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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. CES_D2.4_solar_CMIP3

  -2049. Projections are based on simulations performed with 18 global climate models under the SRES A1B, A2 and B1 greenhouse gas scenar- ios. To facilitate reading the report, only the most essential diagrams and maps are included in the main text, additional material being positioned in the appendix. 1 MODELLED SOLAR RADIATION DATA The quantity examined is incident solar radiation (also termed /media/ces/CES_D2.4_solar_CMIP3.pdf

• 4. Supercomputer in Iceland

  that: DMI operates the supercomputer from remote IMO operates the site infrastructure IMO acts as „remote hands and eyes“ on behalf of DMI DMI deliveres forecast data to IMO The partnership is a stepping stone towards a potential joint Nordic meteorological supercomputer The supercomputer Super computer installed in two phases: ultimo 2015 and ultimo 2017 Each phase consisting of two /about-imo/news/nr/3309

• 5. VI_2009_013

  ...................................... 18  Figure 7. Temporal/spatial evolution of seismicity between 1996 and 2007. .................. 19  Figure 8. Temporal/spatial evolution during the latter intrusion swarm and until 2006. . 19  Figure 9. Mechanisms in selected depth intervals for the three main swarms. ................ 21  Figure 10. Distribution of P- and T-axis for events /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 6. The weather in Iceland 2014

  146 128 22.5 228 133 Miðfjarðarnes 765.0 120 36.4 233 130 Skjaldþingsstaðir 1980.1 179 115.6 237 162 Dalatangi 2069.6 147 132 72.6 275 189 Höfn í Hornafirði 2060.9 162 57.4 253 189 Vatnsskarðshólar 1851.9 119 111 58.9 270 213 Eyrarbakki 1486.1 108 87 50.0 234 200 Hjarðarland 1203.8 89 35.7 198 158 Keflavíkurflugvöllur /about-imo/news/nr/3082

• 7. ved-eng-2014

  130 Skjaldþingsstaðir 1980.1 179 115.6 237 162 Dalatangi 2069.6 147 132 72.6 275 189 Höfn í Hornafirði 2060.9 162 57.4 253 189 Vatnsskarðshólar 1851.9 119 111 58.9 270 213 Eyrarbakki 1486.1 108 87 50.0 234 200 Hjarðarland 1203.8 89 35.7 198 158 Keflavíkurflugvöllur 1130.6 105 105 43.6 249 172 Precipitation equal to or exceeding 1.0 mm was measured on 160 days in Reykjavik, 12 more /media/vedurstofan/utgafa/skylduskil/ved-eng-2014.pdf

• 8. VI_2020_004

  ....................................................................................................................................... 9 Ágrip ......................................................................................................................................... 11 1 General introduction ........................................................................................................... 13 1.1 Main aim of the project /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

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

  the topo- graphic ice divide is assumed (consistent with the SIA for- mulation of the ice flow model) and fixed boundaries of the main ice flow basins may be assumed to be reasonable since the location of the ice divide is to a large degree controlled by the basal topography. However, the assumption of fixed ice divides may be expected to become increasingly inaccu- rate when simulated changes /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 10. VI_2009_006_tt

  -called Skaftá cauldrons in west- ern Vatnajökull have been well known since 1955 (Zóphóníasson and Pálsson, 1996). These jökulhlaups emerge in the river Skaftá and are characterized by a rapid increase in discharge, rising to maximum discharge in one to two days. Jökulhlaups in Skaftá are therefore classified as “fast-rising jökulhlaups” based on a classification of jökul- hlaups into two main /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf