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- W2113103639 abstract "[1] Estimates of the oceanic lateral eddy diffusion coefficient Aredi vary by more than an order of magnitude, ranging from less than a few hundred m2/s to thousands of m2/s. This uncertainty has first-order implications for the intensity of oceanic hypoxia, which is poorly simulated by the current generation of Earth System Models. Using satellite-based estimate of oxygen consumption in hypoxic waters to estimate the required diffusion coefficient for these waters gives a value of order 1000 m2/s. Varying Aredi across a suite of Earth System Models yields a broadly consistent result given a thermocline diapycnal diffusion coefficient of 1 × 10−5 m2/s." @default.
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- W2113103639 date "2013-10-10" @default.
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- W2113103639 title "Critical role for mesoscale eddy diffusion in supplying oxygen to hypoxic ocean waters" @default.
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- W2113103639 doi "https://doi.org/10.1002/grl.50998" @default.
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