TY - JOUR
T1 - Chaotic dynamics and the role of covariance inflation for reduced rank Kalman filters with model error
AU - Grudzien, Colin
AU - Carrassi, Alberto
AU - Bocquet, Marc
N1 - Publisher Copyright:
© 2018 All rights reserved.
PY - 2018/9/4
Y1 - 2018/9/4
N2 - The ensemble Kalman filter and its variants have shown to be robust for data assimilation in high dimensional geophysical models, with localization, using ensembles of extremely small size relative to the model dimension. However, a reduced rank representation of the estimated covariance leaves a large dimensional complementary subspace unfiltered. Utilizing the dynamical properties of the filtration for the backward Lyapunov vectors, this paper explores a previously unexplained mechanism, providing a novel theoretical interpretation for the role of covariance inflation in ensemble-based Kalman filters. Our derivation of the forecast error evolution describes the dynamic upwelling of the unfiltered error from outside of the span of the anomalies into the filtered subspace. Analytical results for linear systems explicitly describe the mechanism for the upwelling, and the associated recursive Riccati equation for the forecast error, while nonlinear approximations are explored numerically.
AB - The ensemble Kalman filter and its variants have shown to be robust for data assimilation in high dimensional geophysical models, with localization, using ensembles of extremely small size relative to the model dimension. However, a reduced rank representation of the estimated covariance leaves a large dimensional complementary subspace unfiltered. Utilizing the dynamical properties of the filtration for the backward Lyapunov vectors, this paper explores a previously unexplained mechanism, providing a novel theoretical interpretation for the role of covariance inflation in ensemble-based Kalman filters. Our derivation of the forecast error evolution describes the dynamic upwelling of the unfiltered error from outside of the span of the anomalies into the filtered subspace. Analytical results for linear systems explicitly describe the mechanism for the upwelling, and the associated recursive Riccati equation for the forecast error, while nonlinear approximations are explored numerically.
UR - https://www.scopus.com/pages/publications/85053153267
U2 - 10.5194/npg-25-633-2018
DO - 10.5194/npg-25-633-2018
M3 - Article
AN - SCOPUS:85053153267
SN - 1023-5809
VL - 25
SP - 633
EP - 648
JO - Nonlinear Processes in Geophysics
JF - Nonlinear Processes in Geophysics
IS - 3
ER -