Evelien Van Dijk

• Van Dijk, Evelien; Gundersen, Ingar Mørkestøl; de Bode, Anna; Høeg, Helge Irgens; Loftsgarden, Kjetil & Iversen, Frode [Vis alle 9 forfattere av denne artikkelen] (2023). Climate and societal impacts in Scandinavia following the 536 and 540 CE volcanic double event. Climate of the Past. ISSN 1814-9324. 19(2), s. 357–398. doi: 10.5194/cp-19-357-2023. Fulltekst i vitenarkiv Vis sammendrag

  In the Northern Hemisphere, the mid-6th century was one of the coldest periods of the last 2000 years, as indicated by both proxy records and Earth System Model (ESM) simulations. This cold period was initiated by volcanic eruptions in 536 CE and 540 CE. Evidence from historical sources, archaeological findings, and proxy records suggests that the extent and severity of this volcanic induced cooling was spatially heterogeneous and that the effect on society resulted in adaptation and resilience at some locations, whereas social crisis has been indicated at others. Here, we study the effect of the volcanic double event in 536 CE and 540 CE on the climate and society in Scandinavia with a special focus on Southern Norway. Using an ensemble of Max Planck Institute ESM transient simulations for 521–680 CE, the temperature, precipitation and atmospheric circulation patterns are studied. The simulated cooling magnitude is then used as input for the growing degree day (GDD) model set-up for Southern Norway. This GDD model indicates the possible effects on agriculture for three different study areas in Southern Norway, representative of typical meteorological and landscape conditions. Pollen from bogs and archaeological records inside the study area are then analysed at high resolution (1–3 cm sample intervals) to give insights into the validity of the GDD model set-up with regard to the volcanic climate impact on the regional scale, and to link the different types of data sets. After the 536/540 CE double event, a maximum surface air cooling of up to 3.5 °C during the mean growing season is simulated regionally in Southern Norway. With a worst-case scenario cooling of 3 °C, the GDD model indicates crop failures were likely in our northernmost and western study areas, while crops were more likely to mature in the southeastern study area. These results are in agreement with the pollen records from the respective areas. During the sixth century, excavations show an abandonment of farms, severe social impact but also a continuation of occupation or a mix of those. In addition, archaeological findings from one of the excavation sites suggest wetter conditions for the mid-sixth century in Scandinavia, as simulated by individual ensemble members. Finally, we discuss the likely climate and societal impacts of the 536/540 CE volcanic double event by synthesising the new and available data sets for the whole Scandinavia.

• Van Dijk, Evelien; Jungclaus, Johann; Lorenz, Stephan; Timmreck, Claudia & Krüger, Kirstin (2022). Was there a volcanic-induced long-lasting cooling over the Northern Hemisphere in the mid-6th-7th century? Climate of the Past. ISSN 1814-9324. 18(7), s. 1601–1623. doi: 10.5194/cp-18-1601-2022. Fulltekst i vitenarkiv

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• Krüger, Kirstin; Fuglestvedt, Herman Fæhn; Van Dijk, Evelien; Zhuo, Zhihong; Sigl, Michael & Toohey, Matthew (2022). Modelling volcanic climate and environmental impacts and their signals in ice cores.
• Van Dijk, Evelien; Gundersen, Ingar Mørkestøl; Loftsgarden, Kjetil; Ballo, Eirik Gottschalk; Krüger, Kirstin & Iversen, Frode (2021). Can we link volcanic impacts on the climate to a change in society?
• Van Dijk, Evelien; Gundersen, Ingar Mørkestøl; Loftsgarden, Kjetil; Krüger, Kirstin & Iversen, Frode (2021). Can we link volcanic impacts on the climate to a change in society in Norway?
• Van Dijk, Evelien & Krüger, Kirstin (2021). 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.
• Van Dijk, Evelien & Krüger, Kirstin (2021). Impact of large volcanic eruptions on the 6th-7th century climate.
• Van Dijk, Evelien (2020). Was there a volcanic induced long lasting cooling in the mid 6th-7th century?
• Van Dijk, Evelien & Krüger, Kirstin (2020). Was there a volcanic induced long lasting cooling in the mid 6th-7th century?
• Van Dijk, Evelien Jacoba Cornelia & Krüger, Kirstin (2020). The impact of the 536/540 CE double volcanic eruption event on the climate.
• Van Dijk, Evelien Jacoba Cornelia & Krüger, Kirstin (2020). Impact of the 536/540 CE double volcanic eruption event on the 6th-7th century climate using model and proxy data.
• Van Dijk, Evelien Jacoba Cornelia & Krüger, Kirstin (2020). Impact of the 536/540 CE double eruption event on the 6th -7th century climate using model and proxy data.
• Van Dijk, Evelien Jacoba Cornelia (2019). The impact of the double volcanic eruption event 536/540 CE on the climate.
• Van Dijk, Evelien Jacoba Cornelia (2019). A first impression of the impact of the 536/540 double eruption event on surface climate.
• Van Dijk, Evelien Jacoba Cornelia (2019). The impact of the 536/540 CE double eruption event on the climate.
• Van Dijk, Evelien Jacoba Cornelia (2019). The impact of the 536/540 CE double eruption event on the climate.

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