Articles | Volume 20, issue 12
https://doi.org/10.5194/nhess-20-3315-2020
https://doi.org/10.5194/nhess-20-3315-2020
Research article
 | 
08 Dec 2020
Research article |  | 08 Dec 2020

What controls the coarse sediment yield to a Mediterranean delta? The case of the Llobregat River (NE Iberian Peninsula)

Juan P. Martín-Vide, Arnau Prats-Puntí, and Carles Ferrer-Boix

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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) (03 Jun 2020) by Maria-Carmen Llasat
AR by Juan P. Martín-Vide on behalf of the Authors (05 Jun 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (25 Jun 2020) by Maria-Carmen Llasat
RR by Carles Ibáñez (29 Jun 2020)
ED: Publish subject to minor revisions (review by editor) (29 Jul 2020) by Maria-Carmen Llasat
AR by Juan P. Martín-Vide on behalf of the Authors (21 Sep 2020)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (29 Sep 2020) by Maria-Carmen Llasat
AR by Katja Gänger on behalf of the Authors (24 Oct 2020)  Author's response
ED: Publish as is (25 Oct 2020) by Maria-Carmen Llasat
AR by Juan P. Martín-Vide on behalf of the Authors (28 Oct 2020)  Author's response    Manuscript
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Short summary
An alluvial Mediterranean river changed its riverine and deltaic landscape. The delta has been heavily retreating (up to 800 m) for more than a century. We focus on the river, channelized in the last 50 years, trying to link its sandy sediment yield to the delta evolution. Sediment availability in the last 30 km of the river channel is deemed responsible for the decrease in the sediment yield to the delta. Sediment supply reduction to the coast jeopardizes the future of the delta and beaches.
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