(Q58114180)

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Ocean carbon transport in a box-diffusion versus a general circulation model

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Ocean carbon transport in a box-diffusion versus a general circulation model (English)

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James C. Orr

2

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Fortunat Joos

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Fortunat Joos

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1

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author name string

Ulrich Siegenthaler

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3

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language of work or name

English

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publication date

15 June 1997

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published in

Journal of Geophysical Research

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volume

102

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issue

C6

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page(s)

12367-12388

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cites work

A Large Northern Hemisphere Terrestrial CO2 Sink Indicated by the 13C/12C Ratio of Atmospheric CO2.

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Radiocarbon evidence for a smaller oceanic carbon dioxide sink than previously believed

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Imbalance in the budget

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Evidence from polar ice cores for the increase in atmospheric CO2 in the past two centuries

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Carbon Dioxide Exchange Between Atmosphere and Ocean and the Question of an Increase of Atmospheric CO2during the Past Decades

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Simulations of radiocarbon in a coarse-resolution world ocean model: 1. Steady state prebomb distributions

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Simulations of radiocarbon in a coarse-resolution world ocean model: 2. Distributions of bomb-produced carbon 14

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A perturbation simulation of CO2uptake in an ocean general circulation model

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Particulate organic matter flux and planktonic new production in the deep ocean

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Ice core record of the 13C/12C ratio of atmospheric CO2 in the past two centuries

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Estimates of the effect of Southern Ocean iron fertilization on atmospheric CO2 concentrations

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Seasonal and interannual variations in atmospheric oxygen and implications for the global carbon cycle

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Evidence for slow mixing across the pycnocline from an open-ocean tracer-release experiment

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Atmospheric carbon dioxide and the ocean

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Rapid atmospheric CO2 variations and ocean circulation

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The relationship between vertical eddy diffusion and buoyancy gradient in the deep sea

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The role of CaCO3 compensation in the glacial to interglacial atmospheric CO2change

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The distribution of bomb radiocarbon in the ocean

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Oceanic radiocarbon: Separation of the natural and bomb components

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retrieved

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(Q58114180)

Ocean carbon transport in a box-diffusion versus a general circulation model

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