Articles | Volume 17, issue 12
https://doi.org/10.5194/nhess-17-2059-2017
https://doi.org/10.5194/nhess-17-2059-2017
Research article
 | 
29 Nov 2017
Research article |  | 29 Nov 2017

Wave–current interaction during Hudhud cyclone in the Bay of Bengal

Volvaiker Samiksha, Ponnumony Vethamony, Charls Antony, Prasad Bhaskaran, and Balakrishnan Nair

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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
ED: Reconsider after major revisions (further review by Editor and Referees) (27 Jun 2017) by Ira Didenkulova
AR by Samiksha Volvaiker on behalf of the Authors (03 Jul 2017)
ED: Referee Nomination & Report Request started (07 Jul 2017) by Ira Didenkulova
RR by Anonymous Referee #2 (18 Jul 2017)
RR by Anonymous Referee #1 (24 Jul 2017)
ED: Reconsider after major revisions (further review by Editor and Referees) (26 Jul 2017) by Ira Didenkulova
AR by Samiksha Volvaiker on behalf of the Authors (19 Aug 2017)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (07 Sep 2017) by Ira Didenkulova
RR by Anonymous Referee #1 (25 Sep 2017)
ED: Reconsider after major revisions (further review by Editor and Referees) (25 Sep 2017) by Ira Didenkulova
AR by Samiksha Volvaiker on behalf of the Authors (03 Oct 2017)
ED: Reconsider after major revisions (further review by Editor and Referees) (17 Oct 2017) by Ira Didenkulova
AR by Samiksha Volvaiker on behalf of the Authors (19 Oct 2017)  Author's response   Manuscript 
ED: Publish as is (21 Oct 2017) by Ira Didenkulova
AR by Samiksha Volvaiker on behalf of the Authors (25 Oct 2017)  Manuscript 
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Short summary
The present work describes the interaction between waves and currents utilizing a coupled ADCIRC+SWAN model for the very severe cyclonic storm Hudhud which made landfall at Visakhapatnam on the east coast of India in October 2014. Model-computed wave and surge heights were validated with measurements near the landfall point. An increase of ≈0.2 m in Hs was observed with the inclusion of model currents.
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