Variability of the Red River Plume in the Gulf of Tonkin as Revealed by Numerical Modeling and Clustering Analysis

We study the daily to interannual variability of the Red River plume in the Gulf of Tonkin from numerical simulations at high resolution over 6 years (2011–2016). Compared with observational data, the model results show good performance. To identify the plume, passive tracers are used in order to (1...

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Autores principales: Tung Nguyen-Duy, Nadia K. Ayoub, Patrick Marsaleix, Florence Toublanc, Pierre De Mey-Frémaux, Violaine Piton, Marine Herrmann, Thomas Duhaut, Manh Cuong Tran, Thanh Ngo-Duc
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Publicado: Frontiers Media S.A. 2021
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spelling oai:doaj.org-article:b4472272517849e0ae340f97f11afba52021-11-12T07:08:32ZVariability of the Red River Plume in the Gulf of Tonkin as Revealed by Numerical Modeling and Clustering Analysis2296-774510.3389/fmars.2021.772139https://doaj.org/article/b4472272517849e0ae340f97f11afba52021-11-01T00:00:00Zhttps://www.frontiersin.org/articles/10.3389/fmars.2021.772139/fullhttps://doaj.org/toc/2296-7745We study the daily to interannual variability of the Red River plume in the Gulf of Tonkin from numerical simulations at high resolution over 6 years (2011–2016). Compared with observational data, the model results show good performance. To identify the plume, passive tracers are used in order to (1) help distinguish the freshwater coming from different continental sources, including the Red River branches, and (2) avoid the low salinity effect due to precipitation. We first consider the buoyant plume formed by the Red River waters and three other nearby rivers along the Vietnamese coast. We show that the temporal evolution of the surface coverage of the plume is correlated with the runoff (within a lag), but that the runoff only cannot explain the variability of the river plume; other processes, such as winds and tides, are involved. Using a K-means unsupervised machine learning algorithm, the main patterns of the plume and their evolution in time are analyzed and linked to different environmental conditions. In winter, the plume is narrow and sticks along the coast most of the time due to the downcoast current and northeasterly wind. In early summer, the southwesterly monsoon wind makes the plume flow offshore. The plume reaches its highest coverage in September after the peak of runoff. Vertically, the plume thickness also shows seasonal variations. In winter, the plume is narrow and mixed over the whole water depth, while in summer, the plume can be detached both from the bottom and the coast. The plume can deepen offshore in summer, due to strong wind (in May, June) or specifically to a recurrent eddy occurring near 19°N (in August). This first analysis of the variability of the Red River plume can be used to provide a general picture of the transport of materials from the river to the ocean, for example in case of anthropogenic chemical substances leaked to the river. For this purpose, we provide maps of the receiving basins for the different river systems in the Gulf of Tonkin.Tung Nguyen-DuyTung Nguyen-DuyNadia K. AyoubPatrick MarsaleixFlorence ToublancPierre De Mey-FrémauxViolaine PitonViolaine PitonMarine HerrmannMarine HerrmannThomas DuhautManh Cuong TranManh Cuong TranThanh Ngo-DucFrontiers Media S.A.articleRed Riverriver plumecoastal ocean modelingK-meansclustering analysispassive tracersScienceQGeneral. Including nature conservation, geographical distributionQH1-199.5ENFrontiers in Marine Science, Vol 8 (2021)
institution DOAJ
collection DOAJ
language EN
topic Red River
river plume
coastal ocean modeling
K-means
clustering analysis
passive tracers
Science
Q
General. Including nature conservation, geographical distribution
QH1-199.5
spellingShingle Red River
river plume
coastal ocean modeling
K-means
clustering analysis
passive tracers
Science
Q
General. Including nature conservation, geographical distribution
QH1-199.5
Tung Nguyen-Duy
Tung Nguyen-Duy
Nadia K. Ayoub
Patrick Marsaleix
Florence Toublanc
Pierre De Mey-Frémaux
Violaine Piton
Violaine Piton
Marine Herrmann
Marine Herrmann
Thomas Duhaut
Manh Cuong Tran
Manh Cuong Tran
Thanh Ngo-Duc
Variability of the Red River Plume in the Gulf of Tonkin as Revealed by Numerical Modeling and Clustering Analysis
description We study the daily to interannual variability of the Red River plume in the Gulf of Tonkin from numerical simulations at high resolution over 6 years (2011–2016). Compared with observational data, the model results show good performance. To identify the plume, passive tracers are used in order to (1) help distinguish the freshwater coming from different continental sources, including the Red River branches, and (2) avoid the low salinity effect due to precipitation. We first consider the buoyant plume formed by the Red River waters and three other nearby rivers along the Vietnamese coast. We show that the temporal evolution of the surface coverage of the plume is correlated with the runoff (within a lag), but that the runoff only cannot explain the variability of the river plume; other processes, such as winds and tides, are involved. Using a K-means unsupervised machine learning algorithm, the main patterns of the plume and their evolution in time are analyzed and linked to different environmental conditions. In winter, the plume is narrow and sticks along the coast most of the time due to the downcoast current and northeasterly wind. In early summer, the southwesterly monsoon wind makes the plume flow offshore. The plume reaches its highest coverage in September after the peak of runoff. Vertically, the plume thickness also shows seasonal variations. In winter, the plume is narrow and mixed over the whole water depth, while in summer, the plume can be detached both from the bottom and the coast. The plume can deepen offshore in summer, due to strong wind (in May, June) or specifically to a recurrent eddy occurring near 19°N (in August). This first analysis of the variability of the Red River plume can be used to provide a general picture of the transport of materials from the river to the ocean, for example in case of anthropogenic chemical substances leaked to the river. For this purpose, we provide maps of the receiving basins for the different river systems in the Gulf of Tonkin.
format article
author Tung Nguyen-Duy
Tung Nguyen-Duy
Nadia K. Ayoub
Patrick Marsaleix
Florence Toublanc
Pierre De Mey-Frémaux
Violaine Piton
Violaine Piton
Marine Herrmann
Marine Herrmann
Thomas Duhaut
Manh Cuong Tran
Manh Cuong Tran
Thanh Ngo-Duc
author_facet Tung Nguyen-Duy
Tung Nguyen-Duy
Nadia K. Ayoub
Patrick Marsaleix
Florence Toublanc
Pierre De Mey-Frémaux
Violaine Piton
Violaine Piton
Marine Herrmann
Marine Herrmann
Thomas Duhaut
Manh Cuong Tran
Manh Cuong Tran
Thanh Ngo-Duc
author_sort Tung Nguyen-Duy
title Variability of the Red River Plume in the Gulf of Tonkin as Revealed by Numerical Modeling and Clustering Analysis
title_short Variability of the Red River Plume in the Gulf of Tonkin as Revealed by Numerical Modeling and Clustering Analysis
title_full Variability of the Red River Plume in the Gulf of Tonkin as Revealed by Numerical Modeling and Clustering Analysis
title_fullStr Variability of the Red River Plume in the Gulf of Tonkin as Revealed by Numerical Modeling and Clustering Analysis
title_full_unstemmed Variability of the Red River Plume in the Gulf of Tonkin as Revealed by Numerical Modeling and Clustering Analysis
title_sort variability of the red river plume in the gulf of tonkin as revealed by numerical modeling and clustering analysis
publisher Frontiers Media S.A.
publishDate 2021
url https://doaj.org/article/b4472272517849e0ae340f97f11afba5
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