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  • 41. Past temperature conditions in Iceland

    being 1995. Since then it has been warm, the warmth culminating in 2002 to 2003. Generally the description above refers to the whole country, but there are slightly diverging details, depending on the source of the cold air. Back to top Comparison of temperature in Stykkishólmur, Akureyri and Reykjavík A comparison of annual temperatures at three stations, Stykkishólmur in the west, Akureyri /climatology/articles/nr/1213/
  • 42. IPPC-2007-ar4_syr

    Arctic sea ice extent has shrunk by 2.7 [2.1 to 3.3]% per decade, with larger decreases in summer of 7.4 [5.0 to 9.8]% per decade. Mountain glaciers and snow cover on average have declined in both hemispheres. The maximum areal extent of sea- sonally frozen ground has decreased by about 7% in the Northern Hemisphere since 1900, with decreases in spring of up to 15%. Temperatures at the top /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 43. vonKorff_etal-2010

    elements they all emphasize are captured in two questions: 1. Which actors should be involved in the decision-making process? 2. What are the actors’ interests? Considered together, the various substeps of the five guides resulted in the following reconstructed steps for the lead agency to take in stakeholder analysis: 1. SA 1: Adjust the team as needed for stakeholder analysis. Check to see /media/loftslag/vonKorff_etal-2010.pdf
  • 44. CES_D2.4_solar_CMIP3

    by the various models. In the large figure, months from Jan- uary (1) to December (12) are depicted. On the right-top corner there is an enlarged illustration for November-February, i.e., the months with the weakest incident radiation. Unit: MJ m−2 month−1. analysis would corrupt the results severely. Therefore, the present analysis will be based on 18 models, with the CSIRO model excluded. Evaluation /media/ces/CES_D2.4_solar_CMIP3.pdf
  • 45. Bárðarbunga and Holuhraun - overview

    A list of links to the relevant web-material 20.8.2014 An overview of the Bárðarbunga seismic events and the Holuhraun eruption, 2014 - 2015, is given here with notes, factsheets and observations. New material was added to the top of each monthly article. Combined /earthquakes-and-volcanism/articles/nr/2947
  • 46. Bárðarbunga and Holuhraun - overview

    A list of links to the relevant web-material 20.8.2014 An overview of the Bárðarbunga seismic events and the Holuhraun eruption, 2014 - 2015, is given here with notes, factsheets and observations. New material was added to the top of each monthly article. Combined /earthquakes-and-volcanism/articles/nr/2947/
  • 47. Fractures in Svínafellsheiði and a potential rockslide on Svínafellsjökull

    News The location of the fracture at the top of Svínafellsheiði discovered in 2014. (Click to enlarge /about-imo/news/fractures-in-svinafellsheidi-and-a-potential-rockslide-on-svinafellsjokull
  • 48. Vertical displacement in the Bárðarbunga caldera

    and the Icelandic Coast Guard, see disclaimer. The vertical displacement (m) was monitored by near real time presentation of data from a GPS station, mounted in the middle of the caldera. The elevation above sea level, top left, refers to the zero value on the y-axis, while such value top right shows the current position of the station (m a.s.l.). The upper graph shows the first two weeks, 12 - 25 /earthquakes-and-volcanism/gps-measurements/bardarbunga/caldera/
  • 49. Hekla eruptions

    This explains why tephra layers from Hekla often have a light coloured base and a dark top, making them ideal tephra marker layers.For more information on the Hekla volcanic system, visit Catalogue of Icelandic volcanoes.Hekla 20th February 1991. Photo: Oddur Sigurðsson.IMO borehole strain station, near Hekla. Photo: Matthew J. Roberts /volcanoes/about-volcanoes/hekla/hekla-eruptions/
  • 50. Supporting structures stopped most of an avalanche

    A snow avalanche was released from the Tvísteinahlíð mountain by the health care centre at Engihlíð in Ólafsvík on 19 March 2012. The fracture line of the avalanche was near the top of the slope and extended from the gully to the west of the hillside and into supporting structures that have been installed as protection measures to reduce avalanche danger in the settlement near /about-imo/news/nr/2476

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