The goal of this study is to provide an improved understanding of the interactions between wildfires and the sea breeze, based both on observations of a fire event and on idealized numerical simulations that describe interactions between a buoyant plume and a density current. Radar observations of a plume associated with a wildfire will be shown that indicate the possibility that the arrival of a sea-breeze front results in a temporary, but significant, increase in fire intensity. There is insufficient evidence to fully explain this intensification; however, the idealized numerical simulations suggest that during the period of interaction preceding the arrival of the density current, slight pressure perturbations may trigger an intensification of the horizontal and vertical velocities within the plume.
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