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Sen Chiao and Gregory S. Jenkins

al. (2008) using satellite observations for the pre–TS Debby environment and limited aircraft measurements for TD 8 suggested that aerosols invigorated the convection. Elevated aerosol optical thickness (AOT) values that extended south toward 10°N are shown in Jenkins et al. (2008) (cf. Fig. 3a ) for 20 August. Visible satellite images at 1200 UTC 20 August showed that dust located to the north of the developing convection (not shown). The 1200 UTC cross section between Dakar, Senegal, and

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