Temporal variability of lagoon–sea water exchange and seawater circulation through a Mediterranean barrier beach
International audience The subterranean flow of water through sand barriers between coastal lagoons and the sea, driven by a positive hydraulic gradient, is a net new pathway for solute transfer to the sea. On the sea side of sand barriers, seawater circulation in the swash‐zone generates a flux of...
Published in: | Limnology and Oceanography |
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Main Authors: | , , , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2019
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Subjects: | |
Online Access: | https://hal.science/hal-02095578 https://hal.science/hal-02095578/document https://hal.science/hal-02095578/file/Tamborski_et_al_2018_LnO_Resubmission_CLEAN.pdf https://doi.org/10.1002/lno.11169 |
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ftmeteofrance:oai:HAL:hal-02095578v1 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Météo-France: HAL |
op_collection_id |
ftmeteofrance |
language |
English |
topic |
lagoons circulation submarine groundwater discharge radium radon [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
spellingShingle |
lagoons circulation submarine groundwater discharge radium radon [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment Tamborski, Joseph Beek, Pieter, Van Rodellas, Valenti Monnin, Christophe Bergsma, Erwin Anschutz, Pierre Stieglitz, Thomas Heilbrun, Christina Cochran, J. Kirk Charbonnier, Celine Bejannin, Simon Beck, Aaron Temporal variability of lagoon–sea water exchange and seawater circulation through a Mediterranean barrier beach |
topic_facet |
lagoons circulation submarine groundwater discharge radium radon [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
description |
International audience The subterranean flow of water through sand barriers between coastal lagoons and the sea, driven by a positive hydraulic gradient, is a net new pathway for solute transfer to the sea. On the sea side of sand barriers, seawater circulation in the swash‐zone generates a flux of recycled and new solutes. The significance and temporal variability of these vectors to the French Mediterranean Sea is unknown, despite lagoons constituting ~ 50% of the coastline. A one‐dimensional 224Raex/223Ra reactive‐transport model was used to quantify water flow between a coastal lagoon (La Palme) and the sea over a 6‐month period. Horizontal flow between the lagoon and sea decreased from ~ 85 cm d−1 during May 2017 (0.3 m3 d−1 m−1 of shoreline) to ~ 20 cm d−1 in July and was negligible in the summer months thereafter due to a decreasing hydraulic gradient. Seawater circulation in the swash‐zone varied from 10 to 52 cm d−1 (0.4–2.1 m3 d−1 m−1), driven by short‐term changes in the prevailing wind and wave regimes. Both flow paths supply minor dissolved silica fluxes on the order of ~ 3–10 mmol Si d−1 m−1. Lagoon–sea water exchange supplies a net dissolved inorganic carbon (DIC) flux (320–1100 mmol C d−1 m−1) two orders of magnitude greater than seawater circulation and may impact coastal ocean acidification. The subterranean flow of water through sand barriers represents a significant source of new DIC, and potentially other solutes, to the Mediterranean Sea during high lagoon water‐level periods and should be considered in seasonal element budgets. |
author2 |
Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Géosciences Environnement Toulouse (GET) Environnements et Paléoenvironnements OCéaniques (EPOC) Observatoire aquitain des sciences de l'univers (OASU) Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) Centre for Tropical Water and Aquatic Ecosystem Research (TropWATER) James Cook University (JCU) Stony Brook University SUNY (SBU) State University of New York (SUNY) Helmholtz Centre for Ocean Research Kiel (GEOMAR) |
format |
Article in Journal/Newspaper |
author |
Tamborski, Joseph Beek, Pieter, Van Rodellas, Valenti Monnin, Christophe Bergsma, Erwin Anschutz, Pierre Stieglitz, Thomas Heilbrun, Christina Cochran, J. Kirk Charbonnier, Celine Bejannin, Simon Beck, Aaron |
author_facet |
Tamborski, Joseph Beek, Pieter, Van Rodellas, Valenti Monnin, Christophe Bergsma, Erwin Anschutz, Pierre Stieglitz, Thomas Heilbrun, Christina Cochran, J. Kirk Charbonnier, Celine Bejannin, Simon Beck, Aaron |
author_sort |
Tamborski, Joseph |
title |
Temporal variability of lagoon–sea water exchange and seawater circulation through a Mediterranean barrier beach |
title_short |
Temporal variability of lagoon–sea water exchange and seawater circulation through a Mediterranean barrier beach |
title_full |
Temporal variability of lagoon–sea water exchange and seawater circulation through a Mediterranean barrier beach |
title_fullStr |
Temporal variability of lagoon–sea water exchange and seawater circulation through a Mediterranean barrier beach |
title_full_unstemmed |
Temporal variability of lagoon–sea water exchange and seawater circulation through a Mediterranean barrier beach |
title_sort |
temporal variability of lagoon–sea water exchange and seawater circulation through a mediterranean barrier beach |
publisher |
HAL CCSD |
publishDate |
2019 |
url |
https://hal.science/hal-02095578 https://hal.science/hal-02095578/document https://hal.science/hal-02095578/file/Tamborski_et_al_2018_LnO_Resubmission_CLEAN.pdf https://doi.org/10.1002/lno.11169 |
long_lat |
ENVELOPE(-67.524,-67.524,-67.581,-67.581) |
geographic |
Swash |
geographic_facet |
Swash |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
ISSN: 0024-3590 EISSN: 1939-5590 Limnology and Oceanography https://hal.science/hal-02095578 Limnology and Oceanography, 2019, 64, pp.2059-2080. ⟨10.1002/lno.11169⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1002/lno.11169 hal-02095578 https://hal.science/hal-02095578 https://hal.science/hal-02095578/document https://hal.science/hal-02095578/file/Tamborski_et_al_2018_LnO_Resubmission_CLEAN.pdf doi:10.1002/lno.11169 IRD: fdi:010088441 WOS: 000485001400016 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1002/lno.11169 |
container_title |
Limnology and Oceanography |
container_volume |
64 |
container_issue |
5 |
container_start_page |
2059 |
op_container_end_page |
2080 |
_version_ |
1802648702675845120 |
spelling |
ftmeteofrance:oai:HAL:hal-02095578v1 2024-06-23T07:55:54+00:00 Temporal variability of lagoon–sea water exchange and seawater circulation through a Mediterranean barrier beach Tamborski, Joseph Beek, Pieter, Van Rodellas, Valenti Monnin, Christophe Bergsma, Erwin Anschutz, Pierre Stieglitz, Thomas Heilbrun, Christina Cochran, J. Kirk Charbonnier, Celine Bejannin, Simon Beck, Aaron Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Géosciences Environnement Toulouse (GET) Environnements et Paléoenvironnements OCéaniques (EPOC) Observatoire aquitain des sciences de l'univers (OASU) Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) Centre for Tropical Water and Aquatic Ecosystem Research (TropWATER) James Cook University (JCU) Stony Brook University SUNY (SBU) State University of New York (SUNY) Helmholtz Centre for Ocean Research Kiel (GEOMAR) 2019 https://hal.science/hal-02095578 https://hal.science/hal-02095578/document https://hal.science/hal-02095578/file/Tamborski_et_al_2018_LnO_Resubmission_CLEAN.pdf https://doi.org/10.1002/lno.11169 en eng HAL CCSD Association for the Sciences of Limnology and Oceanography info:eu-repo/semantics/altIdentifier/doi/10.1002/lno.11169 hal-02095578 https://hal.science/hal-02095578 https://hal.science/hal-02095578/document https://hal.science/hal-02095578/file/Tamborski_et_al_2018_LnO_Resubmission_CLEAN.pdf doi:10.1002/lno.11169 IRD: fdi:010088441 WOS: 000485001400016 info:eu-repo/semantics/OpenAccess ISSN: 0024-3590 EISSN: 1939-5590 Limnology and Oceanography https://hal.science/hal-02095578 Limnology and Oceanography, 2019, 64, pp.2059-2080. ⟨10.1002/lno.11169⟩ lagoons circulation submarine groundwater discharge radium radon [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2019 ftmeteofrance https://doi.org/10.1002/lno.11169 2024-06-10T23:51:13Z International audience The subterranean flow of water through sand barriers between coastal lagoons and the sea, driven by a positive hydraulic gradient, is a net new pathway for solute transfer to the sea. On the sea side of sand barriers, seawater circulation in the swash‐zone generates a flux of recycled and new solutes. The significance and temporal variability of these vectors to the French Mediterranean Sea is unknown, despite lagoons constituting ~ 50% of the coastline. A one‐dimensional 224Raex/223Ra reactive‐transport model was used to quantify water flow between a coastal lagoon (La Palme) and the sea over a 6‐month period. Horizontal flow between the lagoon and sea decreased from ~ 85 cm d−1 during May 2017 (0.3 m3 d−1 m−1 of shoreline) to ~ 20 cm d−1 in July and was negligible in the summer months thereafter due to a decreasing hydraulic gradient. Seawater circulation in the swash‐zone varied from 10 to 52 cm d−1 (0.4–2.1 m3 d−1 m−1), driven by short‐term changes in the prevailing wind and wave regimes. Both flow paths supply minor dissolved silica fluxes on the order of ~ 3–10 mmol Si d−1 m−1. Lagoon–sea water exchange supplies a net dissolved inorganic carbon (DIC) flux (320–1100 mmol C d−1 m−1) two orders of magnitude greater than seawater circulation and may impact coastal ocean acidification. The subterranean flow of water through sand barriers represents a significant source of new DIC, and potentially other solutes, to the Mediterranean Sea during high lagoon water‐level periods and should be considered in seasonal element budgets. Article in Journal/Newspaper Ocean acidification Météo-France: HAL Swash ENVELOPE(-67.524,-67.524,-67.581,-67.581) Limnology and Oceanography 64 5 2059 2080 |