Ground-Based Measurements of the 2014–2015 Holuhraun Volcanic Cloud (Iceland)

The 2014-2015 Bárðarbunga fissure eruption at Holuhraun in central Iceland was distinguished by the high emission of gases, in total 9.6 Mt SO 2 , with almost no tephra. This work collates all ground-based measurements of this extraordinary eruption cloud made under particularly challenging conditio...

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Veröffentlicht in:Geosciences (Basel) 2018-01, Vol.8 (1), p.29
Hauptverfasser: Pfeffer, Melissa, Bergsson, Baldur, Barsotti, Sara, Stefánsdóttir, Gerður, Galle, Bo, Arellano, Santiago, Conde, Vladimir, Donovan, Amy, Ilyinskaya, Evgenia, Burton, Mike, Aiuppa, Alessandro, Whitty, Rachel, Simmons, Isla, Arason, Þórður, Jónasdóttir, Elín, Keller, Nicole, Yeo, Richard, Arngrímsson, Hermann, Jóhannsson, Þorsteinn, Butwin, Mary, Askew, Robert, Dumont, Stéphanie, von Löwis, Sibylle, Ingvarsson, Þorgils, La Spina, Alessandro, Thomas, Helen, Prata, Fred, Grassa, Fausto, Giudice, Gaetano, Stefánsson, Andri, Marzano, Frank, Montopoli, Mario, Mereu, Luigi
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Sprache:eng
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Zusammenfassung:The 2014-2015 Bárðarbunga fissure eruption at Holuhraun in central Iceland was distinguished by the high emission of gases, in total 9.6 Mt SO 2 , with almost no tephra. This work collates all ground-based measurements of this extraordinary eruption cloud made under particularly challenging conditions: remote location, optically dense cloud with high SO 2 column amounts, low UV intensity, frequent clouds and precipitation, an extensive and hot lava field, developing ramparts, and high-latitude winter conditions. Semi-continuous measurements of SO 2 flux with three scanning DOAS instruments were augmented by car traverses along the ring-road and along the lava. The ratios of other gases/SO 2 were measured by OP-FTIR, MultiGAS, and filter packs. Ratios of SO 2 /HCl = 30-110 and SO 2 /HF = 30-130 show a halogen-poor eruption cloud. Scientists on-site reported extremely minor tephra production during the eruption. OPC and filter packs showed low particle concentrations similar to non-eruption cloud conditions. Three weather radars detected a droplet-rich eruption cloud. Top of eruption cloud heights of 0.3-5.5 km agl were measured with ground-and aircraft-based visual observations, web camera and NicAIR II infrared images, triangulation of scanning DOAS instruments, and the location of SO 2 peaks measured by DOAS traverses. Cloud height and emission rate measurements were critical for initializing gas dispersal simulations for hazard forecasting.
ISSN:2076-3263
2076-3263
DOI:10.3390/geosciences8010029