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Journal Article

Dynamic vs. apparent Redfield ratio in the oceans: A case for 3D-models

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Maier-Reimer,  Ernst
MPI for Meteorology, Max Planck Society;

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Maier-Reimer, E. (1996). Dynamic vs. apparent Redfield ratio in the oceans: A case for 3D-models. Journal of Marine Systems, 9, 113-120. doi:10.1016/0924-7963(96)00020-6.


Cite as: http://hdl.handle.net/21.11116/0000-0004-F211-7
Abstract
A three-dimensional model of global biogeochemical cycles (HAMOCC3) is used to discuss potential explanations for apparent observed deviations from a basin-wide Redfield ratio. Two examples are given in which model information can be token to close the gaps of incomplete measurements or data analyses. A third example illustrates how the apparent covariation between phosphate and alkalinity is created by the circulation.