EGU21-12270
https://doi.org/10.5194/egusphere-egu21-12270
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Large volcanic eruptions as a natural hazard: The impact of the 536/540 CE double event on the atmospheric circulation, surface climate, vegetation and society in Scandinavia

Evelien van Dijk1, Ingar Mørkestøl Gundersen2, Manon Bajard1, Helge Høeg1, Kjetil Løftsgård2, Frode Iversen2, Claudia Timmreck3, Johann Jungclaus3, and Kirstin Krüger1
Evelien van Dijk et al.
  • 1Department of Geosciences, University of Oslo, Oslo, Norway (evelievd@geo.uio.no)
  • 2Cultural History Museum, University of Oslo, Oslo, Norway
  • 3Max Planck Institute for Meteorology, Hamburg, Germany

Large volcanic eruptions that reach the stratosphere cool the surface climate and impact the atmospheric circulation, feeding back on the local climate. The mid-6th century is an outstanding period in climate history that featured an extreme cold period, including one of the coldest decades in the past 2000 years. It was triggered by the 536/540 CE volcanic double event, creating the strongest decadal volcanic forcing in the last two millennia. During this period societal changes are recorded around the world, like the Great Migration period and the outbreak of the Justinian Plague. However, not a lot is known about the causal relationships between global cooling and societal change. Less is known also, about the impact of the large-scale atmospheric circulation on the regional climate, vegetation and society in Scandinavia after this volcanic double event. Here we aim to improve this understanding by combining global climate and regional growing-degree-day (GGD) modeling with climate proxies and archaeological records from Southeastern Norway.

We use PMIP4 past2k runs and the MPI-ESM ensemble simulation of the 6th/7th century (520-680 CE), to analyze the atmospheric circulation, surface climate and vegetation changes as a response to the volcanic double event of 536/540 CE, over Scandinavia, specifically Southeastern Norway. Thereby we focus on the response of the major circulation patterns that influence the climate over Northern Europe: the positive and negative North Atlantic Oscillation, the Scandinavian blocking and the Atlantic ridge. The results of the GDD model, driven with the MPI-ESM model input, are compared to local pollen and climate records and archaeological data (e.g. grave density and settlement records) to shed more light on the local climate, vegetation and society impact. This comparison allows us to better understand how a natural hazard influenced local areas and climate records in Southeastern Norway. This study is part of the VIKINGS project, which focuses on the impact of volcanic eruptions on climate, environment and society in Norway/ Scandinavia.

How to cite: van Dijk, E., Gundersen, I. M., Bajard, M., Høeg, H., Løftsgård, K., Iversen, F., Timmreck, C., Jungclaus, J., and Krüger, K.: Large volcanic eruptions as a natural hazard: The impact of the 536/540 CE double event on the atmospheric circulation, surface climate, vegetation and society in Scandinavia, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-12270, https://doi.org/10.5194/egusphere-egu21-12270, 2021.

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