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- W2014782045 abstract "A highly simplified model of the Arctic Ocean cold halocline, incorporating parameterizations of both along-isopycnal and diapycnal transport, has been developed and constrained by observed profiles of temperature, salinity and chlorofluoromethanes (CFM's). The bulk vertical eddy diffusivity is estimated to be ∼ 2 × 10−6 m2 s−1. The model shows that by ignoring diapycnal mixing processes, the lateral exchange timescales derived from purely lateral tracer models can be significantly biased. The model, and two simpler, purely lateral models, are applied to the dissolved oxygen profile in order to calculate apparent oxygen utilization rates (AOUR). All of the models give similar values for the depth-integrated AOUR. The rates of oxygen utilization are too high to be sustained by primary production in the central Arctic Ocean, and they must therefore be balanced by production over the Arctic Ocean continental shelves. AOUR-based estimates of total shelf production range from 18 to 64 g C m−2 y−1, and are consistent with estimates based on sparse 14C production measurements." @default.
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- W2014782045 date "1987-12-01" @default.
- W2014782045 modified "2023-09-27" @default.
- W2014782045 title "Ventilation of the Arctic Ocean cold halocline: rates of diapycnal and isopycnal transport, oxygen utilization and primary production inferred using chlorofluoromethane distributions" @default.
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- W2014782045 doi "https://doi.org/10.1016/0198-0149(87)90093-8" @default.
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