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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7456

Authors: Bonadonna, C.*
Genco, R.*
Gouhier, M.*
Pistolesi, M.*
Cioni, R.*
Alfano, F.*
Hoskuldsson, A.*
Ripepe, M.*
Title: Tephra sedimentation during the 2010 Eyjafjallajökull eruption (Iceland) from deposit, radar, and satellite observations
Title of journal: Journal of Geophysical Research
Series/Report no.: /116(2011)
Publisher: American Geophysical Union
Issue Date: 2011
DOI: 10.1029/2011JB008462
URL: http://www.agu.org/pubs/crossref/2011/2011JB008462.shtml
Keywords: MSG-SEVIRI, PLUDIX
particle aggregation
settling velocity
tephra deposits
weak plumes
Abstract: The April–May 2010 eruption of the Eyjafjallajökull volcano (Iceland) was characterized by a nearly continuous injection of tephra into the atmosphere that affected various economic sectors in Iceland and caused a global interruption of air traffic. Eruptive activity during 4–8 May 2010 was characterized based on short-duration physical parameters in order to capture transient eruptive behavior of a long-lasting eruption (i.e., total grain-size distribution, erupted mass, and mass eruption rate averaged over 30 min activity). The resulting 30 min total grain-size distribution based on both ground and Meteosat Second Generation-Spinning Enhanced Visible and Infrared Imager (MSG-SEVIRI) satellite measurements is characterized by Mdphi of about 2 and a fine-ash content of about 30 wt %. The accumulation rate varied by 2 orders of magnitude with an exponential decay away from the vent, whereas Mdphi shows a linear increase until about 18 km from the vent, reaching a plateau of about 4.5 between 20 and 56 km. The associated mass eruption rate is between 0.6 and 1.2 × 105 kg s−1. In situ sampling showed how fine ash mainly fell as aggregates of various typologies. About 5 to 9 wt % of the erupted mass remained in the cloud up to 1000 km from the vent, suggesting that nearly half of the ash >7 settled as aggregates within the first 60 km. Particle sphericity and shape factor varied between 0.4 and 1 with no clear correlation to the size and distance from vent. Our experiments also demonstrate how satellite retrievals and Doppler radar grain-size detection can provide a real-time description of the source term but for a limited particle-size range.
Appears in Collections:04.04.06. Rheology, friction, and structure of fault zones
04.08.07. Instruments and techniques
Papers Published / Papers in press

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