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  • 1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

    During the conference all of you are requested to act as rapporteur in two or three sessions. A preliminary allocation of rapporteur sessions has been made (see below), while accounting for your expertise in certain areas. Participants can suggest changes in the rapporteur session allocation, on the condition a convincing argumentation is provided as well as a confirmed alternative rapporteur /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. Grímsvötn eruptions

    the last 1100 years. Based on tephrochronological studies on average 7 eruptions have taken place each century during the last ~8000 years. Grímsvötn central volcano last erupted for a week in 2011, emitting ~0.8 km3 of tephra deposited over nearby areas causing few days with complete darkness in the middle of the day.Most eruptions on the Grímsvötn volcanic system are explosive, occur /volcanoes/about-volcanoes/grimsvotn/
  • 4. Bárdarbunga

    Bárðarbunga are basaltic explosive eruptions on the edges of the volcano, but large lavaflows are also known, for example the eruption of the Great Thjórsá Lava (Þjórsárhraun) which formed by an eruption within the system about 8000 years ago. Eruptions from the central volcano can cause glacial floods (jökulhlaup) which would be brought down rivers in the west and/or north of Vatnajökull glacier /volcanoes/about-volcanoes/bardarbunga/
  • 5. Eyjafjallajökull

    with phreatic eruption as tephra. These explosive eruptions can cause jökulhlaup and increase of flooding in glacial rivers around the volcano.Explosive eruptions outside the summit crater/caldera, either partially or completely under the glacier, where the magma is most likely basaltic or andesitic. These eruptions have caused jökulhlaup to the north, south and west of the volcano.Effusive eruption /volcanoes/about-volcanoes/eyjafjallajokull/
  • 6. TF-FMS_20141204_skyrsla

    eldgosavöktunar - samantekt ________________________________________________________ Eruption site and lava field: No major changes in the eruptive activity and the advance of the lava field have been observed. For the limited time that the vent was well visible, lava was rather surging out of the vents and only one larger bubble burst was seen. The largest outbreak of lava was seen /media/jar/TF-FMS_20141204_skyrsla.pdf
  • 7. aerodrome_summaries_20140603

    CLIMATOLOGICAL SUMMARY - TABLE A AERODROME: BIAR - AKUREYRI / Akureyri PERIOD OF RECORD: 2001–2010 LATITUDE: 65 39’31"N LONGITUDE: 18 04’20"W ELEVATION ABOVE MSL: 3 M (9FT) FREQUENCIES (PER CENT) OF THEOCCURRENCEOFRUNWAYVISUAL RANGE/VISIBILITY (BOTH IN METERS) OR HEIGHT OF THE BASE OF THE LOWEST CLOUD LAYER (IN FEET), OF BKN OR OVC EXTENT BELOW SPECIFIED VALUES AT SPECIFIED TIME ANNUAL VIS(m)/Hs(ft) TIME /media/vedur/aerodrome_summaries_20140603.pdf
  • 8. Lettenmaier_Dennis_CES_2010pdf

    ) Colorado River basin C) Washington climate change impacts assessment – Yakima River basin 3a) Hydrology and water management implications: Columbia River Basin PCM Business-as-Usual scenarios Columbia River Basin (Basin Averages) control (2000-2048) historical (1950-99) BAU 3-run average PCM Business-As- Usual Mean Monthly Hydrographs Columbia River Basin @ The Dalles, OR 1 month /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf
  • 9. VI_2020_004

    vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Sara Barsotti, Veðurstofa Íslands Sigrún Karlsdóttir, Veðursstofa Íslands Anna María Ágústsdóttir, Landgræðslan Björn Oddsson, Almannavarnadeild Ríkislögreglustjóra Íris Marelsdóttir, Embætti landlæknis Þorvaldur Þórðarson, Jarðvísindastofnun H áskólans Þórólfur Guðnason, Embætti landlæknis Bogi B. Björnsson, Veðurstofa Íslands /media/vedurstofan-utgafa-2020/VI_2020_004.pdf
  • 10. Climate Report

    been observed in the arrival times of some migratory bird species, as an example the Black-tailed godwit, which winters in Europe, now arrives on average about 10 days earlier than it did in 1990. For other species such as the Whimbrel, which winters in Africa, arrival times have not changed as much. Warmer conditions in lakes have negatively impacted Arctic char, but Brown trout has been /climatology/iceland/climate-report

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