Sea-ice feedbacks influence the isotopic signature of Greenland Ice Sheet elevation changes: Last Interglacial HadCM3 simulations (2020)
Attributed to:
Retreat of Southern Hemisphere Sea Ice, 130 000 to 116 000 years BP
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.5194/cp-2020-40
Publication URI: http://dx.doi.org/10.5194/cp-2020-40
Type: Preprint