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Alfred Wegener Institute for Polar and Marine Research

A regulated localization method for ensemble-based Kalman filters

Lars Nerger, Tijana Janji´c, Wolfgang Hiller, and Jens Schr ¨oter

Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany Contact: Lars.Nerger@awi.de

·

http://www.awi.de

Localization is essential for data assimilation with ensemble-based Kalman filters in large-scale systems.

Two localization methods are commonly used: Covari- ance localization (CL) and domain localization (DL). The former applies a localizing weight to the forecast covari- ance matrix while the latter splits the assimilation into local regions in which independent assimilation updates are performed. The domain localization is usually com- bined with a weighting of the observation error covari- ance matrix, denoted observation localization (OL). OL results in a similar localization effect to that of covari- ance localized filters. In order to improve the perfor- mance of domain localization with weighting of the ob- servation errors, a regulated localization scheme is in- troduced. Using twin experiments with the Lorenz-96 model, it is demonstrated that the regulated localization can lead to a significant reduction of the estimation er- rors as well as increased stability of the assimilation pro- cess. In addition, the numerical experiments point out that the combination of covariance localization with a se- rial processing of observations during the analysis step can destabilize the assimilation process.

Twin experiments are conducted using the Lorenz-96 model [7] implemented in the Parallel Data Assimilation Framework (PDAF, http://pdaf.awi.de). The ensemble size is chosen to consist of 10 model states. The local- ization functions

w

CL

, w

OL are chosen to be 5th-order polynomials mimicking a Gaussian function, but having compact support. In the experiments, the support radius and the forgetting factor (covariance inflation) is varied.

For each pair of these parameters 10 experiments are conducted using different random numbers to generate the initial ensemble from a long state trajectory. The performance of the assimilation experiments is assessed using the time-mean RMS deviations from the true state that was used to generate the observations.

Four combinations of filter algorithms and localization methods are compared:

LSEIK-fix: Local SEIK filter [5] using fixed OL.

LSEIK-reg: Local SEIK filter using regulated OL.

EnKF-sqrt: Square-root formulation of Ensemble Kalman filter (following [2]) using CL.

EnSRF: Ensemble square-root filter with sequential processing of observations [6] using CL.

OL results in a longer effective localization length scale compared to CL. The length scale increases for more accurate observations.

A regulated localization function for OL has been in- troduced. For a single observation, it results in iden- tical effective localizations for CL and OL.

Numerical experiments show a significant improve- ment of the assimilation performance with regulated localization for small observation errors.

The EnSRF method with CL showed an inferior as- similation performance. It is caused by the combi- nation of CL with sequential processing of observa- tions.

Previous studies [1–4] found that CL and OL are not equiv- alent. However, if the observations have only a small in- fluence the difference induced by the localization methods is small. If the influence of the observations is larger, OL requires a smaller localization length scale and, still, can lead to inferior assimilation results than using CL.

The published findings can be explained by considering the effect of the localization on the Kalman gain. Follow- ing [1], the gain for CL is in case of a single observation:

K

CL

=

wCL

HPHT+σ2R

P

f

H

For OL the gain is is:

K

OL

=

wOL

wOLHPHT+σ2R

P

f

H

Here,

w

CL and

w

OL are the localization functions applied in the CL and OL methods. While for CL the localization function enters the gain as a simple factor this is not the case for OL.

The effective localization length scale in the Kalman gain is different for both methods. It depends on the relative size of the estimated state error variance (

P

) and obser- vation error variance

σ

2R as is shown in figure (1). If the observation error is particularly small, the effective local- ization length in OL will be much larger than that of CL.

This behavior can disturb the assimilation performance.

To obtain an identical effective localization length scale in OL, a distinct weight function

w

OLR is required. It can be derived by equating both of the gain equations shown in the left column. The calculation leads to the

regulated localization function

w

OLR

=

w

CLσ2R HPHT+σ2R

1 −

w

CLHPHT HPHT+σ2R

1

The function is always narrower than the weight function

w

CL. It avoids the widening of the effective localization length scale for small observation errors.

0 20 40 60 80 100

0 0.02 0.04 0.06 0.08 0.1

σR2=10

distance

effective weight

0 20 40 60 80 100

0 0.1 0.2 0.3 0.4 0.5

σR2=1

distance

effective weight

0 20 40 60 80 100

0 0.2 0.4 0.6 0.8 1

σR2=0.1

distance

effective weight

Figure 1: Effective localization functions in the Kalman gain for different observation error variances

σ

2R and state

error variance 1. (red): Weighting term for CL and

for OL with regulated localization. (blue): Weighting term for OL. The effective weighting is increasingly wider for observation localization for decreasing

σ

2R.

2 6 10 14 18 22 26 30 34

0.9 0.92 0.94 0.96 0.98 1

LSEIK−fix, obs. error=1.0

forgetting factor

support radius

0.19 0.195 0.2 0.205 0.21 0.215 0.22 0.225 0.23 0.235 0.24 0.245 0.25 0.3 0.4 0.5 0.6 0.8 1

2 6 10 14 18 22 26 30 34

0.9 0.92 0.94 0.96 0.98 1

LSEIK−fix, obs. error=0.5

forgetting factor

support radius

0.09 0.095 0.1 0.105 0.11 0.115 0.12 0.125 0.13 0.135 0.14 0.145 0.15 0.2 0.25 0.3 0.35 0.4 0.5

2 6 10 14 18 22 26 30 34

0.9 0.92 0.94 0.96 0.98 1

LSEIK−fix, obs. error=0.1

forgetting factor

support radius

0.018 0.0185 0.019 0.0195 0.02 0.0205 0.021 0.0215 0.022 0.0225 0.023 0.0235 0.024 0.025 0.03 0.04 0.06 0.08 0.1

2 6 10 14 18 22 26 30 34

0.9 0.92 0.94 0.96 0.98 1

LSEIK−reg, obs. error=1.0

forgetting factor

support radius

0.19 0.195 0.2 0.205 0.21 0.215 0.22 0.225 0.23 0.235 0.24 0.245 0.25 0.3 0.4 0.5 0.6 0.8 1

2 6 10 14 18 22 26 30 34

0.9 0.92 0.94 0.96 0.98 1

LSEIK−reg, obs. error=0.5

forgetting factor

support radius

0.09 0.095 0.1 0.105 0.11 0.115 0.12 0.125 0.13 0.135 0.14 0.145 0.15 0.2 0.25 0.3 0.35 0.4 0.5

2 6 10 14 18 22 26 30 34

0.9 0.92 0.94 0.96 0.98 1

LSEIK−reg, obs. error=0.1

forgetting factor

support radius

0.018 0.0185 0.019 0.0195 0.02 0.0205 0.021 0.0215 0.022 0.0225 0.023 0.0235 0.024 0.025 0.03 0.04 0.06 0.08 0.1

2 6 10 14 18 22 26 30 34

0.9 0.92 0.94 0.96 0.98 1

EnKF−sqrt, obs. error=1.0

forgetting factor

support radius

0.19 0.195 0.2 0.205 0.21 0.215 0.22 0.225 0.23 0.235 0.24 0.245 0.25 0.3 0.4 0.5 0.6 0.8 1

2 6 10 14 18 22 26 30 34

0.9 0.92 0.94 0.96 0.98 1

EnKF−sqrt, obs. error=0.5

forgetting factor

support radius

0.09 0.095 0.1 0.105 0.11 0.115 0.12 0.125 0.13 0.135 0.14 0.145 0.15 0.2 0.25 0.3 0.35 0.4 0.5

2 6 10 14 18 22 26 30 34

0.9 0.92 0.94 0.96 0.98 1

EnKF−sqrt, obs. error=0.1

forgetting factor

support radius

0.018 0.0185 0.019 0.0195 0.02 0.0205 0.021 0.0215 0.022 0.0225 0.023 0.0235 0.024 0.025 0.03 0.04 0.06 0.08 0.1

2 6 10 14 18 22 26 30 34

0.9 0.92 0.94 0.96 0.98 1

EnSRF, obs. error=1.0

forgetting factor

support radius

0.19 0.195 0.2 0.205 0.21 0.215 0.22 0.225 0.23 0.235 0.24 0.245 0.25 0.3 0.4 0.5 0.6 0.8 1

2 6 10 14 18 22 26 30 34

0.9 0.92 0.94 0.96 0.98 1

EnSRF, obs. error=0.5

forgetting factor

support radius

0.09 0.095 0.1 0.105 0.11 0.115 0.12 0.125 0.13 0.135 0.14 0.145 0.15 0.2 0.25 0.3 0.35 0.4 0.5

2 6 10 14 18 22 26 30 34

0.9 0.92 0.94 0.96 0.98 1

EnSRF, obs. error=0.1

forgetting factor

support radius

0.018 0.0185 0.019 0.0195 0.02 0.0205 0.021 0.0215 0.022 0.0225 0.023 0.0235 0.024 0.025 0.03 0.04 0.06 0.08 0.1

Figure 2: Time-mean RMS errors averaged over each 10 experiments.

The regulated localization (LSEIK-reg) results in a significant reduction of the errors compared to fixed-OL (LSEIK-fix), in particular for small obser- vation errors. In addition, the parameter region with minimum errors is increased.

The EnKF-sqrt method shows errors that are very similar to those obtained with LSEIK-reg. How- ever, EnKF-sqrt diverges in case of the smallest observation errors for long localization radii. Here, LSEIK-reg is still stable.

The EnSRF is less stable with larger errors com- pared to LSEIK-reg and EnKF-sqrt. This behavior is caused by the combina- tion of CL with sequential processing of observa- tions, which renders the update equation of the covariance matrix to be inexact.

[1] Miyoshi T, Yamane S. 2007. Lo- cal ensemble transform Kalman filter with an AGCM at a T159/L48 resolu- tion. Mon. Wea. Rev. 135: 3841–

3861

[2] Sakov P, Bertino L. 2011. Rela- tion between two common localisa- tion methods for the EnKF. Comput.

Geosci. 15: 225–237

[3] Greybush SJ, Kalnay E, Miyoshi T, Ide K, Hunt BR. 2011. Balance and ensemble Kalman filter localiza- tion techniques. Mon. Wea. Rev.

139: 511–522.

[4] Janji´c T, Nerger L, Albertella A, Schr ¨oter J, Skachko S. 2011.

On domain localization in ensem- ble based Kalman filter algorithms.

Mon. Wea. Rev. in press.

doi:10.1175/2011MWR3552.1

[5] Nerger L, Danilov S, Hiller W, Schr ¨oter J. 2006. Using sea level data to constrain a finite-element primitive-equation ocean model with a local SEIK filter. Ocean Dynamics 56: 634–649.

[6] Whitaker JS, Hamill TM. 2002.

Ensemble data assimilation without perturbed observations. Mon. Wea.

Rev. 130: 1913–1927.

[7] Lorenz EN. 1996. Predictabil- ity - a problem partly solved. Pro- ceedings Seminar on Predictability, ECMWF, Reading, UK, 1–18.

Introduction

Assimilation experiments

Conclusion

Effective localization of the Kalman gain

Impact of regulated localization

References

Referenzen

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