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Results:

• 51. VI_2015_009

  Figure 5. AMF frequency distributions (Q(D;T ) vs. T ) at target sites treated as ungauged, using best overall index flood model (bµ(D) = q0(AP)q1): vhm59 (top-left), vhm64 (top- right), vhm66 (bottom-left), vhm102 (bottom-right). Solid black line corresponds to the reference GEV distribution fitted to the observed AMF sample. Grey shaded region corre- sponds to the reference 95% CI. Red solid line /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 52. Doctoral Student Position

  a CV by e-mail, while using the e-mail heading: PHD-FMI-HENVI, to kirjaamo@fmi.fi, and c.c. to adriaan.perrels@fmi.fi and kaisa.korhonen@helsinki.fi. The deadline for applications is 23-5-2011 at 15:45 UTC. Further inquiries: HENVI: Dr. Kaisa Korhonen, research co-ordinator, kaisa.korhonen@helsinki.fi + 358 400 624 289 FMI: Dr. Adriaan Perrels, research professor, adriaan.perrels@fmi.fi, +358 50 /nonam/news/nr/2171

• 53. Ice subsidence above eastern Skaftá cauldron

  shows the current position of the station (m a.s.l.). The graph (enlarge) was published 26 Sept. Now it shows the subsidence from 28 Sept until 4 Oct 2015. The total lowering of the ice-surface is shown by the value above the photograph (Heildarsig). The red line shows the median value of relative displacement for every 30 minutes. This presentation was possible throughout the event because /hydrology/research/skafta-cauldron/

• 54. VI_2009_013

  relocated events (thin black line) and selected events with low relative error, within 100 m in latitude and longitude and 300 m in depth (thick line). Stress drop with respect to depth is shown as grey crosses and average stress drop for 1 km intervals is shown as red triangles. 5 Discussion After relocating the earthquakes, many of them form separate clusters, but the overall pattern forms /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 55. VI_2013_006

  Office Guðrún Nína Petersen, Icelandic Met Office Halldór Björnsson, Icelandic Met Office   4 5 Table of contents Introduction ............................................................................................................................ 6 Lightning location data /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf

• 56. Rockslide in Askja, July 21 2014 - Preliminary results of observations

  out, adding to the results and making them more precise. Below are photographs, maps and graphs that show the main results of measurements and analyses that are available, now two weeks after the event. Width of fracture line: 800 m Vertical drop: 350 m Runout length beyond the lake shore: ~1000 m Volume: ~30–50 million m³ Estimated duration of the slide: 20 seconds according to seismographs /avalanches/articles/nr/2929

• 57. VI_2009_012

  Fjölbrautaskólanum við Ármúla Kristín S. Vogfjörð, Veðurstofu Íslands VÍ 2009-012 ISSN 1670-8261 Skýrsla +354 522 60 00 +354 522 60 06 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 9 150 Reykjavík   5 Project no. 036935 Project acronym: SAFER Project title: Seismic eArly warning For EuRope Instrument : Specific Targeted Research Project Thematic Priority: Sustainable development /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 58. On the Bárðarbunga earthquakes

  line shows the seismic moment released in the dyke intrusion south of the Holuhraun eruption site, the blue line represents the moment released in or around the caldera. The lower plot shows the magnitudes of the earthquakes as a function of time, blue for the caldera and orange for the dyke /about-imo/news/on-the-bardarbunga-earthquakes

• 59. The low frequency tremor 23rd August 2014

  is shown in three frequency bands (0,5-1 Hz; 1-2 Hz; 2-4 Hz). A low frequency tremor pulse is clearly seen just before noon 23rd August. This tremor (red line) was interpreted as signs of magma having arrived at the surface under the glacier and prompted IMO to raise the aviation colour code from orange to red. The tremor lasted a few hours and then gradually decreased during the afternoon /earthquakes-and-volcanism/articles/nr/2970

• 60. norsem_atakan_norway

  -resources. The mission of EPOS-Norway is therefore in line with the European vision of EPOS. EPOS-Norway project has started in January 2016 and will during the next five years focus on the implementation of the three main components. These are: (i) Developing a Norwegian e-Infrastructure to integrate the Norwegian Solid Earth data from the seismological and geodetic networks, as well as the data /media/norsem/norsem_atakan_norway.pdf