Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5113762 | Quaternary International | 2016 | 14 Pages |
Abstract
Finally, the Younger Dryas (YD) Stadial is characterized by a land-ocean synchronous returning cold conditions (but not so cold as HS1) and, although dry conditions persisted during this period, extreme winter precipitation occurrences might have affected the most coastal areas of north and central W Iberia and Pyrenees. In contrast, dry conditions persisted during the YD in the western Mediterranean regions. The westerlies migrated further north following the displacement of the Polar Front during the deglaciation precluding the input of moisture in the W Mediterranean region, which persisted very dry during the YD Stadial.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
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Authors
F. Naughton, M.F. Sanchez Goñi, T. Rodrigues, E. Salgueiro, S. Costas, S. Desprat, J. Duprat, E. Michel, L. Rossignol, S. Zaragosi, A.H.L. Voelker, F. Abrantes,