4,172 research outputs found

    Optimal boundary conditions at the staircase-shaped coastlines

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    A 4D-Var data assimilation technique is applied to the rectangular-box configuration of the NEMO in order to identify the optimal parametrization of boundary conditions at lateral boundaries. The case of the staircase-shaped coastlines is studied by rotating the model grid around the center of the box. It is shown that, in some cases, the formulation of the boundary conditions at the exact boundary leads to appearance of exponentially growing modes while optimal boundary conditions allow to correct the errors induced by the staircase-like appriximation of the coastline.Comment: Submitted to Ocean Dynamics. (27/02/2014

    Sensitivity of a Barotropic Ocean Model to Perturbations of the Bottom Topography

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    In this paper, we look for an operator that describes the relationship between small errors in representation of the bottom topography in a barotropic ocean model and the model's solution. The study shows that the model's solution is very sensitive to topography perturbations in regions where the flow is turbulent. On the other hand, the flow exhibits low sensitivity in laminar regions. The quantitative measure of sensitivity is influenced essentially by the error growing time. At short time scales, the sensitivity exhibits the polynomial dependence on the error growing time. And in the long time limit, the dependence becomes exponential

    Boundary conditions control for a Shallow-Water model

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    A variational data assimilation technique was used to estimate optimal discretization of interpolation operators and derivatives in the nodes adjacent to the rigid boundary. Assimilation of artificially generated observational data in the shallow-water model in a square box and assimilation of real observations in the model of the Black sea are discussed. It is shown in both experiments that controlling the discretization of operators near a rigid boundary can bring the model solution closer to observations as in the assimilation window and beyond the window. This type of control allows also to improve climatic variability of the model.Comment: arXiv admin note: substantial text overlap with arXiv:1112.4293, arXiv:1112.3503, arXiv:0905.470

    Singular value decomposition for the 2D fan-beam Radon transform of tensor fields

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    In this article we study the fan-beam Radon transform Dm{\cal D}_m of symmetrical solenoidal 2D tensor fields of arbitrary rank mm in a unit disc D\mathbb D as the operator, acting from the object space L2(D;Sm){\mathbf L}_{2}(\mathbb D; {\bf S}_m) to the data space L2([0,2π)×[0,2π)).L_2([0,2\pi)\times[0,2\pi)). The orthogonal polynomial basis sn,k(±m){\bf s}^{(\pm m)}_{n,k} of solenoidal tensor fields on the disc D\mathbb D was built with the help of Zernike polynomials and then a singular value decomposition (SVD) for the operator Dm{\cal D}_m was obtained. The inversion formula for the fan-beam tensor transform Dm{\cal D}_m follows from this decomposition. Thus obtained inversion formula can be used as a tomographic filter for splitting a known tensor field into potential and solenoidal parts. Numerical results are presented.Comment: LaTeX, 37 pages with 5 figure
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