Oceanographic dynamics and the end of the last interglacial in the subpolar North Atlantic
The last interglacial interval was terminated by the inception of a long, progressive glaciation that is attributed to astronomically influenced changes in the seasonal distribution of sunlight over the earth. However, the feedbacks, internal dynamics, and global teleconnections associated with decl...
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Columbia University
2014
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Online Access: | https://dx.doi.org/10.7916/d83j3bq5 https://academiccommons.columbia.edu/doi/10.7916/D83J3BQ5 |