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Appendix 6: Representative Gas Cloud Models - TP 743 E

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Model Name Technology Approach Model Type
Welker, et al. (1969)
Ref: AGA (1973)
Gaussian Model assumes vapour cloud is neutrally buoyant. Release source is subdivided into a number of point sources.
Drake, et al. (1969)
Ref: AGA (1973)
Gaussian Model assumes vapour cloud is neutrally buoyant. Release source is converted to a line source and then a virtual point source.
Germeles-Drake (1973)
Ref: Germeles and Drake (1975)
Gravity Dispersion followed by Gaussian Model initially assumes vapour cloud is heavier than air and spreads due to the density differences between the cloud and the surrounding air. At a selected cloud density or lateral velocity, gravity dispersion is terminated and Gaussian initiated.
SIGMET (SAI) (1975)
Ref: Havens (1979)
Transport Models cloud dispersion using mass and momentum transport equations. A total of six partial differential equations must be solved. There are a number of constants that must be selected.
Eidsvik (1979)
Ref: Eidsvik (1980)
Gravity Dispersion followed by Gaussian Eidsvik is similar to Germeles-Drake but improves the air / cloud transport mixing portion of the model during gravity dispersion.
HEGADAS (1980)
Ref: Colenbrander (1980)
Gravity Dispersion Similar to Eidsvik and Germeles-Drake. Primary difference is that during gravity spread phase, cloud cross section profile is better modeled.
ZEPHER (1981)
Ref: Woodward, et al. (1981)
Transport Same as SIGMET except for mathematical solution procedures.
MARIAH (1981)
Ref: Woodward, et al. (1981)
Transport Same as SIGMET except for mathematical solution procedures.
Safeti (1986) Combination A "standard box" model with numerous enhancements to the initial cloud development.
Robinson, et al. (1988)
Ref: NOAA (1988)
Transport and Gaussian Dispersion Estimates pollutant concentrations downwind from the source, taking into account the toxicological and physical characteristics of the spilled material.

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