Journal of Tropical Oceanography ›› 2023, Vol. 42 ›› Issue (4): 47-62.doi: 10.11978/2022174CSTR: 32234.14.2022174

• Marine Hydrology • Previous Articles     Next Articles

Investigation into the tidal propagation features along the tidal reach of the West River (Makou — Modaomen)

WU Jiaxing1,2,3(), WANG Haocheng1,2,3, ZHANG Lu1,2,3, ZHANG Zhuo1,2,3(), CHEN Peng1,2,3, LI Yuting1,2,3   

  1. 1. Key Laboratory of Virtual Geographic Environment, Nanjing Normal University, Nanjing 210023, China
    2. Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing 210023, China
    3. Jiangsu Key Laboratory for Numerical Simulation of Large Scale Complex Systems, Nanjing 210023, China
  • Received:2022-08-03 Revised:2022-09-16 Online:2023-07-10 Published:2022-09-21
  • Supported by:
    Open Fund of Key Laboratory of Water and Drought Disaster Defense, Ministry of Water Resources(KYFB202112010704); National Natural Science Foundation of China(42171465)

Abstract:

Based on the daily river discharge time series of Wuzhou station from 2015 to 2017, the spatial and temporal variations of tide levels along the tidal reach of the West River (Makou — Modaomen) were simulated by applying a one-two dimensional coupled numerical model, and considering the flood and dry season variation of Manning's coefficient. During the propagation of tidal waves from the estuary to the upstream of the river, the deformation characteristics of tidal waves, the spatial and temporal distribution of tidal extreme levels and the tide range attenuation characteristics of river were studied. The results show that the water level of the river is influenced by river discharge with obvious characteristics of flood and dry seasons; the daily average water level shows semimonthly cycle variation during spring and neap tide, and the semimonthly variation gradually increases along the upstream of the river, indicating that the ocean tidal waves propagate upstream of the river in the form of a semimonthly low-frequency tidal constituent; the tidal asymmetry is more and more obvious upstream due to the influence of river discharge, and the difference between the flood tide calendar time and ebb tide calendar time increases upstream. The extreme tide level at each hydrographic station tends to increase upstream due to the influence of river discharge, and occurs mostly during spring tide due to the action of the ocean tide. The tide range in the river channel tends to decrease from downstream to upstream, and the seasonal difference is significant, and the downstream stations of Denglongshan and Sanzao have obvious characteristics of semi-annual cycle.

Key words: tidal propagation, river-tide interaction, extreme tidal level