Some limitations of
statistical interpolation
Author:Pierre Gauthier
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Some limitations of statistical interpolation
4D variational data assimilation (4D-Var)
Preconditioning through a change of variable
Operations involved in a single iteration of
4D-Var
Equivalence between the Kalman filter and 4D-Var
Comparison of analysis increments obtained with
3D-Var
vs. that of 4D-Var (6-h) (single surface observation)
Vertical cross-section of the analysis increment
4D Variational Data Assimilation
Definition and properties of an adjoint operator
Computation of the gradient using the adjoint
model
Tangent Linear model and Adjoint Model (LeDimet
and
Talagrand, 1986)
Example: the Lorenz (1963) model
Adjoint of the propagator R(t0,ti) of the TLM
Steps involved in one iteration of 4D-Var
Error growth and the TLM and adjoint models
Other applications of the adjoint model
Sensitivity analyses
Sensitivity analyses (S. Laroche, J. Morneau and
M.
Tanguay)
120 hr forecast and verifying analysis GZ 500
24-h forecast error of the operational model
(Geopotential
at 500 hPa)
Corrections brought by the sensitivity analysis
at
0 hr (Geopotential at 500 hPa)
Forecast error at 24-h (GZ 500 hPa)
Verification of the 5-day forecast, valid on 6
October
2000 at 00 UTC
Corrections brought by the sensitivity analysis
at
0 hr (Geopotential at 500hPa)
Vertical cross-section of the changes brought by
the
sensitivity analysis at 0-hr over the centre of Northern Pacific (valid
on 1 October 2000)
Verification of the 5-day forecast based on the
sensitivity
analysis
Summary
Time series of precipitation rates averaged over
the
Northern Hemisphere (Gauthier and Thepaut, MWR 2001)
Current issues...