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• 1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  with whom a slot is proposed to be swapped. In the closing session on Friday afternoon another two Workshop participants will be offered the opportunity of presenting a brief summary of key impressions and messages (2 x 5 minutes). This will require some degree of co-ordination among the rapporteurs. The Conference organizers need to know in time (Friday morning at the latest) who will present /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 2. About the implementation

  are in the forefront. Architecture It was decided to use the Eplica content management system. It is as a Java based system so specific dynamic components were written in Java. It was decided to use Servlets and the MVC pattern, with minimal usage of Eplica API. This way the components may be moved and reused with minimal efforts in other Java CMS or converted to Portlets (JSR 168) if and when /about-imo/the-web/implementation/

• 3. Sea ice in May 2011

  was within the Greelandic jurisdiction but only minimal scattered ice within the Icelandic one. The ice was closest to land about 82 nm NW off Straumnes and 93 nm NNW off Horn. The Greenland Straight had northeasterly wind directions during the whole month /sea-ice/monthly/2011/nr/2376

• 4. arhrifafylki_web

  Impact Matrix of the Icelandic Meteorological Office Minimal or no hazard. No damage likely. Medium or high likelihood of medium impact weather which can have localized affects. This weather could affect travels between different areas of Iceland. The weather is potentially hazardous if precautions are not taken and can cause damages or accidents. Yellow warnings are fairly common /media/frettir/arhrifafylki_web.pdf

• 5. Publications 2020

  assessment of the Vestmannaeyjar Volcanic System: Impacts of lava flow and tephra deposit on Heimaey Melissa Anne Pfeffer, Sara Barsotti, Esther Hlíðar Jensen, Emmanuel Pierre Pagneux, Bogi Brynjar Björnsson, Guðrún Jóhannesdóttir, Ármann Höskuldsson, Laura Sandri, o.fl. 73 16,0 2020-008 Reassessment of precipitation return levels in Iceland Andréa-Giorgio R. Massad, Guðrún Nína /about-imo/publications/2020/

• 6. Volcanic plumes and tephra

  the volcanic plume due to their size and weight fall close to the volcano and constitute the proximal deposit. Smaller particles can reach higher altitudes and persist in the atmosphere for days and weeks and be advected far away by the wind. This fraction of the pyroclastic material can possibly generate a distal deposit very thin and covering wide areas.Term Size Ballistic d > 64 mm Lapilli 2 mm < d /volcanoes/volcanic-hazards/volcanic-emissions/

• 7. Big_landslides_Table_ENG

  Naustavík/Náttfaravíkur by Skjálfandi bay Heavy snowmelt, accumulation of water at the boundary between rock and loose material 1.2 June 1995 Þormóðsstaðir in Sölvadalur in Eyjafjörður Heavy snowmelt, accumulation of water in ancient rockslide deposit 0.6–0.8 March 2007 Morsárjökull Unstable slope by a glacier 4–4.5 April 2007 Stóra-Selfjall in Múladalur/Geithellnadalur in Álftafjörður /media/frettir-myndasafn-2018/Big_landslides_Table_ENG.pdf

• 8. VI_2020_004

  ......................................................................................................................... 41 5.2.1 Input parameters and synthetic scenario .......................................................... 41 5.2.2 Validating model results with real deposit map ............................................... 43 5.2.3 Probabilistic hazard maps /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 9. Forecast for volcanic ashfall 2010

  20.4.2010 On ashfall in Iceland - 23 May 2010 11:00 The eruption activity is minimal and therefore no significant ashfall is expected. The volcano is still being monitored and an ashfall forecast will be issued if neccessary. For ash at high altitudes, possibly affecting flight traffic, we refer to London VAAC /earthquakes-and-volcanism/articles/nr/1885

• 10. Öræfajökull – frequent questions & answers

  to melt. The pyroclastic flows and jökulhlaup caused by the 1362 eruption are thought to have resulted in the death of ~300 individuals. The magnitude of the 1362 jökulhlaup was of order 100,000 m3/s, whereas the 1727 flood was about half that size. In 1362 tephra fallout buried houses and villages with a deposit >40cm thick.The Öræfajökull eruption in 1362 has been one of the largest eruption /volcanoes/about-volcanoes/oraefajokull/q-a/