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Carbon fluxes during Dansgaard-Oeschger events as simulated by an Earth System Model


Jochum, M and Chase, Z and Nuterman, R and Pedro, J and Rasmussen, S and Vettoretti, G and Zheng, P, Carbon fluxes during Dansgaard-Oeschger events as simulated by an Earth System Model, Journal of Climate, 35, (17) pp. 5745-5758. ISSN 0894-8755 (2022) [Refereed Article]

Copyright Statement

© 2022 American Meteorological Society

DOI: doi:10.1175/JCLI-D-21-0713.1


The Community Earth System Model with marine and terrestrial biogeochemistry is configured to simulate glacial climate. The integration shows transitions from warm to cold states - interstadials to stadials - and back. The amplitude of the associated Greenland and Antarctica temperature changes and the atmospheric CO2 signal are consistent with ice-core reconstructions, and so are the time-lags between termination of a stadial, Antarctic temperature reversal, and the decline of the atmospheric CO2 concentration (for brevity’s sake simply referred to as CO2 from here on). The present model results stand out, because the transitions occur spontaneously (without forcing changes like hosing), and because they reproduce the observed features above in a configuration that uses the same parameterizations as climate simulations for the present day (i.e., no retuning has been done). During stadials, precipitation shifts lead to reduced growth on land, which dominates the CO2 increase; the ocean acts as a minor carbon sink during the stadials. After the end of the stadials, however, the sudden reversal of the stadial anomalies in temperature, wind, and precipitation turn the ocean into a carbon source, which accounts for the continued rise of CO2 for several hundred years into the interstadial. The simulations also provide a novel possible interpretation for the observed correlation between CO2 and Antarctic temperature: rather than both being controlled by Southern Ocean processes, they are both controlled by the North Atlantic ocean, and most of the extra CO2 may not be of Southern hemisphere origin. If the stadials are prolonged through North Atlantic hosing, the upper ocean comes to an equilibrium, and the CO2 response is dominated by a single process: reduced export production in the North Atlantic as result of the collapsed overturning circulation. This is in contrast to the unforced simulation where the net ocean carbon flux anomaly is the sum of several regional responses of both signs and similar magnitudes. Reducing the aeolian iron deposition by half, to account for the observed reduction of southern hemisphere dust fluxes during stadials, reduces biological productivity and export production so that the Southern Ocean emerges as an important carbon source, at least for the three centuries up until a new equilibrium for the upper ocean is reached.

Item Details

Item Type:Refereed Article
Keywords:carbon cycle, abrupt climate change, ocean, ice age, climate variability
Research Division:Earth Sciences
Research Group:Physical geography and environmental geoscience
Research Field:Palaeoclimatology
Objective Division:Expanding Knowledge
Objective Group:Expanding knowledge
Objective Field:Expanding knowledge in the earth sciences
UTAS Author:Chase, Z (Professor Zanna Chase)
UTAS Author:Pedro, J (Dr Joel Pedro)
ID Code:150275
Year Published:2022
Funding Support:Australian Research Council (DP180102357)
Web of Science® Times Cited:19
Deposited By:Oceans and Cryosphere
Deposited On:2022-06-06
Last Modified:2022-11-02

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