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• 61. Bárðarbunga 2014 - December events

  Friday last week (M5.1 on 5 Dec. at 21:04 in the southeastern rim). This marks one of the longest periods without a magnitude 5 events and is in good agreement with the general slight decrease of activity that has been observed over the last months. However, on an absolute scale, earthquake rates and energy release remain at comparably high levels. About 20 earthquakes were detected in the dyke /earthquakes-and-volcanism/articles/nr/3055/

• 62. Bardarbunga-2014_December-events

  magnitude 3 and 4. A total of about 60 earthquakes have been detected around the caldera. No earthquake has exceeded magnitude 5 since Friday last week (M5.1 on 5 Dec. at 21:04 in the southeastern rim). This marks one of the longest periods without a magnitude 5 events and is in good agreement with the general slight decrease of activity that has been observed over the last months. However /media/jar/Bardarbunga-2014_December-events.pdf

• 63. VI_2020_008

  endurkomutíma úrkomu og að endurgera 1M5 kort sem sýnir 24 stunda úrkomu fyrir atburð með 5 ára endurkomutíma. Úrkomumælingar frá 43 veðurstöðvum eru notaðar sem og útreiknuð úrkoma í þéttriðnu neti yfir landinu, byggð á gögnum úr íslensku endurgreiningunni (ICRA). Val á aftakagreiningu er skoðað vandlega og niðurstaðan að nýta þröskuldsaðferðina (e. Peak-over-threshold) þar sem gagnamengin tvö /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 64. Hare-2011-ParticipatoryModelling

  Dispatch: 02.08.11 CE: E E T 5 9 0 No. of Pages: 19 ME: 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Another possible driving force behind its popularity is changing legislation requiring environmental managers and policy-makers to increase stakeholder participation in their work [e.g /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 65. Horsens_case

  level coursed by tides is small with a range of less than 0.5 m. Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2 NONAM Summerschool Copenhagen 22-26 August 2011 2 Physical features and ecosystem The fjord landscape is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations /media/loftslag/Horsens_case.pdf

• 66. Continued inflation around Mt. Þorbjörn

  RVIT and SYRF. Magma can accumulate for longer periods of time without an eruptionAs was already stated by the Civil Protection Scientific Advisory Board, the most likely explanation for this deformation is magma accumulation at depth. “Although we see the signs that uplift has started again, it does not mean that the events at Þorbjörn are accelerating, nor that an eruption will begin any /about-imo/news/continued-inflation-around-mt-thorbjorn

• 67. Possible

  scenarios are considered possible, without stating which is most likely or within what timeframe.1. If the inflation is due to magma accumulation:• Magma accumulation will cease soon without further activity.• Magma accumulation continues for some time without further activity.• Magma accumulation will lead to a magma intrusion.• Magma accumulation will lead to magma intrusion /about-imo/news/possible-magma-accumulation-beneath-mt-thorbjorn-on-reykjanes-peninsula

• 68. Adalgeirsdottir-etal-tc-5-961-2011

  The Cryosphere, 5, 961–975, 2011 www.the-cryosphere.net/5/961/2011/ doi:10.5194/tc-5-961-2011 © Author(s) 2011. CC Attribution 3.0 License. The Cryosphere Modelling the 20th and 21st century evolution of Hoffellsjökull glacier, SE-Vatnajökull, Iceland G. Aðalgeirsdóttir1,2, S. Guðmundsson1, H. Björnsson1, F. Pálsson1, T. Jóhannesson3, H. Hannesdóttir1, S. Þ. Sigurðsson4, and E. Berthier5 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 69. Kok_2-scenarios-lecture-2

  ) Establish scenario team and scenario panel (2) Team proposes goals and outline (3) Panel drafts narrative storylines (6) Panel revises storylines (5) Modelling groups quantify scenarios (4) Team quantifies driving forces (8) General review of scenarios (9) Team & Panel make final revision of scenarios (10) Publication and distribution (7) Repeat step 4-6 Story-And-Simulation approach /media/loftslag/Kok_2-scenarios-lecture-2.pdf

• 70. Perrels-CBA

  / design, availability, materials, ICT, modal split) 26.8.2011Adriaan Perrels/IL 5 Categorising stages of adaptation Passive Adaptation - automatic in nature and economy - only ex post measures (no anticipation) Active Adaptation - automatic in nature and economy - ex ante and ex post policies Emission scenario dependent baseline (A1-T, B1, A2, etc.) Reference costs and benefits /media/loftslag/Perrels-CBA.pdf