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Angelique C. Haza, Tamay M. Özgökmen, Annalisa Griffa, Andrew C. Poje, and M.-Pascale Lelong

. The first set of synthetic trajectories are generated using flow fields from a ° horizontal-resolution Hybrid Coordinate Ocean Model (HYCOM; Chassignet et al. 2006 ) configured in the North Atlantic ( Fig. 1 ). The model is subject to realistic forcing and boundary conditions in the North Atlantic, focusing on the Gulf Stream extension and recirculation area. We have studied this flow field in order to develop Lagrangian parameterizations of submesoscale dispersion ( Haza et al. 2012 ) and to

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