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• 1. Forecasts - Laufbali

  GMT -99° E 6 Cloud cover: 100% 06 GMT -99° ESE 7 Cloud cover: 100% 09 GMT -99° ESE 7 Cloud cover: 80% 12 GMT -99° ESE 6 Cloud cover: 100% 15 GMT -99° ESE 7 Cloud cover: 100% 18 GMT -99° ESE 5 Cloud cover: 100% 21 GMT -99° ESE 8 Cloud cover: 100% Fri 5.05 00 GMT -99° ESE 9 Cloud cover: 100% 03 GMT -99° ESE 8 Cloud cover: 100 /m/forecasts/areas

• 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. 2010_003rs

  ................ 91 Figure B.5. Rake distribution for mapped faults/clusters in boxes E and F, Brennisteinsfjöll-Bláfjöll. ................................................................................. 92 Figure B.6. Rake distribution for mapped faults/clusters in box G, Ölfus. ......................... 93 Figure B.7. Rake distribution for mapped faults/clusters in box H, Hengill, active between January /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 4. VI_2009_012

  Mw(v) plotted against log distance. The coefficient of correlation between Mw(v) and log distance is 0.24. High correlation coefficients have been shown to affect parameter estimates in one step regression methods (see Fukushima and Tanaka, 1990). The Ci values were also calculated from the derived PGA values. Instead of constructing another magnitude scale based on acceleration it was decided /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 5. event_numbers_17022015

  Earthquakes since 16. August 2014 00:00 all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 35.000 - - - - - - - checked ~ 20.000 ~ 8.000 ~ 9.000 ~ 200 ~ 300 ~ 1.800 ~ 600 ~ 20 M3.0-3.9 1208 99 1089 6 2 4 7 1 M4.0-4.9 655 7 646 1 1 0 0 0 M>5.0 79 0 79 0 0 0 0 0 HB / HBT Herðubreið and Herðubreiðartögl TFJ Tungnafellsjökull Kverkfj. Kverkfjöll Kistufell cluster north /media/jar/myndasafn/frodleikur/event_numbers_17022015.pdf

• 6. event_numbers_01102014_1500

  Earthquakes between 16. August 2014 00:00 and 01. October 2014 15:00 all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 25.000 - - - - - - - checked ~ 8.500 ~ 5.500 ~ 1.600 ~ 120 ~ 250 ~ 850 ~ 130 ~15 M3.0-3.9 260 99 148 6 2 3 1 1 M4.0-4.9 83 7 74 1 1 0 0 0 M>5.0 39 0 39 0 0 0 0 0 HB / HBT Herðubreið and Herðubreiðartögl TFJ Tungnafellsjökull Kverkfj. Kverkfjöll Kistufell /media/jar/event_numbers_01102014_1500.pdf

• 7. 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

• 8. event_numbers_31102014_1900

  Earthquakes between 16. August 2014 00:00 and 31. October 2014 19:00 all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 28.000 - - - - - - - checked ~ 11.900 ~ 6.500 ~ 3.550 ~ 140 ~ 260 ~ 1.200 ~ 250 ~15 M3.0-3.9 434 99 321 6 2 3 2 1 M4.0-4.9 228 7 219 1 1 0 0 0 M>5.0 61 0 61 0 0 0 0 0 HB / HBT Herðubreið and Herðubreiðartögl TFJ Tungnafellsjökull Kverkfj. Kverkfjöll /media/jar/event_numbers_31102014_1900.pdf

• 9. 2010_012rs

  ) closest stations, respectively. The 40 highest correlating events are then inverted for the best location. For comparison the manual locations, obtained by an analyst are shown in yellow. The final locations of the events are all within an approximately 1 km2 area, even though their original, automatic locations are up to 5 km away. They are also within a few hundred meters from the manual /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 10. CES_D2.4_task2_CMIP3_winds

  in the average wind speed between the baseline (or control) period 1971-2000 and the scenario period 2046-2065. These periods were chosen based on the availability of model output at daily time resolution. We have analyzed the surface geostrophic wind (hereafter Vg) rather than the actual simulated surface winds, because the latter are sensitive to the details of the boundary layer /media/ces/CES_D2.4_task2_CMIP3_winds.pdf