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• 31. Protective measures

  to avalances: An overview of the need for avalanche protection measures in Iceland (IMO Rep. 96004, 1996, authors T. Jóhannesson, K. Lied, S. Margreth and F. Sandersen) [summary of IMO publication 96003/96004] (html) Adaptation of the Swiss Guidelines for supporting structures for Icelandic conditions (IMO Int. Rep. 99013, 1999, authors T. Jóhannesson and S. Margreth) (pdf 0.1 Mb) Addendum /avalanches/imo/protective/

• 32. 16910025

  Flugskýrsla TF-SIF 30. nóvember 2010 Flug nr. 16910.025 Áhöfn: Flugstjóri Benóný Ásgrímsson Flugmaður Hafsteinn Heiðarsson Flugmaður 2 / Þjálfunarfl. Yfirstýrimaður Auðunn F. Kristinsson Stýrimaður Gunnar Örn Arnarson Stýrimaður Stýrimaður Aðrir Flugtími: Flugvöllur Hreyfing Flugtak Flugvöllur Lending Stöðvað Flugtími Blokktími Sjml. BIRK 08:31 08:35 /media/hafis/skyrslur_lhg/16910025.pdf

• 33. Eyjafjallajokull_status_2010-04-30_IES_IMO

  scientists at Gígjökull; and aerial observations from the Icelandic Coastguard (observation plane TF-SIF). Eruption plume: Height (a.s.l.): Detected by weather radar at 15:20 GMT at an elevation of 2.8 km over the eruption site. TF-SIF observations at 15:40 GMT confirmed a steam plume rising to 4.5–5.1 km (15–17,000 ft). Clouds of ash at lower elevations observed drifting south /media/jar/Eyjafjallajokull_status_2010-04-30_IES_IMO.pdf

• 34. Paper-Olafur-Rognvaldsson_91

  balance data from all the ice caps. REFERENCES Björnsson, H., Pálsson F., Guðmundsson M. T. and Haraldsson H. 1998. Mass balance of western and northern Vatnajökull, Iceland, 1991–1995, Jökull, 45, 35–58. Björnsson, H., Pálsson F. and Haraldsson H. 2002. Mass balance of Vatnajökull (1991–2001) and Langjökull (1996–2001), Iceland. Jökull, 51, 75–78. Bromwich, D. H., Bai L. and Bjarnason G. G. 2005 /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 35. Outline_for_the_case_Road_maintenance_in_a_changing_climate

  course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011 …………………………………………………………………………………………………………………………………………………………………… 6 Figure 1. Flow chart summarizing information and decision flows of an adaptive management inspired adaptation planning cycle for road transport (at national strategic / tactical level) M a n d a t e f r o m g o v e r n m e n t + p r /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf

• 36. 47th Nordic Seismology Seminar - Reykjanes peninsula

  into the terrain require solid shoes and protective cloths. You should also bring something to drink and eat with you, but we will also stop at a gas station, where you can provide yourself with food etc. The whole trip will take around 5 hours. Planned stops during the excursion: Lake Kleifarvatn and Seltún Geothermal Field Gunnuhver Steam Spring and fault systems in its surrounding /norsem/norsem2016/field-trip/

• 37. News

  2010, as seen at 12:00 GMT at an elevation of 3-3.6 km (10-12,000 ft). Light coloured, low-lying clouds of steam were observed over the eruption site, together with occasional bursts of grey to black-coloured cloud, which rise 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 (not visible here /about-imo/news/bigimg/1891

• 38. Bardarbunga_daily_status_report_31082014

  Bárðarbunga update 31082014 2014-08-31 16:41 UTC update 31_08_2014 Compiled by Icelandic Meteorological Office, University of Iceland, ed. Sara Barsotti and Halldór Björnsson. Based on Seismic, GPS, Hydrology, Radar, Webcam, 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 /media/jar/Bardarbunga_daily_status_report_31082014.pdf

• 39. Eyjafjallajokull_status_2010-05-08_IES_IMO

  the rim of the ice edge around the crater. The plume does'nt rise vertically from the crater, but bends SE-wards due to wind. Plume reaches higher after larger explosions. Thephra fallout near the crater is considerably less than was observed on May 6th. There is little lava flow down Gígjökull and the lava front has not changed for the last couple of days. Very little steam rises from /media/jar/Eyjafjallajokull_status_2010-05-08_IES_IMO.pdf

• 40. Factsheet-Bardarbunga-140905

  fissures are substantially smaller than in the older fissure. Steam and gas rises in a south eastern direction from the fissure. o The cauldron in Dyngjujökull seems to have grown deeper since the last observation. o No changes are visible in Bárðarbunga.  Substantial amounts of SO2 are still being released to the atmosphere in association with the eruption.  Conductivity measurements show /media/jar/Factsheet-Bardarbunga-140905.pdf