Simulating the Last Interglacial Greenland stable water isotope peak: The role of Arctic sea ice changes

Last Interglacial (LIG), stable water isotope values (δ¹⁸O) measured in Greenland deep ice cores are at least 2.5‰ higher compared to the present day. Previous isotopic climate simulations of the LIG do not capture the observed Greenland δ¹⁸O increases. Here, we use the isotope-enabled HadCM3 (UK Me...

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Bibliographic Details
Main Authors: Malmierca-Vallet, I, Sime, LC, Tindall, JC, Capron, E, Valdes, PJ, Vinther, BM, Holloway, MD
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2018
Subjects:
Online Access:https://eprints.whiterose.ac.uk/136028/
https://eprints.whiterose.ac.uk/136028/1/revised_QSR_paper_jun2018.pdf