USING FORECAST SENSITIVITY PATTERNS TO IMPROVE FUTURE FORECAST SKILL

Citation
Zx. Pu et al., USING FORECAST SENSITIVITY PATTERNS TO IMPROVE FUTURE FORECAST SKILL, Quarterly Journal of the Royal Meteorological Society, 123(540), 1997, pp. 1035-1053
Citations number
34
Categorie Soggetti
Metereology & Atmospheric Sciences
ISSN journal
00359009
Volume
123
Issue
540
Year of publication
1997
Part
B
Pages
1035 - 1053
Database
ISI
SICI code
0035-9009(1997)123:540<1035:UFSPTI>2.0.ZU;2-8
Abstract
A simple, relatively inexpensive technique has been developed for usin g past forecast errors to improve the future forecast skill. The metho d uses the forecast model and its adjoint and can be considered as a s implified 4-dimensional variational (4-D VAR) system. One- or two-day forecast errors are used to calculate a small perturbation (sensitivit y perturbation) to the analyses that minimizes the forecast error. The longer forecasts started from the corrected initial conditions, altho ugh better than the original forecasts, are still significantly worse than the shorter forecasts started from the latest analysis, even thou gh they both had access to information covering the same period. As a much less expensive alternative to 4-D VAR, the adjusted initial condi tions from one or two days ago are used as a starting point for a seco nd iteration of the regular NCEP analysis and forecast cycle until the present time (t = 0) analysis is reached. Forecast experiments indica te that the new analyses result in improvements to medium-range foreca st skill, and suggest that the technique can be used in operations, si nce it increases the cost of the regular analysis cycle by a maximum f actor of about 4 to 8, depending on the length of the analysis cycle t hat is repeated. Several possible operational configurations are also tested. The model used in these experiments is the NCEP's operational global spectral model with 62 waves triangular truncation and 28 sigma -vertical levels. An adiabatic version of the adjoint was modified to make it more consistent with the complete forecast model, including on ly a few simple physical parametrizations (horizontal diffusion and ve rtical mixing). This adjoint model was used to compute the gradient of the forecast error with respect to initial conditions.