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<article language="en">
	<journal>
		<journal_title>Earth System Science Data</journal_title>
		<journal_url>www.earth-syst-sci-data.net</journal_url>
		<issn>1866-3508</issn>
		<eissn>1866-3516</eissn>
		<volume_number>3</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2011</publication_year>
	</journal>
	<doi>10.5194/essd-3-9-2011</doi>
	<article_url>http://www.earth-syst-sci-data.net/3/9/2011/</article_url>
	<abstract_html>http://www.earth-syst-sci-data.net/3/9/2011/essd-3-9-2011.html</abstract_html>
	<fulltext_pdf>http://www.earth-syst-sci-data.net/3/9/2011/essd-3-9-2011.pdf</fulltext_pdf>
	<start_page>9</start_page>
	<end_page>17</end_page>
	<publication_date>2011-09-05</publication_date>
	<article_title content_type="html">Observations of the altitude of the volcanic plume during the eruption of EyjafjallajÃ¶kull, Aprilâ€“May 2010</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. Arason</name>
			<email>arason@vedur.is</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>G. N. Petersen</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>H. Bjornsson</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Icelandic Meteorological Office, Reykjavik, Iceland</affiliation>
	</affiliations>
	<abstract content_type="html">The eruption of EyjafjallajÃ¶kull volcano in 2010 lasted for 39 days,
14 April&amp;ndash;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 KeflavÃ­k 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 HvolsvÃ¶llur 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
 (&lt;a href=&quot;http://dx.doi.org/10.1594/PANGAEA.760690&quot; target=&quot;_blank&quot;&gt;http://dx.doi.org/10.1594/PANGAEA.760690&lt;/a&gt;).</abstract>
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</article>

