Abstract
Abstract This article discusses several models for background error correlation matrices using the wavelet diagonal assumption and the diffusion operator. The most general properties of filtering local correlation functions, with wavelet formulations, are recalled. Two spherical wavelet transforms based on Legendre spectrum and a gridpoint spherical wavelet transform are compared. The latter belongs to the class of second-generation wavelets. In addition, a nonseparable formulation that merges the wavelets and the diffusion operator model is formally proposed. This hybrid formulation is illustrated in a simple two-dimensional framework. These three formulations are tested in a toy experiment on the sphere: a large ensemble of perturbed forecasts is used to simulate a true background error ensemble, which gives a reference. This ensemble is then applied to compute the required parameters for each model. A randomization method is utilized in order to diagnose these different models. In particular, their ability to represent the geographical variations of the local correlation functions is studied by diagnosis of the local length scale. The results from these experiments show that the spectrally based wavelet formulation filters the geographical variations of the local correlation length scale but it is less able to represent the anisotropy. The gridpoint-based wavelet formulation is also able to represent some parts of the geographical variations but it appears that the correlation functions are dependent on the grid. Finally, the formulation based on the diffusion represents quite well the local length scale.
Highlights
Data assimilation aims to estimate the most likely numerical representation of a real system from known observations
Two of them are based on the wavelet diagonal assumption while the third one is based on the diffusion equation
The spectrally based wavelets (SBWs) has been recalled in detail, especially the filtering properties associated with local spatial averaging offered by the formulation
Summary
Data assimilation aims to estimate the most likely numerical representation of a real system from known observations. As the wavelets cxj are radial (i.e., isotropic) functions and not polarized (i.e., anisotropic or directional; see Antoine et al 2002), the local average at each scale tends to damped anisotropy The result of this averaging is that the geographical variations of the local correlation functions, modeled with the wavelet diagonal assumption, are smooth, associated with a filtering of sampling noise (Pannekoucke et al 2007). Applying the diagonal assumption in wavelet space will damp all coefficients outside the cone of influence at point 08, as shown, which corresponds to the absolute value of the wavelet coefficient of the local correlation function modeled with wavelet assumption To study some of these points, another wavelet formulation is introduced
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