Answers are grounded in this paper and cite their sources.
An analysis correction method is presented that uses directly the sensitivity information coming from gradient fields at initial time to perform an alternative forecast. The method consists in imposing, at initial time, a 'sensitive' structure to the perturbation which is first computed by adjoint tools. The tuning of the perturbation amplitude is obtained by reducing the distance to the observations at the locations where the sensitive structure is of significant amplitude. The method is tested on a severe meteorological event which was operationally badly forecast even at very short ranges. Several sets of homogeneous observations are considered and the method proves its efficiency for part of them.
No takes yet. Share an insight, caveat, or question.
Hello et al. (2000) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: