A Next Generation Ocean Carbon Isotope Model for Climate Studies I: Steady State Controls on Ocean 13 C
Supporting Files
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2021
Details
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Journal Title:Global Biogeochemical Cycles
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Personal Author:
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NOAA Program & Office:
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Description:The 13C/12C of dissolved inorganic carbon ( δ13CDIC) carries valuable information on ocean biological C-cycling, air-sea CO 2 exchange, and circulation. Paleo-reconstructions of oceanic 13C from sediment cores provide key insights into past as changes in these three drivers. As a step toward full inclusion of 13C in the next generation of Earth system models, we implemented 13C-cycling in a 1° lateral resolution ocean-ice-biogeochemistry Geophysical Fluid Dynamics Laboratory (GFDL) model driven by Common Ocean Reference Experiment perpetual year forcing. The model improved the mean of modern δ13CDIC over coarser resolution GFDL-model implementations, capturing the Southern Ocean decline
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Source:Global Biogeochemical Cycles, 35(4)
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DOI:
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ISSN:0886-6236 ; 1944-9224
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Rights Information:Other
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Compliance:Library
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Main Document Checksum:urn:sha256:6afc8665435c9e344fd9370ba7cffcce2737ceaf445e92747310166b60ee9498
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