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Results:

• 31. Ash plume and lightnings

  active volcano. It last erupted in 2004 and the current eruption is in a similar location. Flash floods south of the volcano often occur associated with eruptions, but can also happen in between eruptions. The latest such flood occurred in October 2010, so a big flood currently appears unlikely. The MODIS satellite picture taken around 5 o'clock this morning shows the plume; at sunrise the plume /about-imo/news/nr/2177

• 32. norsem_bryndis

  Crustal accretion along the divergent plate boundary in Iceland is governed by rifting episodes and dyking. Over a period of two weeks in August-September 2014, magma propagated laterally from the subglacial Bárðarbunga central volcano, Iceland, about 50 km along the divergent plate boundary to the NNE where it erupted continuously for six months. The dyke propagation was associated with more /media/norsem/norsem_bryndis.pdf

• 33. Kok_2-scenarios-lecture-2

  extreem events C6; qual nat. systems C7; policies C8; price of resources C9; other sectors C10; industry C11; inrastructure Crimea - Ukraine Manaus - Brazil From FCM to model input FCM – strong points • Easy to develop and apply. The approach is highly intuitive, it can quickly be explained and applied to any new situation. • High level of integration. A FCM can contain any type of information /media/loftslag/Kok_2-scenarios-lecture-2.pdf

• 34. Kok_JGEC658_2009

  and that paving major roads will lead to deforestation. C3: Conservation units. A large percentage of the Amazon (close to 33%) is classified as some kind of protected area. This includes indigenous reserves, federal parks and national parks. Only about 5% is strictly protected, although it is argued that ‘paper parks’ can also be effective. C4: Forest accessibility. The amount of forest /media/loftslag/Kok_JGEC658_2009.pdf

• 35. Kok_et_al._TFSC_published_2011

  ]. There is ample experience with backcasting, and consequently much has been said about the underlying principles (e.g. [20]), the methodological 838 K. Kok et al. / Technological Forecasting & Social Change 78 (2011) 835–851 Author's personal copy framework (e.g. [8,30–32]), and practical applications (e.g. [33–35]). Also the combination between backcasting and other types of scenarios has been /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 36. IMO at the Arctic Circle Assembly 2017

  the USA, the European Space Agency (ESA) and China.Ingvar Kristinsson, managing director at IMO, participated in a session on the potential effects of volcanic ash clouds from Icelandic volcanoes on aviation in the Arctic airspace. In a special session on issues related to Arctic Freshwater, Halldór Björnsson and Þorsteinn Þorsteinsson contributed to a discussion on freshwater fluxes /about-imo/news/imo-at-the-arctic-circle-assembly-2017

• 37. 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

• 38. Dyrrdal_Anita_CES_2010

  parameters – In the light of climate change Norwegian Meteorological Institute met.no Observed changes in Norway between 1961-90 and 1979-08 • Winter precipitation has increased by 5-25 % • Winter temperature has increased by 0.91–1.34 ºC (Hanssen-Bauer et al., 2009) What about snow conditions? Introduction Data & Methods Results Norwegian Meteorological Institute met.no Snow parameters Start End /media/ces/Dyrrdal_Anita_CES_2010.pdf

• 39. VI_2021_008

  off an audio alarm. This feature is especially useful when there is an ongoing eruption (i.e. Fagradalsfjall 2021), as the stations around this eruptive area can be muted to enhance signals from other regions in Iceland. • Remove stations: Stations can be removed from the trigger calculations for all bandpass filters. Removed stations will not be accounted for in the tremor catalog /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 40. Grímsey earthquake swarm

  on February 16, is significantly less than the 2013 sequence, see older news, although this swarm is more steady. Continuous GPS measurements in Grímsey show no detectable deformation associated with the swarm, suggesting that the swarm is tectonic in nature although geothermal activity in the area may act as a trigger. There is no sign of magmatic activity.This area is an active seismic /about-imo/news/grimsey-earthquake-swarm