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  • 31. Linnet_Ulfar_CES_2010

    °C/100y 1975-2000 • 2.35 °C/100y 2000- •Change in precipitation • Average increase 4.8% / 100 y • Range 3.3 – 7.2 % •Glaciers • Results from CES • 25% decrease in volume from 2000 to 2050 Temperature transformation Com parison of series 10000 12000 14000 16000 18000 20000 22000 1 9 5 0 1 9 5 2 1 9 5 4 1 9 5 6 1 9 5 8 1 9 6 0 1 9 6 2 1 9 6 4 1 9 6 6 1 9 6 8 1 9 7 0 1 9 7 2 1 9 7 4 1 9 7 6 1 9 7 8 1 /media/ces/Linnet_Ulfar_CES_2010.pdf
  • 32. Savolainen_Ilkka_CES_2010

    ) and other gases A wide spectrum of measures needed in order to reach deep enough emission reductions 503/02/2010 Global greenhouse gas emissions by sectors in 2005 The emissions sum up to approximately 46,000 MtCO2eq. Data source: CAIT, cait.wri.org. *) The estimated effect of land use change & forestry, 8,000 MtCO2, is for the year 2000. 603/02/2010 Raupach et al 2007; Le Quere et al. 2009 /media/ces/Savolainen_Ilkka_CES_2010.pdf
  • 33. Avalanches in Iceland

    and landslides have caused both death and injury and done great damage to infrastructure and property in Iceland. In the twentieth century, 193 persons died, thereof 69 persons after 1974. Financial cost between 1974 and 2000 amounts to 3.3 billion IKR. Catastrophic avalanches in the villages Súðavík (January) and Flateyri (October) 1995, which killed 34 people and caused extensive economic damage /avalanches/avalanches
  • 34. Final Conference of the SVALI project

    News The western cauldron in Vatnajökull, Iceland, on 19 August 2000, view towards southeast /about-imo/news/nr/3142
  • 35. Increased seismic activity between Krýsuvík and Ölfus

    News Earthquakes over 1 in size at the Reykjanes peninsula, from Jan 2000 to June 2015 /about-imo/news/nr/3150
  • 36. Avalanches in Iceland

    and landslides have caused both death and injury and done great damage to infrastructure and property in Iceland. In the twentieth century, 193 persons died, thereof 69 persons after 1974. Financial cost between 1974 and 2000 amounts to 3.3 billion IKR. Catastrophic avalanches in the villages Súðavík (January) and Flateyri (October) 1995, which killed 34 people and caused extensive economic damage /avalanches/avalanches/
  • 37. Hekla

    on the Eastern Volcanic zone and consists of a central volcano rising to 1490 m.a.s.l. and is about 60 km long fissure swarm. The volcano has been highly active during Holocene and has erupted 23 times in historical time, with its last eruption occurring in 2000. It is considered the third most active volcano in Iceland. About 100 eruptions are known from the system in the past 9000 years, both effusive /volcanoes/about-volcanoes/hekla/
  • 38. The weather in Iceland in 2016

    the ranking of the year‘s temperature at selected stations. The red numbers indicate the deviation from the 1961 to 1990 normal, the red numbers in the brackets the warmest year of the series at that station and the numbers in black the number of years in the station series. PrecipitationThe annual total precipitation was above the 1971 to 2000 mean at most stations. The total in Reykjavík was 933.9 /about-imo/news/the-weather-in-iceland-in-2016
  • 39. ved-eng-2015

    and East, but in the Southwest the weather was slightly more favourable. The autumn (September to November) was the most favourable part of the year, until the end of November when there was an unusually heavy snowfall in the Southwest. The weather in December was stormy. The year 2015 was the coldest in Iceland since 2000, but this period has generally been abnormally warm so the average /media/vedurstofan/utgafa/skylduskil/ved-eng-2015.pdf
  • 40. VI_2021_008

    using data from six recent Icelandic eruptions: Hekla 2000, Eyjafjallajökull 2010, Fagradalsfjall 2021, and Grímsvötn 1998, 2004, and 2011. For tuning, data for these eruptions had to be converted from IMO’s old in-house RSAM data format to the new Tremv csv format. In addition to developing the ALERT module, this project involved several updates to the original Tremv program. Figure 2 /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

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