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Results:

• 21. Traffc-maintenance_expenditures

  229 1 587 160 1970 18 591 42 413 2 166 86 101 - 892 5 131 2 310 201 - - - 157 805 1 652 904 1969 17 559 38 840 2 313 93 776 - 922 4 562 1 571 - - - - 159 543 1 832 354 1968 13 474 36 376 3 074 104 519 - 1 080 4 131 1 156 - - - - 163 811 1 964 368 1967 11 139 34 495 5 940 95 857 - 419 3 032 1 087 - - - - 151 968 1 936 249 1966 9 835 32 581 8 349 94 777 - 587 4 205 1 743 - - - - 152 077 2 032 936 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 22. Daniell_etal-2010

  and evaluating impacts (see also Swallow et al. 2001, van Ast and Boot 2003). METHODS AND DATA This article is based on empirical data that originated from the analysis of the participatory exercise in the Dhuenn basin. The strong involvement of researchers from two research projects (NeWater[1] and ACER[2]) linked by a joint case study led to the variety of sources available for exploration, including /media/loftslag/Daniell_etal-2010.pdf

• 23. Publications 2012

  Nawri, Halldór Björnsson, Guðrún Nína Petersen & Kristján Jónasson 44 pp 3,1 Mb 2012-009 Empirical Terrain Models for Surface Wind and Air Temperature over Iceland Nikolai Nawri, Halldór Björnsson, Guðrún Nína Petersen & Kristján Jónasson 33 pp 1,8 Mb 2012-008 Surface Wind and Air Temperature over Iceland based on Station Records and ECMWF Operational Analyses Nikolai Nawri /about-imo/publications/2012/

• 24. Bardarbunga_Daily_status_report_260814

  a significant part, or all, of the fissure is beneath the glacier. This would most likely produce a flood in Jökulsá á Fjöllum and perhaps explosive, ash-producing activity. Other scenarios cannot be excluded. For example, an eruption inside the Bárdarbunga caldera is possible but presently considered to be less likely. /media/jar/Bardarbunga_Daily_status_report_260814.pdf

• 25. Eyjafjallajokull_status_2010-05-18_IES_IMO

  measurements, web cameras, ATDnet – UK Met. Offices lightning detection system, NOAA satellite images and web-based ash reports from the public. Eruption plume: Height (a.s.l.): According to radar observations, the plume has been mostly at 7 km/21,000 ft. South and southwesterly winds (25-35 kt) over the volcano. Near the surface, the wind was easterly, blowing ash from the ground /media/jar/Eyjafjallajokull_status_2010-05-18_IES_IMO.pdf

• 26. Eyjafjallajokull_status_2010-06-11_IES_IMO

  water to flow up onto a road west of a bridge, as there it now not much difference between the height of the bridge and the river channel. Conditions at eruption site: A lake, about 300 m in diamenter, has formed at the bottom of the big crater. Steam is rising from the rims, especially from the north side. In the morning the steam cloud only rose about 100 m over the crater /media/jar/Eyjafjallajokull_status_2010-06-11_IES_IMO.pdf

• 27. Eyjafjallajokull_status_2010-06-15_IES_IMO

  been observed at GPS stations at or around the glacier. However, a station at the northeastern caldera rim (AUST), moved about three centimeters towards the southwest from the 9th to the 13th of June, inward to the caldera. Overall assessment: The level of water in the crater lake only rose about 1 – 2 meters over the weekend. Several days or weeks are therefore likely to pass /media/jar/Eyjafjallajokull_status_2010-06-15_IES_IMO.pdf

• 28. 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

• 29. 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

• 30. Increased glacial melt due to volcanic ash

  A hydrological year is defined as the period from 1st September to 31st August. After the processing of measurement results, data are analysed and interpreted. Increased glacial melt characterizes the 2009/2010 hydrological year in areas where volcanic ash from the Eyjafjallajökull eruption was sufficiently thick. Surprisingly, glacial melt was lower closer to the eruption where the ash was even /hydrology/articles/nr/2110