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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Discussion papers
https://doi.org/10.5194/cp-2015-190
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-2015-190
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 18 Jan 2016

Research article | 18 Jan 2016

Review status
This discussion paper is a preprint. It has been under review for the journal Climate of the Past (CP). The revised manuscript was not accepted.

A model-data assessment of the role of Southern Ocean processes in the last glacial termination

Roland Eichinger1, Gary Shaffer2,3,4, Nelson Albarrán5, Maisa Rojas1, and Fabrice Lambert6 Roland Eichinger et al.
  • 1Department of Geophysics, University of Chile, Blanco Encalada 2002, Santiago, Chile
  • 2GAIA-Antarctica, University of Magellanes, Avenida Bulnes 01855, Punta Arenas, Chile
  • 3Center for Advanced Research in Arid Zones, Raúl Bitrán 1305, La Serena, Chile
  • 4Niels Bohr Institute, University of Copenhagen, Blegdamsvej 17, Copenhagen, Denmark
  • 5Department of Physics, University of Santiago de Chile, Avenida Ecuador 3493, Santiago, Chile
  • 6Department of Physical Geography, Catholic University of Chile, Vicuña Mackenna 4860, Santiago, Chile

Abstract. The Southern Ocean has been identified as a key player for the global atmospheric temperature and pCO2 rise across the last glacial termination. One leading hypothesis for explaining the initial pCO2 step of 38 ppm (Mystery Interval 17.5 – 14.5 ka) is enhanced upwelling of Southern Ocean deep water that had stayed isolated from surface layers for millennia, thereby accumulating carbon from remineralisation of organic matter. However, the individual influences involved in this interplay of processes are not fully understood. A credible explanation for this remarkable climate change must also be able to reproduce a simultaneous steep decrease of carbon isotope ratios (δ13C and ∆14C). To address this topic, we here apply the Danish Center for Earth System Science (DCESS) Earth System Model with an improved terrestrial biosphere module and tune it to a glacial steady-state within the constraints provided by various proxy data records. In addition to adjustments of physical and biogeochemical parameters to colder climate conditions, a sharp reduction of the oceanic mixing intensity below around 1800 m depth in the high latitude model ocean is imposed, generating a model analogy to isolated deep water while maintaining this water oxygenated in agreement with proxy data records. From this glacial state, transient sensitivity experiments across the last glacial termination are conducted in order to assess the influence of various mechanisms on the climate change of the Mystery Interval. We show that the upwelling of isolated deep water in the Southern Ocean complemented by several physical and biogeochemical processes can explain parts but not all of the atmospheric variations observed across the Mystery Interval.

Roland Eichinger et al.
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Roland Eichinger et al.
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Short summary
We apply the DCESS ESM to assess the process of Southern Ocean deep water upwelling as to whether it can explain the climate change between 17.5 and 14.5 kaBP. From a glacial climate state, which was generated under the guidance of proxy data records, transient climate simulations are conducted to analyse the impact of various parameters. This approach can explain parts but not all of the observed atmospheric variations in temperatures, carbon dioxide and carbon isotopes across that period.
We apply the DCESS ESM to assess the process of Southern Ocean deep water upwelling as to...
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