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• 31. norsem_korja

  reactivation type (reverse, normal or strike slip) based solely on their azimuth. The earthquakes in the seismically most active area, close to Skellefteå, Sweden along the western coast of the Gulf of Bothnia and its north-easterly continuation, appear to cluster around the shoreline and along post-glacial faults, which are mostly oriented optimally for reverse or strike slip faulting /media/norsem/norsem_korja.pdf

• 32. Aurora forecast for Iceland

  or click directly on a day or time. The forecast of auroral activity at midnight, scale 0 to 9, is shown in the upper-right box. The scale changes in accordance with the date selected under the cloud cover map. The timing of sunset, darkness, sunrise and moonrise are valid for Reykjavík. Aurora activity, sun and moon - Aurora forecast /weather/forecasts/aurora/

• 33. First Annual Meeting of FUTUREVOLC

  First Annual Meeting of FUTUREVOLC The first annual meeting of FUTUREVOLC is held in Iceland 24.9.2013 The first Annual Meeting of FUTUREVOLC is held 23-25 September 2013 in Iceland with around 80 participants from 12 countries. After two days of lectures /about-imo/news/nr/2751

• 34. Measuring glaciers

  released, e.g. by World Glacier Monitoring Service in Zürich and Global Land Ice Measurements from Space (GLIMS) in Flagstaff, Arizona. Bird's eye view Snæfellsjökull, western Iceland, 18 October 2001. At that time, the ice-cap had already been observed to retreat and thin in the preceding years and decades, as confirmed by annual measurements in a single location since 1931. This was further /hydrology/glaciers/

• 35. VI_2016_006_rs

  of 100–140 m a.s.l. Several debris flows are recorded in Búðará since the beginning of the 20th century. It is not clear whether the upper or lower area is the main source for these debris flows. The return time for sizeable debris flows in Búðará is around 20 years. It appears that the land- slide activity has been more frequent in the last 30 years than earlier in the 20th century. 4.5 Areas 7 /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 36. The segmented dyke intrusion explained

  to time of occurrence and the colour code is shown at the top of the map. The earthquake locations delineate the track of the dyke intrusion from Bárðarbunga volcano to the eruption site at Holuhraun. Vertical cross sections through the crust are also shown; looking from the south (below) and east (to the right). Triangles mark the locations of seismic stations in and around the glacier. Data /about-imo/news/nr/3038

• 37. Program

  to investigate glacier geomorphic processes Rudolf Sailer, Erik Bollmann, Veronika Ebe, Anna Girstmair, Christoph Klug, Lorenzo Rieg, Maximilian Spross and Johann Stötter, Institute of Geography, University of Innsbruck, Austria. Potentials of ALS in the analysis of geomorphodynamic processes in high alpine regions Coffey 15:00–15:30 Thursday 15:30–17:30 ‒ Lidar measurements from space Beata Csatho /lidar/lidar-2013/program/

• 38. Statistical Analysis

  and Chemistry of the Earth, Special Issue: COST Action (Accepted for publication). Jónsdóttir, J. F., Uvo, C. B. & Clarke, R. T. (2008). Filling gaps in measured discharge series with model-generated series. Technical Notes. Journal of Hydrological Engineering, 13, 9, 905-909. Jónsdóttir, J. F., Uvo, C. B. & Clarke, R. T. (2008). Trend analysis in Icelandic discharge, temperature and precipitation series /ces/publications/nr/1943

• 39. Aurora and the Earth's magnetic field

  currents in its outer core. At the surface, about 90% of the field can be described by a simple dipole field tilting about 10° from the rotation axis. The currents in the Earth's core are slowly varying causing slow changes of the magnetic field, typically on timescales of years and ages. A flow of charged particles from the sun, called the solar wind, hits steadily the magnetic field and bends /weather/articles/nr/2549

• 40. The weather in Iceland in 2050

  stocks. The acidification of the ocean may also adversely impact ocean food webs, with possible consequences on fisheries. Iceland's ice caps have been melting and will continue to do so. According to scientific estimate, they will almost disappear in the next 200 years. Many of these changes can already be seen, for instance: The tiny ice cap Ok, west of Langjökull, has changed beyond /about-imo/news/nr/2989