Articles | Volume 15, issue 2
https://doi.org/10.5194/cp-15-781-2019
© 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-15-781-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Atmospheric blocking induced by the strengthened Siberian High led to drying in west Asia during the 4.2 ka BP event – a hypothesis
Emil Racoviţă Institute of Speleology, Romanian Academy,
Cluj Napoca, 400006, Romania
Stable Isotope Laboratory, Ştefan
cel Mare University, Suceava, 720229, Romania
Monica Ionita
Alfred Wegener
Institute, Helmholtz Center for Polar and Marine Research, 27570 Bremerhaven,
Germany
Harvey Weiss
School of Forestry and Environmental Studies, Yale
University, New Haven, CT, USA
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Discussed (final revised paper)
Latest update: 23 Nov 2024
Short summary
We present a reconstruction of winter climate around 4.2 ka cal BP in Europe, west Asia, and northern Africa that shows generally low temperatures and heterogeneously distributed precipitation. We hypothesize that in the extratropical Northern Hemisphere the 4.2 ka BP event was caused by the strengthening and expansion of the Siberian High, which effectively blocked the moisture-carrying westerlies from reaching west Asia and also resulted in outbreaks of northerly cold and dry winds.
We present a reconstruction of winter climate around 4.2 ka cal BP in Europe, west Asia, and...
Special issue