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• 11. Earthquake sequence east of Grímsey

  been manually revised so far are shown as red dots. The M5.5 mainshock is located on a north-south striking left lateral strike-slip fault, see black lines in the map. The M4.7 event around 9 am was located on a normal fault to the north-west. This cluster at about 7.5 km distance to the main cluster was most likely activated due to static stress changes induced by the M5.5 earthquake /about-imo/news/nr/2681

• 12. Reading material for the PhD Workshop

  A PhD Workshop on 26-28 August 2012 in Helsinki, directly linked to the 2nd Nordic International Climate Change Adaptation Conference, 29-31 August 2012, Helsinki (see pdf, 0.5 Mb). Material 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343 Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication /nonam/adaption/material/

• 13. Eyjafjallajokull_status_2010-06-04_IES_IMO

  lightning detection system, web- based ash reports from the public and research expedition of the IES to the summit on 3/6-2010. Eruption plume: Height (a.s.l.): Clouds and mist have covered the summit of the volcano both yesterday and today. On Wednesday 2nd June a white steam cloud was seen up to 2.5 km a.s.l. On Thursday 3rd of June scientist from IES came to the crater area /media/jar/Eyjafjallajokull_status_2010-06-04_IES_IMO.pdf

• 14. PhD Workshop 2012

  decision support models and procedures and processes applied in analyzing, planning and implementing adaptation to climate change. Virtually all sub-themes mentioned in the Conference call, as well as many others not described, can be related to the practical uptake of adaptation. Studies, that address sectoral or regional dimensions of adaptation, are of particular interest. Character /nonam/adaption/phd-workshop-2012/

• 15. Wind Energy

  Technical University, August 2007. Journal of Physics Conference Series, Vol. 75. 8 pp. Pryor, S. C., Schoof, J. T., Clausen, N.-E. & Drews, M. (2010). Changes in extreme wind and intense wind speeds in Northern Europe. European wind energy conference, Warsaw, April 2010. National Barthelmie, R.J. & Pryor, S. C. (2007). Wind speed trends over the contiguous USA. 30th Annual Applied Geography /ces/publications/nr/1944

• 16. VAT_newsletter_2018_06

  mass balance in a warming climate but also due to calving (ice breaks of the front into lakes or sea) into Jökulsárlón lagoon. Calving currently causes about / of the mass loss of Breiðamerkurjökull. The large ice sheets of Antarctica and Greenland lose large amounts of ice by calving, and the rate of loss has intensied greatly in recent years.    Rapid melting of glacial ice /media/Eplicanámskeið/VAT_newsletter_2018_06.pdf

• 17. 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

• 18. Re-evaluation needed of the size of the hazard area

  activity was characterized by continuous lava fountains, while the activity changed at around midnight on the 2nd of May, and has since been showing pulsating behaviour. These pulses have intermittent active periods of 8-12 minutes, with 1-2 minutes of rest periods in between. The active pulses start with a strong fountain activity, with fountains reaching up to 100-150 m above ground level, and some /about-imo/news/new-fissure-near-the-eruption-site-in-geldingadalir

• 19. 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/

• 20. ved-eng-2015

  stations was unusually small compared to the long term. Temperature anomaly °C (relative to 1961 - 1990) Figure 1. In Akureyri (red) the temperature was above the 1961-1990 mean during the first four months and again in the autumn; September was particularly warm, but May and August very cold. In Reykjavík (blue) May was very cold, but September warm. The absolute maximum temperature /media/vedurstofan/utgafa/skylduskil/ved-eng-2015.pdf