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...
Main Authors: | , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Elsevier
2018
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Subjects: | |
Online Access: | https://eprints.whiterose.ac.uk/136028/ https://eprints.whiterose.ac.uk/136028/1/revised_QSR_paper_jun2018.pdf |