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• 31. VI_2020_004

  Preliminary tephra fallout hazard assessment for selected eruptive scenarios in Iceland Sara Barsotti Sigrún Karlsdóttir Anna María Ágústsdóttir Björn Oddsson Íris Marelsdóttir Þorvaldur Þórðarson Þórólfur Guðnason Bogi B. Björnsson VÍ 2020-004 Skýrsla Preliminary tephra fallout hazard assessment for selected eruptive scenarios in Iceland VÍ 2020-004 ISSN 1670-8261 Skýrsla +354 522 60 00 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 32. Paper-Olafur-Rognvaldsson_91

  is done by using the mesoscale MM5 model (Grell et al., 1995). This paper begins with a description of the model approach, followed by comparison of the model results to data and concluding remarks. MODELLING WITH THE MM5 MODEL The idea of using limited area models (LAMs) for regional climate simula- tions was introduced by Dickinson et al. (1989) and refined by Giorgi (1990). One of the benefits /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 33. IPPC-2007-ar4_syr

  %; exceptionally unlikely <1%. WG II has used a combination of confidence and likelihood assessments and WG I has predominantly used likelihood assessments. This Synthesis Report follows the uncertainty assessment of the underlying WGs. Where synthesised findings are based on information from more than one WG, the description of uncertainty used is consistent with that for the components drawn from /media/loftslag/IPPC-2007-ar4_syr.pdf

• 34. Kok_and_Veldkamp_editorial_ES-2011-4160

  positivism and realism on the one hand, and constructivism and relativism on the other. Particularly political geographers have thoroughly addressed the idea that scales are socially constructed, a notion that is gaining importance. Recognizing the domination of ecological theories, Sayre (2005) for example, states that ecology goes astray if it mistakes the scales of natural processes as sufficient /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 35. Eyjafjallajokull_status_2010-06-07_IES_IMO

  Eruption in Eyjafjallajökull Status Report: 11:00 GMT, 7 June 2010 Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland Compiled by: Gunnar B. Guðmundsson, Sigurlaug Hjaltadóttir, Ármann Höskuldsson, Björn Sævar Einarsson, Haraldur Eiríksson, Þorvaldur Þórðarsson, Guðrún Larsen, Sigrún Hreinsdóttir and Bergthóra S. Thorbjarnardóttir. Based on: IMO seismic /media/jar/Eyjafjallajokull_status_2010-06-07_IES_IMO.pdf

• 36. glacier_mass_balance_poster

  from October 5, 2004 - spatial resolution: 40x40 m - accuracy: 10 m in elevation and 30 m in horizontal position b) SPOT 5 HRS from August 14, 2004 c) EMISAR from August 12, 1998 - reference map for co-registration and offset correction - spatial resolution 5x5 m - accuracy <2 m in elevation and 5 m in horizontal position d) aerial photographs from the 1980s: i. Torfajökull ice cap (To) from /media/ces/glacier_mass_balance_poster.pdf

• 37. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  2000). The concept of IWRM is essentially a response to the much criticised top-down sectoral approach to water management (Pahl-Wostl 2007). Many of the world’s socio-economic systems are becoming linked at an unprecedented rate. The impacts of extreme climates in flood and drought conditions are increasingly witnessed (Easterling et al. 2000). It is within this setting that water managers need /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 38. “The small eruption” in

  swarm in December 2019 until the beginning of the eruption (Graph: Skjálfta-Lísa from the Icelandic Meteorological Office (IMO)). Satellite and GPS signals showed that a magmatic dyke extended southwest from Keilir to Fagradaslfjall (Figure 2 A&B) and was getting shallower day by day. Uncertainty remained whether the intrusion would result in an eruption. “For the deformation team the period /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months

• 39. “The small eruption” in

  swarm in December 2019 until the beginning of the eruption (Graph: Skjálfta-Lísa from the Icelandic Meteorological Office (IMO)). Satellite and GPS signals showed that a magmatic dyke extended southwest from Keilir to Fagradaslfjall (Figure 2 A&B) and was getting shallower day by day. Uncertainty remained whether the intrusion would result in an eruption. “For the deformation team the period /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months/

• 40. Safetravel

  Nothing can replace the safe measure of leaving a travel plan behind. Travel Plan One of the most important things to do when preparing a journey is to make a detailed travel plan and leave with someone who can act if needed. Travel plan should always include the following information: Date of travel, departure time and arrival time Name of those who travel, phone number or other /about-imo/news/nr/2497