Articles | Volume 20, issue 11
https://doi.org/10.5194/acp-20-6861-2020
https://doi.org/10.5194/acp-20-6861-2020
Research article
 | 
11 Jun 2020
Research article |  | 11 Jun 2020

Surface processes in the 7 November 2014 medicane from air–sea coupled high-resolution numerical modelling

Marie-Noëlle Bouin and Cindy Lebeaupin Brossier

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Marie-Noelle Bouin on behalf of the Authors (19 Feb 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (21 Feb 2020) by Christian Barthlott
RR by Anonymous Referee #1 (02 Mar 2020)
RR by Anonymous Referee #3 (21 Mar 2020)
ED: Reconsider after major revisions (25 Mar 2020) by Christian Barthlott
AR by Marie-Noelle Bouin on behalf of the Authors (30 Apr 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (07 May 2020) by Christian Barthlott
RR by Anonymous Referee #3 (13 May 2020)
ED: Publish as is (13 May 2020) by Christian Barthlott
AR by Marie-Noelle Bouin on behalf of the Authors (13 May 2020)  Manuscript 
Download
Short summary
A coupled, kilometre-scale simulation of a medicane is used to assess the impact of the ocean feedback and role of surface fluxes. Sea surface temperature (SST) drop is much weaker than for tropical cyclones, resulting in no impact on the cyclone. Surface fluxes depend mainly on wind and SST for evaporation and on air temperature for sensible heat. Processes in the Mediterranean, like advection of continental air, rain evaporation and dry air intrusion, play a role in cyclone development.
Altmetrics
Final-revised paper
Preprint