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• 11. VI_2020_004

  of an eruption like 1918 at Katla. ................ 69 Figure 42 Impact map for airports in case of an eruption like 1918 at Katla. ......................... 70 Figure 43 Impact map for power line in case of an eruption like 1918 at Katla. .................... 71 Figure 44 Reconstructed Total Grain Size Distribution for the Öræfajökull scenario ............. 73 Figure 45 Model results over /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 12. 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/

• 13. VI_2015_009

  by rescaling a dimensionless regional flood frequency distribution or growth curve, qR(D;T ), com- mon to all sites of the homogeneous region, with the so-called index flood, µi(D), of the target site: bQi(D;T ) = µi(D)qR(D;T ); (1) where bQi(D;T ) is the estimated flood quantile, i.e. the T -year flood peak discharge averaged over duration D, at site i. The regional growth curve, qR(D;T /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 14. 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

• 15. 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

• 16. 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

• 17. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 18. vanRoosmalen_etal-2009-WRR_2007WR006760

  with 20% and 2% for the HIRHAM experiments using HadAM3H and with 30% and 7% for the ECHAM- driven experiments for Middle Europe and Scandinavia, respectively. [18] RCM output is not available for the entire period 1961–2100 because transient RCM simulations are com- putationally very demanding. Instead two 30-year time slices are available; one representative for the climate in the period 1961–1990 /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 19. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf

• 20. VI_2020_005

  and historical data is available to the public on the Norwegian Mapping Authorities website1 (Norwegian Ministry of Climate and Environment, 2018). In Stockholm, manual measurements of sea levels started in 1774. In the mid 1880s, the Swedish king Oskar II decided that mareographs should be installed along the Swedish coast line. One of them was installed in Stockholm in 1889 and at the same site /media/vedurstofan-utgafa-2020/VI_2020_005.pdf