(EnSRF) analysis scheme in the presence of model errors, as a follow-up to a previous
perfect-model comparison. In the hybrid scheme, the ensemble perturbations are updated
by the ensemble transform Kalman filter (ETKF) and the ensemble mean is updated with
a hybridized ensemble and static background-error covariance. The experiments were
conducted with a two-layer primitive equation model. The true state was a T127
simulation. Data assimilation experiments were conducted at T31 resolution,
assimilating imperfect observations drawn from the T127 nature run. By design, the
magnitude of the truncation error was large, which provided a test on the ability of both
schemes to deal with model error. Additive noise was used to parameterize model errors
in the background ensemble for both schemes. In the first set of experiments, additive
noise was drawn from a large inventory of historical forecast errors and in the second set
of experiments, it was drawn from a large inventory of differences between forecasts and
analyses. The static covariance was computed correspondingly from the two inventories.
The hybrid analysis was statistically significantly more accurate than the EnSRF
analysis. The improvement of the hybrid over the EnSRF was smaller when differences
of forecasts and analyses were used to form the random noise and the static covariance.
The EnSRF analysis was more sensitive to the size of the ensemble than the hybrid. A
series of tests were conducted to understand why the EnSRF performed worse than the
hybrid. It was shown that the inferior performance of the EnSRF was likely due to the
sampling error in the estimation of the model-error covariance in the mean update and the
less balanced EnSRF initial conditions due to the extra localizations used in the EnSRF.
Supplementary URL: http://www.cdc.noaa.gov/people/xuguang.wang/hybridpaper2.pdf