Pronounced northward shift of the westerlies during MIS 17 leading to the strong 100-kyr ice age cycles. / Sánchez Goñi, María F.; Ferretti, Patrizia; Polanco-Martínez , Josué M; Rodrigues, Teresa; Alonso-García, Monserrat; Rodríguez-Tovar, Francisco J.; Dorador Rodriguez, Javier; Desprat, S.

In: Earth and Planetary Science Letters, Vol. 511, 01.04.2019, p. 117-129.

Research output: Contribution to journalArticlepeer-review

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  • María F. Sánchez Goñi
  • Patrizia Ferretti
  • Josué M Polanco-Martínez
  • Teresa Rodrigues
  • Monserrat Alonso-García
  • Francisco J. Rodríguez-Tovar
  • Javier Dorador Rodriguez
  • S. Desprat

Abstract

The MIS 17 interglacial, ∼715–675 ka, marks the end of the Mid-Pleistocene Transition as intensified, long and asymmetrical 100-kyr ice age cycles became eminently established. Increasing arrival of moisture to the Northern Hemisphere high latitudes, resulting from the northwestward migration of the Subpolar Front and the intensification of the Norwegian Greenland Seas (NGS) convection, has been put forward to explain the emergence of this quasi-periodic 100-kyr cycle. However, testing this hypothesis is problematic with the available North Atlantic precipitation data. Here we present new pollen-based quantitative seasonal climate reconstructions from the southwestern Iberian margin that track changes
in the position and intensity of the westerlies. Our data compared to changes in North Atlantic deep and surface water conditions show that MIS 17 interglacial was marked by three major changes in the direction and strength of the westerlies tightly linked to oceanographic changes. In particular, we report
here for the first time a drastic two-steps northward shift of the westerlies centered at ∼693 ka that ended up with the sustained precipitation over southern European. This atmospheric reorganization was associated with northwestward migration of the Subpolar Front, strengthening of the NGS deep water formation and cooling of the western North Atlantic region. This finding points to the substantial arrival of moisture to the Northern Hemisphere high latitudes at the time of the decrease in summer energy and insolation contributing to the establishment of strong 100-kyr cycles.
Original languageEnglish
Pages (from-to)117-129
Number of pages13
JournalEarth and Planetary Science Letters
Volume511
Early online date6 Feb 2019
DOIs
Publication statusPublished - 1 Apr 2019
This open access research output is licenced under a Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License.

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