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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. The FutureVolc project and the eruption on National Geographic

  Amounts of Lava, With No Signs of Slowing „A tremendous gush of lava in Iceland that began six weeks ago shows no signs of slowing. The eruption, on a plain of old lava called Holuhraun in the Bárðarbunga volcanic system, has spewed out enough molten rock so far to fill 740 Empire State buildings and has buried, on average, an area the size of an NFL football field every 5.5 minutes /about-imo/news/nr/3003

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

  (green line). Figure 10c shows the sensitivity of the steady state ice vol- ume to the adopted values of the degree-day coefficients for The Cryosphere, 5, 961–975, 2011 www.the-cryosphere.net/5/961/2011/ G. Aðalgeirsdóttir et al.: 20th and 21st century evolution of Hoffellsjökull glacier 971 snow and ice, ddfs and ddfi. The figure shows that a change in ddfs has a greater effect than a change /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 5. VI_2021_008

  amplitude plots for three of the most recent Grímsvötn eruptions, which occurred on December 18, 1998 (Figure 10a), November 1, 2004 (Figure 10b), and May 21, 2011 (Figure 10c). The station skr is plotted and can thus be compared for all three eruptions, exhibiting differing types of pre-eruptive tremor signal for each year. The warning times provided by Tremv-ALERT range between 25 minutes /media/vedurstofan-utgafa-2021/VI_2021_008.pdf