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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. 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. „We need to control our footprint on mother Earth“

  and the systems upon which they rely on, such that they cover all climate related hazards, and this needs to be done globally.”Leading scientists among the speakersDuring the first day, leading scientists presented overviews on the big ice sheets of Greenland and Antarctica, our warming climate and history of climate change. The influence of warming on hydrology in the Arctic, distribution of sea /about-imo/news/we-need-to-control-our-footprint-on-mother-earth

• 4. Flyer_HH_2009_nyr

  of the Hydropower-Hydrology group of CES is carried out by a network of scientists mainly from the national institutes. Thus a wide range of aspects of hydropower and natural conditions are covered, from the glaciated basins in Iceland and Norway, through the big Finnish and Swedish lakes, to the big rivers in Latvia and Lithuania. The following institutes participate in the Hydropower- Hydrology /media/ces/Flyer_HH_2009_nyr.pdf

• 5. Ash plume and lightnings

  active volcano. It last erupted in 2004 and the current eruption is in a similar location. Flash floods south of the volcano often occur associated with eruptions, but can also happen in between eruptions. The latest such flood occurred in October 2010, so a big flood currently appears unlikely. The MODIS satellite picture taken around 5 o'clock this morning shows the plume; at sunrise the plume /about-imo/news/nr/2177

• 6. Focus of the Hydropower-Hydrology group of CES

  in Iceland and Norway, through the big Finnish and Swedish lakes, to the big rivers in Latvia and Lithuania. The following institutes participate in the Hydropower-Hydrology group of CES: The Finnish Environment Institute The Icelandic Meteorological Office The Icelandic National Energy Authority The Latvian Environment, Geology and Meteorology Agency The Lithuanian Energy Institute /ces/project/hydropower/

• 7. On the Askja rockslide

  minutes to travel across the lake and sound takes about 10 sec to cover that distance. Thus, people have a very short time to escape if a big rockslide is released from the other side of the lake. The Icelandic Meteorological Office and the University of Iceland have compiled a collective memo with the preliminary results of observations of this largest rockslide since the settlement of Iceland /about-imo/news/nr/2930

• 8. Severe weather tomorrow

  can increase quickly with increasing winds and blowing snow. The Met. Office recommends that skiers, snowmobiles and others traveling in the mountains avoid known avalanche slopes and do not travel where avalanches can fall. Also, avoid stopping vehicles on parts of the roads where there is a risk of avalanches. Coastal warning: Combination of high tide, low pressure, big waves and storm surge can /about-imo/news/nr/2609

• 9. Eyjafjallajokull_status_2010-06-11_IES_IMO

  water to flow up onto a road west of a bridge, as there it now not much difference between the height of the bridge and the river channel. Conditions at eruption site: A lake, about 300 m in diamenter, has formed at the bottom of the big crater. Steam is rising from the rims, especially from the north side. In the morning the steam cloud only rose about 100 m over the crater /media/jar/Eyjafjallajokull_status_2010-06-11_IES_IMO.pdf

• 10. norsem_ragnar

  at depth, until after the big earthquake. So the result was many “hindsight predictions” and very few successful “pre-earthquake predictions”. These mistakes are gradually convincing more and more scientists that we cannot assume that pre-earthquake activity is the same before any two earthquakes, so statistics does not work at this level. But these early precursor studies had the very /media/norsem/norsem_ragnar.pdf