Estimates of ocean forecast error covariance derived from Hessian Singular Vectors

•Singular value decomposition was used to quantify expected ocean forecast errors.•A reduced rank approximation was used for the inverse analysis error covariance.•The method was applied to an idealized baroclinically unstable temperature gradient.•Forecast error estimates found to be consistent and...

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Veröffentlicht in:Ocean modelling (Oxford) 2015-05, Vol.89, p.104-121
Hauptverfasser: Smith, Kevin D., Moore, Andrew M., Arango, Hernan G.
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Sprache:eng
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Zusammenfassung:•Singular value decomposition was used to quantify expected ocean forecast errors.•A reduced rank approximation was used for the inverse analysis error covariance.•The method was applied to an idealized baroclinically unstable temperature gradient.•Forecast error estimates found to be consistent and reliable using standard measures.•Forecast errors growth primarily via a forward energy cascade. Experience in numerical weather prediction suggests that singular value decomposition (SVD) of a forecast can yield useful a priori information about the growth of forecast errors. It has been shown formally that SVD using the inverse of the expected analysis error covariance matrix to define the norm at initial time yields the Empirical Orthogonal Functions (EOFs) of the forecast error covariance matrix at the final time. Because of their connection to the 2nd derivative of the cost function in 4-dimensional variational (4D-Var) data assimilation, the initial time singular vectors defined in this way are often referred to as the Hessian Singular Vectors (HSVs). In the present study, estimates of ocean forecast errors and forecast error covariance were computed using SVD applied to a baroclinically unstable temperature front in a re-entrant channel using the Regional Ocean Modeling System (ROMS). An identical twin approach was used in which a truth run of the model was sampled to generate synthetic hydrographic observations that were then assimilated into the same model started from an incorrect initial condition using 4D-Var. The 4D-Var system was run sequentially, and forecasts were initialized from each ocean analysis. SVD was performed on the resulting forecasts to compute the HSVs and corresponding EOFs of the expected forecast error covariance matrix. In this study, a reduced rank approximation of the inverse expected analysis error covariance matrix was used to compute the HSVs and EOFs based on the Lanczos vectors computed during the 4D-Var minimization of the cost function. This has the advantage that the entire spectrum of HSVs and EOFs in the reduced space can be computed. The associated singular value spectrum is found to yield consistent and reliable estimates of forecast error variance in the space spanned by the EOFs. In addition, at long forecast lead times the resulting HSVs and companion EOFs are able to capture many features of the actual realized forecast error at the largest scales. Forecast error growth via the HSVs was found to be significantl
ISSN:1463-5003
1463-5011
DOI:10.1016/j.ocemod.2015.03.003