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

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.

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m-r_e_dynamic_vs_apparent_Redfield_ratio_in_the_oceans.pdf (Publisher version), 2MB
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m-r_e_dynamic_vs_apparent_Redfield_ratio_in_the_oceans.pdf
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 Creators:
Maier-Reimer, Ernst1, Author           
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1MPI for Meteorology, Max Planck Society, ou_913545              

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Free keywords: 3-D models; biogeochemical cycle; Redfield ratios
 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.

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Language(s): eng - English
 Dates: 1996
 Publication Status: Issued
 Pages: -
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 Table of Contents: -
 Rev. Type: Peer
 Identifiers: DOI: 10.1016/0924-7963(96)00020-6
BibTex Citekey: Maier-Reimer1996113
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Title: Journal of Marine Systems
Source Genre: Journal
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Publ. Info: Elsevier B.V.
Pages: - Volume / Issue: 9 Sequence Number: - Start / End Page: 113 - 120 Identifier: ISSN: 09247963