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Inverse 3D shallow water flow modelling of the continental shelf

机译:大陆架逆3D浅水流建模

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摘要

The adjoint method has been derived and implemented for solving inverse 3D shallow water flow modelling problems. Attention is concentrated on estimating the harmonic constants in the open boundary conditions, the space varying friction parameter, the space varying viscosity parameter and the depth values in a 3D shallow sea model of the entire European Continental Shelf. Here the estimation problem is formulated as a large-scale optimization problem that is solved with a gradient-based optimization method. The gradient is determined efficiently by using the solution of the adjoint problem. (C) 2002 Elsevier Science Ltd. All rights reserved. [References: 18]
机译:伴随方法已被导出并实现,用于解决逆3D浅水流建模问题。在整个欧洲大陆架的3D浅海模型中,注意力集中在估计开放边界条件下的谐波常数,空间变化的摩擦参数,空间变化的粘度参数和深度值。在此,将估计问题表述为大规模优化问题,可以通过基于梯度的优化方法来解决。通过使用伴随问题的解可以有效地确定梯度。 (C)2002 Elsevier ScienceLtd。保留所有权利。 [参考:18]

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