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• 31. Öræfajökull : Recent research

  and Eyjafjallajökull hazard assessments were applied.The project was funded mainly by the National Avalanche and Landslide Fund, with additional financial contributions from the Icelandic Road and Coastal Administration and the National Power Company.Published materialPagneux, E., Gudmundsson, M. T., Karlsdóttir, S., & Roberts, M. J. (Eds.) (2015). Volcanogenic floods in Iceland: An assessment /volcanoes/about-volcanoes/oraefajokull/new-research/

• 32. 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

• 33. Grimsvotn_status_2011-05-22_IES_IMO

  to 10 kilometers. Heading: Most of the ash cloud heads to the south. Lower and scattered clouds head southwest and travel over the eastern part of the South Iceland Lowlands. The plume forms a 60 km long circular cloud around the eruption site with its lower boundary at a height of about 5 km. Out from this cloud, a scattered cloud lies to the north reaching about 450 km north /media/jar/Grimsvotn_status_2011-05-22_IES_IMO.pdf

• 34. Grimsvotn_status_2011-05-24_IES_IMO

  and around it. The estimated height is below 5 km since clouds over the glacier were at 5-7 km and the plume did not reach above the cloud deck. The ash plume reached 8 km briefly at 14 UTC today, but decreased shortly there after. According to pilot reports the plume is visible at around 10 thousand feet, mostly light gray or brown in color, but pulsating to 15 thousand feet /media/jar/Grimsvotn_status_2011-05-24_IES_IMO.pdf

• 35. vanRoosmalen_etal-2009-WRR_2007WR006760

  and Irrigationa Scenario Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Current 101 85 59 13
  6
  4
  1 6 39 79 84 97 A2 145 132 73 10
  10
  7
  6
  8 4 75 92 123 B2 137 119 75 16
  6
  6
  6
  5 21 74 110 141 aValues are in millimeters. 10 of 18 W00A15 VAN ROOSMALEN ET AL.: CLIMATE AND LAND USE CHANGE W00A15 time and larger area where groundwater levels rise above the drain levels. Table 6 shows the mean discharges /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 36. Flood from Skaftá

  eastern and western, are located in the western part of Vatnajökull Ice-cap. They form because of geothermal activity that melts the glacier from below and water accumulates beneath them. When the hydro static pressure is high enough for the water to lift the ice above and flow from below the cauldrons it causes a flood. Floods from the eastern-cauldron are usually larger than the floods /about-imo/news/flood-in-estern-skafta

• 37. Flood from Skaftá

  eastern and western, are located in the western part of Vatnajökull Ice-cap. They form because of geothermal activity that melts the glacier from below and water accumulates beneath them. When the hydro static pressure is high enough for the water to lift the ice above and flow from below the cauldrons it causes a flood. Floods from the eastern-cauldron are usually larger than the floods /about-imo/news/flood-in-estern-skafta/

• 38. 2013_001_Nawri_et_al

  and a pressure of 1013.25 hPa. In the case of Iceland, the climate deviates significantly from these standard atmospheric conditions. Additionally, terrain elevation varies considerably across the island. Therefore, seasonal and annual differences in air density from the standard value, as well as spatial variability, need to be taken into account. Approximate air density can be calculated by assuming /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 39. VI_Arsskyrsla_2018_vef

  - politan area to raise the awareness of climate change impacts on local scale. Agreements regarding long-term high-quality operations of weather stations have been made. Tailored services as input into the daily decision making and operations of local governments are also being discussed. IMO is undertaking broad evaluation and gap analysis of the different networks used in monitoring /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 40. 2010_012rs

  ) closest stations, respectively. The 40 highest correlating events are then inverted for the best location. For comparison the manual locations, obtained by an analyst are shown in yellow. The final locations of the events are all within an approximately 1 km2 area, even though their original, automatic locations are up to 5 km away. They are also within a few hundred meters from the manual /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf