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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Bibliographic Details
Main Authors: Mokeddem, Zohra, McManus, Jerry F., Oppo, Delia W.
Format: Text
Language:unknown
Published: Columbia University 2014
Subjects:
Online Access:https://dx.doi.org/10.7916/d83j3bq5
https://academiccommons.columbia.edu/doi/10.7916/D83J3BQ5