Abstract
The United States Navy has two approaches for assimilating sea surface height anomaly (SSHA) data, both relying on climatology. One approach is indirect, with the construction of synthetic temperature (T) and salinity (S) profiles based on observationally-derived climatological covariances between SSHA, T, and S. The other approach is direct via a four-dimensional variational system, but it relies on a mean SSH (here, one constrained by observational climatology) to enable comparisons between observed SSHA and model SSH. Because the approaches rely on observational climatology, they can fail when data are outside that climatology. Such a case is reviewed here. A recent field experiment (Borrione et al. 2017) collected glider T/S profiles along altimeter tracks in the Ligurian Sea (northwest Mediterranean Sea). While SSHA data are similar to observational climatology, T/S data are warmer and saltier. In this study, SSHA and T/S data are independently assimilated in separate experiments. It is found that each experiment fits its assimilated data as expected, but the experiments fail to fit the withheld/unassimilated data. Assimilation mechanisms are found to work as designed. Impacts of climatology on results versus withheld data are discussed.
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Osborne, J.J., Carrier, M.J., Ngodock, H.E. (2022). Difficulty with Sea Surface Height Assimilation When Relying on an Unrepresentative Climatology. In: Park, S.K., Xu, L. (eds) Data Assimilation for Atmospheric, Oceanic and Hydrologic Applications (Vol. IV). Springer, Cham. https://doi.org/10.1007/978-3-030-77722-7_17
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