Biogeochemical cycling in the global ocean. I. A new, analytical model with continuous vertical resolution and high-latitude dynamics

G. Shaffer; J. L. Sarmiento

doi:10.1029/94JC01167

Biogeochemical cycling in the global ocean. I. A new, analytical model with continuous vertical resolution and high-latitude dynamics

G. Shaffer, J. L. Sarmiento

Physics of Ice, Climate and Earth

Research output: Contribution to journal › Journal article › Research › peer-review

37 Citations (Scopus)

Abstract

A new, simple analytical model of ocean chemistry is presented which includes continuous vertical resolution, high-latitude dynamics, air-sea exchange and sea ice cover. The results are interpreted in terms of modes of ocean circulation and mixing and compared with results from other models. -from Authors

Original language	English
Journal	Journal of Geophysical Research
Volume	100
Issue number	C2
Pages (from-to)	2659-2672
Number of pages	14
ISSN	0148-0227
DOIs	https://doi.org/10.1029/94JC01167
Publication status	Published - 15 Feb 1995

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10.1029/94JC01167

Cite this

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title = "Biogeochemical cycling in the global ocean. I. A new, analytical model with continuous vertical resolution and high-latitude dynamics",

abstract = "A new, simple analytical model of ocean chemistry is presented which includes continuous vertical resolution, high-latitude dynamics, air-sea exchange and sea ice cover. The results are interpreted in terms of modes of ocean circulation and mixing and compared with results from other models. -from Authors",

author = "G. Shaffer and Sarmiento, {J. L.}",

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AU - Sarmiento, J. L.

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Y1 - 1995/2/15

N2 - A new, simple analytical model of ocean chemistry is presented which includes continuous vertical resolution, high-latitude dynamics, air-sea exchange and sea ice cover. The results are interpreted in terms of modes of ocean circulation and mixing and compared with results from other models. -from Authors

AB - A new, simple analytical model of ocean chemistry is presented which includes continuous vertical resolution, high-latitude dynamics, air-sea exchange and sea ice cover. The results are interpreted in terms of modes of ocean circulation and mixing and compared with results from other models. -from Authors

U2 - 10.1029/94JC01167

DO - 10.1029/94JC01167

M3 - Journal article

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