Model evidence for a seasonal bias in Antarctic ice cores

Abstract

Much of the global annual mean temperature change over Quaternary glacial cycles can be attributed to slow ice sheet and greenhouse gas feedbacks, but analysis of the short-term response to orbital forcings has the potential to reveal key relationships in the climate system. In particular, obliquity and precession both produce highly seasonal temperature… (More)
DOI: 10.1038/s41467-018-03800-0

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