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- W2080452601 abstract "Implementing oxygen isotopes (, ) in coupled climate models provides both an important test of the individual model's hydrological cycle and a powerful tool to explore past climate changes mechanistically while producing results directly comparable to isotope proxy records. Here we describe the addition of oxygen isotopes to the University of Victoria Earth System Climate Model (UVic ESCM). Equilibrium simulations are performed for pre-industrial and Last Glacial Maximum (LGM) conditions. The oxygen isotope content in the model's pre-industrial climate is compared with observations for precipitation and seawater. The distribution of oxygen isotopes during the LGM is compared with available paleo-reconstructions. L'introduction des isotopes de l'oxygène (, ) dans les modèles climatiques couplés fournit à la fois un test important du cycle hydrologique des différents modèles et un puissant outil pour explorer de façon mécaniste les changements climatiques passés tout en produisant des résultats directement comparables aux relevés climatiques indirects des isotopes. Ici, nous décrivons l'addition des isotopes de l'oxygène au modèle ESCM (Earth System Climate Model) de l'Université de Victoria. Nous effectuons des simulations d’équilibre pour les conditions préindustrielles et du dernier maximum glaciaire. Nous comparons le contenu en isotopes de l'oxygène dans le climat préindustriel du modèle avec les observations pour les précipitations et l'eau de mer. Nous comparons la distribution des isotopes de l'oxygène durant le dernier maximum glaciaire avec les paléoreconstructions disponibles." @default.
- W2080452601 created "2016-06-24" @default.
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- W2080452601 date "2012-12-01" @default.
- W2080452601 modified "2023-10-01" @default.
- W2080452601 title "Modelling Oxygen Isotopes in the University of Victoria Earth System Climate Model for Pre-industrial and Last Glacial Maximum Conditions" @default.
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- W2080452601 doi "https://doi.org/10.1080/07055900.2012.707611" @default.
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