Tidal Numerical Modeling by the Optimized Boundary Conditions in Haizhou Bay of the Yellow Sea

HUANG Chenhu; ZHAI Guojun

doi:10.13203/j.whugis20210658

Volume 47 Issue 10

Oct. 2022

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Geomatics and Information Science of Wuhan University > 2022 > 47(10): 1785-1795. > DOI: 10.13203/j.whugis20210658

HUANG Chenhu, ZHAI Guojun. Tidal Numerical Modeling by the Optimized Boundary Conditions in Haizhou Bay of the Yellow Sea[J]. Geomatics and Information Science of Wuhan University, 2022, 47(10): 1785-1795. DOI: 10.13203/j.whugis20210658

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Tidal Numerical Modeling by the Optimized Boundary Conditions in Haizhou Bay of the Yellow Sea

HUANG Chenhu^{1, 2,},
ZHAI Guojun^2, ,

1.
College of Intelligence Science and Technology, National University of Defense Technology, Changsha 410073, China
2.
Tianjin Institute of Hydrographic Surveying and Charting, Tianjin 300061, China

Funds:

The National Natural Science Foundation of China 41974005

The National Natural Science Foundation of China 41876103

The National Natural Science Foundation of China 41804011

More Information

Author Bio:
HUANG Chenhu, PhD candidate, senior engineer, specializes in bathymetry sounding data processing and tide analysis. E-mail: hchhch-1997@163.com
Corresponding author:
ZHAI Guojun, PhD, professor. E-mail: zhaigj@163.com
Received Date: March 02, 2022
Available Online: March 18, 2022
Published Date: October 04, 2022

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Abstract

Abstract

Objectives Due to the joint constraints of boundary conditions, including seabed topography, driven water level at open boundary (DWLOB) and bottom friction coefficient (BFC), the accuracy of the tidal numerical modeling in coastal and offshore waters is relatively low.
Methods This paper intends to synchronously optimize the multiple boundary conditions, including seabed topography, DWLOB, and BFC, to improve the accuracy of the tidal numerical modeling in China's coastal and offshore waters for the hydrographic surveying and mapping. This paper simulates the tidal model of Haizhou Bay of the Yellow Sea in China, using a two-dimensional tide numerical model (2D-MIKE21) and based on the synchronously optimized boundary conditions. The water depth with higher resolution and accuracy than the charted depth is used as the seabed topography. The DWLOB is calculated from 12 tidal constituents of the regional tidal model of China seas(CST1). The calculation of the BFC takes into account the spatial variation of water depth.
Results For validation, we compare the simulated model with the 1-year tide tables from 6 tide gauges in Haizhou Bay and the CST1 model at 24 randomly selected points, and get the total root sum squares of the 12 tidal constituents of 5.52 cm and 7.10 cm, respectively. The simulated tide model and CST1 are also compared with the 1-month observations at two tide gauges in Haizhou Bay, and the former has a smaller mean square error than the latter.
Conclusions The proposed strategy provides a new method for tidal numerical modeling in coastal and offshore waters. This study also shows that it is feasible to obtain the astro-meteorological constituent Sa by tidal numerical modeling. It should be noted that, the wind effect is also not considered in this study due to its strong randomness and the difficulty in obtaining data for one year. We can use the simulated water level heights and the short-term wind velocity and direction as the better open boundary and initial conditions to carry out the short-term tidal modeling in coastal and offshore waters, which can generate the residual water level or storm surge.
- seabed geography,
- driven water level at open boundary,
- bottom friction coefficient,
- astro-meteorological constituent

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Tidal Numerical Modeling by the Optimized Boundary Conditions in Haizhou Bay of the Yellow Sea

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