On Domain Localization in Ensemble-Based Kalman Filter Algorithms

Tijana Janjić Alfred Wegener Institute, Bremerhaven, Germany

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Lars Nerger Alfred Wegener Institute, Bremerhaven, Germany

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Alberta Albertella Institute for Astronomical und Physical Geodesy, Munich, Germany

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Jens Schröter Alfred Wegener Institute, Bremerhaven, Germany

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Sergey Skachko Department of Earth Sciences, University of Quebec in Montreal, Montreal, Canada

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Abstract

Ensemble Kalman filter methods are typically used in combination with one of two localization techniques. One technique is covariance localization, or direct forecast error localization, in which the ensemble-derived forecast error covariance matrix is Schur multiplied with a chosen correlation matrix. The second way of localization is by domain decomposition. Here, the assimilation is split into local domains in which the assimilation update is performed independently. Domain localization is frequently used in combination with filter algorithms that use the analysis error covariance matrix for the calculation of the gain like the ensemble transform Kalman filter (ETKF) and the singular evolutive interpolated Kalman filter (SEIK). However, since the local assimilations are performed independently, smoothness of the analysis fields across the subdomain boundaries becomes an issue of concern.

To address the problem of smoothness, an algorithm is introduced that uses domain localization in combination with a Schur product localization of the forecast error covariance matrix for each local subdomain. On a simple example, using the Lorenz-40 system, it is demonstrated that this modification can produce results comparable to those obtained with direct forecast error localization. In addition, these results are compared to the method that uses domain localization in combination with weighting of observations. In the simple example, the method using weighting of observations is less accurate than the new method, particularly if the observation errors are small.

Domain localization with weighting of observations is further examined in the case of assimilation of satellite data into the global finite-element ocean circulation model (FEOM) using the local SEIK filter. In this example, the use of observational weighting improves the accuracy of the analysis. In addition, depending on the correlation function used for weighting, the spectral properties of the solution can be improved.

Corresponding author address: Tijana Janjić, Alfred Wegener Institute, Bussestrasse 24, D-27570 Bremerhaven, Germany. E-mail: tijana.janjic.pfander@awi.de

This article is included in the Intercomparisons of 4D-Variational Assimilation and the Ensemble Kalman Filter special collection.

Abstract

Ensemble Kalman filter methods are typically used in combination with one of two localization techniques. One technique is covariance localization, or direct forecast error localization, in which the ensemble-derived forecast error covariance matrix is Schur multiplied with a chosen correlation matrix. The second way of localization is by domain decomposition. Here, the assimilation is split into local domains in which the assimilation update is performed independently. Domain localization is frequently used in combination with filter algorithms that use the analysis error covariance matrix for the calculation of the gain like the ensemble transform Kalman filter (ETKF) and the singular evolutive interpolated Kalman filter (SEIK). However, since the local assimilations are performed independently, smoothness of the analysis fields across the subdomain boundaries becomes an issue of concern.

To address the problem of smoothness, an algorithm is introduced that uses domain localization in combination with a Schur product localization of the forecast error covariance matrix for each local subdomain. On a simple example, using the Lorenz-40 system, it is demonstrated that this modification can produce results comparable to those obtained with direct forecast error localization. In addition, these results are compared to the method that uses domain localization in combination with weighting of observations. In the simple example, the method using weighting of observations is less accurate than the new method, particularly if the observation errors are small.

Domain localization with weighting of observations is further examined in the case of assimilation of satellite data into the global finite-element ocean circulation model (FEOM) using the local SEIK filter. In this example, the use of observational weighting improves the accuracy of the analysis. In addition, depending on the correlation function used for weighting, the spectral properties of the solution can be improved.

Corresponding author address: Tijana Janjić, Alfred Wegener Institute, Bussestrasse 24, D-27570 Bremerhaven, Germany. E-mail: tijana.janjic.pfander@awi.de

This article is included in the Intercomparisons of 4D-Variational Assimilation and the Ensemble Kalman Filter special collection.

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  • Albertella, A., R. Savcenko, W. Bosch, and R. Rummel, 2008: Dynamic ocean topography—The geodetic approach. Tech. Rep. 27, Institute for Astronomical and Physical Geodesy, 53 pp.

    • Search Google Scholar
    • Export Citation
  • Bishop, C. H., B. J. Etherton, and S. Majumdar, 2001: Adaptive sampling with the ensemble transform Kalman filter. Part I: Theoretical aspects. Mon. Wea. Rev., 129, 420436.

    • Search Google Scholar
    • Export Citation
  • Brankart, J.-M., C.-E. Testut, P. Brasseur, and J. Verron, 2003: Implementation of a multivariate data assimilation scheme for isopycnic coordinate ocean models: Application to a 1993-1996 hindcast of the North Atlantic Ocean circulation. J. Geophys. Res., 108, 3074, doi:10.1029/2001JC001198.

    • Search Google Scholar
    • Export Citation
  • Brusdal, K., J.-M. Brankart, G. Halberstadt, G. Evensen, P. Brasseur, P. van Leeuwen, E. Dombrowsky, and J. Verron, 2003: An evaluation of ensemble based assimilation methods with a layered OGCM. J. Mar. Syst., 40–41, 253289.

    • Search Google Scholar
    • Export Citation
  • Cohn, S. E., A. da Silva, J. Guo, M. Sienkiewicz, and D. Lamich, 1998: Assessing the effects of data selection with the DAO physical-space statistical analysis system. Mon. Wea. Rev., 126, 29132926.

    • Search Google Scholar
    • Export Citation
  • Evensen, G., 2003: The ensemble Kalman filter: Theoretical formulation and practical implementation. Ocean Dyn., 53, 343367.

  • Gaspari, G., and S. E. Cohn, 1999: Construction of correlation functions in two and three dimensions. Quart. J. Roy. Meteor. Soc., 125, 723757.

    • Search Google Scholar
    • Export Citation
  • Gelb, A., 1974: Applied Optimal Estimation. The M.I.T. Press, 382 pp.

  • Haugen, V. E., and G. Evensen, 2002: Assimilation of SLA and SST data into an OGCM for the Indian ocean. Ocean Dyn., 52, 133151.

  • Horn, R. A., and C. R. Johnson, 1985: Matrix Analysis. Cambridge University Press, 561 pp.

  • Houtekamer, P. L., and H. L. Mitchell, 1998: Data assimilation using an ensemble Kalman filter technique. Mon. Wea. Rev., 126, 796811.

    • Search Google Scholar
    • Export Citation
  • Houtekamer, P. L., and H. L. Mitchell, 2001: A sequential ensemble Kalman filter for atmospheric data assimilation. Mon. Wea. Rev., 129, 123137.

    • Search Google Scholar
    • Export Citation
  • Hunt, B. R., E. J. Kostelich, and I. Szunyogh, 2007: Efficient data assimilation for spatiotemporal chaos: A local ensemble transform Kalman filter. Physica D, 230, 112126.

    • Search Google Scholar
    • Export Citation
  • Janjić, T., and S. E. Cohn, 2006: Treatment of observation error due to unresolved scales in atmospheric data assimilation. Mon. Wea. Rev., 134, 29002915.

    • Search Google Scholar
    • Export Citation
  • Jekeli, C., 1981: Alternative methods to smooth the earth’s gravity field. Department of Geodetic Science and Surveying, Ohio State University, Columbus, OH, Rep. 327, 48 pp.

    • Search Google Scholar
    • Export Citation
  • Kepert, J., 2009: Covariance localisation and balance in an ensemble Kalman filter. Quart. J. Roy. Meteor. Soc., 135, 11571176.

  • Lorenc, A. C., 1981: A global three-dimensional multivariate statistical interpolation scheme. Mon. Wea. Rev., 109, 701721.

  • Lorenz, E. N., and K. A. Emanuel, 1998: Optimal sites for supplementary weather observations: Simulation with a small model. J. Atmos. Sci., 55, 399414.

    • Search Google Scholar
    • Export Citation
  • Mayer-Gürr, T., 2007: ITG-GRACE03s: The latest GRACE gravity field solution computed in Bonn. Joint Grace Science Team and DFG SPP Meeting, Potsdam, Germany.

    • Search Google Scholar
    • Export Citation
  • Mitchell, H. L., P. L. Houtekamer, and G. Pellerin, 2002: Ensemble size, balance, and model-error representation in an ensemble Kalman filter. Mon. Wea. Rev., 130, 27912808.

    • Search Google Scholar
    • Export Citation
  • Miyoshi, T., and S. Yamane, 2007: Local ensemble transform Kalman filter with an AGCM at a T159/L48 resolution. Mon. Wea. Rev., 135, 38413861.

    • Search Google Scholar
    • Export Citation
  • Nerger, L., and W. W. Gregg, 2007: Assimilation of SeaWiFS data into a global ocean-biogeochemical model using a local SEIK filter. J. Mar. Syst., 68, 237254.

    • Search Google Scholar
    • Export Citation
  • Nerger, L., W. Hiller, and J. Schröter, 2005: PDAF—The parallel data assimilation framework: Experiences with Kalman filtering. Use of High Performance Computing in Meteorology: Proceedings of the 11th ECMWF Workshop, W. Zwieflhofer and G. Mozdzynski, Eds., World Scientific, 63–83.

    • Search Google Scholar
    • Export Citation
  • Nerger, L., S. Danilov, W. Hiller, and J. Schröter, 2006: Using sea level data to constrain a finite-element primitive-equation ocean model with a local SEIK filter. Ocean Dyn., 56, 634649.

    • Search Google Scholar
    • Export Citation
  • Ott, E., and Coauthors, 2004: A local ensemble Kalman filter for atmospheric data assimilation. Tellus, 56A, 415428.

  • Penduff, T., P. Brasseur, C.-E. Testut, B. Barnier, and J. Verron, 2002: A four-year eddy-permitting assimilation of sea-surface temperature and altimetric data in the South Atlantic Ocean. J. Mar. Res., 60, 805833.

    • Search Google Scholar
    • Export Citation
  • Pham, D. T., 2001: Stochastic methods for sequential data assimilation in strongly nonlinear systems. Mon. Wea. Rev., 129, 11941207.

  • Pham, D. T., J. Verron, and M. C. Roubaud, 1998: A singular evolutive extended Kalman filter for data assimilation in oceanography. J. Mar. Syst., 16, 323340.

    • Search Google Scholar
    • Export Citation
  • Rio, M.-H., P. Schaeffer, J.-M. Lemoine, and F. Hernandez, 2005: Estimation of the ocean mean dynamic topography through the combination of altimetric data, in-situ measurements and GRACE geoid: From global to regional studies. Proc. GOCINA Int. Workshop, Luxembourg.

    • Search Google Scholar
    • Export Citation
  • Sakov, P., and P. R. Oke, 2008: Implications of the form of the ensemble transformation in the ensemble square root filters. Mon. Wea. Rev., 136, 10421053.

    • Search Google Scholar
    • Export Citation
  • Skachko, S., S. Danilov, T. Janjić, J. Schroeter, D. Sidorenko, R. Savchenko, and W. Bosch, 2008: Sequential assimilation of multi-mission dynamical topography into a global finite-element ocean model. Ocean Sci., 4, 307318.

    • Search Google Scholar
    • Export Citation
  • Wahr, J., F. Bryan, and M. Molenaar, 1998: Time variability of the earth’s gravity field: Hydrological and oceanic effects and their possible detection using GRACE. J. Geophys. Res., 103 (B12), 30 20530 229.

    • Search Google Scholar
    • Export Citation
  • Wang, Q., S. Danilov, and J. Schröter, 2008: Finite element ocean circulation model based on triangular prismatic elements with application in studying the effect of topography representation. J. Geophys. Res., 113, C05015, doi:10.1029/2007JC004482.

    • Search Google Scholar
    • Export Citation
  • Whitaker, J. S., and T. M. Hamill, 2002: Ensemble data assimilation without perturbed observations. Mon. Wea. Rev., 130, 19131924.

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