A simple model for the CaCO3 saturation state of the ocean: The "Strangelove," the "Neritan," and the "Cretan" Ocean
A simple model of the CaCO3 saturation state of the ocean is presented. It can be solved analytically and is intended to identify the fundamental controls on ocean carbonate ion concentration. It should also attract researchers unfamiliar with complex biogeochemical models. Despite its limitations,...
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Veröffentlicht in: | Geochemistry, geophysics, geosystems : G3 geophysics, geosystems : G3, 2003-12, Vol.4 (12), p.n/a |
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Format: | Artikel |
Sprache: | eng |
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