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• 61. VI_2013_006

  Estimation of eruption site location using volcanic lightning Þórður Arason Guðrún Nína Petersen Halldór Björnsson VÍ 2013-006 Report   Estimation of eruption site location using volcanic lightning V Í 201 3 - 006 ISS N 167 0 - 8 261 Report? +354 522 60 00 ved u r@ ve d u r. is Veð u rst of a Ísla n d s Búst a ð a ve gur 7–9 150 Reykja vík Þórður Arason, Icelandic Met /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf

• 62. Bardarbunga_Daily_status_report_290814

  remains at the same high level as in the previous days.The size of the cauldrons recently observed on the glacier has been estimated to be 30-40 million m3, but not clear where the meltwater has gone. Conditions at eruption site At 00:02 UTC signs of a lava eruption were detected on web camera images from Mila. The web-camera is located at Vaðalda, north-east of the eruption site. Around midnight /media/jar/Bardarbunga_Daily_status_report_290814.pdf

• 63. Eyjafjallajokull_status-leidr_2010-05-05_IES_IMO

  measurements, MODIS satellite image; reports from people via phone and the IMO web site, information from the Icelandic Coast Guard flight yesterday. Eruption plume: Height (a.s.l.): Plume at 5.5-6.5 km height according to IMO's weather radar; reached up to 7.2 km 40 SA of eruption site at 17:45 and 8 km height just SE of eruption site at 16:55. Information from ISAVIA: 18-20,000 ft at 14:50 /media/jar/Eyjafjallajokull_status-leidr_2010-05-05_IES_IMO.pdf

• 64. Eyjafjallajokull_status_2010-05-07_IES_IMO

  ; IMO hydrological data; IMO weather radar measurements, MERIS satellite image; reports from sent through the IMO web site, information from commercial flights. Eruption plume: Height (a.s.l.): 7 km according to IMO weather radar measurements at 1155h. Commercial flight heading towards Keflavík at 15:18h: 20,000- 25,000ft (7-7.6 km). Heading: Southeast Colour: Colour: Dark /media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf

• 65. Factsheet_Bardarbunga_140914

  breaking out from the main lava stream towards the east and west. The largest one of these lava tongues stretches towards the east and had become 300 m wide and 2 km long at 18:00 yesterday. An eruption cloud reaches 4 km in height but lowers with distance from the eruption site.  Seismic activity is similar to what it has been in the past days but earthquakes are starting to go down in numbers /media/jar/myndsafn/Factsheet_Bardarbunga_140914.pdf

• 66. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 67. Ash measurements

  in estimating the height of the plume. At this time, the plume reached heights of 8 - 12 km. During the 2010 Eyjafjallajökull eruption, the weather radar proved to be a very useful tool, but the great distance to the eruption site (160 km) reduced the quality of the data. Therefore, a mobile X-band weather radar was purchased, but while this custom made radar was being assembled and tested, another /about-imo/news/nr/2183

• 68. Flight over NW-Vatnajökull 24 Oct 2014

  Snow-covered cauldrons on Dyngjujökull, enlarge. Snow-covered cauldrons on Dyngjujökull, enlarge. Snow-covered cauldrons on Dyngjujökull, enlarge. Faulting on the northern edge of Dyngjujökull, enlarge. Volcanic haze on the northern edge of Dyngjujökull, enlarge. Eruption site, enlarge. Eruption site, enlarge. Eruption site, enlarge. Steam vents over saturated ground beneath /earthquakes-and-volcanism/articles/nr/3008

• 69. Access_conrolled_area_20150213

  the volcanic eruption in Holuhraun. The new hazard assessment is based on the gradual decreased intensity of the volcanic eruption since October, seasonal weather conditions and regular monitoring of gas pollution at the eruption site. A model for weather conditions in the area over the last 10 years and given values of SO2 was also used in the hazard assessment. The risk map that now comes /media/jar/Access_conrolled_area_20150213.pdf

• 70. Eyjafjallajokull_status_2010-04-26_IES_IMO

  : No detections over the eruption site since 19 April 2010 Noises: Report from ~20 km SE of the volcano of booming sounds (02:30 GMT) Meltwater: Continuing discharge of water from Gígjökull due to ice-melt at the eruption site. Discharge at the old Markarfljót bridge, 18 km from Gígjökull, is estimated at 110–130 m3 s–1, of which 30–40 m3 s–1 is baseflow. Conditions at eruption site: No visual /media/jar/Eyjafjallajokull_status_2010-04-26_IES_IMO.pdf