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• 51. Bardarbunga_Daily_status_report_290814

  Bárðarbunga update 29082014 2014-08-29 16:20 UTC Bárðarbunga update Compiled by Icelandic Met Office and University of Iceland Þórður Arason (Ed.) Based on Seismic, GPS, Hydrology, Radar, Webcam, PIREP, visual observations Eruption plume Height (a.s.l.) No plume was detected by radar (detection limit above 1 km) and webcam indicated low level gases and steam from lava fountains during the night /media/jar/Bardarbunga_Daily_status_report_290814.pdf

• 52. Eyjaf_status_2010-05-04_IES_IMO

  site, larger than yesterday. White (steam) plumes rising from Gígjökull outlet glacier, north of the eruption site smaller than yesterday. Tephra fallout: According to the police at Hvolsvöllur there was ash-fall in Álftaver and Meðalland, 65-80 km east-south-east of Eyjafjallajökull, where people could hardly see next farms (in a few kilometres distance). Lightning: No detections today /media/jar/Eyjaf_status_2010-05-04_IES_IMO.pdf

• 53. Eyjafjallajokull_status_2010-04-28_IES_IMO

  from the local police; and geologist’s observations of Eyjafjallajokull, west of the eruption site (no overflight today) Eruption plume: Height (a.s.l.): Plume not detected above a cloud level of 4 km (~13,000 ft). Heading: West-northwest from the eruption site. Colour: White (steam) clouds were visible over the advancing lava front. Grey- coloured (ash) clouds were seen occassionally over /media/jar/Eyjafjallajokull_status_2010-04-28_IES_IMO.pdf

• 54. Eyjafjallajokull_status_2010-05-03_IES_IMO

  the eruptive site. White (steam) plumes rising from Gígjökull otulet glacier, north of the eruption site (similar as yesterday). Tephra fallout: Moderate ash-fall reported in Álftaver, 65-70 km east-south-east of Eyjafjallajökull (07:00-10:00 GMT. An ash cloud also observed over village of Vík (10:00 GMT), 40 km south-east of Eyjafjallajökull. Lightning: No detections today over the eruption site /media/jar/Eyjafjallajokull_status_2010-05-03_IES_IMO.pdf

• 55. Factsheet_Bardarbunga_140908

  due to the lava and river water interaction has been observed, but steam rises from the lava. o The extent of the lava is now approximately 19 square km. o No activity is now detected on the southernmost fissure although small amounts of gas and steam are rising from it.  Air quality in urban areas in East of Iceland: o Measured concentrations of SO2 in Reyðarfjörður, suggest that people /media/jar/Factsheet_Bardarbunga_140908.pdf

• 56. Eyjafj_status_2010-04-27

  the air at 12:00 GMT at an elevation of 3–3.6 km (10–12,000 ft). Heading: West–northwest from the eruption site. Colour: Light, low-lying clouds of steam observed over the eruption site, together with occasional bursts of grey to black-coloured cloud, which rose to up to half of the total height of the eruption plume. Above this level, the plume was lighter in colour with a capping of white cloud /media/jar/myndsafn/Eyjafj_status_2010-04-27.pdf

• 57. High resolution precipitation maps for Iceland

  maps for 1971-2000 Daily precipitation maps are available on request and further information on the making of the maps. IMO's contacts for this project are Philippe Crochet and Tómas Jóhannesson. Reference: Crochet, P., T. Jóhannesson, T. Jónsson, O. Sigurðsson, H. Björnsson, F. Pálsson and I. Barstad (2007): Estimating the spatial distribution of precipitation in Iceland using a linear model /weather/articles/nr/1625

• 58. Isskyrsla_20100120

  Flugskýrsla TF-SIF Dags 20.01.2010. Flug nr. 00410.025 Áhöfn: Flugstjóri: Benóny Ásgrímsson Flugmaður: Hafsteinn Heiðarsson Yfirstýrimaður: Auðunn F. Kristinsson Stýrimaður: Guðmundur E. Sigurðsson Stýrimaður: Vilhjálmur Ó. Valsson Aðrir: Earl Wilson Flugtími: Flugvöllur Hreyfing Flugtak Flugvöllur Lending Stöðvað Flugtími Blokktími Sjml. BIRK 18:45 18:50 BIRK ########### ########### 720 00:00 00 /media/hafis/skyrslur_lhg/Isskyrsla_20100120.pdf

• 59. norsem_lindholm

  Neotectonics in Nordland; NEONOR 2 C. Lindholm, O. Olesen, I. Janutyte, S. Gradman, M. Keiding, H. Kierulf, M. Ask, J. Dehls, Y. Maystrenko, F. Riis, L. Rise and other project partners The Nordland shore region is known to be seismically active with deep local sediment basins on the continental shelf that stretches some 200 km west of the coastline. The offshore areas west of Nordland have /media/norsem/norsem_lindholm.pdf

• 60. Update on activity in Eyjafjallajökull 2010

  in the crater. Possibly, some degassing of magma still occurs in a small path located at the western or soutwestern rim of the crater, see brownish veils at the right hand side of the photograph below. Steam rises from the surface of the water, mostly at the northern edge. Lake in the crater Eyjafjallajökull 11th June 2010 07:55. A lake has formed in the crater. Photo: Sigurlaug /earthquakes-and-volcanism/articles/nr/1884