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David Halpern, Dimitris Menemenlis, and Xiaochun Wang

assimilated in 2010 compared to 2004. The geographical coverage and quantity of temperature and salinity profiles assimilated in the EUC and NECC regions were greatest in 2011. No estimate was made of the minimum amount of in situ data required for a reliable description of the equatorial currents’ variability because a lack of resources prevented ECCO2 data selection experiments, in which certain datasets are excluded from the assimilation scheme to determine ECCO2 solutions. Table 1. Assimilated

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