Articles | Volume 19, issue 5
https://doi.org/10.5194/nhess-19-1023-2019
https://doi.org/10.5194/nhess-19-1023-2019
Research article
 | 
15 May 2019
Research article |  | 15 May 2019

Synoptic-scale conditions and convection-resolving hindcast experiments of a cold-season derecho on 3 January 2014 in western Europe

Luca Mathias, Patrick Ludwig, and Joaquim G. Pinto

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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
ED: Reconsider after major revisions (further review by editor and referees) (09 Mar 2019) by Ricardo Trigo
AR by Luca Mathias on behalf of the Authors (12 Mar 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (13 Mar 2019) by Ricardo Trigo
RR by David Leutwyler (18 Mar 2019)
RR by Anonymous Referee #2 (01 Apr 2019)
ED: Publish subject to minor revisions (review by editor) (16 Apr 2019) by Ricardo Trigo
AR by Luca Mathias on behalf of the Authors (18 Apr 2019)  Author's response   Manuscript 
ED: Publish as is (29 Apr 2019) by Ricardo Trigo
AR by Luca Mathias on behalf of the Authors (30 Apr 2019)  Manuscript 
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Short summary
Convective systems producing severe winds occasionally affect Europe during wintertime and the majority of these storms develop along well-defined cold fronts of extratropical cyclones. However, on 3 January 2014, a storm formed in a postfrontal air mass over western Europe. This study analyses the prevailing environmental conditions and the predictability of this storm. Our results reveal the difficulty of forecasting cold-season convective storms when they are not associated with a cold front.
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