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Global ocean data from the Max Planck Institute for Meteorology provides mapped, gap-filled fields of dissolved inorganic carbon (DIC) in the water column. The dataset is a monthly climatology based on observations from 2004 through 2017, produced using a self-organizing map and feed-forward network (SOM-FFN) method extended to four dimensions. An ensemble mean from ten bootstrapping runs provides the final DIC field, with an ensemble spread representing methodological uncertainty.
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