Understanding why the volume of suboxic waters does not increase over centuries of global warming in an Earth System Model

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A. Gnanadesikan; J. P. Dunne; J. John;
(2012)

Global warming is expected to reduce oxygen solubility and vertical exchange in the ocean, changes which would be expected to result in an increase in the volume of hypoxic waters. A simulation made with a full Earth System model with dynamical atmosphere, ocean, sea ic... View more
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