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Real-time data streams and environmental forecasts are used to optimize Naval operations by providing insight to how the environment will impact fleet operations. In the open ocean, broad oceanographic features typical of the deep sea can be reasonably described by models assimilating satellite estimates of sea surface temperature (SST) and sea surface heights (SSH) combined with any available in situ observations that provide vertical information; however this is not the case for the littoral ocean where the dynamics are complex and prominent hydrographic features are often not resolved using SST and SSH. Until new sustained spatial data streams are available and the data assimilative models capable of using them are developed our ability to nowcast and forecast ocean conditions on continental shelves will remain an elusive goal. This is unfortunate as many areas of highest naval interest are broad western boundary continental shelves and shallow semi-enclosed seas. On continental shelves the optical properties are complex representing variable contributions of phytoplankton, Colored Dissolved Organic Matter (CDOM), and non-algal particles. These constituents reflect the water column biology and chemistry, driven by the physical forcing, and are very effective at detecting hydrographic features not evident in SST or SSH data (Figure 1). These optical properties are particularly effective at distinguishing minor density discontinuities where biological communities tend to accumulate. Numerous biological models of varying complexity are available to describe the dynamics that underlie the variability in ocean color (Ishizaka 1990, Lawson et al. 1995, Fasham and Evans 1995, Matear 1995, Robinson et al. 1996, Bissett et al. 1998, 2005); however the issue of how complex the biological models need to be is still unresolved. This is especially true for continental shelves where a significant fraction of the organic matter is remineralized and recycled by the foodweb, with concurrent feedbacks on the optical properties. In the recent past, limited availability of data and biological data assimilation approaches have precluded predictive skill experiments of the coupled physical-optical models. Given the recent advances in ocean observation capabilities it is now possible to collect spatially extensive ocean color data appropriate for data assimilation (Glenn and Schofield 2003). To this end, we propose to develop a data assimilative physical-optical modeling-observation system consisting of an ensemble of optical models of varying complexity in order 1) to improve our predictive skill for forecasting ocean color and 2) improve physical models by using ocean color to discriminate hydrographic features not detected using traditional data streams. We will study the regulation of ocean color for a broad western boundary continental shelf with a specific focus on regions of high optical variability (fronts), which coincide with regions of high acoustic uncertainty.
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