The performance of an ensemble prediction system is inherently flow dependent.
This dissertation investigates the flow dependence of the ensemble performance with
the help of linear diagnostics applied to the ensemble perturbations in a small local
neighborhood of each model grid point location ℓ. A local error covariance matrix Pℓ
is defined for each local region and the diagnostics are applied to the linear space Sℓ
defined by the range of the ensemble based estimate of Pℓ. The particular diagnostics are chosen to help investigate the ability of Sℓ to efficiently capture the space of
true forecast or analysis uncertainties, accurately predict the magnitude of forecast
or analysis uncertainties, and to distinguish between the importance of different state
space directions. Additionally, we aim to better understand the roots of the underestimation of the magnitude of uncertainty by the ensemble at longer forecast lead
times.
Numerical experiments are carried out with an implementation of the Local Ensemble Transform Kalman Filter (LETKF) data assimilation system on a reduced
(T62L28) resolution version of the National Centers for Environmental Prediction
(NCEP) Global Forecast System (GFS). Both simulated observations under the perfect model scenario and observations of the real atmosphere are used in these experiments. It is found that (i) paradoxically, the linear space Sℓ provides an increasingly
better estimate of the space of forecast uncertainties as the time evolution of the ensemble perturbations becomes more nonlinear with increasing forecast time, (ii) Sℓ
provides a more reliable linear representation of the space of forecast uncertainties for
cases of more rapid error growth, (iii) the E-dimension is a reliable predictor of the
performance of Sℓ in predicting the space of forecast uncertainties, (iv) the ensemble
grossly underestimates the forecast error variance in Sℓ, (v) when realistic observation
coverage is used, the ensemble typically overestimates the uncertainty in the leading
eigen-directions of ˆP ℓ and underestimates the uncertainty in the trailing directions
at analysis time and underestimates the uncertainty in all directions by the 120-hr
forecast lead time, and (vi) at analysis time, with a constant covariance inflation
factor, the ensemble typically underestimates uncertainty in densely observed regions
and overestimates the uncertainty in sparsely observed regions.
| Identifer | oai:union.ndltd.org:tamu.edu/oai:repository.tamu.edu:1969.1/ETD-TAMU-2010-08-8258 |
| Date | 2010 August 1900 |
| Creators | Satterfield, Elizabeth A. |
| Contributors | Szunyogh, Istvan |
| Source Sets | Texas A and M University |
| Language | en_US |
| Detected Language | English |
| Type | thesis, text |
| Format | application/pdf |
Page generated in 0.0019 seconds