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

  During the conference all of you are requested to act as rapporteur in two or three sessions. A preliminary allocation of rapporteur sessions has been made (see below), while accounting for your expertise in certain areas. Participants can suggest changes in the rapporteur session allocation, on the condition a convincing argumentation is provided as well as a confirmed alternative rapporteur /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 2. Refsgaard_1-Welcome

  – Print yourselves • Case descriptions and tasks/questions • Lecturers’ presentations – Handouts during the week – Pdfs will be uploaded at website afterwards Practicalities • PC login – Internet access • Printing • Lunch • Coffee – tea • Posters Monday afternoon + refreshments • Dinner Tuesday at 19:00 Students • Brief presentation round – now • 2-minutes presentation of research topics /media/loftslag/Refsgaard_1-Welcome.pdf

• 3. Avalanche dams

  ofan byggðarinnar. (Náttúrufræðingurinn, 69, 1, 3−10, 1999, authors T. Jóhannesson, O. Pétursson, J. G. Egilsson and G. G. Tómassson) [abstract] (html) A map on a selected front page shows recent observations of avalanches. For user access to avalanche and landslide data, an avalanche map viewer is available /avalanches/imo/dams/

• 4. hafisskyrsla_11052011

  Hafísskýrsla TF-SIF 11. maí 2011 Flug nr. 03511.025 Ískönnunarflug 11. maí 2011 Í dag var farið í ískönnunarflug um vesturmið. Enginn hafís var sjáanlegur í íslenskri lögsögu, en þéttur hafís rétt inn þeirrar grænlensku. Gerðum hafískönnun með SLAR ratsjá og ELTA eftirlitsratsjá. Skyggni á svæðinu leifði ekki athugun með berum augum. Hér að neðan fylgir punktalisti yfir legu /media/hafis/skyrslur_lhg/hafisskyrsla_11052011.pdf

• 5. 2013_001_Nawri_et_al

  and a pressure of 1013.25 hPa. In the case of Iceland, the climate deviates significantly from these standard atmospheric conditions. Additionally, terrain elevation varies considerably across the island. Therefore, seasonal and annual differences in air density from the standard value, as well as spatial variability, need to be taken into account. Approximate air density can be calculated by assuming /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 6. Hare_1_PartINONAM

  Participatory methods and processes for adaptive management Dr Matt Hare Independent Consultant, Mexico City Adaptive and participatory water management Matt Hare, hare@gmx.de 2011 – Summer School About myself ... • Bachelor in artificial intelligence (88-92) • PhD environmental modelling in knowledge and data-poor domains (95-99) • Co-founder of Seeconsult GmbH (03-onwards /media/loftslag/Hare_1_PartINONAM.pdf

• 7. Avalanches in Iceland

  and landslides have caused both death and injury and done great damage to infrastructure and property in Iceland. In the twentieth century, 193 persons died, thereof 69 persons after 1974. Financial cost between 1974 and 2000 amounts to 3.3 billion IKR. Catastrophic avalanches in the villages Súðavík (January) and Flateyri (October) 1995, which killed 34 people and caused extensive economic damage /avalanches/avalanches

• 8. Avalanches in Iceland

  and landslides have caused both death and injury and done great damage to infrastructure and property in Iceland. In the twentieth century, 193 persons died, thereof 69 persons after 1974. Financial cost between 1974 and 2000 amounts to 3.3 billion IKR. Catastrophic avalanches in the villages Súðavík (January) and Flateyri (October) 1995, which killed 34 people and caused extensive economic damage /avalanches/avalanches/

• 9. aerodrome_summaries_20140603

  CLIMATOLOGICAL SUMMARY - TABLE A AERODROME: BIAR - AKUREYRI / Akureyri PERIOD OF RECORD: 2001–2010 LATITUDE: 65 39’31"N LONGITUDE: 18 04’20"W ELEVATION ABOVE MSL: 3 M (9FT) FREQUENCIES (PER CENT) OF THEOCCURRENCEOFRUNWAYVISUAL RANGE/VISIBILITY (BOTH IN METERS) OR HEIGHT OF THE BASE OF THE LOWEST CLOUD LAYER (IN FEET), OF BKN OR OVC EXTENT BELOW SPECIFIED VALUES AT SPECIFIED TIME ANNUAL VIS(m)/Hs(ft) TIME /media/vedur/aerodrome_summaries_20140603.pdf

• 10. Flood from Skaftá

  eastern and western, are located in the western part of Vatnajökull Ice-cap. They form because of geothermal activity that melts the glacier from below and water accumulates beneath them. When the hydro static pressure is high enough for the water to lift the ice above and flow from below the cauldrons it causes a flood. Floods from the eastern-cauldron are usually larger than the floods /about-imo/news/flood-in-estern-skafta