Lagoon water-level oscillations driven by rainfall and wave climate
Barrier breaching and subsequent inlet formation represent critical processes that ensure the temporary or permanent connection and transference of water, nutrients, or living organisms between a lagoon and the open sea. Here, we investigate the conditions inducing natural barrier breaching through...
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ftunivalgarve:oai:sapientia.ualg.pt:10400.1/12913 2023-05-15T17:36:56+02:00 Lagoon water-level oscillations driven by rainfall and wave climate Gonzalez-Villanueva, R. Perez-Arlucea, M. Costas, S. 2017-12 http://hdl.handle.net/10400.1/12913 https://doi.org/10.1016/j.coastaleng.2017.09.013 eng eng Elsevier 0378-3839 1872-7379 http://hdl.handle.net/10400.1/12913 doi:10.1016/j.coastaleng.2017.09.013 openAccess https://creativecommons.org/licenses/by/4.0/ CC-BY North-Atlantic oscillation Dominated tidal inlet Iberian Peninsula Seasonal closure Coastal lakes Model Precipitation Estuaries Africa Impact article 2017 ftunivalgarve https://doi.org/10.1016/j.coastaleng.2017.09.013 2022-05-30T08:48:46Z Barrier breaching and subsequent inlet formation represent critical processes that ensure the temporary or permanent connection and transference of water, nutrients, or living organisms between a lagoon and the open sea. Here, we investigate the conditions inducing natural barrier breaching through a 34 months monitoring program of water-level oscillations within a shallow lagoon and the adjacent nearshore, at the Northern coast of the Iberian Peninsula, Louro lagoon. Seven natural openings were identified to have occurred during the three monitored wet seasons, from the 2009 to 2012, (Wet1, Wet2 and Wet3); four in the Wetl, two in the Wet2 and one in. the Wet3. The openings were grouped in three types depending on the observed relation between the lagoon water-level (L-wl), the estimated berm height (B-h) and the water-level at the beach (B-wl): (i) openings by lagoon outflow, which include those characterized by L-wl higher than B-h and lower B-wl; (ii) openings by wave inundation, including those induced by B-wl higher than B-h, and (iii) mixed openings, which result from a combination of the two previous conditions. We observed that L-wl is modulated by the rainfall regime (R-f) and can be explained by the accumulated precipitation. We estimated applying runup equations to obtain B-h and B-wl which depend on the wave climate and tidal level. The inlet lifespan was found to be regulated by the wave climate and rainfall regime; in particular barrier sealing was associated with a sudden increase in wave period and a reduction in precipitation. This work proves that the natural openings could be predicted successfully with support to medium term water-level monitoring programs, which in turn may significantly contribute to strategic decision making for management and conservation purposes. Xunta de Galicia [08MDS036000PR, PlanI2C-ED481B 2014/132-0] MICINN [CTM2012-39599-C03-01] Portuguese Science Foundation [IF/01047/2014] info:eu-repo/semantics/publishedVersion Article in Journal/Newspaper North Atlantic North Atlantic oscillation Universidade do Algarve: Sapienta Coastal Engineering 130 34 45 |
institution |
Open Polar |
collection |
Universidade do Algarve: Sapienta |
op_collection_id |
ftunivalgarve |
language |
English |
topic |
North-Atlantic oscillation Dominated tidal inlet Iberian Peninsula Seasonal closure Coastal lakes Model Precipitation Estuaries Africa Impact |
spellingShingle |
North-Atlantic oscillation Dominated tidal inlet Iberian Peninsula Seasonal closure Coastal lakes Model Precipitation Estuaries Africa Impact Gonzalez-Villanueva, R. Perez-Arlucea, M. Costas, S. Lagoon water-level oscillations driven by rainfall and wave climate |
topic_facet |
North-Atlantic oscillation Dominated tidal inlet Iberian Peninsula Seasonal closure Coastal lakes Model Precipitation Estuaries Africa Impact |
description |
Barrier breaching and subsequent inlet formation represent critical processes that ensure the temporary or permanent connection and transference of water, nutrients, or living organisms between a lagoon and the open sea. Here, we investigate the conditions inducing natural barrier breaching through a 34 months monitoring program of water-level oscillations within a shallow lagoon and the adjacent nearshore, at the Northern coast of the Iberian Peninsula, Louro lagoon. Seven natural openings were identified to have occurred during the three monitored wet seasons, from the 2009 to 2012, (Wet1, Wet2 and Wet3); four in the Wetl, two in the Wet2 and one in. the Wet3. The openings were grouped in three types depending on the observed relation between the lagoon water-level (L-wl), the estimated berm height (B-h) and the water-level at the beach (B-wl): (i) openings by lagoon outflow, which include those characterized by L-wl higher than B-h and lower B-wl; (ii) openings by wave inundation, including those induced by B-wl higher than B-h, and (iii) mixed openings, which result from a combination of the two previous conditions. We observed that L-wl is modulated by the rainfall regime (R-f) and can be explained by the accumulated precipitation. We estimated applying runup equations to obtain B-h and B-wl which depend on the wave climate and tidal level. The inlet lifespan was found to be regulated by the wave climate and rainfall regime; in particular barrier sealing was associated with a sudden increase in wave period and a reduction in precipitation. This work proves that the natural openings could be predicted successfully with support to medium term water-level monitoring programs, which in turn may significantly contribute to strategic decision making for management and conservation purposes. Xunta de Galicia [08MDS036000PR, PlanI2C-ED481B 2014/132-0] MICINN [CTM2012-39599-C03-01] Portuguese Science Foundation [IF/01047/2014] info:eu-repo/semantics/publishedVersion |
format |
Article in Journal/Newspaper |
author |
Gonzalez-Villanueva, R. Perez-Arlucea, M. Costas, S. |
author_facet |
Gonzalez-Villanueva, R. Perez-Arlucea, M. Costas, S. |
author_sort |
Gonzalez-Villanueva, R. |
title |
Lagoon water-level oscillations driven by rainfall and wave climate |
title_short |
Lagoon water-level oscillations driven by rainfall and wave climate |
title_full |
Lagoon water-level oscillations driven by rainfall and wave climate |
title_fullStr |
Lagoon water-level oscillations driven by rainfall and wave climate |
title_full_unstemmed |
Lagoon water-level oscillations driven by rainfall and wave climate |
title_sort |
lagoon water-level oscillations driven by rainfall and wave climate |
publisher |
Elsevier |
publishDate |
2017 |
url |
http://hdl.handle.net/10400.1/12913 https://doi.org/10.1016/j.coastaleng.2017.09.013 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
0378-3839 1872-7379 http://hdl.handle.net/10400.1/12913 doi:10.1016/j.coastaleng.2017.09.013 |
op_rights |
openAccess https://creativecommons.org/licenses/by/4.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1016/j.coastaleng.2017.09.013 |
container_title |
Coastal Engineering |
container_volume |
130 |
container_start_page |
34 |
op_container_end_page |
45 |
_version_ |
1766136589080068096 |