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Results:

• 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. norsem_harris

  to search the 116 years of data at the ISC. There are three main datasets held at the ISC available to search: the ISC Bulletin, the EHB Bulletin and the IASPEI Ground Truth data. In addition there are the ISC Event Bibliography and Station Registry. These all have their own search tools on the ISC website (www.isc.ac.uk) with an FDSN web-service event search for the ISC /media/norsem/norsem_harris.pdf

• 4. Post-conference field trip on 31 October

  Plate. The source fault of one of the earthquakes of 2000 will be visited before we cross the plate boundary back to the North America Plate. The guide will be Professor Páll Einarsson of the University of Iceland. The trip, departing from Reykjavík on Saturday 31 October, will last about nine hours. The estimated cost of the trip is 5000 ISK (30 EUR). This fee covers the hire of a bus /earthquakes-and-volcanism/conferences/jsr-2009/fieldtrip/

• 5. Demers_Claude_CES_2010

  1 9 6 5 1 9 6 7 1 9 6 9 1 9 7 1 1 9 7 3 1 9 7 5 1 9 7 7 1 9 7 9 1 9 8 1 1 9 8 3 1 9 8 5 1 9 8 7 1 9 8 9 1 9 9 1 1 9 9 3 1 9 9 5 1 9 9 7 1 9 9 9 2 0 0 1 2 0 0 3 2 0 0 5 2 0 0 7 2 0 0 9 G W h Écarts énergétiques annuels du parc total hydraulique d'Hydro-Québec + Churchill Falls Années ConclusionAdaptationClimate & HydrologyContext Hydro-Québec and Climate Change The question to be answered • How /media/ces/Demers_Claude_CES_2010.pdf

• 6. Case_B___Road_transport_operation_and_infrastructure_planning

  on the Shifts of climatic zones from cooler or wetter to warmer or drier (a) 1971-2000 (b) 2010-39 A1B observational data set (0.25º grid) from Haylock et al. (2008) (b-d) Based on CMIP3 GCM runs for A1B & the delta-change method (c) 2040-69 A1B (d) 2070-99 A1B Jylhä et al. (2010) Uncertainties in climate change schematically Observed climate Future climate Natural /media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf

• 7. Pollution

  closer to Reykjavík, eight years before that. As elsewhere in Europe sulphur concentration is lower now than when measurements began. Average value of sulphur is about 0.5 mg/l in precipitation, about 0.1 μg/m3 in aerosol and about 0.07 μg/m3 in air. Stórhöfði - a seashore background station Stórhöfði is at the south end of island Heimaey which is the largest of the Westman islands /pollution-and-radiation/pollution/

• 8. Flood in Grímsvötn

  is calculated to be around 5000 m3/s. This size of flood will most likley not affect the infastructure in the area such as roads or bridges. These forecasts are uncertain at this early stage. There are past examples of Grímsvötn eruptions starting following a flood. The loss of the water from Grímsvötn lake reduces the pressure on top of the volcano and this can allow an eruption to begin /about-imo/news/icesheet-in-grimsvotn-subsiding

• 9. Group3-Road-scenarios

  in asphalt, road maintenace Change: 30% more than BAU Socio-economic scenario Climate scenario Worst case (4.4 C increase; 17 % increase in prec) Best case (1.5 C increase; 2% increase in prec) BAU A B Change +30 % C D Spatial analogues: - regions which today have a similar climate to the expected future one the study region (IPCC TAR, 2001) - limited by possible lack /media/loftslag/Group3-Road-scenarios.pdf

• 10. 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