Earth System Science Data (Oct 2012)

Two weather radar time series of the altitude of the volcanic plume during the May 2011 eruption of Grímsvötn, Iceland

  • G. N. Petersen,
  • H. Bjornsson,
  • P. Arason,
  • S. von Löwis

DOI
https://doi.org/10.5194/essd-4-121-2012
Journal volume & issue
Vol. 4, no. 1
pp. 121 – 127

Abstract

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The eruption of Grímsvötn volcano in Iceland in 2011 lasted for a week, 21&ndash;28 May. The eruption was explosive and peaked during the first hours, with the eruption plume reaching 20&ndash;25 km altitude. The height of the plume was monitored every 5 min with a C-band weather radar located at Keflavík International Airport and a mobile X-band radar, 257 km and 75 km distance from the volcano respectively. In addition, photographs taken during the first half-hour of the eruption give information regarding the initial rise. Time series of the plume-top altitude were constructed from the radar observations. This paper presents the two independent radar time series. The series have been cross validated and there is a good agreement between them. 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.778390"target="_blank">doi:10.1594/PANGAEA.778390</a>).