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• 1. 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

• 2. 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

• 3. Sea ice photos

  Photo: Jón Guðjónsson Photo: Jón Guðjónsson Photo: Jón Guðjónsson Iceberg Iceberg Iceberg Iceberg Iceberg Iceberg Iceberg Bergy bit Bergy bit An Iceborg offshore Húnaflói in September 1983 Photo: Rafn Ólafsson Iceberg Photo: Þór Jakobsson Bergy bits Photo: Jón Guðjónsson /sea-ice/sea/gallery/older/

• 4. Sitemap

  Sitemap | Observations | Icelandic Meteorological office Invalid parameter 'g'. Its value is: 77/ but should be an integer. Sitemap Front page Text forecasts | Station forecasts | El. forecasts | Observations Large quakes | Latest quakes | © IMO - Bústaðavegur 9 | 150 Reykjavík | Tel: 522 6000 /m/observations/areas

• 5. norsem_sahar

  effects as well as quantifying the uncertainties over multiple hierarchy levels. The main goal of the proposed BHM lies in combining different main factors which directly influence the ground-motion intensities. We find that the total uncertainty is a bit larger in comparison with the calibrated local ground motion prediction equations’ standard deviation obtained for south Iceland /media/norsem/norsem_sahar.pdf

• 6. The weather in Iceland in 2016

  especially on the 12th to 15th. There was some wind related damages, especially in the Northwest. AprilThe weather was favourable, and the temperature well above the 1961 to 1990 mean. It was very wet in the East, but dry and sunny in the West. MayA favourable month, but a bit on the dry side for the spring vegetation. The temperature was above the average. In spite of the dry weather cloud /about-imo/news/the-weather-in-iceland-in-2016

• 7. Sea ice in October 2009

  was observed close to the mouth of Önundarfjörður. The Cost Guard went on ice-survey the 6th of October. They observed 14 icebergs west and northwest of Westfjords, and most of them were approximately 200 nm from the cost. The iceberg closest to shore was located 77 nm westnorthwest of Bjarg. In addition to a detailed map of the icebergs location, the Cost Guard issued as well infrared (IR) images /sea-ice/monthly/2009/nr/2332

• 8. Gradual fading of seismic activity at Bárðarbunga and the dyke intrusion

  larger than M2 occurred around the end of October. The caldera For the caldera, things are a bit more complicated, although a clear trend of decreasing activity is found here as well. Most moment is released during the week prior to the eruption, but in contrast to the dyke, activity remains high for several weeks and has been slowly fading since. The moment release around the caldera has only /earthquakes-and-volcanism/articles/nr/3039

• 9. Wind turbines

  and each spade measures 22 metres in length. When the spades are at their highest position each unit will achieve a height of 77 metres. Like all large structures, wind turbines have an inevitable visual impact. However, a permanent impact on the overall appearance of the environment is not considered high in comparison to other types of power plants. Wind turbines can be easily dismantled, leaving /about-imo/news/nr/2642

• 10. VI_2020_004

  -laid with the deposit isopach for the 1362 eruption. ................ 74 Figure 46 Vertical velocity profile for the eruptive mixture (Öræfajökull) ............................. 75 Figure 47 Probabilistic hazard map for a load ≥1.0 kg/m2 (Öræfajökull) ............................... 76 Figure 48 Probabilistic hazard map for a load ≥100 kg/m2 (Öræfajökull) ............................. 77 Figure /media/vedurstofan-utgafa-2020/VI_2020_004.pdf