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William A. Komaromi and James D. Doyle

2014. The number of dropsondes in each bin is labeled in magenta. A meaningful relationship between the θ of the maximum 100–500-km radially averaged V r and the present intensity was not observed ( Fig. 9c ). However, a notable positive relationship between the θ of the outflow layer and the θ e of the boundary layer inflow, which is a proxy for low-level moisture and SSTs, does occur ( Fig. 9d ). These values are obtained by first computing azimuthal-mean V r in radius– θ (radius θ e

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