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results are assessed in terms of the accuracy of the analysis and forecast fields as well as the spectral properties of the error of the estimated fields. a. Experimental setup The experiments conducted here are analogous to Skachko et al. (2008) with a few modifications. Skachko et al. (2008) updated only the sea surface height (SSH) field with a local SEIK filter, while temperature and salinity are updated following the first baroclinic mode in the vertical direction. In contrast, we use the
results are assessed in terms of the accuracy of the analysis and forecast fields as well as the spectral properties of the error of the estimated fields. a. Experimental setup The experiments conducted here are analogous to Skachko et al. (2008) with a few modifications. Skachko et al. (2008) updated only the sea surface height (SSH) field with a local SEIK filter, while temperature and salinity are updated following the first baroclinic mode in the vertical direction. In contrast, we use the
