Carbon fluxes during Dansgaard-Oeschger events as simulated by an Earth System Model
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...
| Published in: | Journal of Climate |
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| Main Authors: | , , , , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Amer Meteorological Soc
2022
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| Subjects: | |
| Online Access: | https://doi.org/10.1175/JCLI-D-21-0713.1 http://ecite.utas.edu.au/150275 |
| Summary: | 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 CO 2 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 CO 2 concentration (for brevitys sake simply referred to as CO 2 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 CO 2 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 CO 2 for several hundred years into the interstadial. The simulations also provide a novel possible interpretation for the observed correlation between CO 2 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 CO 2 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 CO 2 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 ... |
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