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the claim

The 2010 Eyjafjallajökull eruption caused major aviation disruption.

the verdict
SUPPORTED
the evidence backs this
Recorded sources
7 sources for · 0 against

Counts group repeated records of the same source within each side. They do not measure evidence strength or source independence.

Is it true that the 2010 Eyjafjallajökull eruption caused major aviation disruption?

Yes. Multiple peer-reviewed sources and a reference article state that the April–May 2010 Eyjafjallajökull eruption caused major or unprecedented disruption to European air traffic, with airspace closures and millions of passengers stranded.

Verdict: SUPPORTED · 7 sources for, 0 against · Last checked

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Evidence for · 7
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Air travel disruption after the 2010 Eyjafjallajökull eruption - Wikipedia. (n.d.). en.wikipedia.org. https://en.wikipedia.org/wiki/Air_travel_disruption_after_the_2010_Eyjafjallaj%C3%B6kull_eruption

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More for · 6
2011
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Ulfarsson, G. F. & Unger, E. A. (2011). Impacts and Responses of Icelandic Aviation to the 2010 Eyjafjallajökull Volcanic Eruption. doi.org. https://doi.org/10.3141/2214-18

2010
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Petersen, G. N. (2010). A short meteorological overview of the Eyjafjallajökull eruption 14 April–23 May 2010. doi.org. https://doi.org/10.1002/wea.634

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Volcanic SO 2 , BrO and plume height estimations using GOME‐2 satellite measurements during the eruption of Eyjafjallajökull in May 2010. (n.d.). cir.nii.ac.jp. https://doi.org/10.1029/2011jd016718

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Determination of time- and height-resolved volcanic ash emissions and their use for quantitative ash dispersion modeling: the 2010 Eyjafjallajökull eruption. (n.d.). cir.nii.ac.jp. https://doi.org/10.5194/acp-11-4333-2011

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Improved detection of sulphur dioxide in volcanic plumes using satellite‐based hyperspectral infrared measurements: Application to the Eyjafjallajökull 2010 eruption. (n.d.). cir.nii.ac.jp. https://doi.org/10.1029/2011jd016810

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Atmospheric Dispersion Modelling at the London VAAC: A Review of Developments since the 2010 Eyjafjallajökull Volcano Ash Cloud. (n.d.). cir.nii.ac.jp. https://doi.org/10.3390/atmos11040352

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