2011
DOI: 10.1002/fld.2523
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A dual‐weighted trust‐region adaptive POD 4‐D Var applied to a finite‐volume shallow water equations model on the sphere

Abstract: SUMMARYIn this paper we study solutions of an inverse problem for a global shallow water model controlling its initial conditions specified from the 40-yr ECMWF Re-analysis (ERA-40) data sets, in the presence of full or incomplete observations being assimilated in a time interval (window of assimilation) with or without background error covariance terms.

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Cited by 31 publications
(20 citation statements)
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“…In a series of papers (see e.g. [31,36,37]) Navon et al proposed a dual-weighted POD method, where the weights assigned to each snapshot were derived from an adjoint related to the optimality system of a variational data assimilation problem in meteorology. It is also known that for compressible flows the choice of inner product and weighting of the different flow variables (velocity, pressure, speed of sound) in the snapshot matrix can have a large effect on the stability and accuracy of the ROM [14,35].…”
Section: "If It Is Not In the Snapshots It Is Not In The Rom"mentioning
confidence: 99%
“…In a series of papers (see e.g. [31,36,37]) Navon et al proposed a dual-weighted POD method, where the weights assigned to each snapshot were derived from an adjoint related to the optimality system of a variational data assimilation problem in meteorology. It is also known that for compressible flows the choice of inner product and weighting of the different flow variables (velocity, pressure, speed of sound) in the snapshot matrix can have a large effect on the stability and accuracy of the ROM [14,35].…”
Section: "If It Is Not In the Snapshots It Is Not In The Rom"mentioning
confidence: 99%
“…Thus, the inverse background-error covariance cannot be computed numerically. This issue is addressed in our 4D-Var implementation with the approach used in Chen et al (2011), i.e. by applying the change-of-variables transformation δ b (x) = x − x b = B 1/2 z and using z as the control variable.…”
Section: Background-error Covariance Matrixmentioning
confidence: 99%
“…Proper orthogonal decomposition (POD) provides optimal basis for the reduced-order model (ROM) and has many industrial applications, which includes climate modeling of atmospheric and oceanic flows. 2,[4][5][6][7][8][9] Its other applications are structural vibrations, 3, 10, 11 ecosystems, 12 low-dimensional dynamics modeling, 13-17 stochastic partial-differential equations, [18][19][20] and optimization. [21][22][23] The conventional ROM is developed by Galerkin projection of the POD modes onto the governing equations that include heat equation, Burgers equation, and Navier-Stokes equations.…”
Section: Introductionmentioning
confidence: 99%