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Both field studies pointed to the importance of the shoreline thermal internal boundary in determining ground-level concentrations. This was particularly important during the 2005 study when ground-level concentrations were governed by the rate of entrainment of the buoyant elevated plume by TIBL. The performance of TAPM in describing the results from these field studies was compared with that of a semi-empirical dispersion model, which assumes a Gaussian concentration profile in the horizontal, and uniform mixing in the vertical of the plume entrained into the TIBL. The height of the TIBL height was computed with a simple model in which the height grows as the square root of the distance from the shoreline. The meteorological inputs for the semi-empirical model were constructed from measurements made at the site.
TAPM's performance in explaining concentration estimates during the 2004 surface releases was comparable to that from the semi-empirical model. However, it did not provide adequate concentration estimates during the 2005 study. One reason for this is the inability of TAPM in simulating the growth of TIBL with distance from the shoreline. The paper provides a detailed examination of other factors that contribute to the performance of TAPM.