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Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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Volume 6, issue 5
Geosci. Model Dev., 6, 1493-1504, 2013
https://doi.org/10.5194/gmd-6-1493-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: The iLOVECLIM earth system model

Geosci. Model Dev., 6, 1493-1504, 2013
https://doi.org/10.5194/gmd-6-1493-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Model evaluation paper 12 Sep 2013

Model evaluation paper | 12 Sep 2013

δ18O water isotope in the iLOVECLIM model (version 1.0) – Part 2: Evaluation of model results against observed δ18O in water samples

D. M. Roche1,2 and T. Caley1 D. M. Roche and T. Caley
  • 1Earth and Climate Cluster, Faculty of Earth and Life Sciences, Vrije Universiteit Amsterdam, Amsterdam, the Netherlands
  • 2Laboratoire des Sciences du Climat et de l'Environnement (LSCE), UMR8212, CEA/CNRS-INSU/UVSQ, Gif-sur-Yvette Cedex, France

Abstract. The H218O stable isotope was previously introduced in the three coupled components of the earth system model iLOVECLIM: atmosphere, ocean and vegetation. The results of a long (5000 yr) pre-industrial equilibrium simulation are presented and evaluated against measurement of H218O abundance in present-day water for the atmospheric and oceanic components. For the atmosphere, it is found that the model reproduces the observed spatial distribution and relationships to climate variables with some merit, though limitations following our approach are highlighted. Indeed, we obtain the main gradients with a robust representation of the Rayleigh distillation but caveats appear in Antarctica and around the Mediterranean region due to model limitation. For the oceanic component, the agreement between the modelled and observed distribution of water δ18O is found to be very good. Mean ocean surface latitudinal gradients are faithfully reproduced as well as the mark of the main intermediate and deep water masses. This opens large prospects for the applications in palaeoclimatic context.

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