1976
DOI: 10.1016/0004-6981(76)90176-1
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The application of correlation spectroscopy to the study of dispersion from tall stacks

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Cited by 37 publications
(25 citation statements)
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“…This average is made with the coordinates related to the centre of gravity of each profile; thus, meandering effects are not taken into account. This profile, averaged in time but not in space, shows the relative diffusion of the plume and keeps its morphologic features (Millán et al, 1976): bifurcation, directional shear effect, wind-speed shear effect (i.e., Kurtosis), etc. Further details in Appendix A.…”
Section: Methodsmentioning
confidence: 94%
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“…This average is made with the coordinates related to the centre of gravity of each profile; thus, meandering effects are not taken into account. This profile, averaged in time but not in space, shows the relative diffusion of the plume and keeps its morphologic features (Millán et al, 1976): bifurcation, directional shear effect, wind-speed shear effect (i.e., Kurtosis), etc. Further details in Appendix A.…”
Section: Methodsmentioning
confidence: 94%
“…A2) and those that would be obtained by measuring directly over that plane (Millán et al, 1976;Hoff and Gallant, 1985).…”
Section: Pseudo-lagrangian Data Processing Methodology For Remote Senmentioning
confidence: 99%
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