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- W2084294469 abstract "Dansgaard–Oeschger events are warm events appearing and disappearing abruptly within the last glacial period. Several mechanisms have been put forward to explain these rapid climatic switches: forced oscillations of the atmosphere-ocean-ice-sheet system or instabilities of the ocean circulation, of the ice-sheets, or of the atmosphere-ocean-ice-sheet system. Here, this last hypothesis is examined through the use of the climate model of intermediate complexity CLIMBER2.3, coupled to a very simple ice-sheet model of the Fennoscandian ice-sheet. To cite this article: M. Kageyama, D. Paillard, C. R. Geoscience 337 (2005). Les événements de Dansgaard–Oeschger sont des périodes chaudes apparaissant et se résorbant brutalement au cours de la dernière période glaciaire. Plusieurs mécanismes ont été avancés pour expliquer ces bascules climatiques brutales, faisant appel à des oscillations forcées du système atmosphère-océan-calottes glaciaires ou aux instabilités des calottes glaciaires, de la circulation océanique ou du système couplé atmosphère-océan-calottes glaciaires. C'est cette dernière hypothèse que nous examinons à l'aide du modèle climatique de complexité intermédiaire CLIMBER2.3, couplé à un modèle très simple de la calotte fennoscandinave. Pour citer cet article : M. Kageyama, D. Paillard, C. R. Geoscience 337 (2005)." @default.
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- W2084294469 date "2005-08-01" @default.
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- W2084294469 title "Dansgaard–Oeschger events: an oscillation of the climate-ice-sheet system?" @default.
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- W2084294469 doi "https://doi.org/10.1016/j.crte.2005.04.013" @default.
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