EGU21-9433
https://doi.org/10.5194/egusphere-egu21-9433
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Global reorganization of atmospheric circulation during Dansgaard-Oschger cycles

Jens Fohlmeister1, Natasha Sekhon2, Andrea Columbu3, Kira Rehfeld4, Louise Sime5, Cristina Veige-Pires6, Norbert Marwan1, and Niklas Boers1,7,8
Jens Fohlmeister et al.
  • 1Potsdam Institute for Climate Impact Research, Germany (jens.fohlmeister@pik-potsdam.de)
  • 2Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas, USA, 78712
  • 3Department of Biological, Geological and Environmental Sciences, University of Bologna, Via Zamboni 67, 40126 Bologna, Italy
  • 4Institute of Environmental Physics, Heidelberg University, INF229, 69120 Heidelberg, Germany
  • 5Ice Dynamics and Palaeoclimate, British Antarctic Survey, Cambridge CB3 0ET, United Kingdom
  • 6CIMA – Centre for Marine and Environmental Research, Faculty of Sciences and Technology FCT, Universidade do Algarve, Campus de Gambelas, 8005-139 Faro, Portugal
  • 7Department of Mathematics and Computer Science, Free University of Berlin, Berlin, Germany
  • 8Global Systems Institute and Department of Mathematics, University of Exeter, Exeter, UK

Ice core records from Greenland provide evidence for multiple abrupt warming events recurring at millennial time scales during the last glacial interval. Although climate transitions strongly resembling these Dansgaard-Oeschger (DO) transitions have been identified in several speleothem records, our understanding of the climate and ecosystem impacts of the Greenland warming events in lower latitudes remains incomplete.

Here, we investigate the influence of DO transitions on the global atmospheric circulation pattern. We comprehensively analyse d18O changes during DO transitions in a globally distributed dataset of speleothems (SISALv2; Comas-Bru et al., 2020). Speleothem d18O signals mostly reflect changes in precipitation amount and moisture source. Thereby this proxy allows us to infer spatially resolved changes in global atmospheric dynamics that are characteristically linked to DO transitions. We confirm the previously proposed shift of the Intertropical Convergence Zone towards more northerly positions. In addition, we find evidence for a similar northward shift of the westerly winds of the Northern Hemisphere. Furthermore, we identify a decreasing trend in the transition amplitudes with increasing distances from the North Atlantic region. This confirms previous suggestions of this region being the core and origin of these past abrupt climate changes.

 

References:

Comas-Bru et al., 2020, Earth System Science Data 12, 2579–2606

 

How to cite: Fohlmeister, J., Sekhon, N., Columbu, A., Rehfeld, K., Sime, L., Veige-Pires, C., Marwan, N., and Boers, N.: Global reorganization of atmospheric circulation during Dansgaard-Oschger cycles, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-9433, https://doi.org/10.5194/egusphere-egu21-9433, 2021.

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