Nonlinear advection, Coriolis force, and frictional influence in the South Channel of the Yangtze Estuary, China

Zhong Yong Yang; He Qin Cheng; Jiu Fa Li

doi:10.1007/s11430-014-4946-9

Nonlinear advection, Coriolis force, and frictional influence in the South Channel of the Yangtze Estuary, China

Zhong Yong Yang
, He Qin Cheng^*
, Jiu Fa Li

^*此作品的通讯作者

河口海岸科学研究院

East China Normal University
China Three Gorges University

科研成果: 期刊稿件 › 文章 › 同行评审

13 引用（Scopus）

摘要

Observation data of along-estuary and lateral current velocities over a transect located at the South Channel of the Yangtze estuary was obtained during a spring tide in August 2011. Harmonic analysis was done on the current velocities to get a mean component and a semi-diurnal component. Based on these two components, the driving mechanisms of mean lateral flow and M₂ lateral tidal flow are shown and analyzed respectively. The dominant driving force of mean lateral flow is nonlinear advection and that of lateral M₂ tidal flow is Coriolis force. The friction plays an important role near the bottom and surface for both lateral mean flow and M₂ tidal flow.

源语言	英语
页（从-至）	429-435
页数	7
期刊	Science China Earth Sciences
卷	58
期	3
DOI	https://doi.org/10.1007/s11430-014-4946-9
出版状态	已出版 - 3月 2015

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@article{453e649665fe4680a277d10ae049139a,

title = "Nonlinear advection, Coriolis force, and frictional influence in the South Channel of the Yangtze Estuary, China",

abstract = "Observation data of along-estuary and lateral current velocities over a transect located at the South Channel of the Yangtze estuary was obtained during a spring tide in August 2011. Harmonic analysis was done on the current velocities to get a mean component and a semi-diurnal component. Based on these two components, the driving mechanisms of mean lateral flow and M2 lateral tidal flow are shown and analyzed respectively. The dominant driving force of mean lateral flow is nonlinear advection and that of lateral M2 tidal flow is Coriolis force. The friction plays an important role near the bottom and surface for both lateral mean flow and M2 tidal flow.",

keywords = "Coriolis force, friction, lateral flow, nonlinear advection",

author = "Yang, \{Zhong Yong\} and Cheng, \{He Qin\} and Li, \{Jiu Fa\}",

note = "Publisher Copyright: {\textcopyright} 2014, Science China Press and Springer-Verlag Berlin Heidelberg.",

year = "2015",

month = mar,

doi = "10.1007/s11430-014-4946-9",

language = "英语",

volume = "58",

pages = "429--435",

journal = "Science China Earth Sciences",

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TY - JOUR

T1 - Nonlinear advection, Coriolis force, and frictional influence in the South Channel of the Yangtze Estuary, China

AU - Yang, Zhong Yong

AU - Cheng, He Qin

AU - Li, Jiu Fa

PY - 2015/3

Y1 - 2015/3

N2 - Observation data of along-estuary and lateral current velocities over a transect located at the South Channel of the Yangtze estuary was obtained during a spring tide in August 2011. Harmonic analysis was done on the current velocities to get a mean component and a semi-diurnal component. Based on these two components, the driving mechanisms of mean lateral flow and M2 lateral tidal flow are shown and analyzed respectively. The dominant driving force of mean lateral flow is nonlinear advection and that of lateral M2 tidal flow is Coriolis force. The friction plays an important role near the bottom and surface for both lateral mean flow and M2 tidal flow.

AB - Observation data of along-estuary and lateral current velocities over a transect located at the South Channel of the Yangtze estuary was obtained during a spring tide in August 2011. Harmonic analysis was done on the current velocities to get a mean component and a semi-diurnal component. Based on these two components, the driving mechanisms of mean lateral flow and M2 lateral tidal flow are shown and analyzed respectively. The dominant driving force of mean lateral flow is nonlinear advection and that of lateral M2 tidal flow is Coriolis force. The friction plays an important role near the bottom and surface for both lateral mean flow and M2 tidal flow.

KW - Coriolis force

KW - friction

KW - lateral flow

KW - nonlinear advection

UR - https://www.scopus.com/pages/publications/84925496549

U2 - 10.1007/s11430-014-4946-9

DO - 10.1007/s11430-014-4946-9

M3 - 文章

AN - SCOPUS:84925496549

SN - 1674-7313

VL - 58

SP - 429

EP - 435

JO - Science China Earth Sciences

JF - Science China Earth Sciences

IS - 3

ER -

Nonlinear advection, Coriolis force, and frictional influence in the South Channel of the Yangtze Estuary, China

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