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• 61. 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

• 62. 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

• 63. 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

• 64. 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

• 65. 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

• 66. 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

• 67. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 68. 2005EO260001

  from 5 years of continuous GPS measurements in Iceland, submitted to Journal of Geophysical VOLUME 86 NUMBER 26 28 JUNE 2005 PAGES 245–252 Eos, Vol. 86, No. 26, 28 June 2005 EOS, TRANSACTIONS, AMERICAN GEOPHYSICAL UNION PAGES 245, 248 Forecasting and Monitoring a Subglacial Eruption in Iceland Fig. 1. (a) Map of Iceland illustrating the location of monitoring networks discussed in the text /media/jar/myndsafn/2005EO260001.pdf

• 69. VI_2014_005

  mode ................................................... 14 5 Errors associated with SURFEX .................................................................... 15 6 Statistical correction of model results .............................................................. 19 7 Original and corrected 2-m air temperature .................................................... 22 8 Original and corrected 10-m /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 70. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  improving management policies and practices by learning from the outcomes of implemented management strategies. Partici- patory integrated assessment is here a form of problem structuring for identification of gaps, ambiguity and multiple frames, confrontation, and integration of the most divergent views with respect to a given problem situation. Additional methods and tools that AM require com /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf