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-16-2485-2020
Publication URI: http://dx.doi.org/10.5194/cp-16-2485-2020
Type: Journal Article/Review
Parent Publication: Climate of the Past
Issue: 6