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Stratospheric volcanic ash emissions from the 13 February 2014 Kelut eruption

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dc.contributor.author Kristiansen, N. I. en
dc.contributor.author Prata, A. J. en
dc.contributor.author Stohl, A. en
dc.contributor.author Carn, Simon A. en
dc.date.accessioned 2015-04-20T15:16:03Z
dc.date.available 2015-04-20T15:16:03Z
dc.date.issued 2015
dc.identifier.citation Kristiansen, N. I., Prata, A. J., Stohl, A., and Carn, Simon A. 2015. "Stratospheric volcanic ash emissions from the 13 February 2014 Kelut eruption." <em>Geophysical Research Letters</em>. 42 (2):588&ndash;596. <a href="https://doi.org/10.1002/2014GL062307">https://doi.org/10.1002/2014GL062307</a> en
dc.identifier.issn 0094-8276
dc.identifier.uri http://hdl.handle.net/10088/25762
dc.description.abstract Mount Kelut (Indonesia) erupted explosively around 15:50 UT on 13 February 2014 sending ash and gases into the stratosphere. Satellite ash retrievals and dispersion transport modeling are combined within an inversion framework to estimate the volcanic ash source term and to study ash transport. The estimated source term suggests that most of the ash was injected to altitudes of 16 17?km, in agreement with space-based lidar data. Modeled ash concentrations along the flight track of a commercial aircraft that encountered the ash cloud indicate that it flew under the main ash cloud and encountered maximum ash concentrations of 9?±?3?mg?m-3, mean concentrations of 2?±?1?mg?m-3over a period of 10 11?min of the flight, giving a dosage of 1.2?±?0.3?g?s?m-3. Satellite data could not be used directly to observe the ash cloud encountered by the aircraft, whereas inverse modeling revealed its presence. en
dc.relation.ispartof Geophysical Research Letters en
dc.title Stratospheric volcanic ash emissions from the 13 February 2014 Kelut eruption en
dc.type Journal Article en
dc.identifier.srbnumber 134037
dc.identifier.doi 10.1002/2014GL062307
rft.jtitle Geophysical Research Letters
rft.volume 42
rft.issue 2
rft.spage 588
rft.epage 596
dc.description.SIUnit NH-Mineral Sciences en
dc.description.SIUnit NMNH en
dc.description.SIUnit Peer-reviewed en
dc.citation.spage 588
dc.citation.epage 596


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