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  • 11. The outflow of the jökulhlaup at the terminus of Skaftárjökull

    article. Ice blocks Ice blocks close to the outflow points. Photo: Tómas Jóhannesson. The flood waters appear to have flowed through the glacier for some time and concentrated in one or more circular channels that the flow melted through the glacier. Channels An outflow point where the water burst through the ice. Photo: Tómas Jóhannesson. The flow up through the glacier did /about-imo/news/nr/3214
  • 12. Radiation

    have been launched from Keflavík at 64º N, 22º W. Classic ozone measurements are done at IMO's headquarters, i.e. Dobson which yield total ozone from the measuring point and up through the atmosphere. The results are processed and mapped at Environment Canada. Bolungarvík Figure 1. Bolungarvík in the West Fjords with the mountain Ernir above. © Sigvaldi Árnason. Gamma rays /pollution-and-radiation/radiation/
  • 13. 2010_005_

    warming towards the northeast. The warming from 1961–90 to 2070–99 on an annual basis was about 1 K in the southwest of Iceland, but reached 2–3 K in the interior and on the east coast. Of the two emission scenarios used (A2 and B2), the higher emitting one (A2) produced slightly more warming, but a very similar spatial structure. The HIRHAM results also showed an increase in precipitation, with more /media/ces/2010_005_.pdf
  • 14. Glossary

    We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208
  • 15. Glossary

    We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208/
  • 16. IPPC-2007-ar4_syr

    notably popula- tion projections. However, for those studies incorporating these new population projections, changes in other drivers, such as economic growth, result in little change in overall emission levels. Economic growth projections for Africa, Latin America and the Middle East to 2030 in post-SRES baseline scenarios are lower than in SRES, but this has only minor effects on global /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 17. Jökulhlaup from Grímsvötn subsides

    Meltwater along the margin Figure 3. The jökulhlaup flowing westwards in its course along the margin of the Skeiðarárjökull outlet glacier. Photo: Þorsteinn Þorsteinsson. The new pathway Figure 4. View towards the Skaftafell mountains, east of Skeiðarárjökull. A sediment bank is visible to the left and a continuation of this feature is seen on the right hand side of the photo. The water /about-imo/news/2010/nr/2042
  • 18. Jökulhlaup from Grímsvötn subsides

    Meltwater along the margin Figure 3. The jökulhlaup flowing westwards in its course along the margin of the Skeiðarárjökull outlet glacier. Photo: Þorsteinn Þorsteinsson. The new pathway Figure 4. View towards the Skaftafell mountains, east of Skeiðarárjökull. A sediment bank is visible to the left and a continuation of this feature is seen on the right hand side of the photo. The water /about-imo/news/nr/2042
  • 19. ESC-IASPEI-statement-LAquila-2012-1

    26 October 2012 ESC statement on L’Aquila sentence The European Seismological Commission (ESC) as a Commission of the International Association of Seismology and Physics of the Earth’s Interior (IASPEI) endorses and adheres to the IASPEI Press Release on the L'Aquila sentence (http://www.iaspei.org/news_items/laquila_IASPEI_press_release_final.pdf /media/vedurstofan/utgafa/hlidarefni/ESC-IASPEI-statement-LAquila-2012-1.pdf
  • 20. Adalgeirsdottir-etal-tc-5-961-2011

    ). The accu- mulation zone is a part of the eastern sector of the ice cap between two mountain ranges, the subglacial Breiðabunga and Goðahnúkar, at 1350–1450 m elevation. From the ac- cumulation area, the ice flows in two branches, west and east of the central nunatak Nýju Núpar. The branches meet below the nunatak and the ice is funnelled through a 2 km wide ice fall at 600–700 m elevation where /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

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