Encountering shoaling internal waves on the dispersal pathway of the pearl river plume in summer
Abstract Fundamentally, river plume dynamics are controlled by the buoyancy due to river effluent and mixing induced by local forcing such as winds and tides. Rarely the influence of far-field internal waves on the river plume dynamics is documented. Our 5-day fix-point measurements and underway aco...
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doaj-903e357f35ce4df2b20851c4b48209142021-01-17T12:43:28ZengNature Publishing GroupScientific Reports2045-23222021-01-0111111510.1038/s41598-020-80215-2Encountering shoaling internal waves on the dispersal pathway of the pearl river plume in summerJay Lee0James T. Liu1I-Huan Lee2Ke-Hsien Fu3Rick J. Yang4Wenping Gong5Jianping Gan6Department of Oceanography, National Sun Yat-Sen UniversityDepartment of Oceanography, National Sun Yat-Sen UniversityDepartment of Oceanography, National Sun Yat-Sen UniversityDepartment of Oceanography, National Sun Yat-Sen UniversityDepartment of Oceanography, National Sun Yat-Sen UniversitySchool of Marine Sciences, Sun Yat-Sen UniversityDepartment of Ocean Science & Department of Mathematics, School of Science, The Hong Kong University of Science and TechnologyAbstract Fundamentally, river plume dynamics are controlled by the buoyancy due to river effluent and mixing induced by local forcing such as winds and tides. Rarely the influence of far-field internal waves on the river plume dynamics is documented. Our 5-day fix-point measurements and underway acoustic profiling identified hydrodynamic processes on the dispersal pathway of the Pearl River plume. The river plume dispersal was driven by the SW monsoon winds that induced the intrusion of cold water near the bottom. The river effluent occupied the surface water, creating strong stratification and showing on-offshore variability due to tidal fluctuations. However, intermittent disruptions weakened stratification due to wind mixing and perturbations by nonlinear internal waves (NIWs) from the northern South China Sea (NSCS). During events of NIW encounter, significant drawdowns of the river plume up to 20 m occurred. The EOF deciphers and ranks the contributions of abovementioned processes: (1) the stratification/mixing coupled by wind-driven plume water and NIWs disruptions (81.7%); (2) the variation caused by tidal modulation (6.9%); and (3) the cold water intrusion induced by summer monsoon winds (5.1%). Our findings further improve the understanding of the Pearl River plume dynamics influenced by the NIWs from the NSCS.https://doi.org/10.1038/s41598-020-80215-2 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Jay Lee James T. Liu I-Huan Lee Ke-Hsien Fu Rick J. Yang Wenping Gong Jianping Gan |
spellingShingle |
Jay Lee James T. Liu I-Huan Lee Ke-Hsien Fu Rick J. Yang Wenping Gong Jianping Gan Encountering shoaling internal waves on the dispersal pathway of the pearl river plume in summer Scientific Reports |
author_facet |
Jay Lee James T. Liu I-Huan Lee Ke-Hsien Fu Rick J. Yang Wenping Gong Jianping Gan |
author_sort |
Jay Lee |
title |
Encountering shoaling internal waves on the dispersal pathway of the pearl river plume in summer |
title_short |
Encountering shoaling internal waves on the dispersal pathway of the pearl river plume in summer |
title_full |
Encountering shoaling internal waves on the dispersal pathway of the pearl river plume in summer |
title_fullStr |
Encountering shoaling internal waves on the dispersal pathway of the pearl river plume in summer |
title_full_unstemmed |
Encountering shoaling internal waves on the dispersal pathway of the pearl river plume in summer |
title_sort |
encountering shoaling internal waves on the dispersal pathway of the pearl river plume in summer |
publisher |
Nature Publishing Group |
series |
Scientific Reports |
issn |
2045-2322 |
publishDate |
2021-01-01 |
description |
Abstract Fundamentally, river plume dynamics are controlled by the buoyancy due to river effluent and mixing induced by local forcing such as winds and tides. Rarely the influence of far-field internal waves on the river plume dynamics is documented. Our 5-day fix-point measurements and underway acoustic profiling identified hydrodynamic processes on the dispersal pathway of the Pearl River plume. The river plume dispersal was driven by the SW monsoon winds that induced the intrusion of cold water near the bottom. The river effluent occupied the surface water, creating strong stratification and showing on-offshore variability due to tidal fluctuations. However, intermittent disruptions weakened stratification due to wind mixing and perturbations by nonlinear internal waves (NIWs) from the northern South China Sea (NSCS). During events of NIW encounter, significant drawdowns of the river plume up to 20 m occurred. The EOF deciphers and ranks the contributions of abovementioned processes: (1) the stratification/mixing coupled by wind-driven plume water and NIWs disruptions (81.7%); (2) the variation caused by tidal modulation (6.9%); and (3) the cold water intrusion induced by summer monsoon winds (5.1%). Our findings further improve the understanding of the Pearl River plume dynamics influenced by the NIWs from the NSCS. |
url |
https://doi.org/10.1038/s41598-020-80215-2 |
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