Observations of the altitude of the volcanic plume during the eruption of Eyjafjallajökull, April–May 2010

The eruption of Eyjafjallajökull volcano in 2010 lasted for 39 days, 14 April–23 May. The eruption had two explosive phases separated by a phase with lava formation and reduced explosive activity. The height of the plume was monitored every 5 min with a C-band weather radar located in...

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Main Authors: P. Arason, G. N. Petersen, H. Bjornsson
Format: Article
Language:English
Published: Copernicus Publications 2011-09-01
Series:Earth System Science Data
Online Access:http://www.earth-syst-sci-data.net/3/9/2011/essd-3-9-2011.pdf
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spelling doaj-20e35eb7de3e4e70aa0b000bb201a0ce2020-11-24T21:40:47ZengCopernicus PublicationsEarth System Science Data1866-35081866-35162011-09-013191710.5194/essd-3-9-2011Observations of the altitude of the volcanic plume during the eruption of Eyjafjallajökull, April–May 2010P. ArasonG. N. PetersenH. BjornssonThe eruption of Eyjafjallajökull volcano in 2010 lasted for 39 days, 14 April–23 May. The eruption had two explosive phases separated by a phase with lava formation and reduced explosive activity. The height of the plume was monitored every 5 min with a C-band weather radar located in Keflavík International Airport, 155 km distance from the volcano. Furthermore, several web cameras were mounted with a view of the volcano, and their images saved every five seconds. Time series of the plume-top altitude were constructed from the radar observations and images from a web camera located in the village Hvolsvöllur at 34 km distance from the volcano. This paper presents the independent radar and web camera time series and performs cross validation. The results show good agreement between the time series for the range when both series are available. However, while the radar altitudes are semi-discrete the data availability was much higher than for the web camera, indicating how essential weather radars are as eruption plume monitoring devices. The echo top radar series of the altitude of the volcanic plume are publicly available from the Pangaea Data Publisher (<a href="http://dx.doi.org/10.1594/PANGAEA.760690" target="_blank">http://dx.doi.org/10.1594/PANGAEA.760690</a>).http://www.earth-syst-sci-data.net/3/9/2011/essd-3-9-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author P. Arason
G. N. Petersen
H. Bjornsson
spellingShingle P. Arason
G. N. Petersen
H. Bjornsson
Observations of the altitude of the volcanic plume during the eruption of Eyjafjallajökull, April–May 2010
Earth System Science Data
author_facet P. Arason
G. N. Petersen
H. Bjornsson
author_sort P. Arason
title Observations of the altitude of the volcanic plume during the eruption of Eyjafjallajökull, April–May 2010
title_short Observations of the altitude of the volcanic plume during the eruption of Eyjafjallajökull, April–May 2010
title_full Observations of the altitude of the volcanic plume during the eruption of Eyjafjallajökull, April–May 2010
title_fullStr Observations of the altitude of the volcanic plume during the eruption of Eyjafjallajökull, April–May 2010
title_full_unstemmed Observations of the altitude of the volcanic plume during the eruption of Eyjafjallajökull, April–May 2010
title_sort observations of the altitude of the volcanic plume during the eruption of eyjafjallajökull, april–may 2010
publisher Copernicus Publications
series Earth System Science Data
issn 1866-3508
1866-3516
publishDate 2011-09-01
description The eruption of Eyjafjallajökull volcano in 2010 lasted for 39 days, 14 April–23 May. The eruption had two explosive phases separated by a phase with lava formation and reduced explosive activity. The height of the plume was monitored every 5 min with a C-band weather radar located in Keflavík International Airport, 155 km distance from the volcano. Furthermore, several web cameras were mounted with a view of the volcano, and their images saved every five seconds. Time series of the plume-top altitude were constructed from the radar observations and images from a web camera located in the village Hvolsvöllur at 34 km distance from the volcano. This paper presents the independent radar and web camera time series and performs cross validation. The results show good agreement between the time series for the range when both series are available. However, while the radar altitudes are semi-discrete the data availability was much higher than for the web camera, indicating how essential weather radars are as eruption plume monitoring devices. The echo top radar series of the altitude of the volcanic plume are publicly available from the Pangaea Data Publisher (<a href="http://dx.doi.org/10.1594/PANGAEA.760690" target="_blank">http://dx.doi.org/10.1594/PANGAEA.760690</a>).
url http://www.earth-syst-sci-data.net/3/9/2011/essd-3-9-2011.pdf
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