Articles | Volume 16, issue 13
Atmos. Chem. Phys., 16, 8511–8519, 2016
Atmos. Chem. Phys., 16, 8511–8519, 2016

Research article 13 Jul 2016

Research article | 13 Jul 2016

Why did the storm ex-Gaston (2010) fail to redevelop during the PREDICT experiment?

Thomas M. Freismuth et al.


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Anna Wenzel on behalf of the Authors (17 May 2016)  Author's response
ED: Publish as is (16 Jun 2016) by Timothy J. Dunkerton
Short summary
Numerical model analyses are used to investigate the role of dry, environmental air in the failed redevelopment of a tropical cyclone (ex-Gaston, 2010). As early as 12:00 UTC 2 September 2010, a dry layer at and above 600 hPa results in a decrease in the vertical mass flux and vertical, relative vorticity. The intrusion of dry air led to a reduction in vorticity and a compromised pouch at these middle levels. This study supports work looking at the role of dry air in moist convection.
Final-revised paper