Articles | Volume 15, issue 5
https://doi.org/10.5194/cp-15-1665-2019
© 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-15-1665-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Is there evidence for a 4.2 ka BP event in the northern North Atlantic region?
Raymond S. Bradley
CORRESPONDING AUTHOR
Department of Geosciences/Climate System Research Center, University
of Massachusetts, Amherst, USA
Jostein Bakke
Department of Earth Science/Bjerknes Centre for Climate Research,
University of Bergen, Bergen, Norway
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Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
We review paleoceanographic and paleoclimatic records from the northern North Atlantic to assess the nature of climatic conditions at 4.2 ka BP. There was a general decline in temperatures after ~ 5 ka BP, which led to the onset of neoglaciation. Although a few records do show a distinct anomaly around 4.2 ka BP (associated with a glacial advance), this is not widespread and we interpret it as a local manifestation of the overall climatic deterioration that characterized the late Holocene.
We review paleoceanographic and paleoclimatic records from the northern North Atlantic to assess...
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