Articles | Volume 14, issue 8
https://doi.org/10.5194/cp-14-1119-2018
https://doi.org/10.5194/cp-14-1119-2018
Research article
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09 Aug 2018
Research article | Highlight paper |  | 09 Aug 2018

Testing the consistency between changes in simulated climate and Alpine glacier length over the past millennium

Hugues Goosse, Pierre-Yves Barriat, Quentin Dalaiden, François Klein, Ben Marzeion, Fabien Maussion, Paolo Pelucchi, and Anouk Vlug

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Brief Communication: annual large-scale atmospheric circulation reconstructed from a data assimilation framework cannot explain local East Antarctic ice rises’ surface mass balance records
Marie Genevieve Paule Cavitte, Hugues Goosse, Quentin Dalaiden, and Nicolas Ghilain
EGUsphere, https://doi.org/10.5194/egusphere-2024-3140,https://doi.org/10.5194/egusphere-2024-3140, 2024
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The role of atmospheric conditions in the Antarctic sea ice extent summer minima
Bianca Mezzina, Hugues Goosse, François Klein, Antoine Barthélemy, and François Massonnet
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Investigating the spatial representativeness of East Antarctic ice cores: a comparison of ice core and radar-derived surface mass balance over coastal ice rises and Dome Fuji
Marie G. P. Cavitte, Hugues Goosse, Kenichi Matsuoka, Sarah Wauthy, Vikram Goel, Rahul Dey, Bhanu Pratap, Brice Van Liefferinge, Thamban Meloth, and Jean-Louis Tison
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Ice core chemistry database: an Antarctic compilation of sodium and sulfate records spanning the past 2000 years
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Future changes in the mean and variability of extreme rainfall indices over the Guinea coast and role of the Atlantic equatorial mode
Koffi Worou, Thierry Fichefet, and Hugues Goosse
Weather Clim. Dynam., 4, 511–530, https://doi.org/10.5194/wcd-4-511-2023,https://doi.org/10.5194/wcd-4-511-2023, 2023
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Cited articles

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Short summary
Glaciers provide iconic illustrations of past climate change, but records of glacier length fluctuations have not been used systematically to test the ability of models to reproduce past changes. One reason is that glacier length depends on several complex factors and so cannot be simply linked to the climate simulated by models. This is done here, and it is shown that the observed glacier length fluctuations are generally well within the range of the simulations.