Data assimilation for volcanic ash plumes using a satellite observational operator: a case study on the 2010 Eyjafjallajökull volcanic eruption
Using data assimilation (DA) to improve model forecast accuracy is a powerful approach that requires available observations. Infrared satellite measurements of volcanic ash mass loadings are often used as input observations for the assimilation scheme. However, because these primary satellite-retrie...
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doaj-d484e9b569a345b1bf873d82c9258a8e2020-11-24T21:07:21ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242017-01-011721187120510.5194/acp-17-1187-2017Data assimilation for volcanic ash plumes using a satellite observational operator: a case study on the 2010 Eyjafjallajökull volcanic eruptionG. Fu0F. Prata1H. X. Lin2A. Heemink3A. Segers4S. Lu5Delft University of Technology, Delft Institute of Applied Mathematics, Mekelweg 4, 2628 CD Delft, the NetherlandsNicarnica Aviation AS, Gunnar Randers vei 24, 2007 Kjeller, NorwayDelft University of Technology, Delft Institute of Applied Mathematics, Mekelweg 4, 2628 CD Delft, the NetherlandsDelft University of Technology, Delft Institute of Applied Mathematics, Mekelweg 4, 2628 CD Delft, the NetherlandsTNO, Department of Climate, Air and Sustainability, P.O. box 80015, 3508 TA Utrecht, the NetherlandsDelft University of Technology, Delft Institute of Applied Mathematics, Mekelweg 4, 2628 CD Delft, the NetherlandsUsing data assimilation (DA) to improve model forecast accuracy is a powerful approach that requires available observations. Infrared satellite measurements of volcanic ash mass loadings are often used as input observations for the assimilation scheme. However, because these primary satellite-retrieved data are often two-dimensional (2-D) and the ash plume is usually vertically located in a narrow band, directly assimilating the 2-D ash mass loadings in a three-dimensional (3-D) volcanic ash model (with an integral observational operator) can usually introduce large artificial/spurious vertical correlations.<br><br>In this study, we look at an approach to avoid the artificial vertical correlations by not involving the integral operator. By integrating available data of ash mass loadings and cloud top heights, as well as data-based assumptions on thickness, we propose a satellite observational operator (SOO) that translates satellite-retrieved 2-D volcanic ash mass loadings to 3-D concentrations. The 3-D SOO makes the analysis step of assimilation comparable in the 3-D model space.<br><br>Ensemble-based DA is used to assimilate the extracted measurements of ash concentrations. The results show that satellite DA with SOO can improve the estimate of volcanic ash state and the forecast. Comparison with both satellite-retrieved data and aircraft in situ measurements shows that the effective duration of the improved volcanic ash forecasts for the distal part of the Eyjafjallajökull volcano is about 6 h.http://www.atmos-chem-phys.net/17/1187/2017/acp-17-1187-2017.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
G. Fu F. Prata H. X. Lin A. Heemink A. Segers S. Lu |
spellingShingle |
G. Fu F. Prata H. X. Lin A. Heemink A. Segers S. Lu Data assimilation for volcanic ash plumes using a satellite observational operator: a case study on the 2010 Eyjafjallajökull volcanic eruption Atmospheric Chemistry and Physics |
author_facet |
G. Fu F. Prata H. X. Lin A. Heemink A. Segers S. Lu |
author_sort |
G. Fu |
title |
Data assimilation for volcanic ash plumes using a satellite observational operator: a case study on the 2010 Eyjafjallajökull volcanic eruption |
title_short |
Data assimilation for volcanic ash plumes using a satellite observational operator: a case study on the 2010 Eyjafjallajökull volcanic eruption |
title_full |
Data assimilation for volcanic ash plumes using a satellite observational operator: a case study on the 2010 Eyjafjallajökull volcanic eruption |
title_fullStr |
Data assimilation for volcanic ash plumes using a satellite observational operator: a case study on the 2010 Eyjafjallajökull volcanic eruption |
title_full_unstemmed |
Data assimilation for volcanic ash plumes using a satellite observational operator: a case study on the 2010 Eyjafjallajökull volcanic eruption |
title_sort |
data assimilation for volcanic ash plumes using a satellite observational operator: a case study on the 2010 eyjafjallajökull volcanic eruption |
publisher |
Copernicus Publications |
series |
Atmospheric Chemistry and Physics |
issn |
1680-7316 1680-7324 |
publishDate |
2017-01-01 |
description |
Using data assimilation (DA) to improve
model forecast accuracy is a powerful approach that requires available observations.
Infrared satellite measurements of volcanic ash mass loadings
are often used as input observations for the assimilation scheme.
However, because these primary satellite-retrieved data
are often two-dimensional (2-D) and
the ash plume is usually vertically located in a narrow band,
directly assimilating the 2-D ash mass loadings
in a three-dimensional (3-D) volcanic ash model (with an integral observational operator)
can usually introduce large
artificial/spurious vertical correlations.<br><br>In this study, we look at an approach to avoid the artificial vertical
correlations by not involving the integral operator.
By integrating available data of ash mass loadings and cloud top heights, as
well as
data-based assumptions on thickness, we propose a
satellite observational operator (SOO) that translates satellite-retrieved
2-D volcanic ash mass loadings to
3-D concentrations. The 3-D SOO makes the analysis step of assimilation
comparable in the 3-D model space.<br><br>Ensemble-based DA is used to
assimilate the extracted measurements of ash concentrations.
The results show that satellite DA with SOO
can improve the estimate of volcanic ash state and the
forecast. Comparison with both satellite-retrieved data and aircraft in situ measurements
shows that the effective duration of
the improved volcanic ash forecasts for the distal part of the
Eyjafjallajökull volcano is about 6 h. |
url |
http://www.atmos-chem-phys.net/17/1187/2017/acp-17-1187-2017.pdf |
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