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• 61. Update on activity in Eyjafjallajökull 2010

  in Europe last week, confirm the results of the dispersion models for ashfall. The Volcanic Ash Advisory Centre in London, VAAC, issues new graphics intended for flight traffic every few hours (see red link at top of page). Conditions and assessment - 25 April 2010 22:30 The following is based on a status report issued collectively by IMO and the Institute of Earth Sciences at 18:00 /earthquakes-and-volcanism/articles/nr/1884

• 62. News

  2015. For an updated graph, see link in main text. News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 2013 2012 2011 2010 2009 2008 2007 2006 /about-imo/news/bigimg/3203

• 63. Radiation

  Radiation © Veðurstofa Íslands An example of a graph showing UV-index for a single day. See life link in text /pollution-and-radiation/radiation/bigimg/1215

• 64. VI_2020_004

  to sub-glacial eruptions, eruptions in vicinity of urban areas, ash- and gas- rich eruptions, pyroclastic flows, volcanic firebombs. In addition research will be conducted where necessary to fill in knowledge gaps and strengthen the hazard and risk assessment, those include estimation of eruption at sea, modelling of sub-glacial thermal activity and link to unexpected and fast glacial outburst /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 65. CES_D2.4_task1

  and http://www.atm. helsinki.fi/~jaraisan/CES_D2.4/Tables_P. In constructing these tables, it was assumed that the signal of anthropogenic climate change varies smoohtly in space and can therefore be estimated from global and regional climate model simulations. To the extent that this assumption is violated, for example due to local water bodies and small-scale variations /media/ces/CES_D2.4_task1.pdf

• 66. Lorenzoni_Pidgeon_2006

  and negativity associated with climate change as an environmental, but not necessarily as a ‘domestic’, issue. However, more detailed studies on national samples serve to highlight more complex public attitudes towards climate change. Individuals characterise climate change in multiple terms, related to their everyday experiences and locality, distinguishing effects on different scales in space and time /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 67. A new banner on our web-site

  A new banner on our web-site 2.10.2009 For easy promotion of projects, conferences and lectures, a new banner will appear intermittently on our web-site, at the top of each page. The banner is a link which takes the reader directly to relevant information /about-imo/news/nr/1724

• 68. glacier_mass_balance_poster

  2LEGOS, Toulouse, France 3National Space Institute, Technical University of Denmark, Lyngby, Denmark Abstract. We assess the mean mass balance of three ice caps in South Iceland, for two periods, 1980 to 1998 and 1998 to 2004, by comparing digital elevation models (DEMs) covering the entire glaciers; Eyjafjallajökull (81 km2), Tindfjallajökull (15 km2) and Torfajökull (14 km2). The DEMs were /media/ces/glacier_mass_balance_poster.pdf

• 69. VI_2016_006_rs

  or even more but these volume estimates clearly show that slides of this size cannot be confined within debris flow containment measures that can be fitted in the available space above the settlement. 20 Figure 6. Main potential starting zones for landslides in the mountainside south of Seyðis- fjörður between Þófi and Botnahlíð. Numbers denote starting areas that are described in separate /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 70. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  Reykjavı´k IS-101, Iceland 2 Centre National de la Recherche Scientifique, Universite´ de Toulouse, Laboratoire d’Etudes en Ge´ophysique et Oce´anographie Spatiale, Universite´ de Toulouse, 14 Avenue Edouard Belin, Toulouse FR-31400, France 3 National Space Institute, Technical University of Denmark, Lyngby DK-2800, Denmark Keywords Remote sensing; glacier mass balance; regional warming /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf