In meteorological and oceanological studies the classical approach for finding the numerical solution of the regional model consists in formulating and solving a Cauchy- Dirichlet problem. The boundary conditions are obtained by linear interpolation of coarse-grid data provided by a global model. Errors in boundary conditions due to interpolation may cause large deviations from the correct regional solu- tion. The methods developed to reduce these errors deal with continuous dynamic assimilation of known global data avail- able inside the regional domain. One of the approaches of this assimilation procedure performs a nudging of large-scale components of regional model solution to large-scale global data components by introducing relaxation forcing terms into the regional model equations. As a result, the obtained solu- tion is not a valid numerical solution to the original regional model. Another approach is the use a four-dimensional vari- ational data assimilation procedure which is free from the above-mentioned shortcoming. In this work we formulate the joint problem of finding the regional model solution and data assimilation as a PDE-constrained optimization prob- lem. Three simple model examples (ODE Burgers equa- tion, Rossby-Oboukhov equation, Korteweg-de Vries equa- tion) are considered in this paper. Numerical experiments indicate that the optimization approach can significantly im- prove the precision of the regional solution.
Continuous dynamic assimilation of the inner region data in hydrodynamics modelling: optimization approach
Feodor Pisnitchenko,I. A. Pisnichenko,J. Martínez,S. Santos
Published 2008 in Nonlinear Processes in Geophysics
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2008
- Venue
Nonlinear Processes in Geophysics
- Publication date
2008-01-10
- Fields of study
Mathematics, Physics, Engineering, Environmental Science
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