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A. Köhl, D. Stammer, and B. Cornuelle

1. Introduction In this paper we describe the results of a global synthesis obtained by the Estimating the Circulation and Climate of the Ocean (ECCO) Consortium (see Stammer et al. 2002a ) on a 1° spatial grid (±80°) for the 11-yr period 1992–2002. The synthesis is obtained by forcing the ECCO ocean circulation model to near consistency (within specified error margins) with most of the World Ocean Circulation Experiment (WOCE) observations by using the model’s adjoint to modify the initial

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