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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 4, issue 2
Clim. Past, 4, 125–136, 2008
https://doi.org/10.5194/cp-4-125-2008
© Author(s) 2008. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 4, 125–136, 2008
https://doi.org/10.5194/cp-4-125-2008
© Author(s) 2008. This work is distributed under
the Creative Commons Attribution 3.0 License.

  25 Jun 2008

25 Jun 2008

Modeling variations of marine reservoir ages during the last 45 000 years

J. Franke1, A. Paul2,1, and M. Schulz2,1 J. Franke et al.
  • 1Department of Geosciences, University of Bremen, Germany
  • 2MARUM – Center for Marine Environmental Sciences, University of Bremen, Germany

Abstract. When dating marine samples with 14C, the reservoir-age effect is usually assumed to be constant, although atmospheric 14C production rate and ocean circulation changes cause temporal and spatial reservoir-age variations. These lead to dating errors, which can limit the interpretation of cause and effect in paleoclimate data. We used a global ocean circulation model forced by transient atmospheric Δ14C variations to calculate reservoir ages for the last 45 000 years for a present day-like and a last glacial maximum-like ocean circulation. A ~30% reduced Atlantic meridonal overturning circulation leads to increased reservoir ages by up to ~500 years in high latitudes. Temporal variations are proportional to the absolute value of the reservoir age; regions with large reservoir age also show large variation. Temporal variations range between ~300 years in parts of the subtropics and ~1000 years in the Southern Ocean. For tropical regions, which are generally assumed to have nearly stable reservoir ages, the model suggests variations of several hundred years.

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