Cao, A., Guo, Z. & Lü, X. Inversion of two-dimensional tidal open boundary conditions of M2 constituent in the Bohai and Yellow Seas., Chin. J. Ocean. Limnol. 30, 868–875 (2012). https://doi.org/10.1007/s00343-012-1185-9
DOI:
Cao, A., Guo, Z. & Lü, X. Inversion of two-dimensional tidal open boundary conditions of M2 constituent in the Bohai and Yellow Seas., Chin. J. Ocean. Limnol. 30, 868–875 (2012). https://doi.org/10.1007/s00343-012-1185-9DOI:
Inversion of two-dimensional tidal open boundary conditions of M2 constituent in the Bohai and Yellow Seas
摘要
Abstract
Two-dimensional tidal open boundary conditions of the M2 constituent in the Bohai and Yellow Seas (BYS) have been estimated by assimilating T/P altimeter data. During inversion
independent point (IP) strategy was used
in which several IPs on the open boundary is assumed
values at these IPs can be optimized with an adjoint method
and those at other grid points are determined by linearly interpolating the values at IPs. The reasonability and feasibility of the model are tested by ideal twin experiments. In the practical experiment (PE) after assimilation
the cost function may reach 1% or less of its initial value. Mean absolute errors in amplitude and phase can be less than 5 cm and 5°
respectively
and the obtained co-chart can show the character of the M2 constituent in the BYS. The results of the PE indicate that using only two IPs on the open boundary can yield better simulated results.
关键词
Keywords
references
Fang G H. 1986. Tide and tidal current charts for the marginal seas adjacent to China. Chin. J. Oceanol. Limn., 4(1): 1–16.
Han G J, Li W, He Z J, L K, Ma J R. 2006. Assimilated tidal results of tidal gauge and TOPEX/POSEIDON data over the China Seas using a variational adjoint approach with a nonlinear numerical model. Adv. Atmos. Sci., 23: 449–460.
He Y J, Lü X Q, Qiu Z F, Zhao J P. 2004. Shallow water tidal constituents in the Bohai and the Yellow Sea from a numerical adjoint model with TOPEX/POSEIDON altimeter data. Cont. Shelf Res., 24: 1 521–1 529.
Kang S K, Lee S R, Lie H J. 1998. Fine grid tidal modeling of the Yellow and East China Seas. Cont. Shelf Res., 18: 739–772.
Lardner R W. 1993. Optimal control of an open boundary condition for a numerical tidal model. Comput. Method. Appl. M., 102: 367–387.
Lardner R W. 1995. Optimal assimilation of current and surface elevation data in a two-dimensional numerical tidal model. Appl. Math. Model., 19: 30–38.
Lefevre F, Le Provost C, Lyard F H. 2000. How can we improve a global ocean tide model at a redional scale? A test on the Yellow Sea and the East China Sea. J. Geophys. Res., 105: 8 707–8 725.
Lü X Q, Zhang J C. 2006. Numerical study on spatially varying bottom friction coefficient of a 2D tidal model with adjoint method. Cont. Shelf Res., 26: 1 905–1 923.
Munk W H. 1997. Once again: once again-tidal friction. Prog. Oceanogr., 40: 7–35.
Myers P E, Baptista M A. 2001. Inversion for tides in the Eastern North Pacific Ocean. Adv. Water Resour., 24: 505–519.
Seiler U. 1993. Estimation of open boundary conditions with the adjoint method. J. Geophys. Res., 98: 22 855–22 870.
Zhang J C, Lü X Q. 2010. Inversion of three-dimensional tidal currents in marginal seas by assimilating satellite altimetry. Comput. Method. Appl. M., 199: 3 125–3 136.
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