“…We used the MIT Multidisciplinary Simulation, Estimation, and Assimilation Systems (MIT-MSEAS) primitive equation ocean modeling system [Haley and Lermusiaux, 2010;Haley Jr et al, 2015] to compute ocean surface velocity forecasts in the Martha's Vineyard coastal region during August 2018. The modeling system provided forecasts of the ocean state variable fields (three-dimensional velocity, temperature, salinity, and sea-surface height) every hour, with a spatial resolution of 200 m. More details about the model forecast initialization, tidal forcing, atmospheric flux forcing, and CTD data assimilation can be found in [Serra et al, 2020;Filippi et al, 2020]. The deterministic two-way nesting ocean forecast initialized from the estimated ocean state conditions at a particular time is referred to as the central forecast, and ensemble forecasts were initialized using Error Subspace Statistical Estimation procedures [Lermusiaux, 2002].…”