The Southern Ocean biogeochemical divide
I. Marinov (),
A. Gnanadesikan,
J. R. Toggweiler and
J. L. Sarmiento
Additional contact information
I. Marinov: Atmospheric and Oceanic Sciences Program, Princeton University
A. Gnanadesikan: NOAA/Geophysical Fluid Dynamics Laboratory
J. R. Toggweiler: NOAA/Geophysical Fluid Dynamics Laboratory
J. L. Sarmiento: Atmospheric and Oceanic Sciences Program, Princeton University
Nature, 2006, vol. 441, issue 7096, 964-967
Abstract:
The Southern Ocean has central roles in carbon dioxide exchange between the oceans and the atmosphere, and in nutrient supply to the rest of the world's oceans — but these are physically separated due to the nature of ocean circulation, creating a biogeochemical divide. The area south of the divide has the most important influence on carbon dioxide exchange with the atmosphere; while the area to the north has the most significant effect on global oceanic productivity.
Date: 2006
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Persistent link: https://EconPapers.repec.org/RePEc:nat:nature:v:441:y:2006:i:7096:d:10.1038_nature04883
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DOI: 10.1038/nature04883
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