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• 31. Bárðarbunga earthquakes - interactive model

  and explored. The list of earthquakes updates every five minutes. Click this link to run the model: An interactive 3D model of the earthquakes in Bárðarbunga – preliminary version However, this is a preliminary version; the model is still being developed. There are some browser issues, e.g. Google Chrome and Firefox run it, IE10 does not; other browsers have yet to be tested. In some instances /earthquakes-and-volcanism/articles/nr/2971/

• 32. ICEWIND

  in the Nordic countries. In Iceland the main focus has been on establishment of atlases for wind and icing as well as integration of wind power with other energy sources. A wind atlas for Iceland created under the project can now be found on IMO's Icelandic web-site (English legend). Ísvindar Alongside the cooperative Nordic project, an ongoing Icelandic project ÍSVINDAR is run, where /about-imo/arctic/icewind/

• 33. The FutureVolc project and the eruption on National Geographic

  map of the earthquakes and a run of continuous GPS measurements in the vicinity of the Bárðarbunga central volcano which shows horizontal displacements. News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 /about-imo/news/nr/3003

• 34. Intense rainfall - possible floods and flows

  ). The most intense rainfall is expected in the south and south-east of the country, especially around Mýrdalsjökull and south of Vatnajökull, as well as nearby mountainous areas. In these regions, the combined effects of rainfall and snow-melt will produce the 24-hour equivalent of over 250 mm of run-off. By Saturday, rising river levels are expected throughout the south of the country. The severity /about-imo/news/nr/3108

• 35. Ice subsidence above eastern Skaftá cauldron

  the subsidence did not disrupt the line-of-sight for the radio link. Ice surface lowering above eastern Skaftá cauldron 2015. This graph was updated every five minutes. These measurements are funded by FutureVolc and the research funds of the National Power Company of Iceland and of the Icelandic Road and Coastal Administration. The project is run by the Icelandic Met Office with support from /hydrology/research/skafta-cauldron/

• 36. The crust has changed

  network used for monitoring crustal movement. The network is run by IMO in co-operation with other institutes, in Iceland and overseas. At Selfoss, lateral displacement was 20 cm to the southeast and at Hveragerði 17 cm to the northwest. Landrise was 5 cm and 3.5 cm, respectively. These tectonic changes are permanent and in concordance with a dextral fault through the mountain Ingólfsfjall /about-imo/news/nr/1326

• 37. Energy System Analysis

  temperatures gives reduced need for electrical heating, and altered wind-speeds may affect wind-power generation. Altered precipitation will however give the largest climate-change impact on the Nord Pool market because of the large share of hydropower. Previous studies have shown that the geographical and seasonal distribution as well as the annual amount of inflow to reservoirs and run-of-river /ces/project/energy/

• 38. norsem_schmidt

  event a simple hazard analysis is performed, classifying the event as unlikely, potential or likely to cause harm to society. The customers of this product are Swedish civil protection and crisis management authorities. The system is run in a highly automated manner with only limited human interaction. Input data to the system are event parameters from our in-house processing /media/norsem/norsem_schmidt.pdf

• 39. VI_2009_006_tt

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 40. VI_2014_001

  calculated on a 1x1 km grid for the period 1961 to 2006, were used in this study to run the hydrological model and for the development of the index flood method (see below). Wind-speed, vapor pressure and incoming short wave radiation were obtained from the MM5 NWP model (Grell et al. 1995) at approximately 8 km resolution and interpolated to the 1x1 km grid. 2.4 GIS data A 1 km digital elevation /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf