 • 05'24"E). Measurements have been done in the framework of determining atmospheric stability according to the turbulence scheme of SCK•CEN (Bultynck and Malet, 1972). It is placed in a rural area on flat terrain with pine trees in the immediate vicinity.…”
Section: Tower Observationsmentioning
confidence: 99%
“…From the Lidar measurements, horizontal and vertical plume dispersion parameters (σ y , σ z ) can be derived along with the mean position and elevation of the plume. In Figure 2, measured dispersion parameters for Friday October 5 are compared to two different model results: a) the SCK•CEN model, in which Pasquill-Gifford stability classes are determined from the wind speed at 69 m and potential temperature gradient over the range 8 m -114 m, and the diffusion parameters are calculated for each stability class (Bultynck and Malet, 1972); b) the RIMPUFF model in which the puff growth is calculated based on similarity scaling (Thykier-Nielsen et al, 2002;Astrup et al, 2001). Also this model uses the wind speed at 69 m and the temperature differences between 48 m and 78 m, in addition to an assumed surface roughness length of 1 m for the area in question.…”
Section: Plume Geometrymentioning
confidence: 99%