Workshop on the USE OF ENSEMBLES IN DATA ASSIMILATION
April 13-14, 1999, NCEP, Camp Springs, MD
LOCAL ARRANGEMENTS
John Derber:
Data assimilation plans at
NCEP (20 mins)
Jan Barkmeijer:
Recent
developments in the ECMWF Ensemble Prediction System (30
mins)
Zoltan Toth:
Estimating analysis uncertainty
using the NCEP global ensemble (30 mins)
Dale Barker:
The
Specification and Use of Synoptically-Dependent Background Errors in 3DVAR
using information from an Error Breeding Cycle
Eugenia Kalnay:
Preliminary experiments on
applications of ensembles to data assimilation
Peter Houtekamer:
Prospects
for an operational ensemble Kalman filter (30 mins)
Martin Ehrendorfer (Presented by J. Barkmeijer,
10 mins):
TBA
Craig Bishop:
The Ensemble Transform Kalman
Filter (30 mins)
Jeff Whitaker:
Spread/Analysis Error relationships
in a simple model (20 mins)
Chris Snyder:
Dynamics
and statistics of forecast errors in a quasi-geostrophic model (10-30
mins)
Tom Hamill:
Analysis and Forecast Errors
and the Ensemble Kalman Filter (30 mins)
Jim Purser:
Estimates of flow dependent
covariance structures (20 mins)
Lars Peter Riishojgaard:
Anisotropic flow-dependent
modeling of the forecast error correlations
Jeff Anderson, GFDL
Dale Barker, UK Met. Office, Bracknell, UK
Jan Barkmeijer, ECMWF, Reading, England
Craig Bishop, Pennsylvania State University,
State College, PA
Kerry Emanuel, MIT, Boston, MA
Brian Etherton, Pennsylvania State University,
State College, PA
Peter Houtekamer, AES, Dorval, Canada
Tom Hamill, NCAR, Boulder, CO
Eugenia Kalnay, University of Oklahoma, Norman,
OK
Sharan Majumdar, Pennsylvania State University,
State College, PA
Lars Peter Riishojgaard, NASA GSFC, Greenbelt,
MD
Chris Snyder, NCAR, Boulder, CO
Jeff Whitaker, CDC, Boulder, CO
From NCEP:
John Derber
Steve Lord
Dave Parrish
Jim Purser
Istvan Szunyogh
Zoltan Toth
Steve Tracton
Wan-Shu Wu
The Specification and Use of Synoptically-Dependent
Background Errors
in 3DVAR using information from an Error Breeding
Cycle
A study is currently under way at the UKMO to
use 3D synoptically-dependent
background error modes (SBEMs) within 3DVAR.
Current background errors are
`static', derived via the `NMC' method.
An error-breeding cycle is used to
provide SBEMs which are used in 3DVAR via a new
control variable and cost
function. Details of the methodology and early
results will be presented.
Recent developments in the ECMWF Ensemble Prediction System\\
Perturbations used in ensemble forecasting ask
for a careful computation.
One of the conditions they should satisfy is
that their statistics
resemble what is known of the analysis error.
Prelimenary results on the
EPS performance will be presented of singular
vectors computed
with a Reduced Rank Kalman Filter. Such singular
vectors are constrained
by the analysis error covariance matrix at initial
time. This is achieved
by using the Hessian of the full 4D-Var costfunction.
Also the use of different
analyses in the EPS or the construction a so-called
consensus analysis
will be discussed.
Prospects for an operational ensemble Kalman filter
An ensemble of short-range forecasts can provide
the flow-dependent
covariances of the forecast error, needed by
the Kalman filter.
The finite ensemble size causes the estimated
correlations to be noisy.
To filter small forecast-error correlations associated
with remote
observations, a Schur (termwise) product of the
covariances of the
forecast error and a correlation function with
local support is used.
To solve the Kalman filter equations, the observations
are organized
into batches which are assimilated sequentially.
The ensemble of
background fields is updated at each step, and
thus provides a measure
of the improving quality of the background fields
as more and more
batches of observations are assimilated. For
each batch, a Cholesky
decomposition method is used to solve the linear
system of equations.
Observations from several regions of the globe
may be selected for a
single batch, such that information from different
regions
has zero correlation due to the Schur product.
The linear system
then becomes block diagonal.
A prototype sequential filter has been developed
for atmospheric
data assimilation. Application in real time would
appear to be
feasible.
Dynamics and statistics of forecast errors in a quasi-geostrophic model.
Results from QG model. Time scale
for collapse
of specified initial ensemble to "the attractor",
characteristics
of perturbations on the attractor.
Instantaneous statistics of
analysis and forecast errors for 3DVAR,
in particular influence of
past dynamics through projection of errors
onto leading Lyapnov
subspace. Singular vectors for approximate
"analysis error covariance
norm" and their differences from energy
SV's.