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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. New article on glacier changes in

    to approx. 1890 and create a time series of the volume and mass changes of the glaciers that spans about 130 years.The results clearly show that the average mass loss of the Icelandic glaciers per unit area is among the highest of the main glacierized areas of the world, outside of Antarctica and Greenland. Such glaciers are now rapidly losing mass all over the Earth, causing rising sea level /about-imo/news/new-article-on-glacier-changes-in-iceland-over-the-past-130-years
  • 4. Wind, temperature and precipitation forecasts

    = Reykjavík area 1 = Faxaflói 2 = Breiðafjörður 3 = West fjords 1301 = West fjords - Djúpið 4 = North West 5 = North East 6 = Eastern coastal areas 7 = East fjords 8 = South East 9 = South 10 = Central highlands The width of the frame is 600 pixels; the hight of the frame is different for each area. On the Modernus web measure A web-page containing an IMO frame must NOT be registered for Coordinated /about-imo/the-web/iframes/wind-temp-precip/
  • 5. Station forecasts, text forecasts or observations

    . The area codes are as follows: 101 = whole country 111 = Reykjavík area 1 = Faxaflói 2 = Breiðafjörður 3 = West fjords 1301 = West fjords - Djúpið 4 = North West 5 = North East 6 = Eastern coastal areas 7 = East fjords 8 = South East 9 = South 10 = Central highlands Depending on whether text forecasts or observations should appear each time the page is opened, rather than station forecast /about-imo/the-web/iframes/wst-txt-obs/
  • 6. event_numbers_07102014_1800

    Earthquakes between 16. August 2014 00:00 and 07. October 2014 18:00 all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 26.000 - - - - - - - checked ~ 8.900 ~ 5.600 ~ 1.800 ~ 120 ~ 250 ~ 950 ~ 135 ~15 M3.0-3.9 307 99 195 6 2 3 1 1 M4.0-4.9 117 7 108 1 1 0 0 0 M>5.0 45 0 45 0 0 0 0 0 HB / HBT Herðubreið and Herðubreiðartögl TFJ Tungnafellsjökull Kverkfj. Kverkfjöll Kistufell /media/jar/event_numbers_07102014_1800.pdf
  • 7. Spatial_perception_of_flood_hazard_in_the_urban_area_of_Selfoss,_Iceland

    A survey on flood risk perception was conducted in the town of Selfoss from May to August 2009 among the residents aged above 18. The respondents were proposed to draw the boundaries of areas flooded from the beginning of the 20th century on an orthophotograph of Selfoss at scale 1:10.000. The spatial representations of the flood area were processed with a regulated grid of 10 x 10 metres /media/loftslag/Spatial_perception_of_flood_hazard_in_the_urban_area_of_Selfoss,_Iceland.pdf
  • 8. 47th Nordic Seismology Seminar

    on the respective day. Poster presentations (during all three coffee breaks) Tuesday 11 October Arrival and check-in. Most flights will arrive in the afternoon, so you should be at your hotel around 17:00/18:00.19:00 Kickoff party at IMO (Bústaðavegur 7, 108 Reykjavík). We will meet you at 18:30 outside Grand Hotel and walk together to IMO. Should anybody prefer to get a lift by car, please /norsem/norsem2016/program/
  • 9. Glacier change sessions at this year's Arctic Circle

    from other parts of the archipelago. (Photo; Fr. Marek Michalski). A new accurate high-resolution digital elevation model of Iceland A special workshop on the use of the above-mentioned ArcticDEM and upcoming new data to monitor glacier changes was organized by IMO during the Arctic Circle Assembly, with participation from universities and surveying institutes in Austria, Canada, Denmark /about-imo/news/glacier-change-sessions-at-this-year-s-arctic-circle-assembly
  • 10. Cradden_Lucy_CES_2010

    superimpose both heating and cooling effects, i.e., – wind = cooling – temperature, solar radiation = heating June 2010 5 • Limit to how much heat the wire can be exposed to • Amount of allowable current based on ambient conditions is known as ‘rating’ Network capacity (ampacity) Too much heat causes ‘sag’ where minimum ground clearance is not achieved June 2010 6 How are ratings determined /media/ces/Cradden_Lucy_CES_2010.pdf

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