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