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Impact of the Ocean’s Overturning Circulation on Atmospheric CO2

ScholarsArchive at Oregon State University

Field Value
Title Impact of the Ocean’s Overturning Circulation on Atmospheric CO2
Names Schmittner, Andreas (creator)
Brook, Edward J. (creator)
Ahn, Jinho (creator)
Date Issued 2007 (iso8601)
Abstract A coupled climate-carbon cycle model and ice core CO2 data from the last glacial
period are used to explore the impact of changes in ocean circulation on atmospheric
CO2 concentrations on millennial time scales. In the model, stronger wind
driven circulation increases atmospheric CO2. Changes in the buoyancy driven
deep overturning in the Atlantic affect atmospheric CO2 only indirectly through
their effect on Southern Ocean stratification. In simulations with an abrupt and
complete shutdown of the Atlantic overturning, stratification in the Southern Ocean
decreases due to salinification of surface waters and freshening of the deep sea.
Deeper mixed layers and steeper isopycnals lead to outgassing of CO2 in the
Southern Ocean and hence gradually increasing atmospheric CO2 concentrations
on a multi-millennial time scale. The rise in CO2 terminates at the time of rapid
resumption of deep water formation and warming in the North Atlantic, and CO2
levels subsequently gradually decrease. These model responses and a strong correlation
between simulated atmospheric CO2 and Antarctic surface air temperatures
with little or no time lag are consistent with newly synchronized ice core data from
the last ice age. Sensitivity experiments reveal that the amplitude of the response of
atmospheric CO2 is sensitive to the model background climatic state and decreases
in a colder climate owing to smaller changes in the overturning.
Genre Book chapter
Topic modeling
Identifier Schmittner, A., E. Brook and J. Ahn, 2007, Impact of the ocean’s overturning circulation on atmospheric CO2, in Ocean Circulation: Mechanisms and Impacts, AGU Geophysical Monograph Series, vol. 173, edited by A. Schmittner, J. Chiang, and S. Hemming, pp. 209-246, American Geophysical Union.

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