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Daniel T. Eipper, Steven J. Greybush, George S. Young, Seth Saslo, Todd D. Sikora, and Richard D. Clark

the thermodynamic structure of each band and environmental baroclinity. The density potential temperature θ ρ accounts for the effects of both water vapor and hydrometeors on potential temperature; the formula for its computation is provided in Markowski and Richardson [2010 , their Eq. (2.22)]. We chose to position the cross sections over the approximate landfall location and inland portion of each band, where greater human impacts occur. Specifically, the cross sections were generated every 0

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