Stratospheric volcanic ash emissions from the 13 February 2014 Kelut eruption

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...

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Bibliographic Details
Published inGeophysical research letters Vol. 42; no. 2; pp. 588 - 596
Main Authors Kristiansen, N. I., Prata, A. J., Stohl, A., Carn, S. A.
Format Journal Article
LanguageEnglish
Published Washington Blackwell Publishing Ltd 28.01.2015
John Wiley & Sons, Inc
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Summary: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. Key Points Combining satellite retrievals and modeling gives valuable information Volcanic ash source term is constrained by satellite observations Estimates of modeled ash concentrations encountered by a commercial aircraft
Bibliography:Aura Science Team - No. NNX11AF42G
ArticleID:GRL52507
MEaSUREs - No. NNX13AF50G
istex:C9F223C7B16DC70728FE72FDE27C99CC315C9856
European Space Agency
ark:/67375/WNG-33Q9JBMT-J
Data S1Readme
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0094-8276
1944-8007
DOI:10.1002/2014GL062307