Fitting Cotidal Charts of Eight Major Tidal Components in the Bohai Sea, Yellow Sea Based on Chebyshev Polynomial Method

被引:6
作者
Wang, Qixiang [1 ,2 ,3 ]
Zhang, Yibo [1 ,2 ,3 ]
Wang, Yonggang [3 ,4 ,5 ,6 ]
Xu, Minjie [7 ]
Lv, Xianqing [1 ,2 ,3 ]
机构
[1] Ocean Univ China, Frontier Sci Ctr Deep Ocean Multispheres & Earth, Qingdao 266005, Peoples R China
[2] Ocean Univ China, Phys Oceanog Lab, Qingdao 266005, Peoples R China
[3] Pilot Natl Lab Marine Sci & Technol, Lab Reg Oceanog & Numer Modeling, Qingdao 266237, Peoples R China
[4] Minist Nat Resources, Inst Oceanog 1, Qingdao 266061, Peoples R China
[5] Minist Nat Resources, Key Lab Marine Sci & Numer Modeling, Qingdao 266061, Peoples R China
[6] Shandong Key Lab Marine Sci & Numer Modeling, Qingdao 266061, Peoples R China
[7] Yantai Univ, Ocean Sch, Yantai 264005, Peoples R China
基金
中国国家自然科学基金;
关键词
Chebyshev polynomial fitting; satellite observations; harmonic constants; data processing; MARGINAL SEAS; LEVEL; TIDES; ALTIMETER; INVERSION; REGION; MODEL;
D O I
10.3390/jmse10091219
中图分类号
U6 [水路运输]; P75 [海洋工程];
学科分类号
0814 ; 081505 ; 0824 ; 082401 ;
摘要
High-precision tidal harmonic constants are necessary for studies involving tides. This study proposes a new method combined with the adjoint assimilation model and the Chebyshev polynomial fitting (CPF) method to obtain the tidal harmonic constants in the shallow-water region of the Bohai and Yellow Sea (BYS). Based on the CPF method, the full-field harmonic constants and reliable cotidal charts of the eight major constituents (M-2, S-2, K-1, O-1, N-2, K-2, P-1 and Qi) were fitted from the X-TRACK products briefly and this method was effectively for coastal conditions. Compared with the observations of the X-TRACK products and tidal gauges, for the M-2 constituent, the TPXO9, Finite Element Solutions 2014 (FES2014), National Astronomical Observatory 99b (NAO.99b) and Empirical Ocean Tide 20 (EOT20) models yield the root-mean-square errors (RMSEs) of 18.50, 7.31, 18.73 and 13.32 cm, respectively, while the CPF method yields an RMSE of 10.74 cm. These results indicate that the CPF method could maintain high resolution and obtain accurate cotidal charts consistent with the simulations of the four models in shallow-water regions.
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页数:17
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