Loading…
Hydrodynamical transport structure and lagrangian connectivity of circulations in the Pearl River Estuary
Using a three-dimensional (3D) hydrodynamic model, this study explored the seasonal hydrodynamic transport structure in the Pearl River Estuary and illustrated the intrinsic connectivity under multiscale motions from a Lagrangian perspective. Generally, the surface Lagrangian residual current (U L )...
Saved in:
Published in: | Frontiers in Marine Science 2022-10, Vol.9 |
---|---|
Main Authors: | , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
cited_by | cdi_FETCH-LOGICAL-c354t-e37e03319f6d42c72d35443d2817a34fb686b3991064aaaaaaf11724f68e7a4b3 |
---|---|
cites | cdi_FETCH-LOGICAL-c354t-e37e03319f6d42c72d35443d2817a34fb686b3991064aaaaaaf11724f68e7a4b3 |
container_end_page | |
container_issue | |
container_start_page | |
container_title | Frontiers in Marine Science |
container_volume | 9 |
creator | Chu, Nanyang Liu, Guangliang Xu, Jie Yao, Peng Du, Yan Liu, Zhiqiang Cai, Zhongya |
description | Using a three-dimensional (3D) hydrodynamic model, this study explored the seasonal hydrodynamic transport structure in the Pearl River Estuary and illustrated the intrinsic connectivity under multiscale motions from a Lagrangian perspective. Generally, the surface Lagrangian residual current (U
L
) is uniformly southwestward/southeastward in summer/winter, with a stronger intensity in the lower estuary. The bottom U
L
features in the southeastward direction in the upper estuary and northwest direction in the lower estuary. The fluvial–tide interaction line advances southeastward and northwestward in summer and winter, respectively. The U
L
captured the major transport processes and was in good agreement with the mean surface sediment transport patterns. In the transition region between Lantau Island and Neilingding Island, where it is largely affected by the interaction between the periodic tidal current and river discharge, the spatially averaged U
L
showed intensified intratidal variations and had a larger difference with the locally temporally averaged Eulerian residual current. The remarkable Lagrangian coherent structures that illustrated the transport paths and transport convergence regions were identified, which are generally consistent with the bottom sediment depocenters. Based on the Lagrangian connectivity analysis, it was revealed that a barrier between the western and eastern estuaries existed, which was weakened by the strong river discharge during summer. Two convergence regions near the Macau and Hong Kong waters were identified, where the sediment and pollutants easily settled. The study demonstrated the importance of the Lagrangian view in understanding the hydrodynamic process and transport structure in the estuary–shelf regions. |
doi_str_mv | 10.3389/fmars.2022.996551 |
format | article |
fullrecord | <record><control><sourceid>doaj_cross</sourceid><recordid>TN_cdi_doaj_primary_oai_doaj_org_article_ce775f7b1d384b0ba6a5e46e252515ab</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><doaj_id>oai_doaj_org_article_ce775f7b1d384b0ba6a5e46e252515ab</doaj_id><sourcerecordid>oai_doaj_org_article_ce775f7b1d384b0ba6a5e46e252515ab</sourcerecordid><originalsourceid>FETCH-LOGICAL-c354t-e37e03319f6d42c72d35443d2817a34fb686b3991064aaaaaaf11724f68e7a4b3</originalsourceid><addsrcrecordid>eNpNkM1KAzEUhQdRsNQ-gLu8wNT8Z2YppdpCQRFdhzuZpKZMJyXJFObt7Y-Id3Mu58C3-IrikeA5Y1X95PYQ05xiSud1LYUgN8WE0lqWSnFx---_L2Yp7TDGhHEseD0p_GpsY2jHHvbeQIdyhD4dQswo5TiYPESLoG9RB9vTsvXQIxP63prsjz6PKDhkfDRDB9mHPiHfo_xt0buF2KEPf7QRLVMeII4PxZ2DLtnZb06Lr5fl52JVbt5e14vnTWmY4Lm0TFnMGKmdbDk1iranmrOWVkQB466RlWxYXRMsOVzOEaIod7KyCnjDpsX6ym0D7PQh-pOcUQfw-lKEuNUQszed1cYqJZxqSMsq3uAGJAjLpaWCCiLgzCJXlokhpWjdH49gfVavL-r1Wb2-qmc_8dZ6WA</addsrcrecordid><sourcetype>Open Website</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Hydrodynamical transport structure and lagrangian connectivity of circulations in the Pearl River Estuary</title><source>Publicly Available Content Database</source><creator>Chu, Nanyang ; Liu, Guangliang ; Xu, Jie ; Yao, Peng ; Du, Yan ; Liu, Zhiqiang ; Cai, Zhongya</creator><creatorcontrib>Chu, Nanyang ; Liu, Guangliang ; Xu, Jie ; Yao, Peng ; Du, Yan ; Liu, Zhiqiang ; Cai, Zhongya</creatorcontrib><description>Using a three-dimensional (3D) hydrodynamic model, this study explored the seasonal hydrodynamic transport structure in the Pearl River Estuary and illustrated the intrinsic connectivity under multiscale motions from a Lagrangian perspective. Generally, the surface Lagrangian residual current (U
L
) is uniformly southwestward/southeastward in summer/winter, with a stronger intensity in the lower estuary. The bottom U
L
features in the southeastward direction in the upper estuary and northwest direction in the lower estuary. The fluvial–tide interaction line advances southeastward and northwestward in summer and winter, respectively. The U
L
captured the major transport processes and was in good agreement with the mean surface sediment transport patterns. In the transition region between Lantau Island and Neilingding Island, where it is largely affected by the interaction between the periodic tidal current and river discharge, the spatially averaged U
L
showed intensified intratidal variations and had a larger difference with the locally temporally averaged Eulerian residual current. The remarkable Lagrangian coherent structures that illustrated the transport paths and transport convergence regions were identified, which are generally consistent with the bottom sediment depocenters. Based on the Lagrangian connectivity analysis, it was revealed that a barrier between the western and eastern estuaries existed, which was weakened by the strong river discharge during summer. Two convergence regions near the Macau and Hong Kong waters were identified, where the sediment and pollutants easily settled. The study demonstrated the importance of the Lagrangian view in understanding the hydrodynamic process and transport structure in the estuary–shelf regions.</description><identifier>ISSN: 2296-7745</identifier><identifier>EISSN: 2296-7745</identifier><identifier>DOI: 10.3389/fmars.2022.996551</identifier><language>eng</language><publisher>Frontiers Media S.A</publisher><subject>circulation connectivity ; hydrodynamical transport structure ; Lagrangian analysis ; pearl river estuary ; residual current</subject><ispartof>Frontiers in Marine Science, 2022-10, Vol.9</ispartof><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c354t-e37e03319f6d42c72d35443d2817a34fb686b3991064aaaaaaf11724f68e7a4b3</citedby><cites>FETCH-LOGICAL-c354t-e37e03319f6d42c72d35443d2817a34fb686b3991064aaaaaaf11724f68e7a4b3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Chu, Nanyang</creatorcontrib><creatorcontrib>Liu, Guangliang</creatorcontrib><creatorcontrib>Xu, Jie</creatorcontrib><creatorcontrib>Yao, Peng</creatorcontrib><creatorcontrib>Du, Yan</creatorcontrib><creatorcontrib>Liu, Zhiqiang</creatorcontrib><creatorcontrib>Cai, Zhongya</creatorcontrib><title>Hydrodynamical transport structure and lagrangian connectivity of circulations in the Pearl River Estuary</title><title>Frontiers in Marine Science</title><description>Using a three-dimensional (3D) hydrodynamic model, this study explored the seasonal hydrodynamic transport structure in the Pearl River Estuary and illustrated the intrinsic connectivity under multiscale motions from a Lagrangian perspective. Generally, the surface Lagrangian residual current (U
L
) is uniformly southwestward/southeastward in summer/winter, with a stronger intensity in the lower estuary. The bottom U
L
features in the southeastward direction in the upper estuary and northwest direction in the lower estuary. The fluvial–tide interaction line advances southeastward and northwestward in summer and winter, respectively. The U
L
captured the major transport processes and was in good agreement with the mean surface sediment transport patterns. In the transition region between Lantau Island and Neilingding Island, where it is largely affected by the interaction between the periodic tidal current and river discharge, the spatially averaged U
L
showed intensified intratidal variations and had a larger difference with the locally temporally averaged Eulerian residual current. The remarkable Lagrangian coherent structures that illustrated the transport paths and transport convergence regions were identified, which are generally consistent with the bottom sediment depocenters. Based on the Lagrangian connectivity analysis, it was revealed that a barrier between the western and eastern estuaries existed, which was weakened by the strong river discharge during summer. Two convergence regions near the Macau and Hong Kong waters were identified, where the sediment and pollutants easily settled. The study demonstrated the importance of the Lagrangian view in understanding the hydrodynamic process and transport structure in the estuary–shelf regions.</description><subject>circulation connectivity</subject><subject>hydrodynamical transport structure</subject><subject>Lagrangian analysis</subject><subject>pearl river estuary</subject><subject>residual current</subject><issn>2296-7745</issn><issn>2296-7745</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>DOA</sourceid><recordid>eNpNkM1KAzEUhQdRsNQ-gLu8wNT8Z2YppdpCQRFdhzuZpKZMJyXJFObt7Y-Id3Mu58C3-IrikeA5Y1X95PYQ05xiSud1LYUgN8WE0lqWSnFx---_L2Yp7TDGhHEseD0p_GpsY2jHHvbeQIdyhD4dQswo5TiYPESLoG9RB9vTsvXQIxP63prsjz6PKDhkfDRDB9mHPiHfo_xt0buF2KEPf7QRLVMeII4PxZ2DLtnZb06Lr5fl52JVbt5e14vnTWmY4Lm0TFnMGKmdbDk1iranmrOWVkQB466RlWxYXRMsOVzOEaIod7KyCnjDpsX6ym0D7PQh-pOcUQfw-lKEuNUQszed1cYqJZxqSMsq3uAGJAjLpaWCCiLgzCJXlokhpWjdH49gfVavL-r1Wb2-qmc_8dZ6WA</recordid><startdate>20221014</startdate><enddate>20221014</enddate><creator>Chu, Nanyang</creator><creator>Liu, Guangliang</creator><creator>Xu, Jie</creator><creator>Yao, Peng</creator><creator>Du, Yan</creator><creator>Liu, Zhiqiang</creator><creator>Cai, Zhongya</creator><general>Frontiers Media S.A</general><scope>AAYXX</scope><scope>CITATION</scope><scope>DOA</scope></search><sort><creationdate>20221014</creationdate><title>Hydrodynamical transport structure and lagrangian connectivity of circulations in the Pearl River Estuary</title><author>Chu, Nanyang ; Liu, Guangliang ; Xu, Jie ; Yao, Peng ; Du, Yan ; Liu, Zhiqiang ; Cai, Zhongya</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c354t-e37e03319f6d42c72d35443d2817a34fb686b3991064aaaaaaf11724f68e7a4b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>circulation connectivity</topic><topic>hydrodynamical transport structure</topic><topic>Lagrangian analysis</topic><topic>pearl river estuary</topic><topic>residual current</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Chu, Nanyang</creatorcontrib><creatorcontrib>Liu, Guangliang</creatorcontrib><creatorcontrib>Xu, Jie</creatorcontrib><creatorcontrib>Yao, Peng</creatorcontrib><creatorcontrib>Du, Yan</creatorcontrib><creatorcontrib>Liu, Zhiqiang</creatorcontrib><creatorcontrib>Cai, Zhongya</creatorcontrib><collection>CrossRef</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>Frontiers in Marine Science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Chu, Nanyang</au><au>Liu, Guangliang</au><au>Xu, Jie</au><au>Yao, Peng</au><au>Du, Yan</au><au>Liu, Zhiqiang</au><au>Cai, Zhongya</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Hydrodynamical transport structure and lagrangian connectivity of circulations in the Pearl River Estuary</atitle><jtitle>Frontiers in Marine Science</jtitle><date>2022-10-14</date><risdate>2022</risdate><volume>9</volume><issn>2296-7745</issn><eissn>2296-7745</eissn><abstract>Using a three-dimensional (3D) hydrodynamic model, this study explored the seasonal hydrodynamic transport structure in the Pearl River Estuary and illustrated the intrinsic connectivity under multiscale motions from a Lagrangian perspective. Generally, the surface Lagrangian residual current (U
L
) is uniformly southwestward/southeastward in summer/winter, with a stronger intensity in the lower estuary. The bottom U
L
features in the southeastward direction in the upper estuary and northwest direction in the lower estuary. The fluvial–tide interaction line advances southeastward and northwestward in summer and winter, respectively. The U
L
captured the major transport processes and was in good agreement with the mean surface sediment transport patterns. In the transition region between Lantau Island and Neilingding Island, where it is largely affected by the interaction between the periodic tidal current and river discharge, the spatially averaged U
L
showed intensified intratidal variations and had a larger difference with the locally temporally averaged Eulerian residual current. The remarkable Lagrangian coherent structures that illustrated the transport paths and transport convergence regions were identified, which are generally consistent with the bottom sediment depocenters. Based on the Lagrangian connectivity analysis, it was revealed that a barrier between the western and eastern estuaries existed, which was weakened by the strong river discharge during summer. Two convergence regions near the Macau and Hong Kong waters were identified, where the sediment and pollutants easily settled. The study demonstrated the importance of the Lagrangian view in understanding the hydrodynamic process and transport structure in the estuary–shelf regions.</abstract><pub>Frontiers Media S.A</pub><doi>10.3389/fmars.2022.996551</doi><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 2296-7745 |
ispartof | Frontiers in Marine Science, 2022-10, Vol.9 |
issn | 2296-7745 2296-7745 |
language | eng |
recordid | cdi_doaj_primary_oai_doaj_org_article_ce775f7b1d384b0ba6a5e46e252515ab |
source | Publicly Available Content Database |
subjects | circulation connectivity hydrodynamical transport structure Lagrangian analysis pearl river estuary residual current |
title | Hydrodynamical transport structure and lagrangian connectivity of circulations in the Pearl River Estuary |
url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-02T11%3A10%3A55IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-doaj_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Hydrodynamical%20transport%20structure%20and%20lagrangian%20connectivity%20of%20circulations%20in%20the%20Pearl%20River%20Estuary&rft.jtitle=Frontiers%20in%20Marine%20Science&rft.au=Chu,%20Nanyang&rft.date=2022-10-14&rft.volume=9&rft.issn=2296-7745&rft.eissn=2296-7745&rft_id=info:doi/10.3389/fmars.2022.996551&rft_dat=%3Cdoaj_cross%3Eoai_doaj_org_article_ce775f7b1d384b0ba6a5e46e252515ab%3C/doaj_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c354t-e37e03319f6d42c72d35443d2817a34fb686b3991064aaaaaaf11724f68e7a4b3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true |