Articles | Volume 15, issue 2
https://doi.org/10.5194/cp-15-463-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/cp-15-463-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Western Mediterranean hydro-climatic consequences of Holocene ice-rafted debris (Bond) events
Christoph Zielhofer
CORRESPONDING AUTHOR
Institute of Geography, Leipzig University, Leipzig, 04103, Germany
Anne Köhler
Institute of Geography, Leipzig University, Leipzig, 04103, Germany
Steffen Mischke
Faculty of Earth Sciences, University of Iceland, Reykjavík, 101, Iceland
Abdelfattah Benkaddour
Department of Earth Sciences, Faculty of Science and Technology, Cadi Ayyad University, Marrakech-Guéliz, Morocco
Abdeslam Mikdad
Institut National des Sciences de l'Archéologie et du Patrimoine, Rabat, Morocco
William J. Fletcher
Department of Geography, School of Environment, Education and Development, University of Manchester, Manchester, M13 9PL, UK
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Discussed (final revised paper)
Latest update: 20 Nov 2024
Short summary
Based on a Holocene oxygen stable isotope record from Lake Sidi Ali (Morocco) we correlate Western Mediterranean precipitation anomalies with North Atlantic ice-rafted debris (Bond) events to identify a probable teleconnection between Western Mediterranean winter rains and subpolar North Atlantic cooling phases. Our data show a noticeable similarity between Western Mediterranean winter rain minima and Bond events during the Early Holocene and an opposite pattern during the Late Holocene.
Based on a Holocene oxygen stable isotope record from Lake Sidi Ali (Morocco) we correlate...
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